The country of Mongolia, even though is very big, in fact 19th biggest in the world by area, it still only has around 3 million people living in it, and there's a big part of the population that is still practicing the nomadic lifestyle like in the time of Genghis Khan.
The country is landlocked, and is located between Russia and China, and has the role of a buffer state, but it seems to struggle more and more with that role and it wouldn't be weird if it loses its independence in the near future. Even though Mongolia is not in conflict with any of the two big neighbors, it is a country of interest for both of them, especially because recently huge deposits of multiple natural resources have been found there. Since both countries are much powerful and can overtake Mongolia in a day or two (without exaggeration), it wouldn't be weird if they do that inway or another in the near future.
Sedimentary rocks that are formed due to the accumulation of sediments that are derived from the deposition of small particles and their cementation of minerals and organic particles in the seafloor by the impact of various geological and earth processes like the wind, water, and glacier erosion.
Earth's crust is covered by 73% of sedimentary rocks and about 8% of the total crustal surface. Based on their formation, these rocks are thus classified as Siliciclastic, Carbonate, Evaporite, Iron-rich, and Phosphatic sedimentary rocks.
The color of these rocks is always determined by the iron and oxide contents, their size texture is a result of the density and permeability of the rocks like in the case of sandstone and limestone.
The relationship between the plate tectonics and the earthquakes is explained through the seismic waves that travel; through the three-layer of the earth from core to mantle to crust.
Earthquakes are directly related to plate boundaries as these are areas where these waves come out in the form of shocks and shaking of lands thus we expect of seeing three types of boundaries as Convergent, Divergent and Transform.
