For the New Zealand islet called Puddingstone Rock, see Otago Harbour.
A polished section of Hertfordshire puddingstone
Puddingstone, also known as either pudding stoneorplum-pudding stone, is a popular name applied to a conglomerate that consists of distinctly rounded pebbles whose colours contrast sharply with the colour of the finer-grained, often sandy, matrix or cement surrounding them. The rounded pebbles and the sharp contrast in colour gives this type of conglomerate the appearance of a raisin or Christmas pudding.[1][2] There are different types of puddingstone, with different composition, origin, and geographical distribution. Examples of different types of puddingstones include the Hertfordshire, Schunemunk, Roxbury, and St. Joseph Island (Drummond Island) puddingstones.
Hertfordshire puddingstone is a silica-cemented conglomerate composed of rounded flintpebbles and cobbles with matrix of fine sand and silica cement. The Hertfordshire Puddingstone is characterized by silica-cemented flint gravel that is brown to deep red in colour and often exhibits black exteriors and thin rinds on cut or polished surfaces. It typically occurs scattered across the land surface as isolated concretion-like masses in the areas of Hertfordshire and Plumstead Common, England. Large masses of Hertfordshire Puddingstone often occur within local Pleistocene glacial tills. More than a dozen large blocks of this puddingstone were recovered from Paleogene sediments during construction of the A10 bypass from Thundridge to Puckeridge in 2004. This indicates that the loose blocks of Hertfordshire Puddingstone were probably eroded out of these sediments. Although it is hypothesized that it is groundwater silcrete, its origin remains unresolved.[3][4]
The Schunemunk puddingstone, which is exposed extensively on Bearfort Mountain, Boonton, Rockaway Township and Schunemunk Mountain, is a conglomerate in New York and New Jersey that is part of a 3,000 feet (910 m) thick geologic formation formally known as the Skunnemunk Conglomerate. This puddingstone is a distinctive, Late Devonian, grayish-purple to grayish-red, thin to very thick-bedded, cross–bedded, conglomerate. Within the Skunnemunk Conglomerate, it is interbedded with grayish-purple to grayish-red sandstone, thin-bedded, medium-gray sandstone, and greenish-gray and grayish-red shale with mudcracks. This conglomerate consists of pebbles and cobbles of white vein quartz, red and green quartzite, sandstone, red and gray chert, and red shale. The grayish-purple to grayish-red conglomerate and sandstone is cemented largely by hematite and microcrystalline quartz. The cobbles that it contains range in size from 2.5 in (6.4 cm) to 6.5 in (17 cm).[5][6] Pieces of Skunnemunk Conglomerate are easy to recognize and have been found in glacial deposits throughout the lower Hudson Valley region.[7]
The Roxbury puddingstone is a massive, Ediacaran, clast-supported pebble and cobble conglomerate that occurs within the Brookline Member of the Roxbury Conglomerate that is exposed around Boston, Massachusetts region. This conglomerate is composed of a grey feldspathic sand matrix and well-rounded pebbles and cobbles of quartzite, granite, felsite, and quartz monzonite. The beds of ‘puddingstone’ are complexly interbedded with layers of massive diamictite and laminated and graded argillite and sandstone. It likely accumulated as turbidites and submarine slumps within a submarine fan or outer slope environment within a deep rift basin submerged by marine waters.[8][9]
Jasper conglomerate
[edit]Jasper-quartz pebble conglomerate from Ontario, Canada
