1 because the crust is not that big
the temperture of earths crust is -70 to +750
The temperature of Earth's crust can range from -70 degrees Fahrenheit to +750 degrees Fahrenheit depending on location and depth. Higher temperatures would be recorded in regions of crustal melting from magmatic intrusions. Technically, regions heated by magmatic intrusions are still crustal rock, and could reach well over 1,000 degrees Fahrenheit
213.8 Fahrenheit
96.8 degrees Fahrenheit.
The crust has about 13 major plates.
1,600 degrees Fahrenheit...
the temperture of earths crust is -70 to +750
from -220 to 68 Fahrenheit
The sun does not have an outer crust as it is not solid. The "surface" of the sun, called the photosphere, is about 10,000 degrees Fahrenheit.
The temperature of Earth's crust can range from -70 degrees Fahrenheit to +750 degrees Fahrenheit depending on location and depth. Higher temperatures would be recorded in regions of crustal melting from magmatic intrusions. Technically, regions heated by magmatic intrusions are still crustal rock, and could reach well over 1,000 degrees Fahrenheit
Pizza. It makes the crust very crisp.
There are about 92 elements in the crust.
The crust is the cool part of the Earth. It is the surface we live on. It should be at a comfortable temperature until it reaches down to the mantle, the next layer. That area will be hotter. Then at the center, is the core. That is the hot part of the Earth's interior. It is about 3500° C. Estimates vary from 2000 to 7000, but it is HOT!About 447 in Fahrenheit
All life in the universe that we know of, occurs there.The crust is the coldest layer of all the layers of Earth.The crust makes up less than 1% of the Earth's mass.On average, it's about 27 miles thick, but can range from 2-70 miles.The crust is composed of solid, brittle, igneous, metamorphic, and sedimentary rock.The main mineral group making up the rock of the crust are silicates, which include feldspars, micas, and quartz.The crust is the outermost chemical layer of the Earth, composed of two types: oceanic crust and continental crust.Oceanic crust has a density of 3 grams per cubic centimeter; continental crust averages 2.7 grams per cubic centimeter. The difference lies in the rock which composes each type of crust. Oceanic crust is mainly basalt and continental crust is more like granite. Basalt is more dense (heavier) than granite.The majority of the crust is oceanic crust, basaltic in nature.The crust is attached to the uppermost rigid mantle, which together is referred to as the lithosphere.The temperature of Earth's crust can range from -70 degrees Fahrenheit to +750 degrees Fahrenheit depending on location and depth. Higher temperatures would be recorded in regions of crustal melting from magmatic intrusions. Technically, regions heated by magmatic intrusions are still crustal rock, and could reach well over 1,000 degrees Fahrenheit.1. The earth outermost surface is called crust.2.The crust is about 25m. thick beneath the continents.3.The crust is relatively light and brittle.4.Most earthquakes occur within in the crust.Crust is the uppermost layer of earth. the crust is solid rock and mainly consists of ferromagnesium silicates.In the ocean, earths crust is 5-10 miles deep and on land its 5-25 miles before you reach the earths mantle.Thinnest layer.1600 degrees Fahrenheit.1. the most important thing is the volcano2. the second thing is how the crust was created3.where does the crust come from underground or on top of ground.4.when volcanoes erupt when the crust goes in the air with everything else.
The crust is the top layer of the earth. Here are some sentences.Earth's crust can be many miles thick.Below Earth's crust is the mantle.Earth's crust is broken into many plates, which shift about on the liquid interior.We live atop Earth's crust.
213.8 Fahrenheit
96.8 degrees Fahrenheit.