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, continents and plates are not the same. Continents are large land masses that form the Earth's surface, while tectonic plates are pieces of the Earth's lithosphere that move and interact with each other, causing geological phenomena like earthquakes and volcanic eruptions. Continents are located on top of tectonic plates and can be made up of one or more plates.
No, tectonic plates move in different directions. Some plates move towards each other (convergent boundaries), some move away from each other (divergent boundaries), and others slide past each other horizontally (transform boundaries).
the modern theory is that all the continents used to be connected (Pangaea). The evidence is that the coastal boundaries fit together like a puzzle piece. another example is that the same species of animals are found on the coasts of the continents that once were touching
Most earthquakes occur at the boundaries of tectonic plates. And i think Most earthquakes occur along the edge of the oceanicand continental plates. The earth's crust (the outer layer of the planet) is made up of several pieces, called plates. The plates under the oceans are called oceanic plates and the rest are continental plates. The plates are moved around by the motion of a deeper part of the earth (the mantle) that lies underneath the crust. These plates are always bumping into each other, pulling away from each other, or past each other. The plates usually move at about the same speed that your fingernails grow. Earthquakes usually occur where two plates are running into each other or sliding past each other. I think so.
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.
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. There can be multiple plates within one continent.
No, continents and plates are not the same. Continents are large land masses that form the Earth's surface, while tectonic plates are pieces of the Earth's lithosphere that move and interact with each other, causing geological phenomena like earthquakes and volcanic eruptions. Continents are located on top of tectonic plates and can be made up of one or more plates.
No, there are several more plates than continents (twelve I think) and the plates include both oceans and land. Earthquakes are the result of plates moving, but don't worry, plates do not move fast, only about a centimeter a year.
No, the sizes and shapes of the continents do not directly correspond to the sizes and shapes of tectonic plates. Tectonic plates are larger and different in shape compared to the continents they contain. Continental plates can span multiple tectonic plates and vice versa.
Convergent boundaries are boundaries where tectonic plates are moving together. Since the edges of both can't be in the same place, one plate will be forced under another plate (and the other above). The plate going 'down' will thus go deeper into the earth - allowing deeper earthquakes to occur.
Plates slide past each other at transform boundaries. These boundaries occur when two plates slide horizontally in opposite directions parallel to each other. The movement can be either in the same direction but at different speeds, or in opposite directions.
Tectonic Plates can't carry both ocean floor and continents on the same plate.