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shtirl [24]
3 years ago
11

In the convection currents, where is there hifhhigh density

Geography
1 answer:
zhenek [66]3 years ago
7 0
The current<span> begins when the air over the hot sand is heated and begins to rise because of its lowered </span>density<span>.  That is a sea breeze.</span>
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Sorry

Explanation:

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2. How does your model demonstrate the differences between the types of tectonic plates and the resulting observations in the as
jonny [76]

The model demonstrates the differences between the types of tectonic plates and the resulting observations in the asthenosphere there are two foremost sorts of tectonic plates: Oceanic and Continental. Continental crust is often fashioned of granite and is typically referred to as sial because of a large amount of silica and aluminum gift. Continental crust is much less dense than the basaltic oceanic crust, sima, which is constructed from silica and magnesium. Due to the fact it's far denser, oceanic crust plunges beneath the continental crust. The department between the 2 layers is known as the Conrad Discontinuity.

Asthenosphere, a sector of Earth's mantle mendacity beneath the lithosphere and believed to be a whole lot hotter and more fluid than the lithosphere. The asthenosphere extends from about 100 km (60 miles) to about 700 km (450 miles) underneath Earth's floor. Cross-section of a tectonic plate.

It's miles a layer of stable rock where the intense pressure and warmth cause the rocks to flow like a liquid. The rocks in the asthenosphere are not as dense because of the rocks in the lithosphere. This allows the tectonic plates within the lithosphere to move around on the planet's floor.

The asthenosphere is the robotically weak and ductile vicinity of the upper mantle of Earth. It lies underneath the lithosphere, between approximately 80 and two hundred km below the surface, and extends as deep as seven-hundred km. But, the decreased boundary of the asthenosphere isn't always well described.

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7 0
2 years ago
How does the atmosphere transfer heat from Areas which experience a net radiation surplus to areas which experience net radiatio
Brums [2.3K]
Solar radiation is highly absorbed on land where the latitudes receive direct sunlight. Then scatters to the polar regions.  The heat gathered between land and the reflection of heat from land to the atmosphere creates the net radiation surplus.

When solar radiation stretches to the polar regions it slowly loses heat and it becomes lesser than the heat reflected back to the atmosphere. This creates the net radiation loss.   
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4 years ago
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Option: clearing the land to raise crops.

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4 years ago
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