Age is how old the rock is relative to other rocks, position is where the rock is in relation to other rocks. Tectonic motion and other forces can easily turn a portion of the Earths crust upside down resulting in older rock lying above younger layers.
Both are igneous rocks of intermediate coposition.
how is metamorphic rock different than intrusive rock
Folds and faults are both formed from compression on opposite sides due to tectonic movement of the earth's crust. However, in a fold, the crust does not break, it simply is deformed in a curved pattern. In a fault, the rocks in the crust actually shatter, and movement is seen along a fault line, wheby rocks are displaced relative to each other.
The configuration of the atoms. Some bonds are stronger than others.
Igneous rock is formed from the solidification of magma or lava. Sedimentary rock is formed from the lithification of sediments, generally.
relative dating.Relative dating is used to determine the relative age of rocks.
Relative age is the age of a rock relative to the rock layers around it, absolute age is a rock's exact age.
classic rocks are not minerals. limestone is
The difference between breccias and conglomerate is that breccias are angular and conglomerates are smooth. What causes rocks to be smooth is transportation, such as when rocks are in a stream and are worn down. Therefore transportation is what causes the difference between breccias and conglomerates.
monomineralic - one mineral polymineralic - multiple minerals
describe the textural difference between coarse-grained (phaneritic) and fine-grained (aphaneritic) rocks
Gems are valuable rocks aren't.
A rock is a rock, and a diamond is a gem.
most metamophic rocks contain a high amount of oxygen and silicon
Paleozoic rocks contain fossils while Precambarian rocks had no fossils since at that time there was only single celled organisms.
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relative age