When two continents collide, their tectonic plates push against each other, causing intense pressure to build up. This pressure can force rocks to deform and fold, leading to the formation of mountain ranges. The collision may also cause crustal uplift and the thickening of the Earth's crust, further contributing to mountain formation.
The theory of plate tectonics explains that the Earth's lithosphere is divided into large plates that float on the semi-fluid asthenosphere. These plates move due to the heat-driven convective currents in the mantle. Continental drift is the movement of the continents across the Earth's surface over geologic time. The continents have shifted over time due to the movement of these tectonic plates, leading to the formation of supercontinents like Pangaea, which later broke apart into the continents we see today.
The theory that explains why and how continents move is called plate tectonics. It states that Earth's outer shell is divided into several large plates that float on the semi-fluid asthenosphere below, and these plates move and interact with each other, leading to phenomena such as earthquakes, volcanic activity, and the formation of mountain ranges.
Wegener proposed the theory of continental drift, suggesting that the continents were once connected in a single landmass called Pangaea. He proposed that the continents drifted apart over time due to the movement of the Earth's crustal plates.
Wegener believed that all continents were once part of a supercontinent called Pangaea, which began breaking apart about 200 million years ago. He proposed the theory of continental drift to explain the movement of the continents over time.
The current shape and position of continents provide evidence for the theory of plate tectonics, which suggests that continents were once part of a supercontinent called Pangaea that has since drifted apart. This movement helps explain the similarities between the geology and fossils of now widely separated continents, as well as the presence of matching coastlines and mountain ranges.
conpression
The theory of plate tectonics helps to explain how earthquakes and volcanic eruptions occur.
Understanding plate tectonics helps explain the movement of Earth's lithosphere, including the formation of mountains, earthquakes, and volcanic activity. It provides insight into how continents have shifted over time and how various geologic events are interconnected globally.
There is no reason to explain, this is just how it is. High elevation is due to mostly mountains, and Europe just does not currently have many mountains. There are lots of plains in Europe.
Dr. Suess proposed the theory of plate tectonics to explain the formation of mountains. According to this theory, Earth's outer shell, known as the lithosphere, is divided into several large, rigid plates that move and interact with each other. Mountains are formed when these plates collide, causing the crust to buckle and uplift, creating geological features such as mountain ranges.
mountains, thus proposing the theory of uniformitarianism to explain the formation of geological features on Earth.
The theory that explains why continents move is called plate tectonics. This theory suggests that the Earth's lithosphere is divided into plates that float on the semi-fluid asthenosphere below. The movement of these plates is driven by the heat generated from the Earth's core, causing them to drift and collide, leading to the formation of mountains, earthquakes, and volcanic activity.
Geologists classify mountains based on their formation process, height, and steepness of slopes. Some features called mountains may not meet the specific criteria set by geologists, such as being formed by tectonic processes like folding and faulting. Therefore, they may be referred to as hills or other landforms instead.
Explain the difference between young and mature mountains?
By boook
when continents collide you bum your pet hamster
By boook