Maine, Nevada, and North Dakota do not have large populations. What are some reasons for such small populations

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Answer 1

Answer:

Explanation:

I have been to Maine several times. There are two issues about living there.They have hard winters, most of the time. Do not live there if you cannot deal with a long, hard winter. Its good if you can stay inside and write, like Stephen King.

another thing is job diversity because they rely on Lumber, fishing and other natural resources


Related Questions

What are gases that accumulate in the atmosphere and contribute to global warming?

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The gases that accumulate in the atmosphere and contribute to global warming are known as greenhouse gases. They trap heat from the sun and cause the Earth's temperature to increase.

What is global warming?

Global warming refers to the phenomenon of Earth's average surface temperature increasing due to human activities that increase the concentration of greenhouse gases in the atmosphere. Greenhouse gases such as carbon dioxide, methane, and water vapor trap heat in the Earth's atmosphere, causing global temperatures to rise. This is referred to as the greenhouse effect.

What is the greenhouse effect?

The greenhouse effect is a natural process that occurs when certain gases in the Earth's atmosphere, referred to as greenhouse gases, trap heat from the sun, preventing it from escaping into space. As a result, the Earth's temperature is kept within a range that is conducive to life as we know it.

However, human activities such as burning fossil fuels, deforestation, and industrial processes have led to an increase in the concentration of greenhouse gases in the atmosphere, intensifying the greenhouse effect and causing global warming. This is a significant concern, as global warming can have a range of negative impacts on the environment and human societies.

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Question 1 3 pts The style of eruption depends on the plate tectonic setting in which the volcano is situated. Compare the different eruption styles you could observe at a divergent versus a convergent plate boundary. Make sure to address the roles that composition, viscosity, and gas content play in your answer.

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At a divergent plate boundary, the plates are moving away from each other. This type of plate boundary is typically associated with less explosive eruptions.

Eruptions in this type of setting are usually composed of basaltic magma, which is low in silica content and very fluid.

These eruptions produce lava flows and rarely cause ash and pyroclastic flows. Since the viscosity of basaltic magma is low, gas bubbles can escape easily and cause less explosive eruptions.

At a convergent plate boundary, the plates are pushing together. This type of plate boundary is typically associated with explosive eruptions.

Eruptions in this type of setting are usually composed of andesitic or rhyolitic magma, which is high in silica content and more viscous than basaltic magma.

These eruptions produce ash and pyroclastic flows, and can be more explosive due to the higher viscosity of andesitic or rhyolitic magma.

The gas bubbles are more difficult to escape, so pressure builds up and causes more explosive eruptions.

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The Aleutian and Hawaiian Islands form from completely different processes related to Plate Tectonics. Using Plate Tectonic theory and correct technical terms, explain how they form.

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The Aleutian and Hawaiian Islands form from two different processes related to Plate Tectonics. The Aleutian Islands are formed by the subduction of the Pacific plate beneath the North American plate at the Aleutian Trench. This process is also known as a convergent plate boundary.

During subduction, the oceanic lithosphere is consumed and in the process magma is produced and rises to the surface. This magma then cools and hardens to form the Aleutian Islands.

The Hawaiian Islands are formed by a process known as hotspot volcanism. Hotspots are stationary mantle plumes that rise from the mantle and melt the lithosphere.

This process is also known as a divergent plate boundary. The Hawaiian hotspot is located beneath the Pacific plate and has created the Hawaiian Ridge of islands, as the Pacific plate has moved over it.

The molten material erupts to the surface to create new volcanoes and as the older volcanoes move away from the hotspot, they become inactive and form islands.

Both processes create volcanic islands, but the way in which the volcanoes form differs between the Aleutian and Hawaiian Islands. The Aleutian Islands are formed through subduction while the Hawaiian Islands are formed through hotspot volcanism.

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air flowing toward the equator is pushed and air flowing away from the equator is pushed is called

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The phenomenon of air flowing toward the equator being pushed and air flowing away from the equator being pushed is known as the Hadley Cell.

This atmospheric circulation is named after George Hadley, an English lawyer who first proposed the concept in 1735.

The Hadley Cell is a two-celled atmospheric circulation in which air near the equator rises up and is pushed to the tropics, cooling as it moves away from the equator.

At the tropics, the air sinks back down to the surface and is pushed away from the equator, heating up as it moves towards the poles.

This circulation pattern helps to redistribute heat around the Earth and keeps the equator warm while cooling off the poles. This is why temperatures decrease significantly the further away you are from the equator.

The Hadley Cell is an important part of the global climate system, and without it, the planet would be significantly colder overall.

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