The uplifted area is called a dome. This area is the support to the uplifted area.
The Earth's iron core doesn't melt despite its extremely high temperature and pressure because the pressure from the weight of all the material above it raises its melting temperature significantly. This results in the iron core remaining solid even at temperatures well above its melting point.
mantle
Approximately 29% of Earth's surface is above sea level.
Heat from inside the Earth is called geothermal (Earth-heart). The heat is produced by the radioactive decay of elements such as uranium and thorium in the core and mantle. This raises the core's temperature to over 5000 oC.
Scientists who study Earth's structure are called geologists or seismologists. Geologists focus on the composition and processes of the Earth's crust, while seismologists study how seismic waves propagate through the Earth to understand its internal structure.
The inner core is under enormous pressure, which raises the temperature needed to melt it above its actual temperature.
the heat in the core raises and heat raises to a cold spot. so the convection currents raises to the surface of the earth.
The Earth's iron core doesn't melt despite its extremely high temperature and pressure because the pressure from the weight of all the material above it raises its melting temperature significantly. This results in the iron core remaining solid even at temperatures well above its melting point.
its above the earth. it is one of the layers of the atmosphere.
The sky above the Earth extends into space, which is about 62 miles (100 kilometers) above the Earth's surface.
A vixen raises its young foxes in an earth.
Global warming will not threaten the structure of the earth. It will raise sea levels, and it will change croplands into deserts, and vice versa, but the earth's structure will not change.
The Earth's crust lies above the mantle.
Astronomy This is the study of the earth and physical structure and history
The Earth is an oblate spheroid.
The structure of the earth can be described by either the rheological or chemical properties. The structure of the earth is composed of the atmosphere, crust, continent, ocean, hydrosphere, ice cap, mantle, and the asthenosphere.
Geology