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Contents

   



(Top)
 


1 Location  





2 Ponte del Ciolo (Ciolo's Bridge)  





3 The Ciolo's Caves  



3.1  Grotta Piccola Del Ciolo  





3.2  Grotta Grande Del Ciolo  





3.3  Grotta Delle Prazziche  







4 Geology  





5 Flora  



5.1  Ferns  





5.2  Alyssum of Leuca  





5.3  Vicia Giacominiana  





5.4  Fiordaliso of Leuca  





5.5  Carnation of Salento  







6 Fauna  



6.1  Marine Fauna  





6.2  Plankton  





6.3  Land Fauna  





6.4  Paleoenviroment  







7 Tourism  



7.1  Trekking  



7.1.1  Sentiero del vecchio Ciolo  







7.2  High diving  





7.3  Scuba diving  





7.4  Rock climbing  







8 Curiosities  



8.1  The Legend  







9 The Regional Coastal Park  



9.1  The oak-trees Park of Castro  





9.2  The Wood of Tricase  





9.3  The Wood "Le chiuse di Tiggiano"  







10 Gallery  





11 See also  





12 Notes  





13 References  





14 External links  














Ciolo (Apulia): Difference between revisions






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| name = Ciolo

| name = Ciolo

| other_name =

| other_name =

| native_name = "Ciole"

| native_name = {{native_name|scn|Ciole}}

| native_name_lang =

| translation = [[Magpies]]

| translation = [[Magpies]]

| photo = Ponte Ciolo.jpg

| photo = Ponte Ciolo.jpg

| photo_size = 249

| photo_size = 248

| photo_caption = Panoramic view of Ponte del Ciolo (Ciolo's Bridge)<!-- MAP -->

| photo_caption = Panoramic view of Ponte del Ciolo (Ciolo's Bridge)<!-- MAP -->

| map = Italy#Italy Apulia

| map = Italy#Italy Apulia

Line 38: Line 37:

}}

}}



'''Ciolo''' is a narrow coastal [[inlet]] and a site of historical and environmental interest, which is located in [[Apulia]], [[Italy]]. The location is also known as a geological site and for the presence of numerous sea caves, the largest one being the Grotta del Ciolo. Since October 2006 the Ciolo's area has become part of the Regional Park "''Costa [[Otranto]] - [[Santa Maria di Leuca]] e Bosco di [[Tricase]]"'', created by the Apulia region to protect the eastern coast of [[Salento]], specifically the architectural assets as well as important animal and plant species.

'''Ciolo''' is a narrow coastal [[inlet]] and a site of historical and environmental interest, which is located in the south of [[Apulia]], in the historical region of [[Salento]], [[Italy]]. The location is also known as a geological site and for the presence of numerous sea caves, the largest one being the Grotta del Ciolo. Since October 2006 the Ciolo's area has become part of the Regional Park "''Costa [[Otranto]] - [[Santa Maria di Leuca]] e Bosco di [[Tricase]]"'', created by the Apulia region to protect the eastern coast of [[Salento]], specifically the architectural assets as well as important animal and plant species.



The name Ciolo comes from the noun in [[salentino dialect]] "''ciole",'' which refers to [[crows]] or [[magpies]], which are widespread in this region..<ref name=":8">

The name Ciolo comes from the noun in [[salentino dialect]] "''ciole",'' which refers to [[crows]] or [[magpies]], which are widespread in this region.<ref name=":8">

{{Cite web|last=Piccinini|first=Marco|date=7 March 2015|title=Grotta Grande del Ciolo|trans-title=Grotta Grande del Ciolo|url=http://www.salogentis.it/2015/03/07/grotta-grande-del-ciolo/|url-status=live|archive-url=|archive-date=|access-date=|website=www.salogentis.it|language=it}}</ref><ref name=":9">

{{Cite web|last=Piccinini|first=Marco|date=7 March 2015|title=Grotta Grande del Ciolo|trans-title=Grotta Grande del Ciolo|url=http://www.salogentis.it/2015/03/07/grotta-grande-del-ciolo/|url-status=live|archive-url=https://web.archive.org/web/20160714230426/http://www.salogentis.it:80/2015/03/07/grotta-grande-del-ciolo/ |archive-date=2016-07-14 |website=www.salogentis.it|language=it}}</ref><ref name=":9">

{{Cite book

{{Cite book

|last=Ingravallo

|last=Ingravallo

Line 80: Line 79:

Ciolo is dominated by Ponte Ciolo (Ciolo's Bridge), a road bridge built in the 1960s. It crosses the inlet and connects the two shores of ''Santa Maria di Leuca'' and ''Novaglie''. The single-span bridge is approximately ''30 meters'' above water, ''60 meters'' long and ''10 meters'' wide.

Ciolo is dominated by Ponte Ciolo (Ciolo's Bridge), a road bridge built in the 1960s. It crosses the inlet and connects the two shores of ''Santa Maria di Leuca'' and ''Novaglie''. The single-span bridge is approximately ''30 meters'' above water, ''60 meters'' long and ''10 meters'' wide.



The first structure, part of a project for the entire coastal road by the engineer ''Mario Carrone'', envisaged a bridge with two continuous spans. This project was unfeasible due to the impossibility to build the central pile, as evidenced by the geo-technical report by the professor and engineer ''Vincenzo Cotecchia''. At that point the engineer ''Antonio La Tegola'' was appointed. He adopted the technique of the Swiss engineer ''[[Robert Maillart]]'', which required the incorporation of a thin vault and a stiffening deck. For this reason the structure the bridge was called Maillart's Bridge in the preliminary plans and studies.<ref name=":02">{{Cite web|last=DeGiuseppe|first=Alfredo|year=2020|title=Speciale Ponte Ciolo|trans-title=Special Ponte Ciolo|url=https://www.alfredodegiuseppe.it/index.php/archivio-2020/725-2020-06-speciale-ponte-ciolo-39-parallelo|url-status=live|archive-url=|archive-date=|access-date=|website=|publisher=39 ° Parallelo|language=it}}</ref>

The first structure, part of a project for the entire coastal road by the engineer ''Mario Carrone'', envisaged a bridge with two continuous spans. This project was unfeasible due to the impossibility to build the central pile, as evidenced by the geo-technical report by the professor and engineer ''Vincenzo Cotecchia''. At that point the engineer ''Antonio La Tegola'' was appointed. He adopted the technique of the Swiss engineer ''[[Robert Maillart]]'', which required the incorporation of a thin vault and a stiffening deck. For this reason the structure the bridge was called Maillart's Bridge in the preliminary plans and studies.<ref name=":02">{{Cite web|last=DeGiuseppe|first=Alfredo|year=2020|title=Speciale Ponte Ciolo|trans-title=Special Ponte Ciolo|url=https://www.alfredodegiuseppe.it/index.php/archivio-2020/725-2020-06-speciale-ponte-ciolo-39-parallelo|url-status=live|archive-url=https://web.archive.org/web/20200813054917/https://www.alfredodegiuseppe.it/index.php/archivio-2020/725-2020-06-speciale-ponte-ciolo-39-parallelo |archive-date=2020-08-13 |website=|publisher=39 ° Parallelo|language=it}}</ref>



Ciolo's Bridge was built by rotating the previously planned road axis, an operation that was necessary to find the right supports for the span. There are still some concrete stumps under the current span, which were necessary for the construction of the rib.<ref name=":02" />

Ciolo's Bridge was built by rotating the previously planned road axis, an operation that was necessary to find the right supports for the span. There are still some concrete stumps under the current span, which were necessary for the construction of the rib.<ref name=":02" />



Since the construction in the 1960s the bridge has been object of reinforcement and consolidation's works, the last being in the summer of 2019.<ref name=":02" /><ref>{{Cite web|last=|first=|date=19 June 2019|title=I tuffi adrenalitici dal Ponte del Ciolo|trans-title=Dives from the Ciolo Bridge|url=https://www.regionepuglia.org/i-tuffi-adrenalitici-del-ponte-del-ciolo/|url-status=live|archive-url=|archive-date=|access-date=|website=www.regionepuglia.org|language=it}}</ref>

Since the construction in the 1960s the bridge has been object of reinforcement and consolidation's works, the last being in the summer of 2019.<ref name=":02" /><ref>{{Cite web|last=|first=|date=19 June 2019|title=I tuffi adrenalitici dal Ponte del Ciolo|trans-title=Dives from the Ciolo Bridge|url=https://www.regionepuglia.org/i-tuffi-adrenalitici-del-ponte-del-ciolo/|url-status=live|archive-url=https://web.archive.org/web/20200813195033/https://www.regionepuglia.org/i-tuffi-adrenalitici-del-ponte-del-ciolo/ |archive-date=2020-08-13 |website=www.regionepuglia.org|language=it}}</ref>



== The Ciolo's Caves ==

== The Ciolo's Caves ==

In Ciolo canyon there are several [[Sea cave|sea caves]] formed during the [[Neolithic]] and [[Paleolithic]] age. In total this area includes three different major caves: the Grotta Grande del Ciolo (''Ciolo's Huge Cave''), the Grotta Piccola Del Ciolo (''Ciolo's Small Cave'') and the Grotta Delle Prazziche (''Cave of the Prazziche'').

In Ciolo canyon there are several [[sea cave]]s formed during the [[Neolithic]] and [[Paleolithic]] age. In total this area includes three different major caves: the Grotta Grande del Ciolo (''Ciolo's Huge Cave''), the Grotta Piccola Del Ciolo (''Ciolo's Small Cave'') and the Grotta Delle Prazziche (''Cave of the Prazziche'').

<ref name=":1">

<ref name=":1">

{{Cite web

{{Cite web

Line 100: Line 99:

|trans-title=Tour guide of Gagliano del Capo/Ponte Ciolo

|trans-title=Tour guide of Gagliano del Capo/Ponte Ciolo

|url=http://rete.comuni-italiani.it/wiki/Gagliano_del_Capo/Ponte_Ciolo

|url=http://rete.comuni-italiani.it/wiki/Gagliano_del_Capo/Ponte_Ciolo


|url-status=live

|archive-url=

|archive-date=

|access-date=

|website=rete.comuni-italiani.it

|website=rete.comuni-italiani.it

|language=it

|language=it

}}</ref><ref>{{Cite web|last1=Parise|first1=Mario|last2=Sammarco|first2=Mariangela|year=2005|title=Cipolliane's Caves in Salento (Apulia, southern italy): karst geomorphology and the filling deposits.|url=https://www.researchgate.net/publication/235634552|url-status=live|archive-url=|archive-date=|access-date=|website=|language=en}}</ref>

}}</ref><ref>{{Cite web|last1=Parise|first1=Mario|last2=Sammarco|first2=Mariangela|year=2005|title=Cipolliane's Caves in Salento (Apulia, southern italy): karst geomorphology and the filling deposits.|url=https://www.researchgate.net/publication/235634552 |website=ResearchGate|language=en}}</ref>



{| class="wikitable"

{| class="wikitable"

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|first2=Belmonte

|first2=Belmonte

|date=2008

|date=2008

|orig-year=2008

|orig-date=2008

|title=Censimento 2008

|title=Censimento 2008

|trans-title=2008 Census

|trans-title=2008 Census

|url=https://core.ac.uk/download/pdf/41166452.pdf

|url=https://core.ac.uk/download/pdf/41166452.pdf

|url-status=live

|archive-url=

|archive-date=

|access-date=

|website=Salento University

|website=Salento University

|publisher=Università di Zoogeografia e Faunistica, DiSTeBA, Università del Salento

|location=73100 Lecce, Italy

|language=it

|language=it

}}</ref><ref name=":6">

}}</ref><ref name=":6">

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|trans-title=The sea caves of Salento: classification, location and description

|trans-title=The sea caves of Salento: classification, location and description

|url=https://www.researchgate.net/publication/312982635

|url=https://www.researchgate.net/publication/312982635

|website=ResearchGate

|url-status=live

|archive-url=

|archive-date=

|access-date=

|website=www.researchgate.net

|language=it

|language=it

}}</ref> From a strictly biological point of view, different studies have been carried out during the years in the cave by different research teams coordinated by the [[University of Salento]], [[University of Modena and Reggio Emilia]] and [[University of Urbino]]. Since 2000, studies have been performed on benthic hard substrate stands living in the cave as well as taxonomic studies on the fauna able to live on the sea bottom and on the planktonic one.<ref name=":14" /> The studies have revealed a diverse sea bottom community even on little scale but very stable in time even if decreasing. The plankton analysed has appeared rich in nutrition, indicating that the decline of the community may relate to other factors, such as the possible infiltration of fresh water.<ref name=":14" />

