How can deserts exist

How can deserts exist?

Deserts in the desert, usually in the form of extreme heat and water scarce sand.  It is generally said that the desert develops through excessive intervention by humans, but we have no evidence of new deserts, other than the existing ones.  We recognize that the sea, oceans and seas are not the same structure as the natural land, sea, and polar ice caps.  Sea water concentrations, temperatures, and biodiversity are not always the same.  There is varied biodiversity on the land and on each major.  Due to the high heat and desert springs and thorns there is no place to be called "desert land".  Currently, basic science is studying "an area where wildlife is destroyed and habitat-less water is evolving over time into a desert."  When the question of how crude oil deposits are located beneath the surface of the earth - sand, dust, and heat - the "world of science" must answer how it dumped the biosphere 300/400 million years ago.  This is not to say that high temperatures are the cause of warming - so much so that the world's highest Himalayas and the Alps are covered with dust instead of ice.  The Great Victoria Desert of Australia would be contrary if the large continents of the African continent were said to have been so warm and so warm.

 About 20% of the land's land area is considered a desert.  The general character of its structure, then, is large sandstones, intense heat, and heavy dust.  Despite the high rock formations, you will find no trees or animals anywhere else.  There are only bush and small plants near the holes, known as oasis.  Regardless of the amount of rainfall, the water is drained to the depths where the roots of the trees cannot reach.  There is no soil available for plant growth.  Although a part of the rain falls deep into the groundwater, most of it evaporates and disappears under the sandy rock.

 The emergence of the desert can be analyzed in a way that science and common sense can understand.

 For example, look at the seismic regions of Africa, Europe and Asia.  The Mediterranean Sea, the Black Sea, the Caspian Sea, the Arabian Gulf, and the Red Sea and the Dead Sea are some of the most extensive Sahara and Arabian deserts.  If the rivers dry up, we can see large sand dunes and cobblestones, and we know that when the heavy rain falls, the big dam is built and the large mud remains.  The Sahara and Arabian Deserts are a good example of what can happen if an old community changes course.  It must be read that we have to witness the Dead Sea as a dry sea.

 The 40-km radius of the "Sahara's eye" (the Richt Structure), astonishing the geologic world, is still the subject of controversy among geologists today.  The main problem is how it could have been so circular in the non-volcanic region.  Others claim that the asteroid may have been struck, but that it is not the general structure of the craters that would cause such an event.  If you try to drain a large pool of mud and sewage through a bathtub or sink hole in it, you will get a bit of a richer structure.  Initially, the water goes out with great force, but when the dirt and sewage is blocked, the flow is blocked, and the slower the slurry, the less waste and mud accumulates.  The Richt Structure is a closed hole face of a sea drain that has taken ages.