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How Many Meteorites Have Landed In Western Canada? Prospects For The Missing Holocene Impact Record

Date:
December 1, 2008
Source:
Geological Society of America
Summary:

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Herd et al. report the discovery of a 36-m-diameter impact crater located in a forested area near the town of Whitecourt, Alberta, Canada. Although too overgrown to be seen in air photos or satellite images, the crater is revealed using a bare-Earth digital elevation model obtained through airborne Light Detection and Ranging (LiDAR).

The crater formed in deglacial sediments, with impact ejecta burying a soil with a radiocarbon age of ~1100 years. Seventy-four iron meteorites (0.1-1196 g) have been recovered, most having an angular, shrapnel-like shape.

These meteorites were buried at depths of <25 cm and are interpreted to result from fragmentation of the original larger mass of the impactor, either at low altitude or during the impact event.

Impact of the main mass formed the simple bowl-shaped impact structure associated with an ejecta blanket and crater fill. Herd et al. show that LiDAR may be a useful tool to look for additional small impact craters.

Journal referernce: C.D.K. Herd et al., Geology, December issue, Pages 955-958.


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The above story is based on materials provided by Geological Society of America. Note: Materials may be edited for content and length.


Cite This Page:

Geological Society of America. "How Many Meteorites Have Landed In Western Canada? Prospects For The Missing Holocene Impact Record." ScienceDaily. ScienceDaily, 1 December 2008. <www.sciencedaily.com/releases/2008/11/081126091541.htm>.
Geological Society of America. (2008, December 1). How Many Meteorites Have Landed In Western Canada? Prospects For The Missing Holocene Impact Record. ScienceDaily. Retrieved March 2, 2015 from www.sciencedaily.com/releases/2008/11/081126091541.htm
Geological Society of America. "How Many Meteorites Have Landed In Western Canada? Prospects For The Missing Holocene Impact Record." ScienceDaily. www.sciencedaily.com/releases/2008/11/081126091541.htm (accessed March 2, 2015).

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