}}</ref> From a strictly biological point of view, different studies have been carried out during the years in the cave by different research teams coordinated by the [[University of Salento]], [[University of Modena and Reggio Emilia]] and [[University of Urbino]]. Since 2000, studies have been performed on benthic hard substrate stands living in the cave as well as taxonomic studies on the fauna able to live on the sea bottom and on the planktonic one.<ref name=":14" /> The studies have revealed a diverse sea bottom community even on little scale but very stable in time even if decreasing. The plankton analysed has appeared rich in nutrition, indicating that the decline of the community may relate to other factors, such as the possible infiltration of fresh water.<ref name=":14" />

Line 171: Line 157:

The Grotta Grande Del Ciolo is also known by different names, such as Grotta degli Spiriti ''(Ghosts' Cave)'', Grotta dei Passeri ''(Sparrows' Cave)''{{efn|Both [[tree sparrow]] and [[willow sparrow]] are native to the area.}} and Bocca del Pozzo ''([[Well|Well's]] Mouth)''. The cave is semi-submerged and is characterized by a wide entrance, the result of an ancient phenomenon of collapse that partially occluded a portion of the archeological substrate of the cave, about ''20 meters'' above the sea level, leaving the remaining portion exposed to sea erosion provoked by the constant inflow and then outflow of water and waves.<ref name=":3" /> The cave develops longitudinally by ''120 meters'' and the height of the entrance is over ''30 meters,'' progressively decreasing along its longitudinal development.<ref name=":3" />

The Grotta Grande Del Ciolo is also known by different names, such as Grotta degli Spiriti ''(Ghosts' Cave)'', Grotta dei Passeri ''(Sparrows' Cave)''{{efn|Both [[tree sparrow]] and [[willow sparrow]] are native to the area.}} and Bocca del Pozzo ''([[Well|Well's]] Mouth)''. The cave is semi-submerged and is characterized by a wide entrance, the result of an ancient phenomenon of collapse that partially occluded a portion of the archeological substrate of the cave, about ''20 meters'' above the sea level, leaving the remaining portion exposed to sea erosion provoked by the constant inflow and then outflow of water and waves.<ref name=":3" /> The cave develops longitudinally by ''120 meters'' and the height of the entrance is over ''30 meters,'' progressively decreasing along its longitudinal development.<ref name=":3" />



The cave contains a pond generated by a source of fresh water which originates from a subterranean source near its location.<ref>{{Cite web|last=Montagna|first=Maria Teresa|date=|title=Indagini micologiche in alcune grotte della murgia barese e del territorio salentino: risultati preliminari|trans-title=Mycological investigations in some caves of the Bari murgia and the Salento territory: preliminary results|url=https://digilander.libero.it/speleocars/Spelaion%202000/04%20atti/pdf/attispelaion2000_097.pdf|url-status=live|archive-url=|archive-date=|access-date=|website=|language=it}}</ref>

The cave contains a pond generated by a source of fresh water which originates from a subterranean source near its location.<ref>{{Cite web|last=Montagna|first=Maria Teresa|date=|title=Indagini micologiche in alcune grotte della murgia barese e del territorio salentino: risultati preliminari|trans-title=Mycological investigations in some caves of the Bari murgia and the Salento territory: preliminary results|url=https://digilander.libero.it/speleocars/Spelaion%202000/04%20atti/pdf/attispelaion2000_097.pdf|website=|language=it}}</ref>



=== Grotta Delle Prazziche ===

=== Grotta Delle Prazziche ===

Grotta Delle Prazziche

Grotta Delle Prazziche

<ref name=":8" /> is one of the main caves near Ciolo, and is accessible by boat. The structure of the cave is circular, and at the top there is a vertical [[Siphon|syphon]] to the open air.<ref name=":3" />

<ref name=":8" /> is one of the main caves near Ciolo, and is accessible by boat. The structure of the cave is circular, and at the top there is a vertical [[Siphon|syphon]] to the open air.<ref name=":3" />

Many studies have been carried out inside and some prehistoric remains have been found, including handcrafts belonging to the Neolithic, [[Ceramic|ceramics]] and remains of [[Rhinoceros|rhinos]].<ref name=":1" />

Many studies have been carried out inside and some prehistoric remains have been found, including handcrafts belonging to the Neolithic, [[ceramic]]s and remains of [[Rhinoceros|rhinos]].<ref name=":1" />



== Geology ==

== Geology ==

The eastern coast of Salento is a noteworthy geological location due to the events that took place in the [[Mediterranean Sea|Mediterranean]] area starting from the [[Cretaceous]] period.<ref name=":10">

The eastern coast of Salento is a noteworthy geological location due to the events that took place in the [[Mediterranean Sea|Mediterranean]] area starting from the [[Cretaceous]] period.<ref name=":10">

{{Cite journal|last1=Margiotta|first1=S.|last2=Sansò|first2=P.|date=25 June 2014|title=The Geological Heritage of Otranto-Leuca Coast (Salento, Italy)|journal=Geoheritage|url=https://link.springer.com/article/10.1007/s12371-014-0126-8|url-status=live|archive-url=|archive-date=|access-date=|volume=6|issue=4|pages=305–316|doi=10.1007/s12371-014-0126-8|s2cid=128873613|language=en}}

{{Cite journal|last1=Margiotta|first1=S.|last2=Sansò|first2=P.|date=25 June 2014|title=The Geological Heritage of Otranto-Leuca Coast (Salento, Italy)|journal=Geoheritage|volume=6|issue=4|pages=305–316|doi=10.1007/s12371-014-0126-8|s2cid=128873613|language=en}}

</ref>

</ref>

[[File:Canalone del Ciolo.jpg|thumb|229x229px|Limestone ridge of Ciolo|left]]

[[File:Canalone del Ciolo.jpg|thumb|229x229px|Limestone ridge of Ciolo|left]]

Ciolo is mostly formed by a lower part of the stratigraphic succession, which includes [[Cretaceous]] bioclastic limestones and [[Breccia|breccias]] and [[Conglomerate (geology)|conglomerates]] of the dating to the late Oligocene ([[Chattian]]). In this area there are deposits of [[Phosphate|phosphatic]] limestone formations, phosphatic conglomerates and phosphatic concentrations. The upper part consists of [[Miocene]] aged limestone.<ref name=":0">

Ciolo is mostly formed by a lower part of the stratigraphic succession, which includes [[Cretaceous]] bioclastic limestones and [[breccia]]s and [[Conglomerate (geology)|conglomerates]] of the dating to the late Oligocene ([[Chattian]]). In this area there are deposits of [[Phosphate|phosphatic]] limestone formations, phosphatic conglomerates and phosphatic concentrations. The upper part consists of [[Miocene]] aged limestone.<ref name=":0">

{{Cite web

{{Cite journal

|last=Delle Rose

|last=Delle Rose

|first=Marco|year=2001

|first=Marco|year=2001

Line 190: Line 176:

|url=http://siba-ese.unisalento.it/index.php/thalassiasal/article/view/2243

|url=http://siba-ese.unisalento.it/index.php/thalassiasal/article/view/2243

|url-status=live

|url-status=live

|archive-url=https://web.archive.org/web/20200229195215/http://siba-ese.unisalento.it/index.php/thalassiasal/article/view/2243 |archive-date=2020-02-29 |journal=Thalassia Salentina

|archive-url=

|volume=25 |pages=41–66 |publisher=Salento University

|archive-date=

|doi=10.1285/i15910725v25p41 |language=en

|access-date=

|website=siba-ese.unisalento.it

|publisher=Salento University

|language=en

}}</ref><ref name=":11">

}}</ref><ref name=":11">

{{Cite web|last=Parente|first=Mariano|year=1994|title=A revised stratigraphy of the Upper Cretaceous to Oligocene units from southeastern Salento (Apulia, southern Italy)|url=https://www.researchgate.net/publication/281193356|url-status=live|archive-url=|archive-date=|access-date=|website=www.researchgate.net|language=en}}

{{Cite web|last=Parente|first=Mariano|year=1994|title=A revised stratigraphy of the Upper Cretaceous to Oligocene units from southeastern Salento (Apulia, southern Italy)|url=https://www.researchgate.net/publication/281193356 |website=ResearchGate |language=en}}

</ref><ref name=":12">

</ref><ref name=":12">

{{Cite book

{{Cite book

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|trans-title=Geological map of Italy 1:50.000.

|trans-title=Geological map of Italy 1:50.000.

}}

}}

</ref> The limestones present in the Ciolo area is characterized by [[Bioclast|bioclastic]] calcarenites and calcirudites and it is recognizable by its parallel and oblique lamination.<ref name=":2" />

</ref> The limestones present in the Ciolo area is characterized by [[bioclast]]ic calcarenites and calcirudites and it is recognizable by its parallel and oblique lamination.<ref name=":2" />




== Flora ==

== Flora ==

In Ciolo<nowiki/>'s area several botanical rarities can be found: [[mediterranean onion]] species, [[Fern|ferns]], the [[Alyssum]] of Leuca, the [[Cornflower blue|Fiordaliso]] of Leuca, the [[Campanula]] pugliese, the [[Vicia]] Giacominiana and several type of rare [[Orchidaceae|orchids]].<ref>{{Cite web|last=|first=|year=1987|title=Contributo alla distribuzione e alla cariologica di Allium commutatum guss in Puglia|trans-title=Contribution to the distribution and cariological of Allium commutatum guss in Puglia|url=https://www.academia.edu/9896256|url-status=live|archive-url=|archive-date=|access-date=|website=|language=it}}</ref>

In Ciolo<nowiki/>'s area several botanical rarities can be found: [[mediterranean onion]] species, [[fern]]s, the [[Alyssum]] of Leuca, the [[Cornflower blue|Fiordaliso]] of Leuca, the [[Campanula]] pugliese, the [[Vicia]] Giacominiana and several type of rare [[Orchidaceae|orchids]].<ref>{{Cite web|year=1987|title=Contributo alla distribuzione e alla cariologica di Allium commutatum guss in Puglia|trans-title=Contribution to the distribution and cariological of Allium commutatum guss in Puglia|url=https://www.academia.edu/9896256|website=Academia |language=it|last1=Alla|first1=Alla}}</ref>



=== Ferns ===

=== Ferns ===

Ciolo is an hypogeal habitat for botanical species like [[Cryptogam|cryptogams]]: [[algae]], [[Moss|mosses]] and [[ferns]]. There are about sixty species of [[Bryophyte|bryophytes]] living in the caves of Apulia which have been studied, including fifteen types of ferns.

Ciolo is an hypogeal habitat for botanical species like [[cryptogam]]s: [[algae]], [[moss]]es and [[ferns]]. There are about sixty species of [[bryophyte]]s living in the caves of Apulia which have been studied, including fifteen types of ferns.



Focusing the attention on the caves in Apulia, it is worth considering the distribution of ferns ([[Filicopsida]]). Ferns have interested many scientists since the 1950s and 1960s, the biggest contributions to the studies in this area were made by: ''Franco Anelli, Francesco Orfino and Pietro Parenzan''. They mainly focused on [[Castellana Caves|Grotta di Castellana]] but extended their studies also to Ciolo. The [[University of Lecce]] undertook pteridological studies on this territory.

Focusing the attention on the caves in Apulia, it is worth considering the distribution of ferns ([[Filicopsida]]). Ferns have interested many scientists since the 1950s and 1960s, the biggest contributions to the studies in this area were made by Franco Anelli, Francesco Orfino and Pietro Parenzan. They mainly focused on [[Castellana Caves|Grotta di Castellana]] but extended their studies also to Ciolo. The [[University of Lecce]] undertook pteridological studies on this territory.

