Convergent Boundaries.
The southeast Indian Ridge is a divergent plate boundary, where two tectonic plates are moving away from each other. This movement causes magma to rise from the mantle, creating new crust as the plates separate.
The Himalayas resulted from the collision of the Indian Plate into the European plate. The softer Indian Plate was forced underneath the harder European Plate, which caused the European Plate to rise up and form the Himalayas.
A convergent boundary between two continental plates causes both plates to crumple to form fold mountains e.g. the HimalayasA convergent boundary between a continental and an oceanic causes one to rise above the other. Granite is less dense than basalt, so the continental plate rises above the oceanic plate. This also forms mountains, like the Andes.
The eruption of Eyjafjallajökull in 2010 was caused by the movement of the Eurasian and North American tectonic plates along a divergent boundary in Iceland. This boundary, known as the Mid-Atlantic Ridge, allowed magma to rise to the surface and resulted in the volcanic eruption.
Mid-ocean ridges are caused by divergent plate boundaries, where tectonic plates move away from each other. This movement allows magma to rise to the surface, creating new crust and forming underwater mountain ranges.
The southeast Indian Ridge is a divergent plate boundary, where two tectonic plates are moving away from each other. This movement causes magma to rise from the mantle, creating new crust as the plates separate.
The Himalayas resulted from the collision of the Indian Plate into the European plate. The softer Indian Plate was forced underneath the harder European Plate, which caused the European Plate to rise up and form the Himalayas.
A convergent boundary between two continental plates causes both plates to crumple to form fold mountains e.g. the HimalayasA convergent boundary between a continental and an oceanic causes one to rise above the other. Granite is less dense than basalt, so the continental plate rises above the oceanic plate. This also forms mountains, like the Andes.
The eruption of Eyjafjallajökull in 2010 was caused by the movement of the Eurasian and North American tectonic plates along a divergent boundary in Iceland. This boundary, known as the Mid-Atlantic Ridge, allowed magma to rise to the surface and resulted in the volcanic eruption.
Yes. Generally that is where the tectonic plates are. Mountain and volcanoes are formed by tectonic plate movement, so yes they are 2 features that are most commonly found at plate boundaries. Fault Block Mountains(:
Mid-Atlantic Ridge and East Pacific Rise
Mid-ocean ridges are caused by divergent plate boundaries, where tectonic plates move away from each other. This movement allows magma to rise to the surface, creating new crust and forming underwater mountain ranges.
The force tension at a divergent plate boundary causes the two plates to move away from each other. As the plates separate, magma rises from the mantle to fill the gap, forming new crust. This process is known as seafloor spreading.
a constructive plate boundary is where two plates move apart from eachother forming a gap which allows magma to rise and that leads to a earthquake.
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.
The boundary between the Indo-Australian Plate and the Pacific Plate is mainly a divergent boundary in the region of the East Pacific Rise and a transform boundary along the Tonga Trench and the Alpine Fault in New Zealand. Additionally, there are some regions of convergence near New Zealand and the New Hebrides Trench.
At the western edge of the Nazca plate and the eastern edge of the Pacific plate lies the East Pacific Rise. The East Pacific Rice is known as a mid-ocean ridge, formed from a divergent boundary.