About 3 cent. a year
About 3 cent. a year
About 3 cent. a year
About 3 cent. a year
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If you want to learn to type fast, it helps a lot to learn ten-finger typing, and to do at least most typing (at the very least, the letters) without having to look at the keyboard.
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The boundaries between lithospheric plates are most effectively outlined by features such as earthquakes, volcanic activity, and the distribution of mountain ranges. These boundaries can be further classified into divergent, convergent, and transform plate boundaries based on the type of plate movement occurring.
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Mid-ocean ridges and deep sea trenches (with their associated volcanos). Also in limited areas strike-slip fault systems (e.g. California), continental collision zones (e.g. India & Asia), etc.
The most common way for mountains to form is when two lithospheric plates collide. This can cause volcanism and folding of rocks in the crust forming mountain belts.
Yes, lithospheric plates can include both continental and oceanic crust. These plates are composed of the rigid outer layer of Earth's surface, which consists of the upper part of the mantle and the crust. Continental crust is less dense and thicker than oceanic crust, but both can form part of lithospheric plates.
The lithosphere includes the crust (oceanic and continental) and the uppermost part of the mantle. The lithospheric plates are thinnest at the ocean, varying from between a few kilometers to 100 kilometers in deep-ocean basins. The continental lithosphere, on the other hand, is generally about 100 to 250 kilometers thick. The most important feature of the lithosphere is its divisions into lithospheric plates. These plates move and collide, creating earthquakes, fault lines, etc.
The most important factor when determining the types of boundaries that form when two lithospheric plates collide is the relative motion between the plates. Depending on whether the plates are moving towards each other, away from each other, or past each other, different types of boundaries like convergent, divergent, or transform boundaries will form.
The edges of most lithospheric plates are characterized by either being divergent (moving apart), convergent (coming together), or transform (sliding past each other) boundaries. These interactions can lead to various tectonic activities such as earthquakes, volcanic eruptions, and mountain formation. The type of boundary and the resulting geological features depend on the direction and speed of the plate movements.
The most common way for mountains to form is when two lithospheric plates collide. This can cause volcanism and folding of rocks in the crust forming mountain belts. Good examples of these are the Andes and the Himalayas.
Tectonic plates are typically composed of a rigid outer layer known as the lithosphere, which includes the crust and upper part of the mantle. This lithospheric layer is broken into several large and small plates that float on the semi-fluid asthenosphere beneath them. These plates interact along their boundaries, which can be convergent, divergent, or transform faults.
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Volcanic eruptions occur only in certain places and do not occur randomly. That's because the Earth's outermost shell -- the lithosphere -- is broken into a series of slabs known as lithospheric ortectonic plates. These plates are rigid, but they float on the hotter, softer layer in the Earth's mantle. There are 16 major plates. As the plates move about, they spread apart, collide, or slide past each other. Volcanoes occur most frequently at plate boundaries.