Yes, because the mountains are still being developed as the Indian Plate is colliding with the the Eruasian Plate.
No. There is no such thing as a passive plate edge. They are near a passive continental margin.
The continental margin is the submerged outer edge of a continent. It is generally divided into two sections: the continental shelf and the continental slope.
A passive continental margin lacks tectonic activity because it is not located near a plate boundary where volcanic and seismic activity typically occurs. Instead, passive margins form as plates pull apart, leading to subsidence and sediment accumulation rather than volcanic eruptions or earthquakes.
Far from the mid oceanic ridge, near the continental margin (oldest oceanic rock ages 200 mya)
Yes, fracture zones can be found on the ocean floor near continental margins. They are areas of intense tectonic activity where tectonic plates slide past each other, creating fractures in the Earth's crust. These zones are often associated with transform plate boundaries.
The U.S. east coast is not considered an active continental margin because there are no plate boundaries near it. Off the coast there is merely a slope with a transition from continental to oceanic crust.
A passive continental margin is not tectonically active, meaning it does not experience significant geological activity like earthquakes or volcanic eruptions. In contrast, an active continental margin is located near a tectonic plate boundary, leading to geological activity such as subduction zones, earthquakes, and volcanic eruptions.
A passive continental margin is characterized by a broad, gently sloping continental shelf and is typically associated with tectonically stable regions, where there is little to no seismic activity. In contrast, an active margin is located near tectonic plate boundaries and is marked by significant geological activity, including earthquakes and volcanic activity. Essentially, a passive margin has a well-defined continental shelf and a lack of tectonic activity, while an active margin does not.
No. There is no such thing as a passive plate edge. They are near a passive continental margin.
Himalayas: Continental-continental North American Cordillera: Terrane accretion Aleutian: Oceanic-oceanic Andes: Near an active continental margin _______________________________ Himalayas: Two continents colliding Grand Tetons: Plates spreading Aleutian: Two ocean plates colliding. Andes: Near a subduction zone
An active continental margin is characterized by tectonic activity, where an oceanic plate is subducting beneath a continental plate, leading to the formation of features such as deep-sea trenches, volcanic arcs, and earthquake zones. These margins are typically found along the edges of continents near tectonic plate boundaries, like the Pacific Ring of Fire. The geological processes at these margins often result in significant landform changes and can impact marine ecosystems. Examples include the coasts of California and Chile, where the interactions between tectonic plates are prominent.
The continental margin is the submerged outer edge of a continent. It is generally divided into two sections: the continental shelf and the continental slope.
A passive continental margin lacks tectonic activity because it is not located near a plate boundary where volcanic and seismic activity typically occurs. Instead, passive margins form as plates pull apart, leading to subsidence and sediment accumulation rather than volcanic eruptions or earthquakes.
Yes. Earthqyakes are common at active continental margins.
The Himalayas are a mountain range in Asia.
No.
The Himalayas are near India