the side of the volcanoes and other pyroclastic ejecta become saturated with water
Explanation:
A pyroclastic flows can generate the lahar when they are extreme ty hot and flows with the rocks bedrock. This debris mixes up with the snow met and ice and gets rapidly traveled upwards.
It travels rapidly down steep slopes and a larger can also be formed when a high volume of long duration of rainfall occurs after the eruption. And the volcanic landslides are mixed with water.
The upliftment weathering hypothesis suggests that the formations of the uplifted terrains the global climate into an icehouse state and the main factor that influences the global state of the chemical weathering are the global rainfall and the high temperatures, like the rocks in the tropical areas, are exposed to the dry and hot weather conditions.
<u>Similar to that of the cold areas the rocks are exposed to the cold and first action and the interaction of the moisture contents that transform the minerals in the rocks. Which are ongoing processes through the impacts of the oxidation and hydrolysis.
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The formation of the acidic contents in the rocks ios created by the impacts of these temperatures on the rocks mass. The carbonization that is an atmospheric process of the addition to carbon contents to the air and impacts the limestone and the chalk rocks.