[[File:Ferns leaves.jpg|thumb|Close up on Ferns' leaves]]

[[File:Ferns leaves.jpg|thumb|Close up on Ferns' leaves]]

The caves have very limited examples of [[Phototroph|phototrophic]] [[vegetation]]. There are some cases in which it is possible to find [[Etiolation|etiolate]] plants inside these caves. These plants grow from seeds transported by water, but without light they do not grow enough and then they die. For their sexed reproduction high [[humidity]] is essential, humidity is also the reason for the low [[desiccation]] process.<ref>{{Cite web|last1=Beccarisi|first1=Leonardo|last2=Chiriacò|first2=Leonardo|last3=Marchiori|first3=Silvano|last4=Medagli|first4=Pietro|year=2001|title=Felci (Filicopsida) spontanee del Salento (Puglia, Italia)|trans-title=Spontaneous ferns (Filicopsida) of Salento (Puglia, Italy)|url=https://www.researchgate.net/publication/270273768|url-status=live|archive-url=|archive-date=|access-date=|website=|language=it}}</ref>

The caves have very limited examples of [[phototroph]]ic [[vegetation]]. There are some cases in which it is possible to find [[Etiolation|etiolate]] plants inside these caves. These plants grow from seeds transported by water, but without light they do not grow enough and then they die. For their sexed reproduction high [[humidity]] is essential, humidity is also the reason for the low [[desiccation]] process.<ref>{{Cite web|last1=Beccarisi|first1=Leonardo|last2=Chiriacò|first2=Leonardo|last3=Marchiori|first3=Silvano|last4=Medagli|first4=Pietro|year=2001|title=Felci (Filicopsida) spontanee del Salento (Puglia, Italia)|trans-title=Spontaneous ferns (Filicopsida) of Salento (Puglia, Italy)|url=https://www.researchgate.net/publication/270273768 |website=ResearchGate |language=it}}</ref>



Ciolo's Caves are the only certified sites in Apulia where [[Asplenium marinum]] exists. Ciolo's Caves are on the boundary of the Eastern area of this species.

Ciolo's Caves are the only certified sites in Apulia where [[Asplenium marinum]] exists. Ciolo's Caves are on the boundary of the Eastern area of this species.

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|first4=Silvano

|first4=Silvano

|date=6 December 2002

|date=6 December 2002

|year=2002

|title=Indagine fitogeografia sulle felci delle grotte pugliesi

|title=Indagine fitogeografia sulle felci delle grotte pugliesi

|trans-title=Phytogeographic research on the ferns present in the Apulian caves

|trans-title=Phytogeographic research on the ferns present in the Apulian caves

|url=https://www.researchgate.net/publication/270339410

|url=https://www.researchgate.net/publication/270339410

|website=ResearchGate

|url-status=live

|archive-url=

|archive-date=

|access-date=

|website=www.researchgate.net

|language=it

|language=it

}}</ref>

}}</ref>



It is possible to track different [[Chorology|chorological]] models in the Ciolo using the distribution of [[Asplenium marinum]]. There is an hypothesis that the species is present in this territory as a relic banished to an [[Hypogeal germination|hypogeal]] habitat due to climate changes.

It is possible to track different [[Chorology|chorological]] models in the Ciolo using the distribution of [[Asplenium marinum]]. There is an hypothesis that the species is present in this territory as a relic banished to an [[Hypogeal germination|hypogeal]] habitat due to climate changes.

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=== Vicia Giacominiana ===

=== Vicia Giacominiana ===

The Vicia Giacominiana is a special type of plant native of Salento. It is a therophyte, and it is usually two meters high. It flowers during the months of April and May.

The Vicia Giacominiana is a special type of plant native of Salento. It is a therophyte, and it is usually two meters high. It flowers during the months of April and May.



Its flowers are [[Fuchsia (color)|fuchsia]], arranged in groups of racemes with a stem twice the length of the leaves. The Vicia Giacominiana is found exclusively within herbaceous communities of plants.

Its flowers are [[Fuchsia (color)|fuchsia]], arranged in groups of racemes with a stem twice the length of the leaves. The Vicia Giacominiana is found exclusively within herbaceous communities of plants.

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|trans-title=The exclusive endemisms of the flora in Salento

|trans-title=The exclusive endemisms of the flora in Salento

|url=https://emerotecadigitalesalentina.it/sites/default/files/allegati/ID07_endemismi-esclusivi-flora-salentina.pdf

|url=https://emerotecadigitalesalentina.it/sites/default/files/allegati/ID07_endemismi-esclusivi-flora-salentina.pdf

|url-status=live

|archive-url=

|archive-date=

|access-date=

|website=emerotecadigitalesalentina.it

|language=it

|language=it

|isbn=9788888156620

|isbn=978-88-88156-62-0

}}</ref>

}}{{dead link|date=August 2023}}</ref>



=== Carnation of Salento ===

=== Carnation of Salento ===

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Studies show that thirty-two different fish species are present.

Studies show that thirty-two different fish species are present.

<ref>

<ref>

{{Cite journal|last1=Guidetti|first1=Paolo|last2=Terlizzi|first2=Antonio|last3=Fraschetti|first3=Simonetta|last4=Boero|first4=Ferdinando|date=28 January 2009|title=Spatio‐temporal variability in fish assemblages associated with coralligenous formations in south eastern Apulia (SE Italy)|url=https://www.tandfonline.com/doi/abs/10.1080/11250000209356477|url-status=live|archive-url=|archive-date=|access-date=|journal=Italian Journal of Zoology|volume=69|issue=4|pages=325–331|doi=10.1080/11250000209356477|s2cid=83805645}}</ref><ref>

{{Cite journal|last1=Guidetti|first1=Paolo|last2=Terlizzi|first2=Antonio|last3=Fraschetti|first3=Simonetta|last4=Boero|first4=Ferdinando|date=28 January 2009|title=Spatio‐temporal variability in fish assemblages associated with coralligenous formations in south eastern Apulia (SE Italy) |journal=Italian Journal of Zoology|volume=69|issue=4|pages=325–331|doi=10.1080/11250000209356477|s2cid=83805645}}</ref><ref>

{{Cite journal|last1=Bussotti|first1=Simona|last2=Guidetti|first2=Paolo|last3=Belmonte|first3=Genuario|date=15 July 2002|title=Distribution patterns of the cardinal fish, Apogon imberbis, in shallow marine caves in southern Apulia (SE Italy)|url=https://www.tandfonline.com/doi/abs/10.1080/11250000309356509|url-status=live|archive-url=|archive-date=|access-date=|journal=Italian Journal of Zoology|volume=70|issue=2|pages=153–157|doi=10.1080/11250000309356509|s2cid=85309163|publication-date=28 January 2009}}

{{Cite journal|last1=Bussotti|first1=Simona|last2=Guidetti|first2=Paolo|last3=Belmonte|first3=Genuario|date=15 July 2002|title=Distribution patterns of the cardinal fish, Apogon imberbis, in shallow marine caves in southern Apulia (SE Italy) |journal=Italian Journal of Zoology|volume=70|issue=2|pages=153–157|doi=10.1080/11250000309356509|s2cid=85309163|publication-date=28 January 2009|doi-access=free}}

</ref>

</ref>



The Grotta Piccola del Ciolo is considered as a protective nursery for the new born of different species of [[fish]] and [[Echinoderm|echinoderms]]; in fact numerously [[starfish]], [[Sea urchin|sea urchins]], [[Brittle star|brittle stars]], [[Sea cucumber|sea cucumbers]], and [[Crustacean|crustaceans]] have been found.

The Grotta Piccola del Ciolo is considered as a protective nursery for the new born of different species of [[fish]] and [[echinoderm]]s; in fact numerously [[starfish]], [[sea urchin]]s, [[brittle star]]s, [[sea cucumber]]s, and [[crustacean]]s have been found.

<ref name=":4">

<ref name=":4">

{{Cite web|last1=Belmonte|first1=G.|last2=Onorato|first2=R.|last3=Denitto|first3=F.|last4=Costantini|first4=A.|last5=Bussotti|first5=S.|last6=Poto|first6=M.|date=|title=Novità esplorative e biologiche nelle grotte sottomarine del Canale d'Otranto|trans-title=Exploratory and biological news in the undersea caves of Canale d'Otranto|url=https://digilander.libero.it/speleocars/Spelaion%202000/04%20atti/pdf/attispelaion2000_173.pdf|url-status=live|archive-url=|archive-date=|access-date=|website=digilander.libero.it|publisher=Università di Lecce|language=it}}</ref><ref>

{{Cite web|last1=Belmonte|first1=G.|last2=Onorato|first2=R.|last3=Denitto|first3=F.|last4=Costantini|first4=A.|last5=Bussotti|first5=S.|last6=Poto|first6=M.|date=|title=Novità esplorative e biologiche nelle grotte sottomarine del Canale d'Otranto|trans-title=Exploratory and biological news in the undersea caves of Canale d'Otranto|url=https://digilander.libero.it/speleocars/Spelaion%202000/04%20atti/pdf/attispelaion2000_173.pdf|website=digilander.libero.it|publisher=Università di Lecce|language=it}}</ref><ref>

{{Cite journal|last1=Guidetti|first1=Paolo|last2=D' Ambrosio|first2=Paolo|date=|title=Spatial distribution patterns of Coris Julis and Thalassoma Pavo (pisces, labridae) along the South-Eastern Apulia Coast (SE Italy)|url=http://siba-ese.unisalento.it/index.php/thalassiasal/article/view/i15910725v27p81/1911|journal=Laboratorio di Zoologia e Biologia Marina, Università di Lecce|location=73100 Lecce, Italy|publisher=Università di Lecce|volume=|pages=10|via=}}

{{Cite journal|last1=Guidetti|first1=Paolo|last2=D' Ambrosio|first2=Paolo|date=January 2004|title=Spatial distribution patterns of Coris Julis and Thalassoma Pavo (pisces, labridae) along the South-Eastern Apulia Coast (SE Italy) |journal=Thalassia Salentina |publisher=Università di Lecce|volume=27|pages=81–90|doi=10.1285/i15910725v27p81 |doi-access=free}}

</ref><ref>{{Cite web|last=Gennaio|first=Roberto|year=2014|title=Diffusion of Percnon Gibbesi (H. Milne Edwards, 1853) (Crustacea, Decapoda, Grapsidae) along the south Salento, Italy|url=http://siba-ese.unisalento.it/index.php/thalassiasal/article/view/14535|url-status=live|archive-url=|archive-date=|access-date=|website=|language=en}}</ref><ref>{{Cite web|last1=Ariani|first1=Antonio|last2=Wittiman|first2=karl|year=2016|title=Mysida (crustacea) from apulian (SE- Italy) Waters. First record of Gastrosaccus roscoffensis bacescu. 1970 italy|url=http://siba-ese.unisalento.it/index.php/thalassiasal/article/view/16537|url-status=live|archive-url=|archive-date=|access-date=|website=|language=en}}</ref>

</ref><ref>{{Cite journal|last=Gennaio|first=Roberto|year=2014|title=Diffusion of Percnon Gibbesi (H. Milne Edwards, 1853) (Crustacea, Decapoda, Grapsidae) along the south Salento, Italy|journal=Thalassia Salentina |url=http://siba-ese.unisalento.it/index.php/thalassiasal/article/view/14535|url-status=live|archive-url=https://web.archive.org/web/20200828053017/http://siba-ese.unisalento.it/index.php/thalassiasal/article/view/14535 |archive-date=2020-08-28 |volume=36|pages=85–90 |publisher=University of Salento |doi=10.1285/i15910725v36p85 |language=en}}</ref><ref>{{Cite journal|last1=Ariani|first1=Antonio|last2=Wittiman|first2=karl|year=2016|title=Mysida (crustacea) from apulian (SE- Italy) Waters. First record of Gastrosaccus roscoffensis bacescu. 1970 italy|journal=Thalassia Salentina |url=http://siba-ese.unisalento.it/index.php/thalassiasal/article/view/16537|url-status=live|archive-url=https://web.archive.org/web/20180511073912/http://siba-ese.unisalento.it/index.php/thalassiasal/article/view/16537 |archive-date=2018-05-11 |volume=38|pages=15–26 |publisher=University of Salento |doi=10.1285/i15910725v38p15 |language=en}}</ref>



Vagile [[Meiofauna]] is a kind of fauna which includes [[Invertebrate|invertebrates]] of marine and fresh water habitats. Knowledge about this particular branch of the fauna is scarce, however the area of the Grotta del Ciolo has been the subject of many studies regarding the community composition of these populations of invertebrates. The studies conducted in 2002 were made using baked-plates, and positioning them in three levels.<ref>

Vagile [[Meiofauna]] is a kind of fauna which includes [[invertebrate]]s of marine and fresh water habitats. Knowledge about this particular branch of the fauna is scarce, however the area of the Grotta del Ciolo has been the subject of many studies regarding the community composition of these populations of invertebrates. The studies conducted in 2002 were made using baked-plates, and positioning them in three levels.<ref>

