Mountains

this is Fatima b. on wikianswers dot com; i don't know if this OK with my mom

Don't listen to the answer above

The real answer is that they support his idea because mountains are usually found by the coast of a continent.

1. Subduction of oceanic plate beneath continental plate causes melting and magma formation.
2. Magma rises towards the surface, creating volcanic activity and forming arc-shaped mountain ranges.
3. Sedimentary rocks are uplifted and folded due to tectonic forces, contributing to the growth of the mountain range.
4. Erosion and weathering continue to shape the mountains over time.

The Pacific mountain ranges were formed primarily through the process of tectonic plate movements. The collision between the Pacific Plate and other plates caused intense pressure and heat, leading to the uplift of the Earth's crust and the formation of mountain ranges such as the Andes and the Sierra Nevada. Additionally, volcanic activity played a role in shaping some of the peaks found in the Pacific mountain ranges.

Mountains can be formed in a couple of different ways. Different kinds of mountains are formed different ways. There are four different kinds of mountains: Volcanic, erosional, fault-block, and folded.

Volcanic mountains, also known as volcanoes, can be standing alone or be part of one big chain of volcanoes. Volcanoes are areas in which lava and magma move to the surface and burst through the crust. Igneous rocks are formed here. Sometimes, hot molten rock spews out of volcanoes. This is earth's way of releasing its internal heat

Island arc mountains are formed when one oceanic plate is subducted beneath another oceanic plate, creating a volcanic island arc.

Blood Mountain was formed by a combination of constructive and destructive forces. The mountain likely started forming through tectonic activity, which is a constructive force, while erosion and weathering played a role in shaping its final features, which are destructive forces.

Eventually, natural weathering (over an extremely long time) will wear the rounded peaks into sharper edges. Most extreme weathering occurred during the ice-ages. Glaciers scoured out 'U' shaped valleys, shaved the sides of the mountains, sharpening the mountains into their present shapes.

Volcanic mountains are not typically formed due to plate collision. Instead, they are created when molten rock from beneath the Earth's surface erupts through the crust and builds up over time, forming a cone-shaped mountain.

This phenomenon is known as orographic rainfall. As moist air is forced to rise over a mountain range, it cools and condenses, leading to greater rainfall on the windward side or the side facing the prevailing wind. The leeward side, or the side sheltered from the wind, experiences less precipitation as the air descends, warms, and becomes drier.

The Pacific Plate is subducting beneath the South American Plate to form the Andes mountain range, not the San Andreas mountain range. The San Andreas Fault is a transform boundary between the Pacific Plate and the North American Plate in California.

The windward side of a mountain typically receives more precipitation due to orographic lifting, which occurs as air is forced to rise over the mountain. This can create a wetter, cooler climate with more vegetation and potentially more cloud cover on the windward side of the mountain.

mount Kilauea is 1,227 meters above sea level

To use a range of fault diagnostic equipment, follow the manufacturer's instructions on setup and operation. Connect the equipment properly to the system being diagnosed and run the diagnostic tests as instructed. Interpret the results to identify the fault and take appropriate action to resolve it.

Smooth mountain rock surfaces typically result in higher rates of runoff because water is less likely to infiltrate into the ground. The smooth surface reduces opportunities for water to be absorbed or slowed down, leading to more water flowing across the surface and contributing to increased runoff.

Mountain ranges do not typically form at divergent boundaries. Divergent boundaries are where tectonic plates move away from each other, leading to the formation of mid-ocean ridges and rift valleys, rather than mountain ranges. Mountain ranges are more commonly associated with convergent boundaries where tectonic plates collide and force rocks to be pushed upwards, forming mountain ranges.

That would be a landslide, which is the movement of rock, soil, and debris down a slope. It can be triggered by factors like heavy rainfall, earthquakes, or human activities, and can cause significant damage to property and infrastructure.

Over the next million years, erosion through natural processes like weathering, water flow, and frost action will likely be the main destructive forces altering the appearance of Stone Mountain. Additionally, seismic activity or geological shifts could also contribute to changing the landscape over such a long timescale.

The temperature changes as you go up a mountain due to the reduction in atmospheric pressure with increasing altitude. This drop in pressure causes the air to expand and cool, resulting in colder temperatures at higher elevations.

Fault block mountains can be found in various locations around the world, including the Sierra Nevada in California, the Teton Range in Wyoming, the Harz Mountains in Germany, and the Vosges Mountains in France. These mountains are formed when blocks of the Earth's crust are uplifted and tilted along faults.

Plains form from the deposition of eroded material like sediment and soil that is carried away from the worn-down mountain by rivers and streams. Over time, as this material settles and accumulates, it creates a relatively flat and low-lying area, known as a plain.

The Rocky Mountains act as a barrier to prevailing westerly winds, causing moisture to be deposited on the western side, resulting in wetter conditions. As the air descends on the eastern side, it warms and becomes drier, leading to a rain shadow effect and drier climate in areas east of the Rockies.

Mountain ranges form through tectonic processes such as plate tectonics, where the movement of the Earth's lithospheric plates causes rock to be pushed upwards and folded. This leads to the accumulation of material that eventually forms mountain ranges through processes like folding, faulting, and volcanic activity. Erosion and other geological forces also play a role in shaping mountain ranges over time.

The Himalayas, which run along the border of China and several other countries, are home to the world's highest peaks, including Mount Everest.

Mountains can form through processes such as uplift from tectonic plate collisions, volcanic activity, and erosion. When two tectonic plates collide, the crust can be forced upward to form mountain ranges. Volcanic activity can also result in the formation of mountains when magma rises to the surface and solidifies. Additionally, erosion can play a role in shaping mountains over time by wearing down the land surface and exposing underlying rock layers.

The climate in the eastern US is influenced by moisture-rich air masses from the Atlantic Ocean, leading to more precipitation and higher humidity. In contrast, the western US is influenced by the dry air from the Pacific Ocean, resulting in less precipitation and more arid conditions. The presence of mountain ranges in the western US also plays a role in creating diverse climates.