The interior core contains many nuclear properties which gives of huge amounts of heat which then heats the core.
The melting temperature of materials is dependent on the pressure that is applied, whereby the higher the pressure, the higher the melting temperature. As such the rocks in the mantle are experiencing such a high pressure, that their melting point is driven up beyond the temperature within the Earth's mantle so they remain solid.
No one can really explore the earths interior. Scientist obtain information about the characteristics of the earth's interior by studying earthquake records. Earthquake waves help scientists figure out the distances to each of the section of the earth's interior. The Earth can be divided into three large sections: the mantle, inner core, and outer core. The inner core is at the center of the earth. The pressure and temperature of the earth increases as one moves closer to the center. First comes the mantle, this is a layer that is bellow the crust of the earth. This is said to go down 2,900 kilometers; it's temperature is about 870 degrees Celsius. The outer core has a very high temperature and ranges from about 4,400 degrees Celsius to about 6,100 degrees Celsius. The outer core beginnings where the mantle stops and it extends further down to the center 2,250 kilometers. The inner core is about 6,400 kilometers below the earths surface. the temperature at the inner core of the earth is at the high is about 7,000 degrees Celsius.So, the temperatures at the center of the earth are actually much hotter than 900 degrees Fahrenheit.what no u loser comon it 899 F
The temperature in the Thermosphere can rise to 2,000° C.
Venus is much hotter than Earth due to the greenhouse effect. Temperatures on Venus can get as high as 860 degrees Fahrenheit.
Earth interior is very hot due to high pressure and from radioactive decay.
The interior core contains many nuclear properties which gives of huge amounts of heat which then heats the core.
This is in Antarctica, no doubt. The coldest temperature was recorded at Vostok research station in the interior of the continent. But it is likely that the coldes location is in a place called Dome C, also in interior Antarctica at high elevations, but observations are obviously sparse here. It is believed that we will see a new record here soon now that there are a few stations up.
The interior core contains many nuclear properties which gives of huge amounts of heat which then heats the core.
The melting temperature of materials is dependent on the pressure that is applied, whereby the higher the pressure, the higher the melting temperature. As such the rocks in the mantle are experiencing such a high pressure, that their melting point is driven up beyond the temperature within the Earth's mantle so they remain solid.
Simply because there is no way to analyse or study it directly. Much of what we know about the Earth's core has to be 'guess work' - as the temperature and pressure is far too high for today's technology to provide definitive answers.
The high temperature and pressure in the Sun's interior causes nuclear fusion.
The inner planet Mercury and Venus has very high temperature and the Earth and Mars has moderate temperature. However, the Earth has nice temperature.
Ultramafic rocks have a very high melting temperature. Earth's interior is no longer hot enough to produce eruptions of molten ultramafic material.
Compared to Earth's, it has:* A high pressure * An extremely high temperature
No one can really explore the earths interior. Scientist obtain information about the characteristics of the earth's interior by studying earthquake records. Earthquake waves help scientists figure out the distances to each of the section of the earth's interior. The Earth can be divided into three large sections: the mantle, inner core, and outer core. The inner core is at the center of the earth. The pressure and temperature of the earth increases as one moves closer to the center. First comes the mantle, this is a layer that is bellow the crust of the earth. This is said to go down 2,900 kilometers; it's temperature is about 870 degrees Celsius. The outer core has a very high temperature and ranges from about 4,400 degrees Celsius to about 6,100 degrees Celsius. The outer core beginnings where the mantle stops and it extends further down to the center 2,250 kilometers. The inner core is about 6,400 kilometers below the earths surface. the temperature at the inner core of the earth is at the high is about 7,000 degrees Celsius.So, the temperatures at the center of the earth are actually much hotter than 900 degrees Fahrenheit.what no u loser comon it 899 F
Higher than earth
Because of the core