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The oceanic crust is made up of basalt while continental crust is made up of mostly granite.
crust
Earth's crust is mostly made up of Silicon and Oxygen
The oceanic crust is mostly made up of basalt, which is a dense volcanic rock that forms from the cooling of lava at the Earth's surface.
Well, darling, the layer you're talking about is the Earth's crust. And yes, it's mostly made up of granite and various rocks. So, there you have it, the crust is the rocky outer layer of our lovely planet.
Yes, the Earth's crust is primarily composed of silicate minerals, which make up the majority of the planet's surface. Silicates are minerals containing silicon and oxygen, forming the most abundant group of minerals in the Earth's crust.
Our earth is mostly made up of silicon oxide (sand) and magnesium oxide, extending from the outer core to the crust. The inner core is mostly iron, enriched to 4% nickel. About 70% of the surface is covered with water.
If you mean "What is the Moon made of ?" It is made of its core witch is mostly rock and iron.The crust is made of more rock and dust.
The layer of the Earth mostly made out of granite and similar rocks is the continental crust. This outermost layer varies in thickness and is primarily composed of lighter, less dense materials compared to the underlying mantle. The continental crust contrasts with the oceanic crust, which is primarily made up of basalt.
The Earth is composed of several layers: the crust, mantle, and core. The crust is the outermost layer and is made up of solid rock. Beneath the crust is the mantle, which is mostly solid but can flow slowly over long periods of time. At the center of the Earth is the core, which is composed mostly of iron and nickel.
The continental crust is made up of igneous, sedimentary, and metamorphic rocks. These rocks form the continents and the continental shelves, areas of seabed close to the shore.
The top layer of the Earth's crust is made up of solid rock called the lithosphere. It includes both continental crust, which is thicker and less dense, and oceanic crust, which is thinner and more dense.