The igneous rock underlying the deep ocean basins is basaltic, as its source material comes from the asthenosphere. Andesitic igneous rock is formed at colliding plate margins, where subducting oceanic crust is partially melted and undergoes differentiation as it rises through the continental crust. Granitic rock is less dense than oceanic crust and composes the continents.
No. Many plate boundaries are on the seafloor far from continents and several are well within continents.
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.
1.westerlies tande currents ke upar se bahte hah aur apna moisture koh dehti haa jab vah western margins par pahunchti haa toh wo dry hoti haa aur koi rain nahi karti. 2.due to cooling efeects of cold currents.
The three main regions of the ocean floor are the continental margins, the ocean basins, and the mid-ocean ridges. Continental margins are the shallow, submerged edges of continents. Ocean basins are the deeper areas of the ocean floor beyond the continental margins. Mid-ocean ridges are underwater mountain ranges where tectonic plates move apart and magma rises to create new oceanic crust.
Yes, earthquakes can occur at constructive margins where tectonic plates are moving apart. As the plates separate, tension builds up in the crust which can lead to faults slipping and causing earthquakes. However, earthquakes at constructive margins tend to be less frequent and less intense compared to those at other types of plate boundaries.
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.
No. Many plate boundaries are on the seafloor far from continents and several are well within continents.
The true edges of continents are known as continental margins, which consist of the continental shelf, continental slope, and continental rise. These margins mark the transition from the continent to the ocean basin and can extend hundreds of kilometers from the shoreline.
Andesitic magma is commonly found in subduction zones where oceanic crust is being forced beneath continental crust. These environments are typically associated with volcanic arcs and stratovolcanoes. Examples of where andesitic magma is found include the Andes Mountains in South America and the Cascades in the western United States.
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.
No. Not all plate boundaries are at the edges of continents, nor do all edges of continents correspond with plate boundaries. Many plate boundaries are found in the middle of oceans, while the continent of Africa is being torn apart by a developing plate boundary. Some edges of continents, such as the west coast of South America are near plate boundaries. These are called active continental margins. Others, such as the east coast of North America, are nowhere near plate boundaries. These are called passive continental margins.
No. Not all plate boundaries are at the edges of continents, nor do all edges of continents correspond with plate boundaries. Many plate boundaries are found in the middle of oceans, while the continent of Africa is being torn apart by a developing plate boundary. Some edges of continents, such as the west coast of South America are near plate boundaries. These are called active continental margins. Others, such as the east coast of North America, are nowhere near plate boundaries. These are called passive continental margins.
No. Not all plate boundaries are at the edges of continents, nor do all edges of continents correspond with plate boundaries. Many plate boundaries are found in the middle of oceans, while the continent of Africa is being torn apart by a developing plate boundary. Some edges of continents, such as the west coast of South America are near plate boundaries. These are called active continental margins. Others, such as the east coast of North America, are nowhere near plate boundaries. These are called passive continental margins.
Paper cutouts of the continents can be pieced together to form a single whole is because the continents were at one point all connected, which was the super continent Pangaea.
The basaltic oceanic crust is more dense than the granitic continental crust. Therefore, when the two meet at plate margins, the oceanic crust usually subducts beneath the continental plate.
because the places there are more warm. if it was for instance England then it would be all wet
It is so because the westerlies(a kind of permanent or planetary wind) loses its moisture while it reaches the western margins of the world so it is not able to shed rains in that particular region.