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At the beginning of the period, glaciation was widespread, and latitudinal climatic belts were strongly developed.
For example, during the last ice age, the maximum extent of glaciation was reached about 18,000 years ago.
It is probable that the Saale episode of glaciation was complex: at least three phases are recognized.
At the beginning of the Permian period glaciation was widespread, and latitudinal climatic belts were strongly developed.
In many areas the interval of glaciation was accompanied by the invasion of cool-water brachiopod fauna even into tropical latitudes, suggesting the onset of significant global cooling.
Milankovitch proposed that the mechanism that brought about periods of glaciation was driven by cyclic changes in eccentricity as well as two other orbital parameters: precession (a change in the directional focus of Earth's axis of rotation) and axial tilt (a change in the inclination of Earth's axis with respect to the plane of its orbit around the Sun).
Similar(41)
Glaciation is evident above 7,500 feet.
Signs of alpine glaciation are widely evident.
Glaciation is less extensive in the Alai and Trans-Alai mountains.
Glaciation is evident, and there are extensive alpine landforms.
Accompanying the last two stages of glaciation were extensive deposits of windblown silt, or loess.
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