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The biome that has permanently frozen ground is the tundra. This frozen ground is known as permafrost and can be found in regions with cold climates, such as the Arctic and high mountain areas. The permafrost layer can vary in depth but remains frozen year-round, influencing the vegetation and wildlife that can survive in these regions.
The biome that includes a layer of soil that is permanently frozen is the tundra biome. This frozen layer of soil is known as permafrost, and it remains frozen year-round, limiting the depth to which plant roots can grow.
The biome with frozen soil is known as a tundra. The permanently frozen layer of soil is called permafrost and it can be found in Arctic and Antarctic tundra regions. The cold temperatures and short growing season in tundras make it difficult for plants to grow, resulting in a unique ecosystem adapted to these harsh conditions.
Permafrost is characteristic of the tundra biome. It is a layer of permanently frozen ground found in high-latitude regions where the ground temperature remains below freezing for two or more years.
The biome that has permanently frozen soil is the tundra, not the desert. The tundra is characterized by cold temperatures and a layer of permafrost beneath the surface that remains frozen year-round, limiting plant growth.
The terrestrial biome characterized by permafrost is the tundra biome. Permafrost is a layer of permanently frozen soil that is found in the arctic and alpine tundra regions, limiting plant growth and affecting ecosystem dynamics in these cold environments.