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inlet. It was formerly believed that these two sites were two separate craters and that they formed a twin impact structure from a large-scale meteorite hit in the late
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Ingólfsson, Ó. .; Lokrantz, H. (2003). "Massive ground ice body of glacial origin at
Yugorski Peninsula, arctic Russia".
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outcrops of the Ust-Kara impact structure are only a part of the Kara impact structure. (Hodge 1994 and NASA 1988)
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occupies the peninsula and extends from northwest to southeast.
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In the southeastern end of the
Yugorsky Peninsula lies the
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site lies offshore, 15 km east of the small Kara or
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Badjukov, DD; Raitala J; Ohmann T; Lorenz CA (2002).
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16:Peninsula in Nenets Autonomous Okrug, Russia
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372:Kara and Ust-Kara impact structures:
456:Landforms of Nenets Autonomous Okrug
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31:Location of the Yugorsky Peninsula.
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254:Kara meteorite crater
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339:2002LPI....33.1480B
197:Югорский полуостров
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189:Yugorsky Peninsula
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299:(3): 199.
276:References
266:Cretaceous
344:3 January
103:Geography
333:: 1480.
258:Ust-Kara
221:Kara Sea
166:Kara Sea
114:, Russia
108:Location
335:Bibcode
270:suevite
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128:69°28′N
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Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
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