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Glaciation had a significant impact on the Earth's landscape by shaping valleys, creating moraines, and depositing sediments as the glaciers advanced and retreated. It also played a role in influencing global climate patterns and sea levels through changes in albedo and the release of freshwater into the oceans.
That would be under: National Basketball Glaciation.
The Earth was in an interglacial period of warming called the Sangamon Interglacial at this time period. The Illinois glaciation preceded it, and the Wisconsin episode of glaciation followed it. We are currently in an interglacial period known as the Holocene.
Glaciation may form anywhere on Earth. However, it is most common in higher latitudes and on land where ice is more readily formed. Alpine glaciers occur at high altitudes (e.g. mountain peaks) and are common at all latitudes.
Changes in Earth's orbit and axial tilt, known as Milankovitch cycles, are responsible for triggering the repeating 100,000-year cycles of ice ages. These variations affect the amount of solar radiation reaching Earth's surface, leading to periods of glaciation and interglacial periods.
The Varangian Glaciation occurred during the Neoproterozoic Era. It is significant because there are deposits found on almost every continent, and deposits are found interbedded with marine limestones. This indicates a mass glaciation which affected even low altitudes. Glaciation was caused by the distribution of the continents. All the continents were situated at low latitudes with open oceans at the poles, a configuration that has never happened since.
biomass can affect the earth
During the Ice Ages, glaciers covered much of the Earth's surface, including parts of the supercontinent Pangaea. The weight of these glaciers contributed to the breakup of Pangaea by altering the Earth's crust and causing sea levels to rise and fall. Glaciation also influenced the climate and environment of Pangaea, affecting the distribution of plant and animal species.
Glaciation
Periods of glaciation cause sea levels to drop, because that water gets locked up in ice on land.
The Pleistocene glaciation refers to a series of ice ages that occurred during the Pleistocene epoch, lasting from about 2.6 million to 11,700 years ago. It was characterized by multiple advances and retreats of ice sheets covering large parts of the Earth's surface, leading to the formation of glaciers, ice caps, and extensive ice sheets. The glaciation had a significant impact on global climate, topography, and biodiversity.