Obsidian, actually a volcanic glass, has no crystalline structure due to its quick solidification.
Mineraloids are mineral like substances that do not have a crystalline structure. Mercury is an example.
Both are igneous rocks, but whereas volcanic rocks are formed from cooling lava on the surface, plutonic rocks are formed from cooling magma below the surface. So plutonic rock is an igneous intrusive rock, while volcanic rock is extrusive.
Marble and quartzite are two examples of metamorphic rocks that lack banding and are massive. The lack of banding may indicate that the metamorphism may be due to a greater factor of heat than of pressure.
Larger crystal size is generally associated with longer cooling times, because large crystals take a long time to form. For this reason, intrusive (underground) igneous rocks have larger crystals than extrucive (above ground) rocks, due to the lack of insulation, and hence faster cooling, at the surface.
Absence of sedimentary rocks = passage of time because over time, sediment breaks down and forms with the earth (land, sea, mountains)
Mineraloids are mineral like substances that do not have a crystalline structure. Mercury is an example.
Both are igneous rocks, but whereas volcanic rocks are formed from cooling lava on the surface, plutonic rocks are formed from cooling magma below the surface. So plutonic rock is an igneous intrusive rock, while volcanic rock is extrusive.
nonfoliated rocks
A porphyritic texture can be a feature of igneous rocks, but 'porphyritic' is not used to describe metamorphic rock texture. Metamorphic rocks can be foliated or non-foliated, terms used to describe mineral alignment or banding, or the lack thereof.
Metamorphic rocks are classified by foliation or lack there of, not sedimentary rocks. They are classified into Clastic Sedimentary, and Chemical Sedimentary.
yes
There are a couple examples. Coal is a rock, but it is organic and so does not contain minerals. Obsidian and pumice are both varieties of volcanic glass. Since they lack a crystal structure, they are not composed of minerals
Lack of banding
No sedimentary rocks are found yet. The reason is moon is lack of atmosphere.
Igneous rocks are called fire rocks and are formed either underground or above ground. Underground, they are formed when the melted rock, called magma, deep within the earth becomes trapped in pockets. As these pockets of magma cool slowly underground, the magma becomes igneous rock . Igneous rocks are also formed when volcanoes erupt, causing the magma to rise above the earth's surface. When magma appears above the earth, it is called lava. Igneous rocks are formed as the lava cools above ground. Metamorphic rocks are rocks that have "morphed" into another kind of rock. These rocks were once igneous or sedimentary rocks. How do sedimentary and igneous rocks change? The rocks are exposed to great heat and pressure from depth of burial or exposure to tectonic forces, and this causes them to change. The change is reflected in the recrystallization of certain mineral crystals, or even the disappearance of some minerals and the appearance of new minerals. Metamorphic rock often displays foliation, in which the minerals are aligned in bands or thin layers perpendicular to the force that was applied in their metamorphosis. Igneous rocks do not display layering.
Marble and quartzite are two examples of metamorphic rocks that lack banding and are massive. The lack of banding may indicate that the metamorphism may be due to a greater factor of heat than of pressure.
Non-foliated