Basalt and gabbro are chemically equivalent rocks. Basalt solidifies above ground and gabbro solidifies below ground.
gabbro is an mafic igneous rock that is formed from the cooling of molten magma.
Gabbro is an intrusive rock, which means it formed underground. Basalt is an extrusive rock, which means it formed above ground .
Gabbro and basalt are both igneous rocks. However, gabbro is an intrusive rock, and basalt is an extrusive rock.
Gabbro has much larger grains that basalt does. This is because basalt cools faster than gabbro and has less time to form crystals.
Basalt and obsidian are extrusive igneous rocks. Gabbro is an intrusive igneous rock.
olivine and pyroxene
Gabbro is an intrusive rock, which means it formed underground. Basalt is an extrusive rock, which means it formed above ground .
Gabbro and basalt are both igneous rocks. However, gabbro is an intrusive rock, and basalt is an extrusive rock.
Gabbro has much larger grains that basalt does. This is because basalt cools faster than gabbro and has less time to form crystals.
They are both lithospheric igneous rocks formed by the cooling and solidification of magma/lava and both of them contains silicon.
Basalt and obsidian are extrusive igneous rocks. Gabbro is an intrusive igneous rock.
Ocean crust is formed by intrusive magma at mid-ocean-ridges. The magma cools and solidifies into peridotite, basalt, or gabbro.
Basalt and pumice.
olivine and pyroxene
The ferromagnesian minerals in the gabbro and basalt are subject to oxidation and chemical breakdown.
Basalt is an Extrusive Igneous Rock, it is a fine grained textured rock, While Gabbro is an Intrusive Igneous Rock and it has a Coarse grain texture.
a hot dogs mother in laws mother to the horse in the backyard
Gabbro is an igneous rock with an intrusive origin. This means that the rock was formed when a body of magma pushed its way into the Earth's crust and formed an intrusion. This magma eventually cools and forms a coarse grained intrusive igneous rock. Gabbro can be found anywhere that a body of magma has risen and cooled.