| Haughton crater | |
|---|---|
Synthetic aperture radar image of Haughton crater
| |
| Impact crater/structure | |
| Confidence | Confirmed |
| Diameter | 23 km (14 mi) |
| Age | 32-31 Ma Oligocene |
| Exposed | Yes |
| Drilled | No |
| Location | |
| Location | Devon Island |
| Coordinates | 75°23′N 89°40′W / 75.383°N 89.667°W / 75.383; -89.667 |
| Country | Canada |
| State | Nunavut |
  Location of the crater in Canada | |
Haughton impact crater is located on Devon Island, Nunavut in far Northern Canada. It is about 23 km (14 mi) in diameter and was formed 31–32 million years ago during the Early Oligocene.[1] The impacting object is estimated to have been approximately 2 km (1.2 mi) in diameter. Devon Island itself is composed of Paleozoic shale and siltstone overlying gneissic bedrock. When the crater formed, the shale and siltstone were peeled back to expose the basement; material from as deep as 1,700 m (5,600 ft) has been identified.
At 75° north latitude, it is one of the highest-latitude impact craters known. The temperature is below the freezing point of water for much of the year, and the limited vegetation is slow-growing, leading to very little weathering. For this reason Haughton retains many geological features that lower-latitude craters lose to erosion.
Because Haughton's geology and climatology are as close to Mars-like as can be had on Earth, Haughton and its environs have been dubbed by scientists working there as "Mars on Earth". For example, the centre of the crater contains impact breccia (ejected rock which has fallen back into the impact zone and partially re-welded) that is permeated with permafrost, thus creating a close analogue to what may be expected at crater sites on a cold, wet Mars. The Mars Institute and the SETI Institute operate the Haughton–Mars Project at this site, designed to test many of the challenges of life and work on Mars. The non-profit Mars Society also operates the Flashline Mars Arctic Research Station (FMARS) at this site and conducts similar research.
