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What term is used for the part of the soil that is always frozen in cold climates?

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The term used for the part of the soil that is always frozen in cold climates is permafrost. Permafrost is a layer of soil or sediment that remains frozen for two or more consecutive years, with temperatures usually between -2 to -4 degrees Celsius. It is found in regions with a frozen subsoil layer, such as the Arctic and Antarctica.
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The term used for the part of the soil that is always frozen in cold climates is permafrost. Permafrost is a layer of soil that remains frozen for long periods of time, even in warmer climates. It is found in areas with very cold temperatures and can be up to hundreds of meters deep.
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The term used for the part of the soil that is permanently frozen in cold climates is "permafrost." Permafrost refers to soil, rock, or sediment that remains at or below 0 degrees Celsius (32 degrees Fahrenheit) for at least two consecutive years. It is typically found in regions with cold temperatures, such as Arctic and sub-Arctic areas. Permafrost can extend to considerable depths and has a significant impact on the landscape, ecosystems, and human activities in these regions.
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The term for the part of the soil that is always frozen in cold climates is "permafrost". Permafrost is soil sediment or rock that remains at or below 0°c(32°F) for atleast two consecutive years . It is a characteristic feature of extremely cold regions such as the Arctic and subarctic areas. Permafrost has significant implications for ecosystem, infrastructure,and climate,as it effect the stability of the ground and the release of green house gases.
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