its nothing like when the change
None. By definition a rocky planet is mostly rock. Venus, by far, has the densest atmosphere of the terrestrial planets, but the planet itself is mostly rock and is similar in composition to Earth.
Igneous rock is a type of rock that forms from the cooling and solidification of magma or lava. It is classified based on its texture (coarse or fine-grained) and composition (silica content and mineralogy). Examples include granite, basalt, and obsidian.
Yes.
I believe you are looking for the word "metamorphism".
Sand is small particles of rock and minerals or other materials, such as coral or slag, and is not defined by its composition but rather by the size of its particles.
The mineral composition of the oceanic crust is similar to the composition of basalt rock. Basalt is a type of volcanic rock that contains minerals such as feldspar, pyroxene, and olivine, which are also commonly found in the oceanic crust.
The type of weathering that does not alter the chemical composition of the rock is called physical weathering. The acid weathering usually alter the chemical composition of a rock.
the answer is... composition
Igneous rock composition basically means how the rock would look if you were to cut it in half. In the case of igneous rock, you would see the different layers of rocks that have melted with it.
The composition of a rock indicates the minerals present in it, which can provide information about how the rock formed. The texture of a rock, such as its grain size and shape, can indicate the conditions under which the rock was formed, like high pressure or temperature. Both composition and texture can help geologists learn more about the rock's history and the processes that created it.
A rock is a naturally occurring solid aggregate of one or more minerals
Andesitic composition refers to a type of igneous rock that is intermediate in composition between basalt and rhyolite. It typically contains minerals such as plagioclase feldspar, amphibole, and pyroxene. Andesitic rocks are commonly found in volcanic arcs and are associated with convergent plate boundaries.