Not exact matches
Thousands of marks on the Antarctic seafloor, caused by icebergs which broke free from
glaciers more than ten thousand years ago, show
how part of the Antarctic
Ice Sheet retreated rapidly at the end of the last ice age as it balanced precariously on sloping ground and became unstab
Ice Sheet retreated rapidly at the end of the last
ice age as it balanced precariously on sloping ground and became unstab
ice age as it balanced precariously on sloping ground and became unstable.
Ask any schoolkid
how the first people came to the Americas, and you might get some version of the following: They crossed a spit of land connecting Alaska and Siberia and made their way south between melting
glaciers at the end of the last
ice age.
The images from this period are not just a window into where the boundaries of
glaciers were when the photographs were taken, but a measure of
how far they had receded from their maximum expansion at the end of the Little
Ice Age.
How, we ask, can a new
Ice Age possibly be shaping up when everybody knows that existing
glaciers — like those in the Swiss passes and Alaska — are melting?
But neither Science nor the AP mentioned that or explained
how the current migrations differ from what's been happening since the last Pleistocene
glaciers retreated and the Little
Ice Age ended.
Just ask the dinosaurs or remember the
ice age and
how huge
glaciers melting and moving formed our Great Lakes.
Three years ago, University College London professor Chronis Tzedakis had just explained the basic cycles of an
ice age to an undergraduate geology class;
how the Earth goes through periods of glaciation followed by warmer periods when
glaciers melt.