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In general, the younger the mountain chain, the taller it is. Plate tectonics builds mountains by thrusting the crust upward, while erosion wears them back down over millenia.

So the Himalayas are a new (and in fact, still growing) mountain chain, while the Appalachians are one of the oldest chains still identifiable as mountains.

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12y ago
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1mo ago

Young mountains tend to have sharp, jagged peaks and steep slopes due to recent tectonic activity, while old mountains have smoother, more rounded peaks and gentler slopes due to erosion and weathering over time. Additionally, young mountains often have more visible rock layers and fault lines compared to older mountains.

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Q: What is one way to tell young mountains from old mountains?
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Continue Learning about Earth Science

If old mountains are worn down over the course of millions of years what is one of the primary reasons that mountains still exist?

Plate tectonics is one of the primary reasons why mountains still exist. The movement of tectonic plates can create new mountain ranges through processes like convergence and uplift, which counteracts the continuous erosion that wears down old mountains.


What is Adirondack mountains bedrock age?

The bedrock in the Adirondack Mountains of New York is primarily Precambrian in age, ranging from about 1.2 billion to 1 billion years old. It is one of the oldest rock formations in North America.


If old mountains wear down over the course of millions of years what is one of the primary reasons that mountains still exist?

The movement of tectonic plates causes mountains to form and uplift, constantly renewing their elevation and preventing complete erosion. Additionally, the Earth's internal heat can cause volcanic activity, creating new mountains. In some cases, climate and erosion patterns can balance out to maintain mountains over long periods of time.


How would you tell the age of a mountain?

One method is to examine the rock composition and structure of the mountain to determine its age. Another way is to study the erosion patterns on the mountain, as older mountains tend to have more rounded features due to weathering over time. Additionally, scientists can use radiometric dating techniques on rocks found on the mountain to estimate its age.


What is one clue that tells you that a mountain is young versus being old?

One clue that a mountain is young is if it has sharp, jagged peaks and steep slopes. This indicates that the mountain has undergone recent tectonic activity, such as uplift or faulting. In contrast, an old mountain would have more rounded peaks and gentle slopes due to erosion over time.

Related questions

What is the difference between young and old fold mountains?

Young fold mountains are characterized by rugged and sharp peaks, steep slopes, and active tectonic activity. Old fold mountains, on the other hand, are more rounded with lower elevations due to erosion over time, and have less tectonic activity. Examples of young fold mountains include the Himalayas, while the Appalachian Mountains are an example of old fold mountains.


How do you tell the age of a mountain?

One way to tell the age of a mountain range is by its height. Another way is by how eroded and worn the edges of the rocks are. The more jagged the edges, the younger the mountains. Heavily worn ranges may be so eroded that they become foothills


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The Wise Old Woman is a story about a kind young farmer and his old mother. The cruel young lord who ruled the village disliked old people, so his decree was to banish anyone over seventy-one from the village and "be left in the mountains to die." When the farmers mother turned seventy-one, he brought her up to the mountains but decided to stay hidden in their home. One day another lord threatened to conquer the village, so the young cruel lord asked for help from people in the village. In summary of what happened, all the wise and intelligent answers that helped save the village from the lord were from the wise old mother, so the young lord started to respect his elders because of their wisdom.


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