How can movements in the lithosphere affect climate?
Shifting of climatic zones
The surface of the Earth is divided in a series of plates that are continuously moving relatively to each other.
The resulting of such movements is that a given specific plate will "migrate" along the surface of the planet likely changing its latitude and longitude. As example areas that are now close to the equator can move towards the poles through the geological time (we are talking of several million of years) thus changing their climatic zone.
England during the Carboniferous period (about 350 Ma) was close to the equator with a warm tropical climate that allowed for the growing of rain forest which vegetation (once buried and fossilized) originated the large deposits of coal called "Coal Measures" that were the main source of energy for the Industrial Revolution.
Moreover the movement of the plates can lead to the formation of mountain ridges and/or the opening of new oceans. Both have great impact on the climate at regional and global scale.
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Lithospheric movements, like plate tectonics, can also affect the climate through influencing ocean currents, which can affect temperature distribution and weather patterns. Volcanic activity related to lithospheric movements can also affect climate conditions by releasing gases and particles into the atmosphere.
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When evaluating a one-sided limit, you need to be careful when a quantity is approaching zero since its sign is different depending on which way it is approaching zero from. Let us look at some examples.
When evaluating a one-sided limit, you need to be careful when a quantity is approaching zero since its sign is different depending on which way it is approaching zero from. Let us look at some examples.
When evaluating a one-sided limit, you need to be careful when a quantity is approaching zero since its sign is different depending on which way it is approaching zero from. Let us look at some examples.
When evaluating a one-sided limit, you need to be careful when a quantity is approaching zero since its sign is different depending on which way it is approaching zero from. Let us look at some examples.

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