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A map showing the glaciation of Japan about 20,000 years ago

Glaciation is the forming of ice (glaciers) on land.[1] It is related to the Milankovich theory.[2]

Causes of glaciation[change | change source]

  • 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 axial tilt[3]

References[change | change source]

  1. 1.0 1.1 1.2 "Archived copy". Archived from the original on 2010-08-21. Retrieved 2010-08-11.{{cite web}}: CS1 maint: archived copy as title (link)
  3. 3.0 3.1