{{Cite web|last=Martinez|first=Valente|date=2011|year=2011|title=Composition and time-space distribution of vagile meiofauna in the marine cave "Il Ciolo" (SE Italy, Mediterranean Sea)|url=http://www.vliz.be/en/imis?refid=208589|url-status=live|archive-url=|archive-date=|access-date=|website=www.vliz.be|language=en|type=Dissertation}}

{{Cite journal|last=Martinez|first=Valente|year=2011|title=Composition and time-space distribution of vagile meiofauna in the marine cave "Il Ciolo" (SE Italy, Mediterranean Sea)|url=http://www.vliz.be/en/imis?refid=208589|website=www.vliz.be|language=en|type=Dissertation}}

</ref><ref>{{Cite web|authors=Gianna Servello, Franco Andaloro, Ernesto Azzurro, Luca Castriota, Marcello Carta, Antonia Chiarore, Fabio Crocetta, Michela D’Alessandro, Francesco Denitto,Carlo Froglia, Cinzia Gravili, Martin R. Langer, Sabrina Lo Brutto,Francesco Mastrototaro, Antonella Petrocelli Carlo Ppipitone, Stefano Piraino,Giulio Relini, Donatella Serio, Nicholas Jason Xentidis and Argyro Zenetos|year=2019|title=Marine alien species in Italy: a contribution to the implementation of descriptor D2 of the Marine Strategy Framework Directive|url=https://www.researchgate.net/publication/331433409|url-status=live|archive-url=|archive-date=|access-date=|website=|language=en}}</ref>

</ref><ref>{{Cite web |author1=Gianna Servello |author2=Franco Andaloro |author3=Ernesto Azzurro |author4=Luca Castriota |author5=Marcello Carta |author6=Antonia Chiarore |author7=Fabio Crocetta |author8=Michela D'Alessandro |author9=Francesco Denitto |author10=Carlo Froglia |author11=Cinzia Gravili |author12=Martin R. Langer |author13=Sabrina Lo Brutto |author14=Francesco Mastrototaro |author15=Antonella Petrocelli Carlo Ppipitone |author16=Stefano Piraino |author17=Giulio Relini |author18=Donatella Serio |author19=Nicholas Jason Xentidis |author20=Argyro Zenetos

|year=2019|title=Marine alien species in Italy: a contribution to the implementation of descriptor D2 of the Marine Strategy Framework Directive|url=https://www.researchgate.net/publication/331433409 |website=ResearchGate |language=en}}</ref>



After 24 months in total (it took 24 months to make the number of [[Taxon|taxa]] and abundances at the three distinguishable positions) the results showed that ''Harpacticoida copepods'', ''[[Nematode|Nematoda]] and [[Foraminifera]]'' were the most abundant [[Meiobenthos|meiofaunal]] taxa (the panel surface removed and studied was a total of 75 taxa). Each position of the three showed different results, they revealed a high colonisation capacity of the [[Meiobenthos|meiofauna]], an active and passive interaction with the [[algae]]. The presence of the algae makes the habitat more complex in terms of protection from [[Predation|predators]] and [[wikt:trophic|trophic]] source.

After 24 months in total (it took 24 months to make the number of [[Taxon|taxa]] and abundances at the three distinguishable positions) the results showed that ''Harpacticoida copepods'', ''[[Nematode|Nematoda]] and [[Foraminifera]]'' were the most abundant [[Meiobenthos|meiofaunal]] taxa (the panel surface removed and studied was a total of 75 taxa). Each position of the three showed different results, they revealed a high colonisation capacity of the [[Meiobenthos|meiofauna]], an active and passive interaction with the [[algae]]. The presence of the algae makes the habitat more complex in terms of protection from [[Predation|predators]] and [[wikt:trophic|trophic]] source.



The way in which the agile [[meiofauna]] is distributed is due to environmental constraints, the artificial substrates and their dispersal properties. These studies concluded that making a better [[Taxonomy (biology)|taxonomical]] identification and using a more effective capture method will help in a more detailed individualism of the differences.

The way in which the agile [[meiofauna]] is distributed is due to environmental constraints, the artificial substrates and their dispersal properties. These studies concluded that making a better [[Taxonomy (biology)|taxonomical]] identification and using a more effective capture method will help in a more detailed individualism of the differences.

<ref>

<ref>

{{Cite journal|last1=Denitto|first1=Francesco|last2=Bussotti|first2=Simona|last3=Costantini|first3=Andrea|last4=Poto|first4=Marco|last5=Onorato|first5=Raffaele|last6=Belmonte|first6=Genuario|year=2009|title=Prima indagine Faunistica della grotta del Sifone (canale d'Otranto, Salento meridionale, Italia)|trans-title=First Survey of the Syphon's cave (canale d'Otranto, Southern Salento, Italy)|url=http://siba-ese.unisalento.it|url-status=live|archive-url=|archive-date=|access-date=|website=siba-ese.unisalento.it|location=Nardò (LE)|language=it|format=PDF|doi=10.1285/i15910725v32p129|issn=0563-3745}}

{{Cite journal|last1=Denitto|first1=Francesco|last2=Bussotti|first2=Simona|last3=Costantini|first3=Andrea|last4=Poto|first4=Marco|last5=Onorato|first5=Raffaele|last6=Belmonte|first6=Genuario|year=2009|title=Prima indagine Faunistica della grotta del Sifone (canale d'Otranto, Salento meridionale, Italia)|trans-title=First Survey of the Syphon's cave (canale d'Otranto, Southern Salento, Italy)|url=http://siba-ese.unisalento.it|website=siba-ese.unisalento.it|location=Nardò (LE)|language=it|format=PDF|doi=10.1285/i15910725v32p129|issn=0563-3745}}

</ref>

</ref>



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<ref name=":4" />

<ref name=":4" />



In the Grotta Piccola del Ciolo, other species have also been found such as: ''Noctiluca Scintillans, Cassidulinacea indet.,Globigerinacea indet., Miliolina indet., Rotaliacea indet., Rotaliina indet. Spirillinidae, Textulariina indet., Astrosphaeridae indet., Spumellaridae indet., Acanthostomella conicoides, Condonella aspera, Codonellopsis monacensis, Codonellopsis schabii, Eutintinnus fraknoi, Eutintinnus tubulosus, Petalotricha ampulla, Rhabdonellaspiralis, Salpingella acuminata, Stenosemella ventricosa, Tiarinafusus, Tintinnopsis beroidea, Tintinnopsis campanula, Tintinnopsis cincta, Tintinnopsis lieni, Tintinnopsis radix, Undella cleparedei, Undella clevei'' and ''Undella subcaudata.''<ref>{{Cite web|last1=Onorato|first1=Michele|last2=Belmonte|first2=Genuario|year=2017|title=Submarine Caves of the Salento Peninsula: Faunal Aspects|url=http://siba-ese.unisalento.it/index.php/thalassiasal/article/view/18771|url-status=live|archive-url=|archive-date=|access-date=|website=|publisher=Centro di Speleologia Sottomarina Apogon|language=en}}</ref>

In the Grotta Piccola del Ciolo, other species have also been found such as: ''Noctiluca Scintillans, Cassidulinacea indet.,Globigerinacea indet., Miliolina indet., Rotaliacea indet., Rotaliina indet. Spirillinidae, Textulariina indet., Astrosphaeridae indet., Spumellaridae indet., Acanthostomella conicoides, Condonella aspera, Codonellopsis monacensis, Codonellopsis schabii, Eutintinnus fraknoi, Eutintinnus tubulosus, Petalotricha ampulla, Rhabdonellaspiralis, Salpingella acuminata, Stenosemella ventricosa, Tiarinafusus, Tintinnopsis beroidea, Tintinnopsis campanula, Tintinnopsis cincta, Tintinnopsis lieni, Tintinnopsis radix, Undella cleparedei, Undella clevei'' and ''Undella subcaudata.''<ref>{{Cite journal|last1=Onorato|first1=Michele|last2=Belmonte|first2=Genuario|year=2017|title=Submarine Caves of the Salento Peninsula: Faunal Aspects|journal=Thalassia Salentina |url=http://siba-ese.unisalento.it/index.php/thalassiasal/article/view/18771|url-status=live|archive-url=https://web.archive.org/web/20180505183455/http://siba-ese.unisalento.it/index.php/thalassiasal/article/view/18771 |archive-date=2018-05-05 |volume=39|pages=47–72 |publisher=Centro di Speleologia Sottomarina Apogon|doi=10.1285/i15910725v39p47 |language=en}}</ref>



=== Plankton ===

=== Plankton ===

[[File:Cyclops.jpg|thumb|284x284px|Cyclopodia]]Since 2000, studies have shown the presence of [[Benthic zone|benthic]] populations of hard substrate living in the caves. The data that emerged refer to a highly varied [[Benthic zone|benthic]] wall community, on a small scale but very stable over time since, studied with two-year engraftment experiments.

[[File:Cyclops.jpg|thumb|284x284px|Cyclopodia]]Since 2000, studies have shown the presence of [[Benthic zone|benthic]] populations of hard substrate living in the caves. The data that emerged refer to a highly varied [[Benthic zone|benthic]] wall community, on a small scale but very stable over time since, studied with two-year engraftment experiments.



The cave [[plankton]] appeared to be more affected by the ''hyperbenthos'' than the external specimens.

The cave [[plankton]] appeared to be more affected by the ''hyperbenthos'' than the external specimens.



[[Mysidacea]] represented the most conspicuous component of the cave plankton, with two species typical in the Salento marine caves, ''Hemimysis margalefi'' and ''Siriella jaltensis''. ''Harpacticoida copepods'', together with [[Asexuality|asexual]] algal propagules, dominate the cave plankton numerically, whereas [[Calanoida]] and [[Cyclopoida]] copepods with [[Mollusca|mollusc veligers]] characterise the plankton of the external environment.

[[Mysidacea]] represented the most conspicuous component of the cave plankton, with two species typical in the Salento marine caves, ''Hemimysis margalefi'' and ''Siriella jaltensis''. ''Harpacticoida copepods'', together with [[Asexuality|asexual]] algal propagules, dominate the cave plankton numerically, whereas [[Calanoida]] and [[Cyclopoida]] copepods with [[Mollusca|mollusc veligers]] characterise the plankton of the external environment.



The annual community composition changes seasonally, with clear horizontal partitioning of the plankton and significant differences between the two stations of the cave.

The annual community composition changes seasonally, with clear horizontal partitioning of the plankton and significant differences between the two stations of the cave.



Higher water turbulence has been proposed as the reason for the presence of asexual propagules even in the inner cave station. An explanation of the benthos impoverishment has been proposed as an alternative to the current ‘trophic depletion’ theory.<ref>{{Cite web|last1=Rubino|first1=Fernando|last2=Moscatello|first2=Salvatore|last3=Saracino|first3=Orestina|last4=Fanelli|first4=Giovanni|year=2004|title=Plankton biodiversity around the Salento Peninsula (South East Italy): An integrated water/sediment approach|url=https://www.researchgate.net/publication/250304932|url-status=live|archive-url=|archive-date=|access-date=|website=|language=en}}</ref> <ref>{{Cite web|last1=Poto|first1=Marco|last2=Belmonte|first2=Genuario|last3=Onorato|first3=Raffaele|year=2006|title=Novità esplorative e biologiche nelle grotte sottomarine del Canale d'Otranto|trans-title=Exploratory and biological innovations in underwater caves of the Otranto Canal|url=https://www.researchgate.net/publication/277042849|url-status=live|archive-url=|archive-date=|access-date=|website=|language=it}}</ref>

Higher water turbulence has been proposed as the reason for the presence of asexual propagules even in the inner cave station. An explanation of the benthos impoverishment has been proposed as an alternative to the current 'trophic depletion' theory.<ref>{{Cite web|last1=Rubino|first1=Fernando|last2=Moscatello|first2=Salvatore|last3=Saracino|first3=Orestina|last4=Fanelli|first4=Giovanni|year=2004|title=Plankton biodiversity around the Salento Peninsula (South East Italy): An integrated water/sediment approach|url=https://www.researchgate.net/publication/250304932 |website=ResearchGate |language=en}}</ref><ref>{{Cite web|last1=Poto|first1=Marco|last2=Belmonte|first2=Genuario|last3=Onorato|first3=Raffaele|year=2006|title=Novità esplorative e biologiche nelle grotte sottomarine del Canale d'Otranto|trans-title=Exploratory and biological innovations in underwater caves of the Otranto Canal|url=https://www.researchgate.net/publication/277042849|website=ResearchGate |language=it}}</ref>



=== Land Fauna ===

=== Land Fauna ===

In the sand present in the bottom of the Grotta Piccola del Ciolo scientists discovered ''Arachnanthus oligopodus,'' previously found only in a cave in [[Marseille]]; ten species of interstitial [[Gastrotrich|Gastrotrichs]], three of which unknown; and, a species of [[Priapulida]], previously only known in the [[tropics]].

