It is called the «driftless» area because glaciers drifted around
this area during the glacial period.
This is known as the «driftless» area of Wisconsin, because glaciers drifted around
this area during the glacial period.
Not exact matches
During each
glacial period the tropics became both cooler and drier, turning some
areas of tropical rain forest into dry seasonal forest or savanna.
Most of these
areas had been dry savanna or arid
during the last
glacial period.
If there was actually glaciation
during cold
periods,
glacial dust might well have blown out to sea, fertilizing large
areas and producing a stronger CO2 pump.
Well drained and rocky substrate there creates a glade ecosystem where sloping ground can encourage the growth of prickly pear cacti and other desert and prairie species such as the collared lizard, Crotaphytus that last covered the whole
area around 7,000 years ago in the Hypsithermal Interval,
during the Holocene
Period, when warming dried out much of the
glacial Northern Hemisphere.
Data from modern ice stream beds are difficult to obtain, but where ice advanced onto continental shelves
during glacial periods, extensive
areas of the former bed can be imaged using modern swath sonar tools.