At divergent boundary, there is a mid ocean ridge where the most recent material is still slightly lighter then the chilled product. This slight elevation soon disappears as the plates move away from the boundary.
A convergent plate boundary occurs between the Nazca Plate and the South American Plate. The Nazca Plate is subducting beneath the South American Plate, leading to the formation of the Andes mountain range.
Mid-Atlantic Trench
The East Pacific Rise is a divergent plate boundary where tectonic plates are moving apart. This boundary is associated with seafloor spreading and the creation of new oceanic crust.
...at constructive plate margins / boundaries.hence the term contructive, new crust is "contructed" here.(and destructed at a destructive plate margin / boundary / subduction zone.)
A consecutive plate boundary is a boundary where two or more tectonic plates interact one after another. This can lead to a series of different tectonic processes such as subduction, transform faulting, and spreading. An example of a consecutive plate boundary is the boundary between the Pacific Plate, North American Plate, and Juan de Fuca Plate in the western United States.
a divergent plate boundary.
These ridges are spreading centers or divergent plate boundaries
Sea-Floor Spreading is your answer.
Divergent boundaries is the other name for a spreading plate boundary.
Yes it is. It is home to the Mid-Atlantic ridge, a divergent plate boundary, where new crust (sea floor) is created. by your mom
Oceanic Plate
A subduction zone occurs at convergent plate margins where an oceanic plate is going underneath a continental plate or a less dense oceanic plate. A mid-ocean ridge is a divergent plate boundary on the ocean floor with a mountain range and a rift running through the center of it. Sea floor spreading also occurs at mid ocean ridges.
Divergent Plate Boundary. (Seafloor Spreading).
The mid-ocean ridge system is the longest continuous divergent plate boundary on Earth.
The Super Continent was broken apart, in part by sea-floor spreading.Scientists discovered that sea-floor spreading continues to move the continents.Sea-floor spreading can be measured using specialized equipment.
Divergent boundary occurs in the new ocean floor where tectonic plates move away from each other, allowing magma to rise up and form new crust. This process is known as seafloor spreading and leads to the creation of mid-ocean ridges.
Seafloor spreading occurs at the boundary between two tectonic plates. As the plates divide, magma comes up through the crack and cools to form new sea floor. The farther away the floor is from the boundary, the older it is.