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Why do volcanoes occur at conservative plate margins?
after earth
What kind of volcanoes are found along continental margins?
Volcanoes found along continental margins are typically stratovolcanoes or composite volcanoes. These volcanoes are characterized by their steep-sided appearance due to alternating layers of lava flows, ash, and volcanic rocks. They are formed where tectonic plates converge and one plate is forced beneath the other in a process known as subduction.
Why earthquakes occur at conservative plate margins?
Because of the big grinding of the conservative plate margin cause the land to go back and forth
What processes can be observed at the margins of lithospheric plates?
At plate margins, processes such as subduction, where one plate is forced beneath another, occur. This can lead to the formation of deep ocean trenches. Additionally, plate margins can be locations of volcanic activity and earthquakes due to the movement and interaction of the plates.
What is the consistency of lava in the composite volcanoes?
Composite volcanoes are found on destructive plate margins , where the oceanic crust sinks beneath the continental crust. Composite volcanoes have the following characteristics: Acidic lava, which is very viscous (sticky). Steep sides as the lava doesn't flow very far before it solidifies
Why do volcanoes occur at conservative plate margins?
after earth
How Compare shield volcanoes and composite volcanoes?
Shield Volcanoes - Wide base found at constructive plate margins Composite Volcanoes - Steeper Sides found at Destructive (subduction) margins
Compare and contrast composite and shield volcanos?
Shield Volcanoes - Wide base found at constructive plate margins Composite Volcanoes - Steeper Sides found at Destructive (subduction) margins
What type of rock forms in volcanoes along the continental margins?
igneous rocks
What is the difference between collision and conservative margins?
collision is when two plates collide conservative is when two plates rub together
What kind of volcanoes are found along continental margins?
Volcanoes found along continental margins are typically stratovolcanoes or composite volcanoes. These volcanoes are characterized by their steep-sided appearance due to alternating layers of lava flows, ash, and volcanic rocks. They are formed where tectonic plates converge and one plate is forced beneath the other in a process known as subduction.
Why do earthquakes occur at conservative plate margins?
Because of the big grinding of the conservative plate margin cause the land to go back and forth
Why earthquakes occur at conservative plate margins?
Because of the big grinding of the conservative plate margin cause the land to go back and forth
What is something similar between active and passive margins continents?
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.
Where do more active volcuranos ocurr?
Active volcanoes are found on mainly plate margins, with the few examples of hot spots all over the place (e.g. Moana Loa on Hawaii). Volcanoes found at constructive plate margins are more effusive and erupt basaltic lava (e.g. Iceland) and volcanoes found NEAR destructive plate margins are explosive and erupt either andesitic or rhyolitic lava (e.g. Mount Saint Helens-however this volcano might not erupt for quite a while whereas the other two example erupt very frequently).
What is usually found at an active margin but NOT at a passive margin?
Active and passive margins describe the various characteristics of continental margins that are a result of plate tectonics. An active margin usually has numerous volcanoes and mountains, while a passive margin typically do not have these formations.
What processes can be observed at the margins of lithospheric plates?
At plate margins, processes such as subduction, where one plate is forced beneath another, occur. This can lead to the formation of deep ocean trenches. Additionally, plate margins can be locations of volcanic activity and earthquakes due to the movement and interaction of the plates.
