Because of their chemical composition, feldspars are more easily attacked by mildly acidic rainwater than say a quartz would be.
Most minerals are opaque, some more than others. Granite is very opaque.
Feldspar, quartz, pyroxene, mica, magnetite among others.
Minerals vary in ways they can be distinduished. Some are easy to identify by hardness, color , streak, or luster
When minerals come into contact with air and water, some dissolve and others react and change into different minerals.
Muscovite and Phlogopite, along with Biotite and Lepidolite and many others are all minerals that cleave into thin sheets with a fair amount of flexibility. However, these minerals are all part of the silicate mineral group known as Micas. Slate can also be cleaved into thin sheets which are slightly flexible, but which are quite brittle. Graphite may also be expanded by chemical treatments to yield a flexible sheet known as graphite foil with interesting electrical and thermal properties.
Most silicate minerals form from molten rock as it cools. Still other silicates form from weathered silicates at Earth's surface, while others form under extreme pressure from mountain building.
Fluorite does not go with the others. It belongs to Halide minerals, while the others (quartz, feldspar, and hornblende) belong to Silicate family of minerals.
Some asteroids are. Most are composed of a mixture of silicate minerals. Others are a mixture of the two.
Certain minerals are harder than others, which means that they are more easily traceable (as they have not been broken down to the extent that they are no longer visible). Quartz is both incredibly hard and common. Silicate minerals are very hard in general, making them the most common minerals. This is also related to the fact that Silicon is the most abundant element in the Crust, or indeed the whole Earth. For this reason, most minerals present in rocks are similar.
oxygen and aluminum
Some rocks are easily broken due to the weak bonds between the molecules in them. For instance, muscovite is easily torn because of the weak bond between the fourth silica in the silicate tetrahedron. There are strong bonds between some molecules and weak bonds between others. The breaks occur along the weak bonds.
Certain minerals are stronger than others because of the way their atomic structures are arranged.
Nitrogen, phosphorus and potassium in abundance and others as trace minerals.
#1.- Some minerals are shinier than others.#2.- A proper balance of vitamins and minerals are necessary for good health.#3.- I've seen those minerals before!#4.- Just look at those beautiful minerals!#5.- A mineral is a naturally occurring substance that is solid and stable at room temperature.#6.- Minerals are usually abiogenic.#7.- Minerals have an ordered atomic structure.#8.- The exact definition of a mineral is still under debate.#9.- The study of minerals is called mineralogy.#10.- Silicate minerals make up over 90% of the Earth's crust.#11.- Native elements, sulfides, halides, sulfates, oxides, carbonates, and phosphates are important mineral groups.#12.- Coal is not a mineral, but diamonds are.
Yes oxygen is in Minerals such as Quartz Feldspar Beryl Hermatite Mica Calcite and others
95%. All others are referred to as rare minerals.
no becase there others name