Answer:
the answer is superior mark me as the brainliest
This is how I would remember it:
Think of a train with two stops. It stops at the parent stop, loads the genetic traits in the caboose, then transmits them to the next stop, the offspring. The train chugs along between parent and offspring, it's only purpose to pass along the traits to the next stop, or offspring. The train's name is Here, Dity!!!!
Hope this helped! :)
It is a matter of time. Crystallization processes can occur more easily when the rock is kept at a certain temperature during a long time. Because of that, well-formed and well crystallized minerals will appear in intrusive igneous rocks (such as granitoids). On the opposite, when a rock spreads rapidly over the Earth's surface, the temperature decreases rapidly, keeping the minerals from forming. A homogeneous paste will form, without any (or few) minerals in it. It is the case for volcanics rock
A 5-carbon sugar, a phosphate, and a nitrogen base are what nucleotides are composed of