the plates crash over each other.
scientists believe that the volcano and earthquakes activity in this area are due to the formation of new part of the Earth's crust along the ridge
From on top of us: Troposphere, Stratosphere, Mesosphere, Thermosphere, Exosphere.
There are a number of causes of graphical issues in Google Earth. In some cases you just need to clear your local cache and restart Google Earth. Another workaround to switch from DirectX to OpenGL Mode (or vice versa) and/or try running in safe mode. You may have to reinstall Google Earth or get the latest version.
An alto cleft looks like this: The middle of the staff (or the middle of the cleft) is middle c.
Nashville is in the middle of Tennessee.
me dont no, me too stupid
felsic
That's because in NZ there are geysers which erupt hot water which weaken the ground and causes the plates to shift, there are only geysers because the magma under the earth heats up the water, and you need a volcano to have a geyser
Hawaiian Islands were formed in the middle of the Pacific Plate from volcanic activity over a hotspot.
Intraplate volcanic activity. These areas are often associated with mantle plumes that create hotspots of magma well away from tectonic plate boundaries, leading to the formation of volcanic features such as volcanic islands or seamounts. One well-known example is the Hawaiian Islands.
The mantle hot spot is located beneath the Earth's lithosphere, usually at the boundary between the mantle and the core. Hot spots are areas where magma from the mantle rises and generates volcanic activity on the Earth's surface. Examples of hot spots include Hawaii and Yellowstone.
magma
Yes, there is volcanic activity in the Pacific Ocean. Most of it occurs near the edges of the Pacific, in a region called the Ring of Fire. These volcanoes are responsible for the formation of Indonesia, Japan, and the Aleutians Islands, to name a few. There are also volcanoes closer to the middle of the Pacific plate, which formed islands such as those of the South Pacific and Hawaii.
An earthquake in the middle of the ocean primarily affects the lithosphere (earth's outer layer) by triggering the movement of tectonic plates and possibly causing tsunamis. It can also impact the hydrosphere as waves propagate outwards, potentially affecting marine life and coastal areas. The atmosphere may be influenced if the quake is powerful enough to generate volcanic activity or release gases into the air.
The Hawaiian islands are not the result of plate techtonics, they are the result of volcanic activity relating to a particular hot spot in the Earth's mantle, from which a plume of hot magma rises upward and causes volcanic eruptions.
Volcanic eruptions are caused by the buildup of magma (molten rock) beneath the Earth's crust. As pressure builds within the magma chamber, it can lead to fractures in the crust, allowing the magma to escape to the surface in the form of an eruption. Other factors such as the composition of the magma, presence of gases, and tectonic activity can also influence the likelihood and intensity of a volcanic eruption.
These are called hotspots, where magma from deep within the Earth rises and creates volcanic activity at the surface. Hotspots can occur in the middle of a tectonic plate, leading to the formation of volcanic island chains like Hawaii.