The most abundant minerals in granite are potassium feldspar, plagioclase feldspar, and quartz; with differing amounts of muscovite, biotite, and hornblende-type amphiboles. The most abundant minerals in basalt are amphibole and pyroxene, sometimes plagioclase, feldspathoids, and/or olivine. In other words, no.
The object that can scratch appetite but not feldspar is quartz. Quartz has a hardness of 7 on the Mohs scale, while feldspar has a hardness of 6. Therefore, quartz can scratch appetite, which has a hardness of about 5.5, but cannot scratch feldspar.
The mineral that can scratch feldspar and can be scratched by garnet is quartz. Quartz has a hardness of 7 on the Mohs scale, making it capable of scratching feldspar, which has a hardness of 6. Meanwhile, garnet has a hardness of around 6.5 to 7.5, allowing it to scratch quartz but not all varieties of garnet will scratch quartz.
Granite.
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.
Mostly feldspar and quartz
Quartz and feldspar are indeed two of the most common minerals found in the Earth's crust. Quartz is known for its hardness and crystal structure, while feldspar is known for its abundance and variety of colors. Both minerals are commonly found in igneous, metamorphic, and sedimentary rocks.
Unakite rocks are metamorphic rocks formed from the alteration of igneous rocks. They are typically composed of pink feldspar, green epidote, and clear quartz.
A steel nail can scratch feldspar but not quartz. Feldspar has a hardness of 6 on the Mohs scale, while quartz has a hardness of 7.
Metamorphic rocks can have a range of textures, from smooth to rough, depending on the minerals present and the intensity of the metamorphic processes they underwent. Some metamorphic rocks, like gneiss, can have a rough texture due to the presence of minerals like quartz and feldspar.
Quartz - the term quartzite is applied to to low grade metamorphic rocks formed predomiently of quartz, mostly they are altered sandstones. Alog with the quartz there may be low abundances of many different minerals e.g. mica, or feldspar.
Arkose forms from the weathering and erosion of feldspar-rich rocks like granite and granodiorite. The feldspar grains undergo chemical weathering to form clay minerals, which are then transported and deposited as sediment. The high quartz content in arkose distinguishes it from other sandstones.
The four major rock-forming minerals are quartz, feldspar, mica, and amphibole. These minerals are commonly found in various types of igneous, sedimentary, and metamorphic rocks and make up a significant portion of the Earth's crust.
Feldspar sand is a type of sand that contains a high proportion of feldspar minerals. Feldspar is a group of rock-forming minerals that are commonly found in igneous and metamorphic rocks. Feldspar sand can be used in a variety of applications such as in construction, ceramics, and glassmaking.
The most abundant minerals in granite are potassium feldspar, plagioclase feldspar, and quartz; with differing amounts of muscovite, biotite, and hornblende-type amphiboles. The most abundant minerals in basalt are amphibole and pyroxene, sometimes plagioclase, feldspathoids, and/or olivine. In other words, no.
Quartz and feldspar are commonly found together in granite and gneiss.
Quartz and feldspar are two common minerals that form rocks. Quartz is often found in granite while feldspar is found in both granite and basalt.