In the sand present in the bottom of the Grotta Piccola del Ciolo scientists discovered ''Arachnanthus oligopodus,'' previously found only in a cave in [[Marseille]]; ten species of interstitial [[Gastrotrich]]s, three of which unknown; and, a species of [[Priapulida]], previously only known in the [[tropics]].

<ref name=":4" />

<ref name=":4" />

<ref>

<ref>

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|title=Stratigraphic Architecture of the Salento Coast from Capo d'Otranto to S. Maria di Leuca (Apulia, Southern Italy)

|title=Stratigraphic Architecture of the Salento Coast from Capo d'Otranto to S. Maria di Leuca (Apulia, Southern Italy)

|url=https://www.researchgate.net/publication/234128210

|url=https://www.researchgate.net/publication/234128210

|website=ResearchGate

|url-status=live

|archive-url=

|archive-date=

|access-date=

|website=www.researchgate.net

|language=en

|language=en

}}

}}

</ref><ref>{{Cite web|last=Parente|first=Mariano|year=1994|title=Cymopolia decastroi n. sp. and Cymopolia barattoloi n. sp.from the upper M aastrichtian of southeastern Salento (Apulia, southern Italy) with some remarks on the problem of species definition in fossil Dasycladales|url=https://www.zobodat.at/pdf/Beitr-Palaeontologie_19_0161-0179.pdf|url-status=live|archive-url=|archive-date=|access-date=|website=|language=en|location=Wien}}</ref>

</ref><ref>{{Cite web|last=Parente|first=Mariano|year=1994|title=Cymopolia decastroi n. sp. and Cymopolia barattoloi n. sp.from the upper M aastrichtian of southeastern Salento (Apulia, southern Italy) with some remarks on the problem of species definition in fossil Dasycladales|url=https://www.zobodat.at/pdf/Beitr-Palaeontologie_19_0161-0179.pdf|url-status=live|archive-url=https://web.archive.org/web/20200810092556/https://www.zobodat.at/pdf/Beitr-Palaeontologie_19_0161-0179.pdf |archive-date=2020-08-10 |website=|language=en|location=Wien}}</ref>



== Tourism ==

== Tourism ==

During the summer season, the Ciolo is a tourist location. The morphology of the territory, with a number of caves and inlets, offers a spot protected from wind and sun, for all those who want to experience the sea and the coast. In the same period of the year the cove is sheltered from the wind and remains accessible in rough sea conditions.<ref name=":5">

During the summer season, the Ciolo is a tourist location. The morphology of the territory, with a number of caves and inlets, offers a spot protected from wind and sun, for all those who want to experience the sea and the coast. In the same period of the year the cove is sheltered from the wind and remains accessible in rough sea conditions.<ref name=":5">

{{Cite web|last=|first=|date=14 August 2020|title=Il Ciolo, il rifugio dell'anima ai confini della terra|trans-title=Ciolo, the soul's haven at the end of the Earth|url=https://www.leccenews24.it/turismo/viaggi-itinerari/il-ciolo-rifugio-dell-anima-ai-confini-della-terra.htm|url-status=live|archive-url=|archive-date=|access-date=|website=www.leccenews24.it|language=it}}

{{Cite web|last=|first=|date=14 August 2020|title=Il Ciolo, il rifugio dell'anima ai confini della terra|trans-title=Ciolo, the soul's haven at the end of the Earth|url=https://www.leccenews24.it/turismo/viaggi-itinerari/il-ciolo-rifugio-dell-anima-ai-confini-della-terra.htm|url-status=live|archive-url=https://web.archive.org/web/20150820081507/http://www.leccenews24.it/turismo/viaggi-itinerari/il-ciolo-rifugio-dell-anima-ai-confini-della-terra.htm |archive-date=2015-08-20 |website=www.leccenews24.it|language=it}}

</ref> The location attracts many tourists also due to its close proximity to Santa Maria di Leuca.

</ref> The location attracts many tourists also due to its close proximity to Santa Maria di Leuca.



=== Trekking ===

=== Trekking ===

The Ciolo's area offers [[trekking]] and [[hiking]] activities via the footpaths of the ''Regional Natural Coastal Park'' to Novaglie'',''. This path is called The S''entiero'' ''del'' ''Vecchio'' ''Ciolo'' (''the path of the Old Ciolo''), and ''The Sentiero delle Cipolliane (the Cipolliane's path)'', and it gives access to the natural and historical features of the region.

The Ciolo's area offers [[trekking]] and [[hiking]] activities via the footpaths of the ''Regional Natural Coastal Park'' to Novaglie'',''. This path is called The S''entiero'' ''del'' ''Vecchio'' ''Ciolo'' (''the path of the Old Ciolo''), and ''The Sentiero delle Cipolliane (the Cipolliane's path)'', and it gives access to the natural and historical features of the region.

<ref>

<ref>

{{Cite book|last=|first=|url=https://books.google.com/books?id=Vj1kEQ5vtMYC&q=Ciolo+puglia|title=Guida Arrampicata a Gagliano del Capo - Località Ciolo (Falesia di): Arrampicata Sportiva in Puglia|publisher=Riecon|year=2014|isbn=|volume=Volume 1301|location=|page=8|language=it|trans-title=Free Climbing Guide at Gagliano Del Capo - Località Ciolo}}

{{Cite book|last=|first=|url=https://books.google.com/books?id=Vj1kEQ5vtMYC&q=Ciolo+puglia|title=Guida Arrampicata a Gagliano del Capo - Località Ciolo (Falesia di): Arrampicata Sportiva in Puglia|publisher=Riecon|year=2014|isbn=|volume=1301|location=|page=8|language=it|trans-title=Free Climbing Guide at Gagliano Del Capo - Località Ciolo}}

</ref>

</ref>



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Ciolo can be reached on foot along a 4 ''kilometer'' path, starting from the center of Gagliano del Capo.<ref name=":13">

Ciolo can be reached on foot along a 4 ''kilometer'' path, starting from the center of Gagliano del Capo.<ref name=":13">

{{Cite web|last=|first=|date=|title=Itinerario 6 le Marine di Gagliano del Capo: Baia del Ciolo, Marina di Novaglie|trans-title=Trail 6 the Marines of Gagliano Del Capo: Ciolo's Bay, Marine of Novaglie|url=http://www.comune.gaglianodelcapo.le.it/territorio/itinerari/item/itinerario-6-le-marine-di-gagliano-del-capo-baia-del-ciolo-marina-di-novaglie?highlight=WyJjaW9sbyJd|url-status=live|archive-url=|archive-date=|access-date=|website=www.comune.gaglianodelcapo.le.it|publisher=Comune di Gagliano Del Capo|language=it}}

{{Cite web|last=|first=|date=|title=Itinerario 6 le Marine di Gagliano del Capo: Baia del Ciolo, Marina di Novaglie|trans-title=Trail 6 the Marines of Gagliano Del Capo: Ciolo's Bay, Marine of Novaglie|url=http://www.comune.gaglianodelcapo.le.it/territorio/itinerari/item/itinerario-6-le-marine-di-gagliano-del-capo-baia-del-ciolo-marina-di-novaglie?highlight=WyJjaW9sbyJd|website=www.comune.gaglianodelcapo.le.it|publisher=Comune di Gagliano Del Capo|language=it}}

</ref> From Ciolo to Gagliano del Capo it is possible to access the trail by a long staircase next to Ciolo's Bridge that provides access to the small cove; from there, leaving the sea behind, it is possible to climb the steep path that leads up to Gagliano del Capo. The route crosses the rock cliffs which contain numerous prehistoric caves; the whole path is completely surrounded by the characteristic Mediterranean landscape and also by certain rare species of plants such as the Alyssum of Leuca, the Vicia Giacominiana, the Anagyris foetida and different rare species of Orchidaceae.<ref name=":13" />

</ref> From Ciolo to Gagliano del Capo it is possible to access the trail by a long staircase next to Ciolo's Bridge that provides access to the small cove; from there, leaving the sea behind, it is possible to climb the steep path that leads up to Gagliano del Capo. The route crosses the rock cliffs which contain numerous prehistoric caves; the whole path is completely surrounded by the characteristic Mediterranean landscape and also by certain rare species of plants such as the Alyssum of Leuca, the Vicia Giacominiana, the Anagyris foetida and different rare species of Orchidaceae.<ref name=":13" />

Bird watchers can observe frequent sightings of migrating [[Wader|waders]], [[jackdaws]] and [[rock pigeons]]; whereas sightings of the [[Eleonora's falcon]] are rarer. It is also possible to see different small [[Chapel|chapels]] and votive [[Aedicula|aediculas]] in honour of ''Madonna di Leuca'', symbolic of the area.<ref name=":13" /><ref>

Bird watchers can observe frequent sightings of migrating [[wader]]s, [[jackdaws]] and [[rock pigeons]]; whereas sightings of the [[Eleonora's falcon]] are rarer. It is also possible to see different small [[chapel]]s and votive [[aedicula]]s in honour of ''Madonna di Leuca'', symbolic of the area.<ref name=":13" /><ref>{{Cite web|last=|first=|date=|title=Sentiero del Ciolo|trans-title=Ciolo's trail|url=http://www.comune.gaglianodelcapo.le.it/territorio/gallerie-immagini/item/sentiero-del-ciolo?highlight=WyJjaW9sbyJd|website=www.comune.gaglianodelcapo.le.it|publisher=Comune di Gagliano del Capo|language=it}}{{Dead link|date=August 2022 |bot=InternetArchiveBot |fix-attempted=yes }}</ref>

{{Cite web|last=|first=|date=|title=Sentiero del Ciolo|trans-title=Ciolo's trail|url=http://www.comune.gaglianodelcapo.le.it/territorio/gallerie-immagini/item/sentiero-del-ciolo?highlight=WyJjaW9sbyJd|url-status=live|archive-url=|archive-date=|access-date=|website=www.comune.gaglianodelcapo.le.it|publisher=Comune di Gagliano del Capo|language=it}}

</ref>

[[File:View from Ciolo's Bridge.jpg|left|thumb|301x301px|View from Ponte Del Ciolo (Ciolo's Bridge)]]

[[File:View from Ciolo's Bridge.jpg|left|thumb|301x301px|View from Ponte Del Ciolo (Ciolo's Bridge)]]



=== High diving ===

=== High diving ===

One of the main tourist attractions is Ponte del Ciolo (Ciolo's Bridge), the bridge that connects the two crags and from which it is possible to [[high diving|high dive]].

One of the main tourist attractions is Ponte del Ciolo (Ciolo's Bridge), the bridge that connects the two crags and from which it is possible to [[high diving|high dive]].



=== Scuba diving ===

=== Scuba diving ===

It is possible to access the sea for swimming and [[scuba diving]].

It is possible to access the sea for swimming and [[scuba diving]].

<ref>

<ref>{{Cite journal

{{Cite journal

|last=

|last=

|first=

|first=

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|publisher=Parco Regionale Costa Otranto - Santa Maria di Leuca

|publisher=Parco Regionale Costa Otranto - Santa Maria di Leuca

|volume=

|volume=

|pages=5

|page=5

|via=

|via=

|access-date=2020-11-16

}}

|archive-date=2015-02-22

</ref> Scuba divers, in Ciolo, have also the opportunity to explore the Grotta Grande del Ciolo. Although some points of the cave are quite narrow, it is possible for divers to explore the cave for its entire length safely with a little preparation.

|archive-url=https://web.archive.org/web/20150222220007/http://www.parcootrantoleuca.it/images/stories/sentierociolo.pdf

}}</ref> Scuba divers, in Ciolo, have also the opportunity to explore the Grotta Grande del Ciolo. Although some points of the cave are quite narrow, it is possible for divers to explore the cave for its entire length safely with a little preparation.



