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Evgen [1.6K]
3 years ago
13

Which of these would be indications that a given mountain range was not formed by subduction?

Geography
2 answers:
melamori03 [73]3 years ago
7 0

Answer:

it is not along on ocean coastlines and There are no volcanoes.

For Apex

Vika [28.1K]3 years ago
6 0

Answer:

it is not along on ocean coastlines.

Explanation:

please mark me as a brainlist....

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Describe Australian Aboriginal culture before European colonization
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They lived in small communities and survived by hunting and gathering. ... Aboriginal and Torres Strait Island communities only used the land for things that they needed - shelter, water, food, weapons. They never overused it or damaged it.
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Which statement best explains the formation and distribution of oil?
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Answer:

Option D, Oil forms because of geologic heat and pressure and can be found around the world in varying amounts.

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Earth's tilted axis causes the seasons. Throughout the year, different parts of Earth receive the Sun's most direct rays. So, when the North Pole tilts toward the Sun, it's summer in the Northern Hemisphere. And when the South Pole tilts toward the Sun, it's winter in the Northern Hemisphere.

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What is the relationship between volcanoes, earthquakes, and tsunamis in Asia? How do seismic events like earthquakes cause tsun
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The top layer of Earth is an interesting place. Also known as the 'crust,' this thin, solid layer is much more than meets the eye. If Earth were an apple, the skin of that apple could represent the crust in terms of thickness and location. But unlike an apple skin, Earth's crust isn't one large piece covering the entire planet. Instead, it's broken up into many different pieces called tectonic plates that fit together like a large puzzle.

Also unlike the apple, underneath the solid crust is not a deliciously crispy interior. Instead, directly below the crust, we have a thick liquid layer called the mantle. Because it is liquid, the mantle flows and moves around, which moves the plates sitting on top like pieces of ice on a pond.

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