Basalt or andesite could fit this description.
Granite is an igneous rock with a coarse-grained texture that is typically light in color and contains quartz, feldspar, and mica minerals. Gabbro is also an igneous rock but has a finer-grained texture and is dark in color, composed mainly of plagioclase feldspar and pyroxene minerals. Overall, granite is lighter in color and coarser-grained compared to gabbro.
Coal is fine grained, lack of visible texture.
Basalt contains minerals such as plagioclase feldspar, pyroxene, and olivine. Gabbro also contains plagioclase feldspar and pyroxene, but generally has a coarser texture due to slower cooling rates underground.
The rock you are referring to is likely gabbro, which is a coarse-grained igneous rock composed mainly of intermediate plagioclase feldspar and pyroxene minerals. Gabbro forms from the slow cooling of molten magma deep within the Earth's crust, resulting in its coarse texture.
Gabbro.
Granite is an igneous rock with a coarse-grained texture that is typically light in color and contains quartz, feldspar, and mica minerals. Gabbro is also an igneous rock but has a finer-grained texture and is dark in color, composed mainly of plagioclase feldspar and pyroxene minerals. Overall, granite is lighter in color and coarser-grained compared to gabbro.
Coal is fine grained, lack of visible texture.
Basalt contains minerals such as plagioclase feldspar, pyroxene, and olivine. Gabbro also contains plagioclase feldspar and pyroxene, but generally has a coarser texture due to slower cooling rates underground.
The rock you are referring to is likely gabbro, which is a coarse-grained igneous rock composed mainly of intermediate plagioclase feldspar and pyroxene minerals. Gabbro forms from the slow cooling of molten magma deep within the Earth's crust, resulting in its coarse texture.
Gabbro.
Igneous rocks often have a fine-grained or glassy texture. These textures typically occur in volcanic rocks, such as basalt and rhyolite, where rapid cooling of lava prevents large crystals from forming. Additionally, obsidian is a volcanic glass that exhibits a glassy texture due to its rapid cooling and lack of crystal structure.
Volcanic rocks are formed from magma that cools quickly at the Earth's surface, resulting in fine-grained crystals due to rapid cooling. This rapid cooling prevents large crystals from forming, giving volcanic rocks a glassy or fine-grained texture. In contrast, rocks formed from intrusions cool slowly beneath the Earth's surface, allowing for the growth of larger crystals. This slow cooling process results in a coarse-grained texture in intrusive rocks, with visible crystals that are often easily distinguishable.
Both gabbro and granite are igneous rocks, but they have different mineral compositions and textures. Gabbro is dark in color and consists mainly of pyroxene, plagioclase feldspar, and olivine minerals, with a coarse-grained texture. Granite, on the other hand, is light in color and composed mainly of quartz, feldspar, and mica minerals, with a medium to coarse-grained texture.
Volcanic rocks can vary in grain size, but many are fine-grained due to their rapid cooling as they solidify from lava or magma. The specific mineral composition and cooling rate influence the final texture of the rock, so not all volcanic rocks are fine-grained.
1.It is extrusive volcanic rock 2.it white,grey or black in color 3.it has fine grained or aphanatic texture
Typically porphyritic with hbl phenocrysts.
The texture is fine-grained.