The crust is the cool part of the Earth. It is the surface we live on. It should be at a comfortable temperature until it reaches down to the mantle, the next layer. That area will be hotter. Then at the center, is the core. That is the hot part of the Earth's interior. It is about 3500° C. Estimates vary from 2000 to 7000, but it is HOT!
Well, the earth's crust is like hot rock, but not melted.
Hot spots in the crust are caused by upwelling of magma from deep within the Earth's mantle, creating localized areas of intense volcanic activity. These hot spots can result in volcanic eruptions and the formation of volcanic islands or seamounts. Examples of hot spots include Hawaii and Yellowstone.
the crust then comes the mantel the inner layer then core
Check your thermometer. That's how hot it is on the outer crust where you are. There exists a geothermal gradient where temperature rises with depth from the surface. See the link below.
Hot spots do not create or destroy oceanic or continental crust. Hot spots are volcanic regions that are stationary relative to moving tectonic plates. As the plates move over the hot spot, they experience volcanic activity, which can result in the formation of volcanic islands or seamounts, but the crust itself is not created or destroyed in the process.
Well, the earth's crust is like hot rock, but not melted.
The lower crust is denser and more mafic in composition compared to the upper crust, which is less dense and more felsic. The lower crust is also usually deeper in the Earth's crust compared to the upper crust.
2,700
2.25
very hot
Hot spots in the crust are caused by upwelling of magma from deep within the Earth's mantle, creating localized areas of intense volcanic activity. These hot spots can result in volcanic eruptions and the formation of volcanic islands or seamounts. Examples of hot spots include Hawaii and Yellowstone.
No, there is a hot spot underyellowstone
No, the inner part of the Earth's crust is not hot melted rock. The inner core of the Earth is made up of solid iron and nickel, while the outer core is composed of liquid iron and nickel. The hot melted rock is found in the mantle layer beneath the crust.
400 degrees
50 to 300 degrees f.
the crust then comes the mantel the inner layer then core
Check your thermometer. That's how hot it is on the outer crust where you are. There exists a geothermal gradient where temperature rises with depth from the surface. See the link below.