Plagioclase.
The most calcium-rich variety of plagioclase feldspar is called anorthite. It contains a high proportion of calcium compared to sodium and aluminum, giving it its characteristic composition and properties.
It depends on the type of feldspar. Potassium Feldspar (also called K-Spar), contains potassium, aluminum, silicate: KAlSi3O8. Plagioclase Feldspar, on the other hand, contains calcium or sodium, aluminum, and silicate: NaAlSi3O8 or CaAl2Si2O8.
Feldspar is the most common rock-forming mineral. I don't know any other properties except that feldspar occurs in igneous, metamorphic, and sedimentary rock That's not a property
Striations are usually caused by glaciers, which act as an agent of erosion by scraping and dragging rocks and debris across the surface of the Earth. This creates long, linear grooves called striations in the bedrock below.
The scratch marks on rocks left by moving glaciers are called glacial striations. These marks are typically parallel and indicate the direction in which the glacier was moving.
The dominant feldspar in basalt is usually plagioclase feldspar, specifically the calcium-rich variety called labradorite. This feldspar is commonly found in basaltic rocks due to the high calcium content in the magma from which basalt is formed.
The most calcium-rich variety of plagioclase feldspar is called anorthite. It contains a high proportion of calcium compared to sodium and aluminum, giving it its characteristic composition and properties.
striations
They are called striations.
It depends on the type of feldspar. Potassium Feldspar (also called K-Spar), contains potassium, aluminum, silicate: KAlSi3O8. Plagioclase Feldspar, on the other hand, contains calcium or sodium, aluminum, and silicate: NaAlSi3O8 or CaAl2Si2O8.
Feldspar is the most common rock-forming mineral. I don't know any other properties except that feldspar occurs in igneous, metamorphic, and sedimentary rock That's not a property
Vertical grooves are called "striations."
Glacial Cracks
As glaciers move over Earth's surface, the ice acts like sandpaper. The scratch marks that are visible when the ice melts are called striations.
Striations are usually caused by glaciers, which act as an agent of erosion by scraping and dragging rocks and debris across the surface of the Earth. This creates long, linear grooves called striations in the bedrock below.
The scratch marks on rocks left by moving glaciers are called glacial striations. These marks are typically parallel and indicate the direction in which the glacier was moving.
Microscopically you could be seeing sacromeres. Otherwise, these streaks are called striations.