Their surface is often quenched by the sea water so often at the surface they are, crystals will grow and be visible deeper in the rock.
Basalts are as common as the formation of the Ocean floor. Basaltic rocks are ferromagnessian rocks and intrusive igneous rocks. This implies they are formed within the Earth's crust, and they make up the ocean floor. They are dark and dense rocks and occurs in large scale as M.O.R.B. (Mid-oceanic Ridge Basalt).
the crust and the core
hard
There is new rocks that build up they first start as lava and they build up and make new crust
The two types of crust that make up the continents and ocean are the continental crust and the oceanic crust.
granite and basalt
Granite
Silicates make up close to 95 percent of the rocks in the Earth's crust
No. If a a rock is "aphanitic" it means that it is so fine-grained that it is impossible to tell which minerals are present in the matrix. The magma itself is not aphanitic. It is the rapid cooling of the magma that inhibits crystal growth and in turn make the rock's matrix aphanitic. Aphanitic rocks are commonly porphyric. Example: A diabase intrusion can be aphantic with white phenocrystals. Intrusions are often more aphanitic near the contact boundary of the rock that is being intruded. This is because the magma cools more rapidly near the cool, pre-existing rock and the crystals there have less time to grow than those in the middle of the intrusion.
17%
Granite is one of the main rocks that makes up the continental crust.
silicates