Want this question answered?
At divergent boundaries, land features associated with orogenesis include rift valleys and mid-ocean ridges. These features form as tectonic plates move apart, causing the crust to stretch and fracture, leading to the creation of new crust and landforms.
Mid-ocean ridges are associated with volcanic activity, earthquakes, and the creation of new oceanic crust through seafloor spreading. These features form where tectonic plates move apart and magma rises to the surface, creating underwater mountain ranges.
Mid-ocean ridges, such as the Mid-Atlantic Ridge and East Pacific Rise, are associated with divergent plate boundaries. These underwater mountain ranges form as tectonic plates move apart, allowing magma to rise and create new oceanic crust.
mountainous topography
Faults, graben and mid oceanic ridges.
At divergent boundaries, land features associated with orogenesis include rift valleys and mid-ocean ridges. These features form as tectonic plates move apart, causing the crust to stretch and fracture, leading to the creation of new crust and landforms.
Mendocino, Molokai, and Galapagos are names of fracture zones in the ocean floor, where tectonic plates are moving away from each other. These fracture zones are characterized by a series of faults and ridges that form due to the movement of the Earth's tectonic plates. They play a significant role in shaping the geology and topography of the ocean floor.
Mid-ocean ridges are associated with seafloor spreading, where new oceanic crust is created as tectonic plates pull apart. This process allows magma to rise from beneath the Earth's surface and solidify, forming new crust along the mid-ocean ridge. The presence of hydrothermal vents, volcanic activity, and earthquakes are also characteristics of mid-ocean ridges.
Definition: Fine ridges on a fracture surface, parallel to the direction of propagation of the fracture. source: About.com
Mid-ocean ridges are associated with volcanic activity, earthquakes, and the creation of new oceanic crust through seafloor spreading. These features form where tectonic plates move apart and magma rises to the surface, creating underwater mountain ranges.
True. Mid-ocean ridges are underwater mountain ranges that form at the boundaries of tectonic plates where new oceanic crust is created through seafloor spreading.
The main boundary associated with mid-ocean ridges are divergent boundaries, because the plates move away from eachother, or "diverge".
divergent
Mid-ocean ridges, such as the Mid-Atlantic Ridge and East Pacific Rise, are associated with divergent plate boundaries. These underwater mountain ranges form as tectonic plates move apart, allowing magma to rise and create new oceanic crust.
Basalt rocks are commonly associated with ocean ridges due to the process of seafloor spreading where magma rises to the surface, cools, and solidifies. These basaltic rocks form the oceanic crust along the ridges.
fracture zones
Yes, mid-ocean ridges are elevated areas on the ocean floor where tectonic plates spread apart, creating new oceanic crust. These ridges can indeed be considered underwater mountain ranges due to their topographic relief and the volcanic activity associated with them.