Bering Land Bridge National Preserve in the context of "Bering Land Bridge"

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⭐ Core Definition: Bering Land Bridge National Preserve

The Bering Land Bridge National Preserve is one of the most remote protected areas of the United States, located on the Seward Peninsula. The National Preserve protects a remnant of the Bering Land Bridge that connected Asia with North America more than 13,000 years ago during the Pleistocene ice age. The majority of this land bridge now lies beneath the waters of the Chukchi and Bering Seas. During the glacial epoch this bridge was a migration route for people, animals, and plants whenever ocean levels fell enough to expose the land bridge. Archeologists debate whether it was across this Bering Land Bridge, also called Beringia, that humans first migrated from Asia to populate the Americas, or whether it was via a coastal route.

Bering Land Bridge National Monument was established in 1978 by Presidential proclamation under the authority of the Antiquities Act. The designation was modified in 1980 to a national preserve with the passage of the Alaska National Interest Lands Conservation Act (ANILCA), which would allow both subsistence hunting by local residents and sport hunting. The preserve includes significant archaeological sites and a variety of geological features. The preserve has seen recent volcanic activity, with lava flows and lake-filled maars. Hot springs are a popular destination for tourists.

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Bering Land Bridge National Preserve in the context of Seward Peninsula

The Seward Peninsula is a large peninsula on the western coast of the U.S. state of Alaska whose westernmost point is Cape Prince of Wales. The peninsula projects about 200 mi (320 km) into the Bering Sea between Norton Sound, the Bering Strait, the Chukchi Sea, and Kotzebue Sound, just below the Arctic Circle. The entire peninsula is about 210 mi (330 km) long and 90–140 mi (145–225 km) wide. Like Seward, Alaska, it was named after William H. Seward, the United States Secretary of State who fought for the U.S. purchase of Alaska.

The Seward Peninsula is a remnant of the Bering land bridge, a roughly thousand-mile-wide swath of land connecting Siberia with mainland Alaska during the Pleistocene Ice Age. This land bridge aided in the migration of humans, as well as plant and animal species, from Asia to North America. Excavations at sites such as the Trail Creek Caves and Cape Espenberg in the Bering Land Bridge National Preserve as well as Cape Denbigh to the south have provided insight into the timeline of prehistorical migrations from Asia to the Seward Peninsula.

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Bering Land Bridge National Preserve in the context of Trail Creek Caves

The Trail Creek Caves are a group of twelve caves found within the Bering Land Bridge National Preserve on the Seward Peninsula of the U.S. state of Alaska. This is a significant archeological site due to the discovery of several artifacts of ancient hunters. These included stone tools and bone fragments dated to 8,500 years or earlier. The caves were discovered in 1928 by Taylor Moto and Alfred Karmun, locals from Deering, Alaska. Geologist David Hopkins tested the site in 1948. This location was first excavated in from 1949-1950 by Danish archeologist Helge Larsen. The caves are located along Trail Creek 65°47′28″N 163°24′58″W / 65.79111°N 163.41611°W / 65.79111; -163.41611 near its mouth at Cottonwood Creek in the Northwest Arctic Borough.

In 2018, researchers sequenced the genome to around .4 coverage from a tooth excavated from Trail Creek Cave 2 in 1949. The tooth, directly dated to around 9000 BP, belonged to a young child. The young child from Trail Creek Cave 2 was found to cluster genetically with USR1 from the Upward Sun River site in an ancient DNA population grouping referred to as Ancient Beringian. As with USR2 from the Upward Sun River site, the child from Trail Creek Cave 2 was also found to carry a basal lineage of Haplogroup B2; this specific mtDNA lineage is different from the derived B2 lineage generally found in the Americas.

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