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Что (кто) такое loop traverse - определение
![A current model of meiotic recombination, initiated by a double-strand break or gap, followed by pairing with an homologous chromosome and strand invasion to initiate the recombinational repair process. Repair of the gap can lead to crossover (CO) or non-crossover (NCO) of the flanking regions. CO recombination is thought to occur by the Double [[Holliday Junction]] (DHJ) model, illustrated on the right, above. NCO recombinants are thought to occur primarily by the Synthesis Dependent Strand Annealing (SDSA) model, illustrated on the left, above. Most recombination events appear to be the SDSA type.](https://commons.wikimedia.org/wiki/Special:FilePath/Homologous Recombination.jpg?width=200 "A current model of meiotic recombination, initiated by a double-strand break or gap, followed by pairing with an homologous chromosome and strand invasion to initiate the recombinational repair process. Repair of the gap can lead to crossover (CO) or non-crossover (NCO) of the flanking regions. CO recombination is thought to occur by the Double [[Holliday Junction]] (DHJ) model, illustrated on the right, above. NCO recombinants are thought to occur primarily by the Synthesis Dependent Strand Annealing (SDSA) model, illustrated on the left, above. Most recombination events appear to be the SDSA type.")
Википедия
Lake Traverse is the southernmost body of water in the Hudson Bay watershed of North America. It lies along the border between the U.S. states of Minnesota and South Dakota. A low continental divide, part of the Laurentian Divide, separates the land at the southern shore of Lake Traverse from Big Stone Lake, the headwaters of the south-flowing Little Minnesota River, which is part of the Mississippi River System. Both lakes lie within a mile of the town of Browns Valley, Minnesota with Wheaton, Minnesota (at the north end of Lake Traverse); and Ortonville, Minnesota (at the south end of Big Stone Lake).
Lake Traverse is an Anglicization of Lac Traverse, a French name meaning "across the lake".
Prehistorically, the south end of Lake Traverse was the southern outlet of glacial Lake Agassiz across the Traverse Gap into Glacial River Warren; that river carved the valley now occupied by the present-day Minnesota River.
Lake Traverse is drained at its north end by the northward-flowing Bois de Sioux River, a tributary of the Red River of the North. A U.S. Army Corps of Engineers dam at the outflow regulates the lake's level. The Mustinka River flows into the lake just above the dam.