=== Rock climbing ===

=== Rock climbing ===

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|url=https://www.planetmountain.com/en/news/climbing/salento-vertical-new-rock-climbs-in-puglia-italy.html

|url=https://www.planetmountain.com/en/news/climbing/salento-vertical-new-rock-climbs-in-puglia-italy.html

|url-status=live

|url-status=live

|archive-url=https://web.archive.org/web/20170406112322/http://www.planetmountain.com:80/en/news/climbing/salento-vertical-new-rock-climbs-in-puglia-italy.html |archive-date=2017-04-06

|archive-url=

|website=Planet Mountain

|archive-date=

|website=www.planetmountain.com

|publisher=Mountain Network s.r.l

}}

}}

</ref>

</ref>

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|date=

|date=

|title=UKC Logbook|url=https://www.ukclimbing.com/logbook/crags/ciolo-26091

|title=UKC Logbook|url=https://www.ukclimbing.com/logbook/crags/ciolo-26091

|website=UKClimbing

|url-status=live

|archive-url=

|archive-date=

|website=www.ukclimbing.com

|publisher=UKClimbing Limited

}}

}}

</ref>

</ref>

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=== The Legend ===

=== The Legend ===

There is a local legend about Ciolo which involves the [[Turks of Western Thrace|Turks]] and a bell. During an invasion in Apulia by the [[Turkish people|Turkish]] Army, the soldiers landed in the Ciolo's area and looted Gagliano del Capo. A bell was part of their loot, however they found themselves in a storm and the bell fell off the boat into the sea. It is said that the bell rings every 24th of December, the day of its disappearance.

There is a local legend about Ciolo which involves the [[Turks of Western Thrace|Turks]] and a bell. During an invasion in Apulia by the [[Turkish people|Turkish]] Army, the soldiers landed in the Ciolo's area and looted Gagliano del Capo. A bell was part of their loot, however they found themselves in a storm and the bell fell off the boat into the sea. It is said that the bell rings every 24 December, the day of its disappearance.

<ref>

<ref>

{{Cite web

{{Cite web

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|trans-title=The Ciolo's fjord: a bridge between the sea and the sky|url=https://www.cortedelsalento.net/salento-dintorni/il-fiordo-del-ciolo-il-ponte-sospeso-tra-cielo-e-mare

|trans-title=The Ciolo's fjord: a bridge between the sea and the sky|url=https://www.cortedelsalento.net/salento-dintorni/il-fiordo-del-ciolo-il-ponte-sospeso-tra-cielo-e-mare

|url-status=live

|url-status=live

|archive-url=https://web.archive.org/web/20200930184224/https://www.cortedelsalento.net/salento-dintorni/il-fiordo-del-ciolo-il-ponte-sospeso-tra-cielo-e-mare |archive-date=2020-09-30 |website=www.cortedelsalento.net

|archive-url=

|archive-date=

|access-date=

|website=www.cortedelsalento.net

|language=it

|language=it

}}</ref><ref>

}}</ref><ref>

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|url=http://www.salogentis.it/2009/07/29/il-ciolo-un-piccolo-fiordo-nel-cuore-del-salento/

|url=http://www.salogentis.it/2009/07/29/il-ciolo-un-piccolo-fiordo-nel-cuore-del-salento/

|url-status=live

|url-status=live

|archive-url=https://web.archive.org/web/20090826025637/http://www.salogentis.it:80/2009/07/29/il-ciolo-un-piccolo-fiordo-nel-cuore-del-salento/ |archive-date=2009-08-26 |website=www.salogentis.it

|archive-url=

|archive-date=

|access-date=

|website=www.salogentis.it

|language=it

|language=it

}}

}}

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== The Regional Coastal Park ==

== The Regional Coastal Park ==

The Otranto coast up to Santa Maria di Leuca is a [[Regional park]] that has been established by the Regional Law of the 26th October 2006 n.30 creating a protected area of priority interest. The park was created with the aim of safeguarding the natural heritage of the protected area and enhancing the territory on a sustainable management model, protecting its biodiversity and supporting the economy of the local communities.

The Otranto coast up to Santa Maria di Leuca is a [[Regional park]] that has been established by the Regional Law of the 26th October 2006 n.30 creating a protected area of priority interest. The park was created with the aim of safeguarding the natural heritage of the protected area and enhancing the territory on a sustainable management model, protecting its biodiversity and supporting the economy of the local communities.



It is one of the biggest natural parks in the province of [[Lecce]]. Its area extends along the Salento coast for 57 ''kilometers'' and embraces an important cultural, geological and landscape heritage characterized by the presence of faunistic and flogistic species.

It is one of the biggest natural parks in the province of [[Lecce]]. Its area extends along the Salento coast for 57 ''kilometers'' and embraces an important cultural, geological and landscape heritage characterized by the presence of faunistic and flogistic species.

[[File:Otranto - baia delle orte12.jpg|thumb|314x314px|A part of the Regional Natural Coastal Park of "''Costa Otranto Santa Maria di Leuca Bosco di Tricase"'']]

[[File:Otranto - baia delle orte12.jpg|thumb|314x314px|A part of the Regional Natural Coastal Park of "''Costa Otranto Santa Maria di Leuca Bosco di Tricase"'']]

The borders of the Regional Park includes 12 municipalities of Lecce province: [[Alessano]], [[Andrano]], [[Castrignano del Capo]], Castro, [[Corsano]], [[Diso]], Gagliano del Capo, [[Ortelle]], Otranto, [[Santa Cesarea Terme]], [[Tiggiano]] and Tricase.

The borders of the Regional Park includes 12 municipalities of Lecce province: [[Alessano]], [[Andrano]], [[Castrignano del Capo]], Castro, [[Corsano]], [[Diso]], Gagliano del Capo, [[Ortelle]], Otranto, [[Santa Cesarea Terme]], [[Tiggiano]] and Tricase.



From a geological point of view the park is formed by a stratification which dates from the [[Late Cretaceous]] to the [[Quaternary]] periods.

From a geological point of view the park is formed by a stratification which dates from the [[Late Cretaceous]] to the [[Quaternary]] periods.

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|url=http://www.parcootrantoleuca.it

|url=http://www.parcootrantoleuca.it

|url-status=live

|url-status=live

|archive-url=https://web.archive.org/web/20110423035828/http://www.parcootrantoleuca.it:80/ |archive-date=2011-04-23 |website=www.parcootrantoleuca.it

|archive-url=

|archive-date=

|access-date=

|website=www.parcootrantoleuca.it

|language=it

|language=it

}}

}}

</ref>

</ref>



Additionally there are also three [[Site of Community Importance]] included in The Regional Coastal Park:

Additionally there are also three [[Site of Community Importance]] included in The Regional Coastal Park:



* The [[Oak|oak-trees]] ''Park of Castro.''

* The [[Oak|oak-trees]] ''Park of Castro.''

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|url=http://www.parks.it/parco.costa.otranto/Eindex.php

|url=http://www.parks.it/parco.costa.otranto/Eindex.php

|url-status=live

|url-status=live

|archive-url=https://web.archive.org/web/20140726100541/http://www.parks.it/parco.costa.otranto/Eindex.php |archive-date=2014-07-26 |website=www.parks.it

|archive-url=

|archive-date=

|access-date=

|website=www.parks.it

|language=it

|language=it

}}

}}

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* [http://www.comune.gaglianodelcapo.le.it Comune of Gagliano del Capo] (in Italian)

* [http://www.comune.gaglianodelcapo.le.it Comune of Gagliano del Capo] (in Italian)



[[Category: Province of Lecce]]

[[Category:Province of Lecce]]

[[Category: Caves]]

[[Category:Caves of Italy]]

[[Category:Apulia]]

[[Category:Landforms of Apulia]]

[[Category:Canyons and gorges]]

[[Category:Canyons and gorges of Italy]]

[[Category:fjords]]

[[Category:Fjords of Italy]]


Latest revision as of 22:22, 15 January 2024

Ciolo
Panoramic view of Ponte del Ciolo (Ciolo's Bridge)
Ciolo is located in Italy
Ciolo

Ciolo

Ciolo is located in Apulia
Ciolo

Ciolo

Floor elevation26 metres (100 ft)
Length190 metres (620 ft) West-East
Width49 metres (161 ft) North-South
Depth144 metres (472 ft)
Naming
Native nameCiole (Sicilian)
English translationMagpies
Geography
Countryflag Italy
State/Provinceflag Apulia
Population centerGagliano del Capo
Coordinates39°50′N 18°23′E / 39.84°N 18.38°E / 39.84; 18.38
Traversed byCiolo's Bridge, Ciolo's Trail, Cipolliane's Trail

Ciolo is a narrow coastal inlet and a site of historical and environmental interest, which is located in the south of Apulia, in the historical region of Salento, Italy. The location is also known as a geological site and for the presence of numerous sea caves, the largest one being the Grotta del Ciolo. Since October 2006 the Ciolo's area has become part of the Regional Park "Costa Otranto - Santa Maria di Leuca e Bosco di Tricase", created by the Apulia region to protect the eastern coast of Salento, specifically the architectural assets as well as important animal and plant species.

The name Ciolo comes from the noun in salentino dialect "ciole", which refers to crowsormagpies, which are widespread in this region.[1][2]

Location[edit]

Ciolo is located in the comune of Gagliano del Capo, in Apulia and it is part of the Regional Natural Coastal Park of "Costa Otranto Santa Maria di Leuca Bosco di Tricase".

Panoramic view of Ponte del Ciolo (Ciolo's Bridge)

Ponte del Ciolo (Ciolo's Bridge)[edit]

Map

Ciolo is dominated by Ponte Ciolo (Ciolo's Bridge), a road bridge built in the 1960s. It crosses the inlet and connects the two shores of Santa Maria di Leuca and Novaglie. The single-span bridge is approximately 30 meters above water, 60 meters long and 10 meters wide.

The first structure, part of a project for the entire coastal road by the engineer Mario Carrone, envisaged a bridge with two continuous spans. This project was unfeasible due to the impossibility to build the central pile, as evidenced by the geo-technical report by the professor and engineer Vincenzo Cotecchia. At that point the engineer Antonio La Tegola was appointed. He adopted the technique of the Swiss engineer Robert Maillart, which required the incorporation of a thin vault and a stiffening deck. For this reason the structure the bridge was called Maillart's Bridge in the preliminary plans and studies.[3]

Ciolo's Bridge was built by rotating the previously planned road axis, an operation that was necessary to find the right supports for the span. There are still some concrete stumps under the current span, which were necessary for the construction of the rib.[3]

Since the construction in the 1960s the bridge has been object of reinforcement and consolidation's works, the last being in the summer of 2019.[3][4]

The Ciolo's Caves[edit]

In Ciolo canyon there are several sea caves formed during the Neolithic and Paleolithic age. In total this area includes three different major caves: the Grotta Grande del Ciolo (Ciolo's Huge Cave), the Grotta Piccola Del Ciolo (Ciolo's Small Cave) and the Grotta Delle Prazziche (Cave of the Prazziche). [5][6]

Caves Coordinates Length (in meters) Width (in meters)
Grotta Piccola Del Ciolo 39° 50' 38'' N 18° 23' 11'' E 120 -missing-
Grotta Grande Del Ciolo 39° 50' 13'' N 18° 23' 04'' E 120 -missing-
Grotta Delle Prazziche 39° 50' 42" N 18° 23' 05.6" E 40 6

Grotta Piccola Del Ciolo[edit]

The Grotta Piccola Del Ciolo, also called the "Grotta della foca monaca" (Cave of the monk seal), is a semi-submerged cave located in the homonymous cove. Its entrance is located on the west side of the canyon (facing the sea) and it is set on a fracture slightly enlarged by water.[7][8]

The main cave develops linearly for more than 120 meters, which makes it one of the longest in all the Salento sub-peninsula. The cave is formed by different chambers: on the west side of the entrance there is a natural chamber about 30 meters long and in the terminal part of the main cave there is a tiny beach. It was in this chamber that the speleologist Franco Grandi found a monk seal, which gave the name to the cave itself. Inside a source of fresh water is available.[7][9] From a strictly biological point of view, different studies have been carried out during the years in the cave by different research teams coordinated by the University of Salento, University of Modena and Reggio Emilia and University of Urbino. Since 2000, studies have been performed on benthic hard substrate stands living in the cave as well as taxonomic studies on the fauna able to live on the sea bottom and on the planktonic one.[8] The studies have revealed a diverse sea bottom community even on little scale but very stable in time even if decreasing. The plankton analysed has appeared rich in nutrition, indicating that the decline of the community may relate to other factors, such as the possible infiltration of fresh water.[8]

Grotta Grande Del Ciolo[edit]

