Passive continental margins are not tectonically active, meaning there is no significant seismic activity or mountain-building processes occurring there. They are typically characterized by a wide continental shelf and a gentle slope leading to the ocean basin. Sediment accumulation is common along passive continental margins due to lower energy conditions compared to active margins.
No, active continental margins typically do not have a continental rise. Instead, they often have a steep continental slope that descends into a deep oceanic trench due to tectonic activity. Continental rises are found at passive continental margins where there is minimal tectonic activity.
Intraplate coastlines or passive margins are continental coastlines that occur within the interior of a tectonic plate, away from active plate boundaries. These areas are characterized by lower tectonic activity and less frequent geological events compared to coastlines near plate boundaries.
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.
they generally have a deep trench.
Passive continental margins are not areas of convergence. There is little volcanic and earthquake activity on passive margins. Active margins are areas of convergence where one plate is descending beneath another. They are associated with volcanic and earthquake activity.
they have a continental rise
passive margins
Earthquakes and volcanic activity are typically found at active margins but not at passive margins. Active margins are characterized by tectonic plate interactions that can lead to these types of geological events.
Both active and passive margins are found at the edges of continents. Active margins are associated with tectonic activity and are typically marked by earthquakes, volcanoes, and mountain building, while passive margins are geologically stable and characterized by broad continental shelves and sediment deposition.
they have a continetal rise (
Passive continental margins are not areas of convergence. There is little volcanic and earthquake activity on passive margins. Active margins are areas of convergence where one plate is descending beneath another. They are associated with volcanic and earthquake activity.
Subduction. A subduction trench.
Passive continental margins are not tectonically active, meaning there is no significant seismic activity or mountain-building processes occurring there. They are typically characterized by a wide continental shelf and a gentle slope leading to the ocean basin. Sediment accumulation is common along passive continental margins due to lower energy conditions compared to active margins.
A continental rise.
Broad sediment-covered continental shelves are typically found in passive margins where there is a lack of tectonic activity and the crust is stable. Active margins, on the other hand, are associated with tectonic activity like subduction zones or rift zones, which can result in narrower shelves due to more abrupt changes in the seafloor elevation.
Sierd Cloetingh has written: 'Evolution of passive continental margins and initiation of subduction zones' -- subject(s): Plate tectonics, Continental margins