Can plate tectonics explain the differences in these beaches?
Plate tectonics explains why some beaches have lots of cliffs and some do not. A beach with lots of cliffs is near a plate boundary. A gentle beach is not. There are exceptions to this rule, but it works in some cases.
Think of a continent, like North America. Surrounding the continent are continental margins . Continental crust grades into oceanic crust at continental margins. Continental margins are under water. Almost all of North America sits on the North American Plate ( Figure below ). Both sides of the continent have continental margins, but each is very different. One continental margin of North America is an active margin. The other is a passive margin. Can you guess which is which?
The North American plate and the plates that surround it.
If a continental margin is near a plate boundary, it is an active margin . The continental margin of western North America is near a set of plate boundaries. There are convergent boundaries, like where there is subduction off of the Pacific Northwest. There is a transform boundary, the San Andreas Fault. The small amount of the North American continent that is not on the North American Plate is across the San Andreas Fault. It is on the Pacific Plate. Western North America has a lot of volcanoes and earthquakes. Mountains line the region. California, with its volcanoes and earthquakes, is an important part of this active margin ( Figure below ).
Big Sur, in central California, has beautiful cliff-lined beaches.
There are no volcanoes and very few earthquakes on the eastern edge of North America. The continental margin is a smooth transition from continental to oceanic lithosphere. The continental margin there becomes oceanic lithosphere, but both are on the North American Plate. There is no plate boundary. The far eastern edge of the North American Plate is the mid-Atlantic Ridge. The portion of a plate that does not meet another plate has no geological activity. It is called a passive margin ( Figure below ).
The eastern U.S. is a passive margin. Daytona Beach in Florida is flat and sandy, typical of a passive margin.
- active margin : Part of a plate that has a lot of geological activity; this is because this part of the plate meets another plate.
- continental margin : Outer edge of a continent where it transitions to oceanic lithosphere; the continental margin is under water.
- passive margin : Part of a plate that has no geological activity; this part of the plate is not meeting with another plate.
- Continental margins can be active or passive depending on whether they are near a plate boundary.
- Volcanoes and earthquakes are common at active margins. Active margins are near plate boundaries.
- Passive margins are passive. They have little or no geological activity.
Use the resource below to answer the questions that follow.
- Features of the Continental Margins at
- What is the continental shelf?
- What does the continental shelf contain?
- What is the continental slope?
- What is the continental margin?
- What is the continental rise?
- Describe the continental margin of Western North America.
- Describe the continental margin of Eastern North America.
- Why are there mountain ranges at passive margins?