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Magma is formed by the heating and cooling of the Earth's crust. Sediment is formed by the soil that is moved downstream from the source of a river to the mouth of the river and the resulting delta.
These pipelike structures within a volcano are called magma conduits. They are formed when molten magma rises from a magma chamber towards the surface. Conduits can vary in size and shape, and they play a crucial role in allowing the movement of magma, gases, and volcanic materials during an eruption.
Plutons
They are not alike: magma is the semi-molton rock layer that forms the mantle. Examples of sediment are the silt (mud) that has dropped out of water to settle on the bottom of rivers or sea; and layers of slate (compressed silt), limestone (the remains of microscopic shelled creatures) and sandstone (compressed sand grains).
they are called lava tubes
Magma emplacements or Batholith are not sedimentary structures.
no
Magma is formed by the heating and cooling of the Earth's crust. Sediment is formed by the soil that is moved downstream from the source of a river to the mouth of the river and the resulting delta.
They're called phenocrysts, allowed to slowly cool in magma before eruption of the magma.
Neither. Natural gas is not a product of magma. It is a product of organic material trapped in sediment as it turns into rock.
compacting and cementaing heat and pressure melting
These pipelike structures within a volcano are called magma conduits. They are formed when molten magma rises from a magma chamber towards the surface. Conduits can vary in size and shape, and they play a crucial role in allowing the movement of magma, gases, and volcanic materials during an eruption.
Plutons
It will be in a volcanic or sediment rock.
They are not alike: magma is the semi-molton rock layer that forms the mantle. Examples of sediment are the silt (mud) that has dropped out of water to settle on the bottom of rivers or sea; and layers of slate (compressed silt), limestone (the remains of microscopic shelled creatures) and sandstone (compressed sand grains).
A dike is an intrusive body of volcanic magma that pushes it's way between layers of rocks and sediment.
igneous, magmatic