Active continental margins are characterized by tectonic activity, such as subduction zones and volcanic arcs. They often have steep topography with deep oceanic trenches and high mountain ranges. Additionally, they may experience frequent earthquakes and have a narrower continental shelf compared to passive margins.
On an active continental margin, you would be likely to find an active ocean trench. This structure would generally not occur at a passive continental margin.
No, the continental margin of Fort Myers is not considered an active continental margin. Active continental margins are typically associated with tectonic activity, such as subduction zones or plate boundaries, which are not present in the area surrounding Fort Myers.
No. There is no such thing as a passive plate edge. They are near a passive continental margin.
continental slope
Submarine canyons are typically found on continental margins, where they cut through the continental slope and descend towards the abyssal plain. They are commonly associated with tectonically active regions or areas with high sediment input from rivers or glaciers.
On a passive continental margin, you can find thick sedimentary layers, wide continental shelves, and less seismic activity compared to an active continental margin.
On an active continental margin, you would be likely to find an active ocean trench. This structure would generally not occur at a passive continental margin.
No, the continental margin of Fort Myers is not considered an active continental margin. Active continental margins are typically associated with tectonic activity, such as subduction zones or plate boundaries, which are not present in the area surrounding Fort Myers.
Passive continental margin.
Subduction. A subduction trench.
An active continental margin may have a trench.
Subduction. A subduction trench.
Subduction. A subduction trench.
active continental margin
active continental margin
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.
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.