Search results
Results from the Go Local Guru Content Network
Opening of an ice-free corridor did not occur until after 13,000 to 12,000 BP. [32] [33] [34] The early environment of the ice-free corridor was dominated by glacial outwash and meltwater, with ice-dammed lakes and periodic flooding from the release of ice-dammed meltwater. [32] Biological productivity of the deglaciated landscape increased ...