No, its around nine thousand degrees Fahrenheit.
12,600 degrees Fahrenheit.9000 thousand degrees Fahrenheit
is the mantle hotter or colder the the inner core
No, the inner core of the Earth is actually estimated to be about 9,000-13,000 degrees Fahrenheit. This extreme heat is due to the immense pressure and radioactive decay that occur within the Earth's core.
No, that is just a little above the surface temp. of Venus; enough to melt lead. Earth's inner and outer core is a searing 10,832 Fahrenheit, give or take about 930 degrees, at a pressure of 3.3 million atmospheres (or 3.3 million times the atmospheric pressure at sea level.
The inner core of the Earth is the hottest part, reaching temperatures of up to 5700 degrees Celsius (10,300 degrees Fahrenheit).
12,600 degrees Fahrenheit.9000 thousand degrees Fahrenheit
False. The inner core of the Earth is actually much hotter, with temperatures estimated to reach around 9,932 degrees Fahrenheit (5,500 degrees Celsius). This extreme heat is primarily due to the pressure and radioactive decay occurring within the Earth's core.
No, the inner core of the Earth is much hotter than nine hundred degrees. The temperature at the inner core can reach up to around 5700 degrees Celsius.
is the mantle hotter or colder the the inner core
No, that is just a little above the surface temp. of Venus; enough to melt lead. Earth's inner and outer core is a searing 10,832 Fahrenheit, give or take about 930 degrees, at a pressure of 3.3 million atmospheres (or 3.3 million times the atmospheric pressure at sea level.
No, the inner core of the Earth is actually estimated to be about 9,000-13,000 degrees Fahrenheit. This extreme heat is due to the immense pressure and radioactive decay that occur within the Earth's core.
It is indeed false. The inner core is closer to ten thousand degrees.
No, that is just a little above the surface temp. of Venus; enough to melt lead. Earth's inner and outer core is a searing 10,832 Fahrenheit, give or take about 930 degrees, at a pressure of 3.3 million atmospheres (or 3.3 million times the atmospheric pressure at sea level.
The inner core of the Earth is the hottest part, reaching temperatures of up to 5700 degrees Celsius (10,300 degrees Fahrenheit).
The temperature of the inner core is estimated to be around 5,700 degrees Celsius (10,300 degrees Fahrenheit). This high temperature is due to the immense pressure from the layers of the Earth above it and the heat generated by radioactive decay.
The inner core's temperature is estimated to be around 5,700 degrees Celsius (10,300 degrees Fahrenheit). This extreme heat is due to the high pressure at the center of the Earth compressing the iron and nickel in the core, causing it to reach such high temperatures.
The inner core of the Earth is the hottest layer, with temperatures reaching up to 11,000 degrees Fahrenheit. The inner core is made of solid iron and nickel, despite the extreme temperatures, due to the immense pressure at that depth.