because if the crater goes towards its self then down it it due to volcano but impact crater is looks more spread out and u may see parts of the meteor or cause of impact marks around the crater
The three main parts of a volcano are the magma chamber where molten rock is stored beneath the surface, the vent where lava erupts to the surface, and the crater which is the bowl-shaped depression at the top of the volcano.
The main parts of a volcano is the crater, main vent, magma chamber, and pipe.
Parts of the ocean floor were formed during various geological eras, such as the Paleozoic, Mesozoic, and Cenozoic. For example, the mid-ocean ridges where new ocean floor is formed through volcanic activity are continuously active processes that have been occurring for millions of years.
There tends to be five main parts that make up a volcano. They include the magma chamber, the main vent, lava, the crater, and the pyroclastic flow , which is fast moving flow of hot gas and rock.
The component parts are formed.
To answer your question accurately, I would need more context about the specific parts you are referring to. Molecules can be formed from various combinations of atoms or smaller molecules depending on the chemical reaction or biological process involved. For example, glucose is formed from carbon dioxide and water during photosynthesis. If you provide more details, I can give you a more precise answer.
Different parts of living organisms are formed as the genetic information is read. This controls how and when various parts are constructed as the organism develops.
There are so many different parts that are on volcano. Some of the main ones include ash cloud, vent, crater, magma, lava and so much more.
A perennial river is a river that has continuous flow in parts of its bed all year round during years of normal rainfall.
The cell membrane and vesicle have to be made of the same parts so that the process can be completed.
The order of parts through which magma reaches the surface of a volcano is the magma chamber where it accumulates, followed by the central vent or conduit where it travels upwards, and finally the crater or vent at the surface where it erupts and flows out as lava.