Erosion for thousands of years. The mountain was a volcano which filled up. Mountain ranges are formed by The Plates of the earth moving against each other ,some pushing up in tremendous forces. Some were not able to be sharply pointed.. Earth quakes happen when these Plates in the earth move to adjust themselves. The crust of the earth is miles deep with cracks here and there,setting on a bed of molten lava. Some of this leaks close to the earth's surface ,causing volcano's ,hot springs. A city in Oregon has so much geo thermal energy ,it heats the side walks to melt snow ,ice in the winter.
they both have rock thy are very cloerfilub and almost as the same miaril as they do
Both, the can scrape past eachother or one can go under the other.
It is the result of weathering processes on earth.
1. Earthquake may sometimes create new coastal plains, by the emergence of a portion of ocean floor. 2. Submergence of coastal land may result in formation of bays and gulfs which are favourable sites for the development of ports harbours. Raghav, neyveli. 3.Earthquakes result in the formation of hot springs and geyser beneficial for medicinal purposes
Mountains can not create a wind. Winds are the result of the heat coming from the Sun and the heat radiated by the Earth into space. They are the atmospheres response to the differential of heat within the atmosphere. All mountains do is modify the the flow of the wind as they act as barriers to this flow.
erosion don't you know
The phenomenon responsible for the formation of the highest mountains is Tectonism. This is caused mostly as a result the collision movements of various lithospheric plates. The process of formation of the mountains is termed Orogeny.
General term for the processes that produce mountains
They are the result of tectonic forces or volcanism.
The Andes mountain range is a result of convergent plate boundary formation, where the South American Plate is subducting beneath the Nazca Plate. This collision has led to the uplift and formation of the Andes mountains through various geological processes over millions of years.
Mountains are produced through the processes of tectonic plate collision, where two plates converge and either compress, producing fold mountains, or one plate is forced beneath another in a subduction zone, creating volcanic mountains. These processes can result in the uplift and deformation of the Earth's crust, leading to the formation of mountain belts over millions of years.
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 vertical and horizontal movement of the Earth's crust that produces mountains is called tectonic activity, specifically associated with the processes of plate tectonics. This includes processes such as folding, faulting, and volcanic activity, which can result in the uplift and formation of mountain ranges over geological time scales.
Formations and other geological features are created through a combination of geological processes such as erosion, sedimentation, tectonic activity, and volcanic activity. These processes can result in the formation of various landforms such as mountains, valleys, canyons, plateaus, and caves over millions of years. The specific type of formation or feature created depends on the underlying geology and the intensity of these processes in a particular area.
Clay formation is primarily a result of chemical weathering, where minerals in rocks are broken down by chemical processes to form clay minerals.
The two processes that result in the formation of igneous rocks are cooling and solidification of molten magma, and crystallization of magma within the Earth's crust or on the surface. These processes lead to the solidification of molten material, which then forms igneous rocks.
by eroison