no we use relative mass
A student could use a digital scale or a balance to compare the masses of two small rocks. Simply place one rock on the scale, record the mass, then repeat with the other rock to make the comparison.
The study of physical characteristics of rocks as mineral masses is called petrology. Petrology involves identifying and analyzing the mineral composition, texture, and structure of rocks to understand their formation processes and history. It is a branch of geology that helps in interpreting the Earth's history and geological processes.
Similar rocks and rock structures on two land masses that were once connected can be explained by the theory of continental drift. When two land masses were connected, they shared the same geological processes and formations. Over time as the land masses drifted apart, the rocks and structures that were initially formed together would exhibit similarities due to their common origin.
Volcanoes can contribute to the production of new land masses through the accumulation of lava and volcanic debris. As lava cools and solidifies, it forms new rocks and land formations. Over time, repeated volcanic activity can lead to the creation of new islands or expand existing land masses.
You can turn in gold rocks at a jewelers, pawn shop, or gold buyer for cash value. Be sure to shop around and compare offers to get the best price for your gold rocks.
balance
A student could use a digital scale or a balance to compare the masses of two small rocks. Simply place one rock on the scale, record the mass, then repeat with the other rock to make the comparison.
We can find large masses on oceans and seas.
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People (geologists) have organized rocks and minerals into categories to better study them and compare their properties. The rocks themselves do not care about organization.
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The study of physical characteristics of rocks as mineral masses is called petrology. Petrology involves identifying and analyzing the mineral composition, texture, and structure of rocks to understand their formation processes and history. It is a branch of geology that helps in interpreting the Earth's history and geological processes.
Similar rocks and rock structures on two land masses that were once connected can be explained by the theory of continental drift. When two land masses were connected, they shared the same geological processes and formations. Over time as the land masses drifted apart, the rocks and structures that were initially formed together would exhibit similarities due to their common origin.
i dont know do i
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The fault will be younger than the rocks it faulted (cross-cutting relationships).
both form from heat-volcanic activity