File:Bigach Impact Crater, Kazakhstan.JPG

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Summary

Description
English: Bigach impact crater, Kazakhstan. At approximately five million years old, Bigach is a relatively young geologic feature. However, active tectonic processes in the region have caused movement of parts of the structure along faults, leading to a somewhat angular appearance (image centre). The roughly circular rim of the 8-kilometer (diameter) structure is still discernible around the relatively flat interior. In addition to modification by faulting and erosion, the interior of the impact structure has also been used for agricultural activities, as indicated by the presence of tan, graded fields. Other rectangular agricultural fields are visible to the north-east and east. The closest settlement, Novopavlovka, is barely visible near the top of the image.
Date
Source NASA Earth Observatory
Author ISS Expedition 28 crew
Camera location48° 36′ 00″ N, 82° 00′ 00″ E Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo
This image or video was catalogued by Johnson Space Center of the United States National Aeronautics and Space Administration (NASA) under Photo ID: ISS028-E-44433.

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Image acquired with a Nikon D2Xs digital camera using a 180 mm lens, and is provided by the ISS Crew Earth Observations experiment and Image Science & Analysis Laboratory, Johnson Space Center.

Licensing

Public domain This file is in the public domain in the United States because it was solely created by NASA. NASA copyright policy states that "NASA material is not protected by copyright unless noted". (See Template:PD-USGov, NASA copyright policy page or JPL Image Use Policy.)
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8 September 2011

48°36'0.000"N, 82°0'0.000"E

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c1c84859555ea7e87a72a37c17191a8c56d8cef1

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current10:16, 3 October 2011Thumbnail for version as of 10:16, 3 October 20114,288 × 2,848 (9.87 MB)Originalwana{{Information |Description ={{en|1=Bigach impact crater, Kazakhstan. At approximately five million years old, Bigach is a relatively young geologic feature. However, active tectonic processes in the region have caused movement of parts of the struc
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