Both are made from volcanic rock. Pumice forms when lava cools very quickly and still has pockets of air trapped inside. This make the rock very lightweight and porous -- it can even float on water! Obsidian also forms when lava is quickly cooled, but it does not have trapped air pockets inside. It looks like glass and is rather brittle, but makes an excellent material for sharp cutting implements.
Basalt and gabbro are both igneous rocks that form from the cooling and solidification of magma. Basalt is fine-grained and forms from lava flows on the Earth's surface, while gabbro is coarse-grained and forms from magma that cools beneath the surface. Obsidian is a volcanic glass that forms when lava with a high silica content cools rapidly, without time for crystal growth, resulting in a smooth, glassy texture.
Gabbro typically has a coarse-grained texture, with interlocking grains that are visible to the naked eye. The texture is formed by the slow cooling of molten rock beneath the Earth's surface.
Obsidian. It has very fine grain or is amorphous, and it has a conchoid fracture, so it can be worked to a sharp edge and point. Gabbro, on the other hand, has a very coarse grain and it difficult to get and edge or point on at all.
The glassy texture of obsidian is the best evidence that it formed in an extrusive environment. Obsidian is rapidly cooled lava with no time for crystal growth, resulting in a smooth, glass-like texture.
Obsidian is an igneous rock that has a smooth glass-like texture. It is formed when lava cools rapidly without crystal formation, resulting in a glassy texture.
Obsidian
Basalt and gabbro are both igneous rocks that form from the cooling and solidification of magma. Basalt is fine-grained and forms from lava flows on the Earth's surface, while gabbro is coarse-grained and forms from magma that cools beneath the surface. Obsidian is a volcanic glass that forms when lava with a high silica content cools rapidly, without time for crystal growth, resulting in a smooth, glassy texture.
A glassy texture.
Gabbro typically has a coarse-grained texture, with interlocking grains that are visible to the naked eye. The texture is formed by the slow cooling of molten rock beneath the Earth's surface.
Obsidian is an extrusive rock that cooled very rapidly without forming crystals. As a result, obsidian has a smooth, shiny texture of a thick piece of glass.
Obsidian is an igneous rock with a glassy texture. Its texture is also called hyaline, the Greek word for texture.
Granite, Basalt, Gabbro, and Obsidian
Obsidian. It has very fine grain or is amorphous, and it has a conchoid fracture, so it can be worked to a sharp edge and point. Gabbro, on the other hand, has a very coarse grain and it difficult to get and edge or point on at all.
The texture of a rock depends on the rate that it cools. Obsidian cools so quickly that no crystals can form, therefore giving it a glassy texture.
Obsidian is a hard, dark volcanic rock that is formed by the rapid solidification of lava. Its texture is glassy and shiny black.
basalt, granite, rhyolite, andesite, gabbro, obsidian, scoria, pumice.
Gabbro, obsidian, and peridotite are examples of igneous rocks. Chert is a sedimentary rock formed from the accumulation of silica-rich microorganisms or chemical precipitation, not from the cooling and solidification of molten magma like igneous rocks.