The Earth's inner core reaches temperatures that are at times greater than 9000°F. What causes this layer to remain solid despite the high temperature?
Temperatures decrease with altitude in the troposphere, the lowest layer of the atmosphere, from an average of about 20° C to below -50° C. In the next layer, the stratosphere, temperatures warm only slightly up to the ozone layer at the top of the stratosphere, where they increase rapidly with altitude until becoming about the same as on the earth's surface. Temperatures in the next layer, the mesosphere, cool rapidly with altitude to below -80° C. Temperatures rise rapidly with increases in altitude in the next layer, the thermosphere, but temperatures there can vary widely. Depending on the activity of ionized particles within this region, they reach a high of over 1,200° C in the daytime and become extremely cold at night. The next layer is the exosphere, which cools with altitude to where it ends about 1,000 km above the earth's surface.
melted rocks are formed when there are high temperatures inside earth.
The particles in plasma shake violently at very high temperatures and are electrically charged.
which environment would mineral formation caused by high pressures and high temperatures most likely occur
The Thermosphere
the thermosphere
Thermosphere
it is simply pie. the answer is pe
The ozone layer has nothing to do with the heat waves.The ozone layer only blocks the high energy ultraviolet radiations but allows the heat waves to paas through it without any deflection or absorption.
achieving high temperatures and containing the plasma reactants
The asthenosphere, part of the upper mantle.
Lennart Mannik has written: 'Pressure induced absorption in carbon dioxide at high temperatures' -- subject(s): Absorption and adsorption, Carbon dioxide, Accommodation coefficient, Physics Theses, Gases
The Earth's inner core reaches temperatures that are at times greater than 9000°F. What causes this layer to remain solid despite the high temperature?
The outer layer of the sun is the Corona. No reactions really take place there, and it is vastly less dense than the rest of the sun. It can reach extremely high temperatures despite that because there is a lot of room for the particles to move around, however the temperatures do not reach that of the inner layers.
th normal summer high temperatures are 105.
When temperatures are high it causes the environment to heat up.