Glaciation
From Wikipedia, the free encyclopedia
Glaciation is the forming of ice (glaciers) on land.[1] It is releated to the Milankovitch theory.[2]
Causes of glaciation [change]
- A temperature decrease about 4-5o C around the world[1]
- Higher amounts of snow near the Arctic[1]
- The difference of the Earth's orbit from a perfect circle[3]
- Changes in Earth's tilt[3]