Sedimentary.
The dominant type of rock in Arctic lowlands is generally sedimentary rock, such as sandstone, siltstone, and shale. These rocks are often deposited by glaciers and rivers and can be found in the flat and low-lying areas of the Arctic region.
The soil in the Interior Plains of North America is typically fertile and a mix of prairie soils and chernozem soils. Prairie soils are rich in organic matter and nutrients, while chernozem soils are dark, fertile soils found in grassland regions.
The southern area of the interior plains is characterized by a mix of grasslands, agricultural fields, and forests. This region may also include wetlands and rivers, depending on the specific location. The land cover can vary depending on factors such as climate, soil type, and human activity.
The middle west region of the United States is mostly covered by flat to gently rolling plains known as the Central Lowland. This area includes the Great Plains and the Interior Low Plateaus, which are characterized by fertile soil, grasslands, and some areas with rolling hills.
The main type of rock in the St. Lawrence Lowlands is sedimentary rock, which was formed from the accumulation and compaction of sediments over time. This region is characterized by flat, fertile plains and river valleys, making it ideal for agriculture and urban development.
bed rock
sedimentary
The dominant rock type in ocean crust is basalt, which forms from solidified lava. In continental crust, the dominant rock type is granite, which forms from the cooling and solidification of magma beneath the Earth's surface.
the pacific ocean
Igneous
Sedimentary.
sedimentary
The dominant type of rock in Arctic lowlands is generally sedimentary rock, such as sandstone, siltstone, and shale. These rocks are often deposited by glaciers and rivers and can be found in the flat and low-lying areas of the Arctic region.
Hot rock and liquid and solid metal.
what is the most dominant vegetation belt in India
The soil in the Interior Plains of North America is typically fertile and a mix of prairie soils and chernozem soils. Prairie soils are rich in organic matter and nutrients, while chernozem soils are dark, fertile soils found in grassland regions.
Contact metamorphism is the type of rock metamorphism where heat is the dominant factor. This occurs when rocks come into contact with a heat source, such as magma, causing them to recrystallize and change without melting.