The most common sand is the remnant of the cooling and crystallization of the crustal components. After several years of drifting into the sea, it can be said to be the sand of time.
The most common sand is the remains of the cooling crystallization of crustal components. After several years of drifting to the sea, it can be said to be the sand of time
The most common sand is the remains of cooling crystallization of crustal components, which drift into the sea after several years, so it can be said that it is the sand of time.