The Grotta Grande Del Ciolo is also known by different names, such as Grotta degli Spiriti (Ghosts' Cave), Grotta dei Passeri (Sparrows' Cave)[a] and Bocca del Pozzo (Well's Mouth). The cave is semi-submerged and is characterized by a wide entrance, the result of an ancient phenomenon of collapse that partially occluded a portion of the archeological substrate of the cave, about 20 meters above the sea level, leaving the remaining portion exposed to sea erosion provoked by the constant inflow and then outflow of water and waves.[7] The cave develops longitudinally by 120 meters and the height of the entrance is over 30 meters, progressively decreasing along its longitudinal development.[7]

The cave contains a pond generated by a source of fresh water which originates from a subterranean source near its location.[10]

Grotta Delle Prazziche[edit]

Grotta Delle Prazziche [1] is one of the main caves near Ciolo, and is accessible by boat. The structure of the cave is circular, and at the top there is a vertical syphon to the open air.[7] Many studies have been carried out inside and some prehistoric remains have been found, including handcrafts belonging to the Neolithic, ceramics and remains of rhinos.[5]

Geology[edit]

The eastern coast of Salento is a noteworthy geological location due to the events that took place in the Mediterranean area starting from the Cretaceous period.[11]

Limestone ridge of Ciolo

Ciolo is mostly formed by a lower part of the stratigraphic succession, which includes Cretaceous bioclastic limestones and breccias and conglomerates of the dating to the late Oligocene (Chattian). In this area there are deposits of phosphatic limestone formations, phosphatic conglomerates and phosphatic concentrations. The upper part consists of Miocene aged limestone.[12][13][14] The limestones present in the Ciolo area is characterized by bioclastic calcarenites and calcirudites and it is recognizable by its parallel and oblique lamination.[15]

Flora[edit]

In Ciolo's area several botanical rarities can be found: mediterranean onion species, ferns, the Alyssum of Leuca, the Fiordaliso of Leuca, the Campanula pugliese, the Vicia Giacominiana and several type of rare orchids.[16]

Ferns[edit]

Ciolo is an hypogeal habitat for botanical species like cryptogams: algae, mosses and ferns. There are about sixty species of bryophytes living in the caves of Apulia which have been studied, including fifteen types of ferns.

Focusing the attention on the caves in Apulia, it is worth considering the distribution of ferns (Filicopsida). Ferns have interested many scientists since the 1950s and 1960s, the biggest contributions to the studies in this area were made by Franco Anelli, Francesco Orfino and Pietro Parenzan. They mainly focused on Grotta di Castellana but extended their studies also to Ciolo. The University of Lecce undertook pteridological studies on this territory.

Close up on Ferns' leaves

The caves have very limited examples of phototrophic vegetation. There are some cases in which it is possible to find etiolate plants inside these caves. These plants grow from seeds transported by water, but without light they do not grow enough and then they die. For their sexed reproduction high humidity is essential, humidity is also the reason for the low desiccation process.[17]

Ciolo's Caves are the only certified sites in Apulia where Asplenium marinum exists. Ciolo's Caves are on the boundary of the Eastern area of this species.

The morphology of the caves has determined their plant colonization. The wide entrance of some of the caves have created an ideal plant habitat and supports a major vegetal population. Populations are small and with a poor capability to adapt. There is scientific evidence that a unique event of colonization gave birth to single fern populations. Protected habitats can function as shelters (they protect some species) if they have particular micro-climatic conditions, thus they act for species which haven't found a balance with the changeable environment.

The status of phytogeographic relict can be defined only for some species of ferns. Following the hypothesis of Pichi Sermolli the Asplenium marines in Apulia in Ciolo could be a relic from the wet period of the Pleistocene. [18]

It is possible to track different chorological models in the Ciolo using the distribution of Asplenium marinum. There is an hypothesis that the species is present in this territory as a relic banished to an hypogeal habitat due to climate changes.

Alyssum of Leuca[edit]

Along the paths that cover the area of Ciolo some botanical species of flowers can be found such as the Alyssum, a typical plant of this part of the region. It can be easily found due to the fact that it usually grows under the solar exposition, it is resistant to both cold and warm weather, and it can grow in stony and dry areas.

Vicia Giacominiana[edit]

The Vicia Giacominiana is a special type of plant native of Salento. It is a therophyte, and it is usually two meters high. It flowers during the months of April and May.

Its flowers are fuchsia, arranged in groups of racemes with a stem twice the length of the leaves. The Vicia Giacominiana is found exclusively within herbaceous communities of plants.

Fiordaliso of Leuca[edit]

The Fiordaliso of Leuca is a rare plant, native from the area of Salento, which grows above limestone cliffs and next to the sea.

It is a perennial, bushy and thick plant, that can reach the height of 30 up to 60 meters. [19]

Carnation of Salento[edit]

The Carnation of Salento, also called Dianthus Japigicus Bianco & Brullo, of the Caryophyllaceae family, is a new species of Cernation born in Salento that grows on the limestone walls between Otranto and Santa Maria di Leuca. These plants have branched stems and their flowers consist of five pink or purple petals with a jagged edge. [19]

  • Campanula pugliese at Ciolo
    Campanula pugliese at Ciolo
  • Carnation of Salento
    Carnation of Salento
  • Fiordaliso Nobile
    Fiordaliso Nobile
  • Alisso of Leuca
    Alisso of Leuca
  • Ophrys
    Ophrys
  • Fauna[edit]

    Marine Fauna[edit]

    The area, being part of the "Regional Park Otranto - Santa Maria di Leuca Coast", has been the subject of numerous studies regarding the fauna. [20] Studies show that thirty-two different fish species are present. [21][22]

    The Grotta Piccola del Ciolo is considered as a protective nursery for the new born of different species of fish and echinoderms; in fact numerously starfish, sea urchins, brittle stars, sea cucumbers, and crustaceans have been found. [23][24][25][26]

    Vagile Meiofauna is a kind of fauna which includes invertebrates of marine and fresh water habitats. Knowledge about this particular branch of the fauna is scarce, however the area of the Grotta del Ciolo has been the subject of many studies regarding the community composition of these populations of invertebrates. The studies conducted in 2002 were made using baked-plates, and positioning them in three levels.[27][28]

    After 24 months in total (it took 24 months to make the number of taxa and abundances at the three distinguishable positions) the results showed that Harpacticoida copepods, Nematoda and Foraminifera were the most abundant meiofaunal taxa (the panel surface removed and studied was a total of 75 taxa). Each position of the three showed different results, they revealed a high colonisation capacity of the meiofauna, an active and passive interaction with the algae. The presence of the algae makes the habitat more complex in terms of protection from predators and trophic source.

    The way in which the agile meiofauna is distributed is due to environmental constraints, the artificial substrates and their dispersal properties. These studies concluded that making a better taxonomical identification and using a more effective capture method will help in a more detailed individualism of the differences. [29]

    In this area the Arachnanthus Oligopodus, a species of the Arachnactidae family, has also been found in the depths of the Grotta Piccola del Ciolo. [23]

    In the Grotta Piccola del Ciolo, other species have also been found such as: Noctiluca Scintillans, Cassidulinacea indet.,Globigerinacea indet., Miliolina indet., Rotaliacea indet., Rotaliina indet. Spirillinidae, Textulariina indet., Astrosphaeridae indet., Spumellaridae indet., Acanthostomella conicoides, Condonella aspera, Codonellopsis monacensis, Codonellopsis schabii, Eutintinnus fraknoi, Eutintinnus tubulosus, Petalotricha ampulla, Rhabdonellaspiralis, Salpingella acuminata, Stenosemella ventricosa, Tiarinafusus, Tintinnopsis beroidea, Tintinnopsis campanula, Tintinnopsis cincta, Tintinnopsis lieni, Tintinnopsis radix, Undella cleparedei, Undella clevei and Undella subcaudata.[30]

    Plankton[edit]

    Cyclopodia

    Since 2000, studies have shown the presence of benthic populations of hard substrate living in the caves. The data that emerged refer to a highly varied benthic wall community, on a small scale but very stable over time since, studied with two-year engraftment experiments.

    The cave plankton appeared to be more affected by the hyperbenthos than the external specimens.

    Mysidacea represented the most conspicuous component of the cave plankton, with two species typical in the Salento marine caves, Hemimysis margalefi and Siriella jaltensis. Harpacticoida copepods, together with asexual algal propagules, dominate the cave plankton numerically, whereas Calanoida and Cyclopoida copepods with mollusc veligers characterise the plankton of the external environment.

    The annual community composition changes seasonally, with clear horizontal partitioning of the plankton and significant differences between the two stations of the cave.

    Higher water turbulence has been proposed as the reason for the presence of asexual propagules even in the inner cave station. An explanation of the benthos impoverishment has been proposed as an alternative to the current 'trophic depletion' theory.[31][32]

    Land Fauna[edit]

    In the sand present in the bottom of the Grotta Piccola del Ciolo scientists discovered Arachnanthus oligopodus, previously found only in a cave in Marseille; ten species of interstitial Gastrotrichs, three of which unknown; and, a species of Priapulida, previously only known in the tropics. [23] [33]

    Paleoenviroment[edit]

    In the Ciolo's area remnants of Hippwrites cornucopiae, Cymopolia decastroi, Cymopolia barattoloi, dating back to the upper Maastrichtian age, were found. [15][34]

    Tourism[edit]

    During the summer season, the Ciolo is a tourist location. The morphology of the territory, with a number of caves and inlets, offers a spot protected from wind and sun, for all those who want to experience the sea and the coast. In the same period of the year the cove is sheltered from the wind and remains accessible in rough sea conditions.[35] The location attracts many tourists also due to its close proximity to Santa Maria di Leuca.

    Trekking[edit]

    The Ciolo's area offers trekking and hiking activities via the footpaths of the Regional Natural Coastal Park to Novaglie,. This path is called The Sentiero del Vecchio Ciolo (the path of the Old Ciolo), and The Sentiero delle Cipolliane (the Cipolliane's path), and it gives access to the natural and historical features of the region. [36]

    Sentiero del vecchio Ciolo[edit]

    The path can be walked in both ways: from Ciolo to Gagliano Del Capo and vice-versa.

    Ciolo can be reached on foot along a 4 kilometer path, starting from the center of Gagliano del Capo.[37] From Ciolo to Gagliano del Capo it is possible to access the trail by a long staircase next to Ciolo's Bridge that provides access to the small cove; from there, leaving the sea behind, it is possible to climb the steep path that leads up to Gagliano del Capo. The route crosses the rock cliffs which contain numerous prehistoric caves; the whole path is completely surrounded by the characteristic Mediterranean landscape and also by certain rare species of plants such as the Alyssum of Leuca, the Vicia Giacominiana, the Anagyris foetida and different rare species of Orchidaceae.[37] Bird watchers can observe frequent sightings of migrating waders, jackdaws and rock pigeons; whereas sightings of the Eleonora's falcon are rarer. It is also possible to see different small chapels and votive aediculas in honour of Madonna di Leuca, symbolic of the area.[37][38]

    View from Ponte Del Ciolo (Ciolo's Bridge)

    High diving[edit]

    One of the main tourist attractions is Ponte del Ciolo (Ciolo's Bridge), the bridge that connects the two crags and from which it is possible to high dive.

    Scuba diving[edit]

    It is possible to access the sea for swimming and scuba diving. [39] Scuba divers, in Ciolo, have also the opportunity to explore the Grotta Grande del Ciolo. Although some points of the cave are quite narrow, it is possible for divers to explore the cave for its entire length safely with a little preparation.

    Rock climbing[edit]

    The Ciolo's cliff is the major sport climbing venue of the Salento region. It was the location of the Salento Climbing Fest event in 2013.

    The cliff is equipped with expansion bolt protection, and was re-equipped as part of the Salento Verticale project, by local climbers and the Ragni di Lecco mountaineering club, in 2013. [40]

    There are over fifty routes, ranging in grade (climbing) from 4 to 7b+. Ciolo is also a location for deep-water soloing. [41]

    Curiosities[edit]

    The Legend[edit]

    There is a local legend about Ciolo which involves the Turks and a bell. During an invasion in Apulia by the Turkish Army, the soldiers landed in the Ciolo's area and looted Gagliano del Capo. A bell was part of their loot, however they found themselves in a storm and the bell fell off the boat into the sea. It is said that the bell rings every 24 December, the day of its disappearance. [42][43]

    The Regional Coastal Park[edit]

    The Otranto coast up to Santa Maria di Leuca is a Regional park that has been established by the Regional Law of the 26th October 2006 n.30 creating a protected area of priority interest. The park was created with the aim of safeguarding the natural heritage of the protected area and enhancing the territory on a sustainable management model, protecting its biodiversity and supporting the economy of the local communities.

