We can find large masses on oceans and seas.
Igneous rocks, such as granite or diorite, are formed when large masses of magma solidify far below Earth's surface. These rocks have a coarse texture due to the slow cooling process, allowing large mineral crystals to form.
Coarse-grained texture
Coarse-grained texture
Coarse-grained texture
Large masses of land are called continents.
Igneous rocks formed from large masses of magma solidifying far below Earth's surface typically have a coarse-grained texture. This is because the slower cooling process allows larger mineral crystals to form within the rock.
The process of breaking down large masses of rock into smaller pieces is called weathering. This can occur through physical, chemical, or biological processes. Physical weathering involves the mechanical breakdown of rocks, while chemical weathering alters the minerals within the rocks. Together, these processes contribute to the formation of soil and sediment.
A glacier. Glaciers are large masses of ice that slowly move downhill, eroding the land and carrying debris like rocks with them.
Metamorphic rocks are buried deep inside Earth. There is enough heat and pressure to change the rocks, but not enough to melt it into magma. Metamorphic rocks can form adjacent to layers of magma, because of the generated heat, however
The thick parts of the Earth's crust that form large land masses are called continents. Continents are made up of a variety of rocks and have different geological features such as mountains, plains, and plateaus. There are currently seven continents on Earth.
Coalesced magma bodies are referred to as plutonic rocks, they have a porphyritic texture or larger crystals since elements are allotted more time to segregate to their desired energy environments and precipitate minerals.
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