The magma forms sills and magma chambers.
A fault forms when rock layers slip or slide along a crack. This movement can create an earthquake if the stress becomes too great for the rocks to hold their position.
Lava does not follow the law of superposition. The law of superposition applies to sedimentary rock layers, where older layers are typically found below younger layers due to the principle of original horizontality. Lava flows do not adhere to this principle as they can be deposited on top of existing layers regardless of their age.
The three primary forms of subaerial volcanoes are stratovolcanoes, shield volcanoes, and cinder cone volcanoes. Stratovolcanoes are characterized by alternating layers of tephra and solidified lava due to their explosive eruptions and lava flows. Shield volcanoes have gentle slopes formed from successive lava flows with occasional tephra layers. Cinder cone volcanoes are small, steep-sided volcanoes made up almost entirely of tephra fragments from explosive eruptions.
Yes, that's correct. Sills are igneous rock formations that form when magma is intruded horizontally between rock layers and then solidifies underground. If the magma solidifies vertically underneath the surface, it will create a sill structure.
A dike is formed when magma intrudes and solidifies in a vertical or near-vertical orientation within pre-existing rock layers. Lava flows, on the other hand, occur when magma erupts onto the surface and flows horizontally along the ground.
The magma forms sills and magma chambers.
A surface current is a wind-powered current that moves water along horizontally. Because the wind is on the surface, a surface current only forms along the first few hundred feet of ocean water.
When magma flows horizontally, it can form igneous rock formations called dikes or sills. Dikes are vertical intrusions, while sills are horizontal intrusions. These structures are formed when magma solidifies within preexisting rock layers.
A fault forms when rock layers slip or slide along a crack. This movement can create an earthquake if the stress becomes too great for the rocks to hold their position.
When lava flows horizontally across a layer of rock, it can form a flat, expansive volcanic plateau known as a lava plateau or lava plain. This occurs when the lava spreads out and solidifies over a large area, creating a relatively flat surface with a thick layer of cooled lava.
AA lava flows look like broken glass and make you say "Ow Ow" when you walk across it barefoot.Pahoehoe lava flows look like pillows.
Lava forms island, land, & shiny rocks
When a river flows into a lake or ocean, the sediments that the river carries settle to the bottom. Layers of sediment may covor the dead organism.
A sill is a horizontal intrusive igneous body that forms between sedimentary rock layers. Sills are formed when magma intrudes parallel to the layering of the surrounding rocks and solidifies underground.
Lava does not follow the law of superposition. The law of superposition applies to sedimentary rock layers, where older layers are typically found below younger layers due to the principle of original horizontality. Lava flows do not adhere to this principle as they can be deposited on top of existing layers regardless of their age.
The three primary forms of subaerial volcanoes are stratovolcanoes, shield volcanoes, and cinder cone volcanoes. Stratovolcanoes are characterized by alternating layers of tephra and solidified lava due to their explosive eruptions and lava flows. Shield volcanoes have gentle slopes formed from successive lava flows with occasional tephra layers. Cinder cone volcanoes are small, steep-sided volcanoes made up almost entirely of tephra fragments from explosive eruptions.