Answer:
Following are the solution to this question:
Explanation:
Throughout layers called sheets or stratification were placed silicate minerals. Any formal credit with a uniform lithology or texture is defined as asleep. Beds are built on top of one another by deposition with disk diffusion.
Physical danger rocks characteristics:
- Bedding is also a sedimentary stone's most obvious feature. It comprises of language service as major corridors marking the boundaries of various layers of the earth.
- Grade grounds are popular when sediment does have a sluggish stream accumulated.
- Fossils, and Fractures and ripples of decomposition, etc.
It is slowly growing, mostly due to immigration
I am good at math but I don’t want to answer this question so I’m really really really really really sorry but a triangle is very season 02300 -3 of this is dilated which of the center of at the origin in the scale factors of two good luck and I’m sorry
The lithosphere, which is the rigid outermost shell of a planet (the crust and upper mantle), is broken up into tectonic plates. The Earth's lithosphere is composed of seven or eight major plates (depending on how they are defined) and many minor plates. Where the plates meet, their relative motion determines the type of boundary: convergent, divergent, or transform. Earthquakes, volcanic activity, mountain-building, and oceanic trench formation occur along these plate boundaries. The relative movement of the plates typically ranges from zero to 100 mm annually.[2]
Tectonic plates are composed of oceanic lithosphere and thicker continental lithosphere, each topped by its own kind of crust. Along convergent boundaries, subduction carries plates into the mantle; the material lost is roughly balanced by the formation of new (oceanic) crust along divergent margins by seafloor spreading. In this way, the total surface of the lithosphere remains the same. This prediction of plate tectonics is also referred to as the conveyor belt principle. Earlier theories, since disproven, proposed gradual shrinking (contraction) or gradual expansion of the globe.[3]
Tectonic plates are able to move because the Earth's lithosphere has greater strength than the underlying asthenosphere. Lateral density variations in the mantle result in convection. Plate movement is thought to be driven by a combination of the motion of the seafloor away from the spreading ridge (due to variations in topography and density of the crust, which result in differences in gravitational forces) and drag, with downward suction, at the subduction zones. Another explanation lies in the different forces generated by tidal forces of the Sun and Moon. The relative importance of each of these factors and their relationship to each other is unclear, and still the subject of much debate.
