Sandstone
Hornfels is a metamorphic rock that is often used in the construction industry for making tiles, countertops, and other decorative building materials. It can also be used as a material for sculptures or as a decorative stone in landscaping.
The protolith of phyllite is shale or mudstone that has been subjected to low-grade metamorphism. This metamorphic process causes the rock to recrystallize, resulting in a foliated texture with fine-grained mica minerals like muscovite and chlorite.
A nonfoliated rock formed by contact metamorphism of a shale or mudstone is called hornfels. It usually has a fine-grained texture and lacks the layering characteristic of foliated rocks. Hornfels forms when the parent rock is subjected to high temperatures and pressures near a magma intrusion.
The protolith of a quartzite is a sedimentary rock called sandstone. Quartzite forms when sandstone undergoes metamorphism, typically due to high heat and pressure, causing the quartz grains in the sandstone to recrystallize and merge together.
A metamorphic rock changes from one form to another by intense heat or pressue. The parent rock, or protolith, is the rock that undergoes change. It can be any rock type, sedimentary, igneous, and even metamorphic.
hornfels is red
Hornfels or gneiss are possible metamorphic rock with a greywacke protolith.
"protolith" refers to the original composition of an altered rock. for example, a basalt was the protolith to a rock thats presently a greenschist.
The protolith of a metamorphic rock can be any pre-existing rock type, such as shale, limestone, basalt, or granite. The type of metamorphic rock that forms from a protolith depends on factors like temperature, pressure, and the mineral composition of the protolith.
peridotite
I too would like an answer to this question as it seems hornfels could be of varying grade dependant on the temperature. The facies of contact metamorphism progress in temperature at relatively low pressure from the Albite-Epidote Hornfels Facies to the Hornblende Hornfels Facies, to the Pyroxene Hornfels Facies. It seems that hornfels do have differant grades.
A protolith of sandstone is a sedimentary rock made up of sand-sized mineral grains or rock fragments that have been compacted and cemented together over time. It can form from the erosion and deposition of pre-existing rocks like granite, quartzite, or basalt.
The protolith of schist is typically shale or slate, which undergoes metamorphism to form schist. The protolith of anthracite coal is primarily bituminous coal, which is subjected to higher temperature and pressure conditions during metamorphism to convert into anthracite coal.
Hornfels is a metamorphic rock that is often used in the construction industry for making tiles, countertops, and other decorative building materials. It can also be used as a material for sculptures or as a decorative stone in landscaping.
The protolith of marble was limestone or dolomite.
The protolith of marble was limestone or dolomite.
it has been on earth forever