Earth's layers—crust, mantle, outer core, and inner core—interact dynamically, with each layer exhibiting distinct properties and behaviors. The crust is the thin, solid outer shell, while the mantle beneath it is semi-solid and convective, driving tectonic activity. The outer core is liquid and generates Earth's magnetic field, and the inner core is solid and extremely hot, with immense pressure. Together, these layers contribute to geological processes like plate tectonics, volcanism, and seismic activity.
The term used in geology to describe the relationship between adjacent layers of sedimentary rock is called stratification. Stratification refers to the layering of sedimentary rocks based on the different characteristics of the sediments deposited over time.
the crust
Crust
Lithosphere
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The term used in geology to describe the relationship between adjacent layers of sedimentary rock is called stratification. Stratification refers to the layering of sedimentary rocks based on the different characteristics of the sediments deposited over time.
was up
Your mom made the earths layers
Transistion zones.
The Inner Core is a liquid. Outer core: solid mantel: inbetween crust: solid
the difference is that the earth's theory is similar to that of a hypotheses , structure and compositional layer of the earth.
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The earths mantle is one of the four major layers, laying between the crust and the outer core. At 2885 kilometers, it is the thickest layer.
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the crust
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the crust