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The sunlight enters as UV radiation, it is absorbed by the lithosphere and so drops in energy, therefore it is re-radiated out as the longer-waved infrared radiation.

The amount any area absorbs is dependant on the albedo effect, dark areas absorb a lot, while high albedo areas (such as snowy/ icy areas) reflect most of it back away from the Earth as UV.

Uv can also be reflected back before reaching the lithosphere by clouds and airborne particles such as sulphur dioxide (hence the drop in global temperatures seen after major volcanic eruptions).

Infrared radiation from the lithosphere can leave the Earth or be captured, absorbed then re-radiated back down to the ground by clouds (which is why it's always warmer in the morning after a cloudy night).

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Radiation in the lithosphere primarily comes from the decay of radioactive elements in rocks and minerals. This radiation can be in the form of alpha, beta, or gamma particles. Over time, this radiation can contribute to the formation of certain minerals and affect the properties of rocks in the lithosphere.

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Q: How does radiation work in the lithosphere?
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How does the lithosphere affect the human life?

The lithosphere provides the solid ground on which humans can build shelters, grow food, and extract resources. It also plays a role in regulating Earth's temperatures and protecting us from harmful solar radiation. However, activities like mining and deforestation can have negative impacts on the lithosphere, leading to soil erosion, land degradation, and natural disasters that can affect human communities.


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What parts of the geosphere are affected by increased radiation?

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