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The Finger Lakes Region was formed by the melting glaciers of the last glacial period, over ten thousand years ago.
There are over 300 algific talus slopes however some are in poor condition.
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Even with snow nonetheless on the ground, they will journey - generally surprisingly lengthy distances - throughout their range to examine the dens of females to see if they are nonetheless occupied and to locate different males that might be encroaching on their territory.
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