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Without decay, dead organisms and waste would not break down, leading to a buildup of organic matter. This would disrupt nutrient cycling, hinder plant growth, and eventually affect the balance of ecosystems. Overall, it would result in a less diverse and less sustainable environment.

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1y ago

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What is the source of heat in the Earth's interior?

The main sources of heat in the Earth's interior are residual heat from the planet's formation, radioactive decay of elements like uranium, thorium, and potassium, and heat generated by ongoing processes like mantle convection and core formation. This heat leads to processes like plate tectonics, volcanic activity, and the Earth's magnetic field.


What would the Earth look like without the biosphere and atmosphere?

Without the biosphere, Earth would likely resemble a barren, lifeless planet with no greenery, animals, or bacteria. Without the atmosphere, Earth would be exposed to harmful solar radiation and extreme temperature fluctuations, making it uninhabitable for most life forms.


What the earth looks like without weathering and erosion?

Without weathering and erosion, the Earth's surface would lack distinct features such as mountains, valleys, and coastlines. The land would essentially be smooth and flat, with fewer variations in elevation. Weathering and erosion are essential processes that shape the Earth's landscape over millions of years.


Would Earth's surface be different without weathering and erosion?

Yes, without weathering and erosion, Earth's surface would look significantly different. These processes help shape our landscapes by breaking down rocks and transporting sediments, creating features like mountains, valleys, and coastlines. Without them, much of Earth's surface would remain unchanged over time.


What internal process is still producing heat within earth's core?

The heat within Earth's core is primarily produced by the radioactive decay of elements like uranium, thorium, and potassium. This process releases energy and generates heat as these elements decay over time. This heat, combined with the residual heat from Earth's formation, contributes to the high temperatures in the core.