The 3 latitude zones: High latitude zone-poop The high latitude zone is cold. Middle latitude zone- The middles latitude zone is hot and cold. Low latitude zone- The low latitude zone is hot.
Crust,Mantle,Core are the three main parts of the Earth.
The three main groups in science are chemistry,biology and physics.
what are the three main weave types?the three main types of weaving are the plain weave, twill weave, and probaly the rib or basket weave.
granite makes up the world's continental crust. there are other types of rocks but granite is the main one.
The Earth has 5 layers start from the deepest: Inner core, outer core, inner mantle, outer mantle, crust.
I'm unable to display images. However, the three main climate zones on Earth are the tropical zone near the equator, the temperate zones in the middle latitudes, and the polar zones near the north and south poles. These zones are determined by the angle of incoming sunlight and the Earth's spherical shape.
The Equator divides the earth into northern and southern latitudes.
The three main layers that make up Earth is:CORE, MANTLE, and the CRUST
the core, the mantle and the crust
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The three main climate zones on Earth are the Polar, Temperate, and Tropical
No. Prevailing winds are global wind patterns that dictate the general movement of weather in different latitudes. There are three main belts of prevailing winds on earth: the Trade Winds in the tropics, the Prevailing Westerlies in the middle latitudes, and the Polar Easterlies. A tornado is a small scale, violent, rotating windstorm that occurs during some thunderstorms.
Both latitudes of 90 degrees mark the north and south poles.
The three main layers that make up Earth is:CORE, MANTLE, and the CRUST
Latitudes closer to the equator receive more direct sunlight throughout the year, leading to higher temperatures. This is due to the Earth's curvature and the angle at which sunlight strikes the Earth's surface at different latitudes.
Different latitudes on Earth receive different amounts of solar energy because of the Earth's spherical shape and its tilted axis. The angle at which sunlight strikes the Earth varies, with higher latitudes receiving sunlight at a more oblique angle, spreading the energy over a larger surface area. This results in less solar energy reaching higher latitudes compared to lower latitudes, which receive sunlight more directly.