Abstract:Lakes region formed as sea caves during higher lake level stages and became increasingly terrestrial as lake levels receded, resulting in an abundance of rockshelters and other shoreline features that are now inland from the current shoreline. Recorded rockshelters in the region have contained human burials, copper caches, rock art, and varying amounts of lithics, ceramics, and fire-cracked rock. Additionally, a considerable amount of regional ethnohistoric accounts demonstrate the importance of rockshelters, … Show more
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