    It is one of the biggest natural parks in the province of Lecce. Its area extends along the Salento coast for 57 kilometers and embraces an important cultural, geological and landscape heritage characterized by the presence of faunistic and flogistic species.

    A part of the Regional Natural Coastal Park of "Costa Otranto Santa Maria di Leuca Bosco di Tricase"

    The borders of the Regional Park includes 12 municipalities of Lecce province: Alessano, Andrano, Castrignano del Capo, Castro, Corsano, Diso, Gagliano del Capo, Ortelle, Otranto, Santa Cesarea Terme, Tiggiano and Tricase.

    From a geological point of view the park is formed by a stratification which dates from the Late Cretaceous to the Quaternary periods.

    The constitution of the park aims principally at safeguarding and the protecting the historic - architectonic heritage, the coastal system and the autocrathonous greenery, with particular attention to the Quercus macrolepis. [44]

    Additionally there are also three Site of Community Importance included in The Regional Coastal Park:

    The oak-trees Park of Castro[edit]

    The park has a surface area of 4.5 hectares, part of the Regional Coastal Park. It is a protected area full of several bird species and vegetation. The Holm oak is predominant, an evergreen tree that can reach the maximum height of 30 metres. Typical Mediterranean plants such as Bay-tree, hawthorn, campanula pugliese, hedera and different types of orchids are also present. Between the park's woods there are several different species of particular birds, including owl, robin, nightingale and turtle doves. In the rocky part of the park there is a big canal which picks up water from the rain and is surrounded by dense and inaccessible vegetation.

    The Wood of Tricase[edit]

    The Wood of Tricase is part of The Regional Coastal Park. It is an area full of oak-trees and orchids. Regarding fauna, it is the area in which the monk seal, one of the rarest mammals in Europe, has been spotted. [45]

    The Wood "Le chiuse di Tiggiano"[edit]

    The Wood of Tiggiano extends along the sloped of the hills that reach the sea. The area is mainly dominated by species of trees such as holm oaks, and in the more precipitous rocky areas the most prevalent are flowers such as the campanula pugliese, the alyssum and the scrofularia pugliese.

    Gallery[edit]

  • Frame from the inside of the Ciolo canyon
    Frame from the inside of the Ciolo canyon
  • View of the Ciolo canyon from the Adriatic Sea
    View of the Ciolo canyon from the Adriatic Sea
  • View of the Ponte del Ciolo (Ciolo's Bridge)
    View of the Ponte del Ciolo (Ciolo's Bridge)
  • Grotta Grande del Ciolo
    Grotta Grande del Ciolo
  • See also[edit]

    Notes[edit]

    1. ^ Both tree sparrow and willow sparrow are native to the area.

    References[edit]

    1. ^ a b Piccinini, Marco (7 March 2015). "Grotta Grande del Ciolo" [Grotta Grande del Ciolo]. www.salogentis.it (in Italian). Archived from the original on 2016-07-14.
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  • ^ a b c DeGiuseppe, Alfredo (2020). "Speciale Ponte Ciolo" [Special Ponte Ciolo] (in Italian). 39 ° Parallelo. Archived from the original on 2020-08-13.
  • ^ "I tuffi adrenalitici dal Ponte del Ciolo" [Dives from the Ciolo Bridge]. www.regionepuglia.org (in Italian). 19 June 2019. Archived from the original on 2020-08-13.
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  • ^ Belmonte, Genuario (1999). "Le grotte marine del Salento: classificazione, localizzazione e descrizione" [The sea caves of Salento: classification, location and description]. ResearchGate (in Italian).
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  • ^ Beccarisi, Leonardo; Medagli, Pietro; Chiriacò, Leonardo; Marchiori, Silvano (6 December 2002). "Indagine fitogeografia sulle felci delle grotte pugliesi" [Phytogeographic research on the ferns present in the Apulian caves]. ResearchGate (in Italian).
  • ^ a b Medagli, Pietro; Albano, Antonella; Mele, Concetta; Marchiori, Silvano (2008). Gli endemismi esclusivi della flora salentina [The exclusive endemisms of the flora in Salento] (PDF) (in Italian). ISBN 978-88-88156-62-0.[dead link]
  • ^ Todaro, M. Antonio; Leasi, Francesca; Bizzarri, Nicoletta; Tongiorgi, Paolo (1 December 2005). "Meiofauna densities and gastrotrich community composition in a Mediterranean sea cave" (PDF). Marine Biology. 149 (5). Springer-Verlag (published 29 March 2006): 1079–1091. doi:10.1007/s00227-006-0299-z. S2CID 53122923.
  • ^ Guidetti, Paolo; Terlizzi, Antonio; Fraschetti, Simonetta; Boero, Ferdinando (28 January 2009). "Spatio‐temporal variability in fish assemblages associated with coralligenous formations in south eastern Apulia (SE Italy)". Italian Journal of Zoology. 69 (4): 325–331. doi:10.1080/11250000209356477. S2CID 83805645.
  • ^ Bussotti, Simona; Guidetti, Paolo; Belmonte, Genuario (15 July 2002). "Distribution patterns of the cardinal fish, Apogon imberbis, in shallow marine caves in southern Apulia (SE Italy)". Italian Journal of Zoology. 70 (2) (published 28 January 2009): 153–157. doi:10.1080/11250000309356509. S2CID 85309163.
  • ^ a b c Belmonte, G.; Onorato, R.; Denitto, F.; Costantini, A.; Bussotti, S.; Poto, M. "Novità esplorative e biologiche nelle grotte sottomarine del Canale d'Otranto" [Exploratory and biological news in the undersea caves of Canale d'Otranto] (PDF). digilander.libero.it (in Italian). Università di Lecce.
  • ^ Guidetti, Paolo; D' Ambrosio, Paolo (January 2004). "Spatial distribution patterns of Coris Julis and Thalassoma Pavo (pisces, labridae) along the South-Eastern Apulia Coast (SE Italy)". Thalassia Salentina. 27. Università di Lecce: 81–90. doi:10.1285/i15910725v27p81.
  • ^ Gennaio, Roberto (2014). "Diffusion of Percnon Gibbesi (H. Milne Edwards, 1853) (Crustacea, Decapoda, Grapsidae) along the south Salento, Italy". Thalassia Salentina. 36. University of Salento: 85–90. doi:10.1285/i15910725v36p85. Archived from the original on 2020-08-28.
  • ^ Ariani, Antonio; Wittiman, karl (2016). "Mysida (crustacea) from apulian (SE- Italy) Waters. First record of Gastrosaccus roscoffensis bacescu. 1970 italy". Thalassia Salentina. 38. University of Salento: 15–26. doi:10.1285/i15910725v38p15. Archived from the original on 2018-05-11.
  • ^ Martinez, Valente (2011). "Composition and time-space distribution of vagile meiofauna in the marine cave "Il Ciolo" (SE Italy, Mediterranean Sea)". www.vliz.be (Dissertation).
  • ^ Gianna Servello; Franco Andaloro; Ernesto Azzurro; Luca Castriota; Marcello Carta; Antonia Chiarore; Fabio Crocetta; Michela D'Alessandro; Francesco Denitto; Carlo Froglia; Cinzia Gravili; Martin R. Langer; Sabrina Lo Brutto; Francesco Mastrototaro; Antonella Petrocelli Carlo Ppipitone; Stefano Piraino; Giulio Relini; Donatella Serio; Nicholas Jason Xentidis; Argyro Zenetos (2019). "Marine alien species in Italy: a contribution to the implementation of descriptor D2 of the Marine Strategy Framework Directive". ResearchGate.
  • ^ Denitto, Francesco; Bussotti, Simona; Costantini, Andrea; Poto, Marco; Onorato, Raffaele; Belmonte, Genuario (2009). "Prima indagine Faunistica della grotta del Sifone (canale d'Otranto, Salento meridionale, Italia)" [First Survey of the Syphon's cave (canale d'Otranto, Southern Salento, Italy)] (PDF). siba-ese.unisalento.it (in Italian). Nardò (LE). doi:10.1285/i15910725v32p129. ISSN 0563-3745.
  • ^ Onorato, Michele; Belmonte, Genuario (2017). "Submarine Caves of the Salento Peninsula: Faunal Aspects". Thalassia Salentina. 39. Centro di Speleologia Sottomarina Apogon: 47–72. doi:10.1285/i15910725v39p47. Archived from the original on 2018-05-05.
  • ^ Rubino, Fernando; Moscatello, Salvatore; Saracino, Orestina; Fanelli, Giovanni (2004). "Plankton biodiversity around the Salento Peninsula (South East Italy): An integrated water/sediment approach". ResearchGate.
  • ^ Poto, Marco; Belmonte, Genuario; Onorato, Raffaele (2006). "Novità esplorative e biologiche nelle grotte sottomarine del Canale d'Otranto" [Exploratory and biological innovations in underwater caves of the Otranto Canal]. ResearchGate (in Italian).
  • ^ Cardone, F.; Corriero, G.; Longo, C. (2020). "Massive bioconstructions built by Neopycnodonte cochlear (Mollusca, Bivalvia) in a mesophotic environment in the central Mediterranean Sea". Scientific Reports. 10 (1) (published 14 April 2020): 6337. Bibcode:2020NatSR..10.6337C. doi:10.1038/s41598-020-63241-y. PMC 7156399. PMID 32286422.
  • ^ Parente, Mariano (1994). "Cymopolia decastroi n. sp. and Cymopolia barattoloi n. sp.from the upper M aastrichtian of southeastern Salento (Apulia, southern Italy) with some remarks on the problem of species definition in fossil Dasycladales" (PDF). Wien. Archived (PDF) from the original on 2020-08-10.
  • ^ "Il Ciolo, il rifugio dell'anima ai confini della terra" [Ciolo, the soul's haven at the end of the Earth]. www.leccenews24.it (in Italian). 14 August 2020. Archived from the original on 2015-08-20.
  • ^ Guida Arrampicata a Gagliano del Capo - Località Ciolo (Falesia di): Arrampicata Sportiva in Puglia [Free Climbing Guide at Gagliano Del Capo - Località Ciolo] (in Italian). Vol. 1301. Riecon. 2014. p. 8.
  • ^ a b c "Itinerario 6 le Marine di Gagliano del Capo: Baia del Ciolo, Marina di Novaglie" [Trail 6 the Marines of Gagliano Del Capo: Ciolo's Bay, Marine of Novaglie]. www.comune.gaglianodelcapo.le.it (in Italian). Comune di Gagliano Del Capo.
  • ^ "Sentiero del Ciolo" [Ciolo's trail]. www.comune.gaglianodelcapo.le.it (in Italian). Comune di Gagliano del Capo.[permanent dead link]
  • ^ "Scheda per il censimento degli itinerari naturalistici del Parco Regionale Costa Otranto - Santa Maria di Leuca" [Sheet for the census of the naturalistic routes of the Regional Natural Coastal Park Otranto - Santa Maria di Leuca] (PDF). Parco Regionale Costa Otranto - Santa Maria di Leuca e Bosco di Tricase (in Italian). Parco Regionale Costa Otranto - Santa Maria di Leuca: 5. Archived from the original (PDF) on 2015-02-22. Retrieved 2020-11-16.
  • ^ Schiantarelli, Davide. "Salento vertical, new rock climbs in Puglia, Italy". Planet Mountain. Archived from the original on 2017-04-06.
  • ^ "UKC Logbook". UKClimbing.
  • ^ Staff Corte del Salento (27 August 2016). "Il fiordo del Ciolo: il ponte sospeso tra cielo e mare" [The Ciolo's fjord: a bridge between the sea and the sky]. www.cortedelsalento.net (in Italian). Archived from the original on 2020-09-30.
  • ^ Piccinini, Marco (29 July 2009). "Ciolo, un "piccolo fiordo" nel cuore del Salento" [Ciolo, a "little fjord" in the heart of Salento]. www.salogentis.it (in Italian). Archived from the original on 2009-08-26.
  • ^ "Il parco Naturale Regionale "Costa Otranto S.M. di Leuca - Bosco di Tricase" [The Regional Natural Park "Costa Otranto S.M di Leuca - Bosco di Tricase"]. www.parcootrantoleuca.it (in Italian). Archived from the original on 2011-04-23.
  • ^ "Bosco di Tricase" [The Wood of Tricase]. www.parks.it (in Italian). 2020. Archived from the original on 2014-07-26.
  • External links[edit]


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