Carswell impact structure
In this article we will be addressing Carswell impact structure, a topic that has captured the attention of numerous individuals around the world. In order to provide a comprehensive and detailed view on Carswell impact structure, we will explore different aspects related to this topic, from its origins to its relevance today. Additionally, we will examine various perspectives and opinions of experts in the field, with the purpose of offering readers a deep and complete understanding of Carswell impact structure. In addition, we will analyze the impact that Carswell impact structure has had in different areas, as well as its possible implications for the future. Ultimately, this article aims to shed light on Carswell impact structure, providing readers with an informed and enriching perspective on this topic.
| Carswell impact structure | |
|---|---|
 In the northern part the rim is visible as a series of low hills, in the southern part it is indicated by the course of Douglas River. Carswell Lake (in the upper right) cuts into the structure. | |
| Impact crater/structure | |
| Diameter | 39 kilometres (24 mi) |
| Age | 115 ± 10 million years (Lower Cretaceous) |
| Exposed | Yes |
| Drilled | Yes |
| Location | |
| Coordinates | 58°26′26″N 109°30′24″W / 58.44056°N 109.50667°W |
| Country | Canada |
| Province | Saskatchewan |
  Carswell impact structure Location of Carswell impact structure in Saskatchewan | |
| Topo map | NTS 74K5 Cluff Lake, 74K6 Jolley Lake |
| Access | Saskatchewan Highway 955 |
Carswell is an impact structure within the Athabasca Basin of the Canadian Shield in northern Saskatchewan, Canada.[1] It is 39 kilometres (24 mi) in diameter and the age is estimated to be 115 ± 10 million years (Lower Cretaceous). The impact structure is exposed at the surface.
The central peak complex of faulted metamorphic rocks displays shatter cones, planar deformation features, pseudotachylyte veins, and impact melts and breccias. There is also evidence of planar deformation features in quartz grains far to the south of the outer ring of present-day hills, which suggests the ring of hills are not the rim of the original crater but a peak ring within a much larger structure. The Carswell Formation, composed of algal limestone, may have formed on seamounts elevated to near the surface as part of the peak ring.[2]
Access
The Carswell impact structure can be reached by Saskatchewan Highway 955. The 245 kilometres (152 mi) gravel road begins in the village of La Loche and ends at the old Cluff Lake mine site within the crater. The Cluff Lake uranium mine produced over 62 million pounds of yellowcake during its 22-year operating life.[3] Since the mine is now closed and decommissioned, there are no travel services in the vicinity and no functional airstrip. Motorists driving to the structure need to carry sufficient fuel and supplies for the round trip back to La Loche.
See also
References
- ^ "Carswell". Earth Impact Database. Planetary and Space Science Centre University of New Brunswick Fredericton. Retrieved 2008-12-30.
- ^ a b Genest, S.; Robert, F.; Duhamel, I. (2010). "The Carswell impact event, Saskatchewan, Canada: Evidence for a pre-Athabasca multiring basin?". In Reimold, W.U.; Gibson, R.L. (eds.). Large Meteorite Impacts and Planetary Evolution IV. Geological Society of America Special Paper. Vol. 465. pp. 543–570. doi:10.1130/2010.2465(26). ISBN 9780813724652.
- ^ "Comprehensive Study Report - Cluff Lake Decommissioning Project" (PDF). Canadian Nuclear Safety Commission. December 2003. Retrieved 2013-10-03.
External links
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