Granite.
Solidification of a coarse-grained igneous rock usually occurs deep beneath the Earth's surface, in a magma chamber or intrusive setting. Here, the slow cooling allows for the formation of larger mineral crystals, resulting in a coarse-grained texture. Examples of coarse-grained rocks include granites and gabbros.
Course igneous rock
A fine-grained igneous rock would likely weather faster than a coarse-grained igneous rock. This is because the smaller grains in a fine-grained rock provide more surface area for weathering processes to act upon, leading to quicker breakdown and erosion.
Granite is a coarse-grained igneous rock, meaning it is made up of large interlocking crystals. These crystals form as the magma cools slowly beneath the Earth's surface, allowing for the growth of larger grains rather than small ones.
Limestone can be both coarse-grained and fine-grained, depending on its composition and how it formed. Coarse-grained limestone typically contains larger mineral grains visible to the naked eye, while fine-grained limestone has smaller mineral grains that are not easily seen without magnification.
fine grained
Granite is a course-grained igneous rock commonly used for buildings and monuments. Its durability, strength, and resistance to weathering make it an ideal material for structures that require longevity and aesthetic appeal. Granite can be polished to a high shine, enhancing its visual appeal for countertops, facades, and memorials. Additionally, its availability in various colors and patterns allows for diverse architectural designs.
Anorthosite typically has a coarse-grained texture, with individual mineral grains that are easily visible to the naked eye. It often appears as a mottled combination of white, gray, and black minerals, with a crystalline structure that can exhibit cleavage planes.
Solidification of a coarse-grained igneous rock usually occurs deep beneath the Earth's surface, in a magma chamber or intrusive setting. Here, the slow cooling allows for the formation of larger mineral crystals, resulting in a coarse-grained texture. Examples of coarse-grained rocks include granites and gabbros.
Coarse
fine grained
Gneiss is course grained but it has a fabric.
Intrusive igneous rocks form underground from magma that cools slowly, resulting in coarse-grained textures. They have large mineral crystals visible to the naked eye, such as feldspar, quartz, and mica. Examples include granite, diorite, and gabbro.
G
No, granite is a coarse-grained igneous rock that is made up of minerals like quartz, feldspar, and mica. Glassy igneous rocks, like obsidian, form when molten lava cools quickly on the surface, resulting in a smooth, glass-like texture.
shale
You can look at the rock texture.If the crystals are Large enough to be visible with your naked eye without stressing it the the texture is likely to be either medium coarse grained or course grained which is an indication that it is Intrusive.The opposite is forExtrusive