The Eltanin and Romanche fracture zones are oceanic transform faults. These types of faults occur at the boundary between two tectonic plates where they slide past each other horizontally. The movement along these faults can cause earthquakes and contribute to the overall plate tectonics process
A volcanic archipelago in the Pacific Ocean
A fracture zone is a group of "cracks" in the ocean floor that cut across a rift. For example, if you look at a picture of the Mid-Atlantic Ridge, you'll see that there are hundreds of smaller fractures in the earth's crust that cut across the ridge. There's a great picture of the Mid-Atlantic Fracture Zone at the link below.
A fracture zone formed when a layer of rock breaks is commonly referred to as a "fault." Faults occur when stress on the rocks exceeds their strength, causing them to fracture and displace. These geological features can lead to earthquakes and are classified into various types based on their movement, such as normal, reverse, and strike-slip faults.
a zone where volcanic activity or earthquake etc. is happening
A fracture zone formed when a layer of rock breaks under strain and moves is called a "fault." Faults are characterized by the displacement of rock on either side of the fracture, which can occur due to tectonic forces. There are various types of faults, including normal, reverse, and strike-slip faults, each defined by the direction of movement.
A place where something bad or violent is happening is typically known as a "danger zone" or a "troubled area."
No. The Mariana Trench is the deepest trench in the world. It is located in the Pacific Ocean.
At a fracture or fault zone, movements of the Earth's crust can occur, leading to earthquakes or seismic activity. These zones can also act as pathways for the movement of fluids such as water or hydrocarbons. Additionally, fault zones can influence the topography of the landscape by creating valleys, mountains, or other geological features.
The Eltanin Transform Fault and Fracture Zone is a series of six or seven dextral transform faults along ~800 km of the Pacific-Antarctic Ridge that offset it ~1600 km. The zone is in the South Pacific, southwest of Easter Island, between 56° S, 145° W and 54.5° S, 118.5° W.
The zone of fracture experiences tension hen the glacier moves over irregular terrain. This tension results in gaping cracks called crevasses. Crevasses can be 50 meters deep. They are often hidden by snow and make travel across glaciers dangerous.
Yes.