Jasper conglomerate, which is also denominated "pebble jasper conglomerate", "Saint Joseph Island puddingstone", "Drummond Island puddingstone", or "Michigan(ian) puddingstone", occurs in Saint Joseph Island and the vicinity of the Saint Mary's River, north and northwest of the Bruce MinesofNorthern Ontario, Canada, circa 65 kilometres (40 mi) east of Sault Sainte Marie, Ontario. In these locales, it occurs as thick beds of Paleoproterozoic pebble conglomerate within the medial part of a geologic formation that is named the Lorrain Formation of the Cobalt Group. The jasper conglomerate consists of subrounded pebbles of red jasper, black chert, white quartzite, hematite, and semi-transparent quartz in a matrix of coarsely grained quartzite. It contains circa 30% to 90% of pebbles. Within the deposits of Lorrain Formation, the jasper conglomerates occur principally as the sedimentary fills of erosional troughs and channels of what are interpreted to be either alluvial fans or deposits of braided river.[10][11] These deposits are inferred to be nonglacial in origin and immediately postdate the Paleoproterozoic Makganyene glaciation.[12]
Elsewhere, e. g. in Drummond Island, Michigan, United States, jasper conglomerate, there denominated "Drummond Island puddingstone", occurs as loose gravel within Pleistoceneglacial drift. These fragments of jasper conglomerate are glacial erratics that continental ice sheets from Northern Ontario eroded and then spread throughout Michigan, including in Drummond Island, and as far south as Ohio and Kentucky during repeated glacial advances and retreats.[13]
^Neuendorf, K.E.K., J.P. Mehl, Jr., and J.A. Jackson (2005) Glossary of Geology. Springer-Verlag, New York, 779 pp., ISBN3-540-27951-2
^The McGraw-Hill Companies (2003) McGraw-Hill dictionary of geology and mineralogy, 2nd ed. The McGraw-Hill Companies, Inc, New York, 420 pp., ISBN0-07-141044-9
^Herman, G.C., and J.P. Mitchell (1991) Bedrock Geologic Map of the Green Pond Mountain Region from Dover to Greenwood Lake, New Jersey. Geological Map Series no. 91-2. New Jersey Geological and Water Survey, Trenton, New Jersey.
^Merguerian, C., and J.E. Sanders (1992) Guide 17: Delaware Water Gap and Vicinity, New Jersey and Pennsylvania, Trip 23: 20 June 1992. Duke Geological Laboratory, Westbury, New York.
^Anonymous (2013a) The Green Pond Outlier. Geology of National Parks, United States Geological Survey, Reston, Virginia.
^Carto, S.L., and N. Eyles (2011) Chapter 43 The Squantum Member of the Boston Basin, Massachusetts, USA In: E. Arnaud, G.P. Halverson, and G. Shields-Zhou, eds. pp. 475-480, The Geological Record of Neoproterozoic Glaciations. Memoirs no. 36. Geological Society, London, England.
^Passchier, S., and E. Erukanure (2010) Palaeoenvironments and weathering regime of the Neoproterozoic Squantum ‘Tillite’, Boston Basin: no evidence of a snowball Earth. Sedimentology. 57(6):1526–1544.
^Lowey, G.W. (1985) Stratigraphy and Sedimentology of the Lorrain Formation, Huronian Supergroup (Aphebian), Between Sault Ste. Marie and Elliot Lake, Ontario, and Implications For Stratiform Gold Mineralization. Open File Report no. 1154. Geological Survey of Canada, Ottawa, Canada.
^Baumann, S. D. J., T. Arrospide, and A. E. Wolosyzn (2011) Preliminary Redefinition of the Cobalt Group (Huronian Supergroup), in the Southern Geologic Province, Ontario, Canada. Midwest Institute of Geosciences and Engineering, Chicago, Illinois, USA.
^Kopp R. E., J. L. Kirschvink, I. A. Hilburn, and C. Z. Nash. (2005) The Paleoproterozoic snowball Earth: a climate disaster triggered by the evolution of oxygenic photosynthesis. Proceedings of the National Academy of Sciences. 102(32): 11131–6.
^Slawson, C. B. (1933) The Jasper Conglomerate, an Index of Drift Dispersion. The Journal of Geology. 41(5): 546–52.
^ abMitchell, R.S. (1985). Dictionary of Rocks. New York: Van Nostrand Reinhold Company. pp. 161–162. ISBN0-442-26328-7.
