Being an igneous rock, a pegmatite can have numerous "origins". A pegmatite is thecoarsest of the igneous rock types, with the largest crystals, resulting from a very slow rate of cooling. At the Boomer Mine in the South Park of Colorado, a single beryl (beryllium aluminum silicate) crystal was mined from the pegmatite rock there which was six feet in diameter and nearly nine feet long. The Boomer Mine pegmatite is part of the Pikes Peak batholith. Unfortunately, it was uncovered on a weekend when the resident geologist was off work and the miners put the crystal into the mills crusher!! It should have gone to the Smithsonian Institute. You may know beryl as the semiprecious stone "aquamarine".
Sedimentary rocks
Eroded rock without form could be the sand produced.
Metamorphic Rock
volcanic mountains are mostly associated with igneous rocks and sedimentary rocks at their slopes can be found due to weathering,but mountains such as fold mountains can contain igneous rocks,metarmophic ro cks and even sedimentary rocks at their slopes
Yes, weathering slowly does break down rocks and makes them pebbles and then soil, but it takes years.
Four felsic igneous rocks include granite, rhyolite, pegmatite, and dacite. These rocks are characterized by their light color and high silica content, making them rich in minerals like quartz, feldspar, and muscovite. They typically form from magma that has cooled and solidified slowly underground.
Aquamarine is a type of beryl mineral that is typically found in pegmatite rocks, rather than in soil. It forms from the crystallization of magma that cooled within these rocks over time. It is usually mined from these pegmatite deposits rather than from soil.
Pegmatite is actually an igneous rock, not a metamorphic rock. It forms from the slow cooling of magma deep underground, resulting in large crystals due to the slow rate of cooling and high concentrations of water and volatile elements. Metamorphic rocks, on the other hand, form from pre-existing rocks that undergo changes in response to heat, pressure, or chemical processes.
Aquamarine is a mineral that forms from the mineral beryl. Beryls can vary in age but typically form in pegmatite veins in igneous rocks. The mineral itself can be found in rocks that are hundreds of millions of years old.
Pegmatite rocks are known for having large crystals that form without a particular pattern. These rocks are often found in granite and have crystals that can be several centimeters to meters in size. The lack of clear crystal orientation in pegmatite is often due to the rapid cooling of the magma that forms them.
Pegmatite rocks can contain some of the largest crystals found in nature, sometimes reaching several meters in length. These crystals are often visually striking due to their size and clarity, making pegmatites popular among mineral collectors and geologists.
Rocks with large crystals are typically found in igneous rocks that cooled slowly beneath the Earth's surface. These rocks are often found in mountainous regions or areas with active volcanic activity where magma can crystallize slowly to form large crystals. Examples include granite, pegmatite, and gabbro.
Beryl is exclusively of a pegmatite mineral. When this pegmatite magma has a rich source of beryllium, the beryl crystals are formed. They are formed in high temperature veins by these beryllium bearing gas content.
This type of rock is called pegmatite. Pegmatites are igneous rocks that have coarse-grained crystals, typically larger than 1 centimeter in size, which can give them a glassy appearance. These rocks form in the late stages of magma cooling and are known for containing valuable minerals such as quartz, feldspar, and mica.
Examples of intrusive rocks include granite, diorite, and gabbro. These rocks form beneath the Earth's surface through the slow cooling and solidification of magma, resulting in coarse-grained textures. Intrusive rocks are typically more resistant to weathering and erosion compared to extrusive rocks.
Rocks with coarse texture typically form deep below the Earth's surface in the magma chamber of a volcano or in the mantle. As the molten rock cools slowly over time, large mineral grains have the opportunity to grow, resulting in a coarse texture. This process allows for the formation of rocks like granite or pegmatite.
There is no such thing as a "pegmatite rock" in the Pokemon D/P games.