Heat is more in the equator...
Surfaces with low specific heat capacity, like sand or concrete, will heat up faster. Surfaces with high specific heat capacity, like water or soil, will heat up more slowly but also cool down more slowly.
I assume you mean the heat in Earth's interior. This heat comes from three sources. (1) Heat left over from when the Earth formed. This part should be quite insignificant, since Earth has had enough time to cool down. (2) Decay of radioactive isotopes. (3) The fact that the liquid part of the Earth is gradually solidifying also generates heat.
The part of the Earth that is about 3500 km thick is the mantle. The mantle is located between the Earth's crust and core and is composed of molten rock material that flows slowly over time due to the intense heat and pressure.
Pressure and heat that produce magma are caused in part by the movement of tectonic plates deep within the Earth's mantle. This movement leads to the melting of rock at high temperatures and pressures, resulting in the formation of magma beneath the Earth's surface.
The heat increases to the point that rocks can begin to melt in the lower part of the Earth's mantle, known as the asthenosphere. This is where the temperature and pressure conditions allow for rocks to melt and form magma.
Land heats up faster than water.
During the day, the part of Earth you are on gets heat from the sun faster than it can radiate that heat back into space. At night, Earth is still radiating heat back into space, but where you are is not getting heat from the sun, so the temperature drops.
water!
No. The speed of the moon's orbit does not depend on Earth's spin; it depends on Earth's mass. However, a faster spin on Earth's part would make the moon appear to move across the sky faster, as it would for the sun and stars.
Heat travels from the Sun to the Earth in waves. These waves are part of the solar radiation process.
No.
The Oceans stores the huge amounts of the sun's heat.
The farther from the equator, the weaker the sunlight gets.
The sun's heat warm the Earth's surface. A part of the radiation that falls on the Earth is absorbed by it and a part of it is reflected back into space. A part of the reflected radiation is trapped by the atmosphere. The trapped radiations further warm the Earth. The Sun's heat is allowed to go in but not allowed to go out. The trapped heat warms the Green House. The trapping of the radiations by the Earth's atmosphere is similar. That is why it is called Green House Effect.
Surfaces with low specific heat capacity, like sand or concrete, will heat up faster. Surfaces with high specific heat capacity, like water or soil, will heat up more slowly but also cool down more slowly.
It has a silver solution on the bottom of it and it helps draw the heat into the metal part of the heatsink and then spreads out between the thinner parts and then the fan blows on it helping it cool the heat faster.
The farther from the equator, the weaker the sunlight gets.