The bedrock of lowlands is typically the result of geological processes such as sediment deposition, erosion, and tectonic movements over millions of years. These processes can include the accumulation of sedimentary rocks, such as sandstone or limestone, or the folding and faulting of existing rock layers. Ultimately, the bedrock of lowlands is shaped by the complex interplay of these geological forces.
The bedrock that underlies the Antarctic continent was formed about 540 million years ago during the formation of the supercontinent Gondwana.
Residual soil is formed from the same material as the bedrock beneath it through weathering processes over time. The characteristics of residual soil often mirror those of the bedrock from which it was derived.
When the soil above it formed from the bedrock below.
Bedrock is formed when molten rock (magma) cools and solidifies beneath the Earth's surface. Over time, this solidified rock gets buried under layers of sediment and undergoes pressure and heat, eventually becoming the solid, durable bedrock that forms the foundation of the Earth's crust.
it is formed by weathering
When the mountains got eroded, sediments broke off, and rolled down the mountain into the lowlands, that were oceans at the time, and the pressure from all the rocks fused them together, making it a sheet of sedimentary rock.
Tug Hill Plateau and St. Lawrence Lowlands
Residual soil is the soil formed from the weathering of the bedrock.
If you are asking for the name of such soils, they are soils formed in residuum, or residual soils. Typically, the soil profile grades into a degraded bedrock called saprolite, with depth, before hiyting hard bedrock.
The bedrock that underlies the Antarctic continent was formed about 540 million years ago during the formation of the supercontinent Gondwana.
Residual soil is formed from the same material as the bedrock beneath it through weathering processes over time. The characteristics of residual soil often mirror those of the bedrock from which it was derived.
The majority of bedrock in the Catskills was formed during the Devonian Period, which is part of the Paleozoic Era. This bedrock consists of sedimentary rocks like sandstones and shales, as well as igneous rocks like granites formed through tectonic and volcanic processes during this time.
When the soil above it formed from the bedrock below.
created with a big bang
Transported soil.
Regolith
Bedrock is formed when molten rock (magma) cools and solidifies beneath the Earth's surface. Over time, this solidified rock gets buried under layers of sediment and undergoes pressure and heat, eventually becoming the solid, durable bedrock that forms the foundation of the Earth's crust.