Obsidian changes into shale through weathering and compaction. Obsidian, an igneous rock, can get worn down into particles, usually through grind up against other rocks. Those tiny obsidian particles are then carried away by wind or water, and deposited in a river bed or out in the ocean. As time goes on, other sediments are then piled on top of the obsidian particles, compacting them down into shale.
Shale turns into slate, granite into gneiss.
Igneous: * Obsidian * Granite * Diorite * Gabbro * Pumice * Basalt Metamorphic: * Slate * Phyllite * Gneiss * Mica schist * Marble * Quartzite * Granulite Sedimentary: * Limestone * Sandstone * Shale * Chert * Mudstone * Chalk
Shale changes into slate through a process called metamorphism, which involves heat, pressure, and chemical changes. The heat and pressure cause the minerals in the shale to recrystallize into a denser, more compact form, resulting in the fine-grained texture and foliation characteristic of slate. The composition of the original shale, as well as the intensity and duration of the metamorphic conditions, influence the final characteristics of the slate.
Another name for shale is mudstone
Schist typically begins as a metamorphic rock called shale, which is composed of clay and other fine-grained sedimentary minerals. Through the process of metamorphism, intense heat and pressure cause the minerals in the shale to recrystallize, forming the distinct foliated structure and mineral composition that characterize schist.
Compaction
D Shale
mudstone
Slate
obsidian
Shale turns into slate, granite into gneiss.
Granite is the rock with the highest tenacity, and therefore the most difficult to sculpt. There are problems with the others, for a variety of reasons. Shale is fissile, and will split into thin sheets. Obsidian is glassy, and will be prone to fracture. Slate is prone to splitting along foliation lines, but would be the easiest to sculpt mechanically.
Sandstone, limestone, and shale are examples of sedimentary rocks. Granite, basalt, and obsidian are examples of igneous rocks.
Igneous: * Obsidian * Granite * Diorite * Gabbro * Pumice * Basalt Metamorphic: * Slate * Phyllite * Gneiss * Mica schist * Marble * Quartzite * Granulite Sedimentary: * Limestone * Sandstone * Shale * Chert * Mudstone * Chalk
Shale changes into slate through a process called metamorphism, which involves heat, pressure, and chemical changes. The heat and pressure cause the minerals in the shale to recrystallize into a denser, more compact form, resulting in the fine-grained texture and foliation characteristic of slate. The composition of the original shale, as well as the intensity and duration of the metamorphic conditions, influence the final characteristics of the slate.
Shale is a noun.
No. Obsidian is brittle.