Small grained rocks have a fine-grained texture. This means that the individual mineral grains in the rock are too small to be visible to the naked eye. Examples include basalt and shale.
Granite has large mineral grains compared to obsidian, basalt, and pumice. Granite is an intrusive igneous rock that forms deep within the Earth's crust, allowing for the growth of large mineral crystals due to slow cooling. Obsidian, basalt, and pumice are extrusive igneous rocks that cool quickly at the Earth's surface, resulting in smaller mineral grains or a glassy texture.
Yes, basalt is the fine-grained equivalent of gabbro. Both rocks are formed from the same magma composition (mafic), but basalt is extrusive, cooling quickly at the Earth's surface, resulting in smaller mineral grains, while gabbro is intrusive, cooling slowly beneath the surface, resulting in larger mineral grains.
slowly from a magma with abundant time to grow. This can suggest an intrusive or plutonic igneous rock type, such as granite. Rapid cooling leads to small crystal grains, characteristic of extrusive or volcanic igneous rocks like basalt.
The grain size of basalt varies depending on how quickly the lava cooled and solidified. Typically, basalt has a fine to medium grain size, with individual grains being less than 1 mm in size. Rapid cooling can result in a fine-grained basalt, while slower cooling may produce a coarser-grained texture.
no
very compact,crystal grains interlocked
Basalt typically has a fine-grained texture, meaning that its individual mineral grains are too small to be seen with the naked eye. The crystals in basalt form due to rapid cooling of lava at the Earth's surface, resulting in a dense and homogeneous rock.
Since basalt is extrusive it cools quickly and forms small crystals.
It is Gabbro
Small grained rocks have a fine-grained texture. This means that the individual mineral grains in the rock are too small to be visible to the naked eye. Examples include basalt and shale.
The seafloor spreads apart, creating new rocks that record magnetic orientation. Small grains of magnetite on the volcanic basalt (ocean floor) have magnetic properties.
The seafloor spreads apart, creating new rocks that record magnetic orientation. Small grains of magnetite on the volcanic basalt (ocean floor) have magnetic properties.
Yes. The grain texture also matters. For example, basalt and gabbro have the same mineral composition, but basalt, which forms on the surface, has microscopic grains while gabbro, which forms underground, has larger mineral grains.
Granite has large mineral grains compared to obsidian, basalt, and pumice. Granite is an intrusive igneous rock that forms deep within the Earth's crust, allowing for the growth of large mineral crystals due to slow cooling. Obsidian, basalt, and pumice are extrusive igneous rocks that cool quickly at the Earth's surface, resulting in smaller mineral grains or a glassy texture.
relativity small
Basalt formations can be massive, encompassing many square miles. The mineral crystals which make up basalt require magnification to see.