The edges are where the plate boundaries (usually) meet.
Yes, earthquakes can occur in the middle of continents. These are known as intraplate earthquakes and can be caused by geological faults or weaknesses within the continental crust. While less common than earthquakes along plate boundaries, intraplate earthquakes can still occur in areas far from tectonic plate boundaries.
I suppose this could be Australia, but it is near New Guinea which has had several earthquakes in the past few decades. Another option is Greenland or Antarctica (yes I'm aware that Greenland isn't a continent). Antarctica has a volcano or two but no earthquakes. While Greenland has no earthquakes and (as far as I know) no volcanoes.
Some countries lie on the border of continents. some continents grind against each other, thus causing earthquakes, so of course, you couldn't have earthquakes in the middle of a continent! hope this was a help! x there are all different types of stressed areas were rocks are being pulled apart and compressed or scraped against each other it all depends upon the geologic setting. There are fault lines everywhere that could be from current stress environment or from prehistoric stress environments there are also isostatic compensations that can cause stresses and incite rupturing. Earthquakes can happen anywhere that these stresses build up although they are usually interplate earthquakes, intraplate earthquakes are not uncommon. For instance New Madrid Missouri is in the center of the laurentia plate however high magnitude earthquakes are common. The New Madrid seismic zone is underlain by the reel-foot rift a failed rifting zone that causes increased seismicity in that area.
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.
There are many proofs and they are as convincing as they are. That is the style of Alfred Wegener. Although he always provided good, reliable and convincing evidences, he was not a good speaker. A few might be that the fossils of the same species of dinosaurs were found on different continents, which are separated by seas and oceans. No dinosaur could have swam that far. Therefore, he concluded that there was once a where all of the current continents are joined together. There must be some force that caused the continents to move apart. Therefore, he came up with the idea that plate tectonics that were located under Earth's surface (lithosphere), which were moving, and brought the continents along with it. Another evidence is the existence of mountains, volcanoes, earthquakes, canyons, tsunamis and other landforms and landscapes. These could not have been formed without plate tectonics.
edges
Volcanoes and earthquakes are typically located along the edges of tectonic plates, where the Earth's crust is more active. These areas include plate boundaries such as subduction zones, transform faults, and spreading centers. While it is less common, volcanic activity can also occur within continents, often associated with hotspots or rift zones.
Earthquakes hardly ever happen in the middle of plates because the is no fault-line to move. The most common earthquakes in the middle of plates are because of Volcanoes.
There are faultlines along the bottom of the Levant coastline, the Red Sea, and the Olduvai Gorge. Earthquakes happen in those areas. There are no significant volcanoes in the Middle East or Africa.
Yes, earthquakes can occur in the middle of continents. These are known as intraplate earthquakes and can be caused by geological faults or weaknesses within the continental crust. While less common than earthquakes along plate boundaries, intraplate earthquakes can still occur in areas far from tectonic plate boundaries.
There're a lot of volcanoes in Antarctica and the "Ring of Fire", most volcanoes are at the "Ring of Fire" since the Ring of Fire is just like a ring and it's not all connected together. The middle of the tectonic plates may have earthquakes, volcanoes... Like if you live in Japen, there're a lot of volcanoes in Japen and since it's close to the Ring of Fire, it may have earthquakes. If you live in somewhere around Texas, there will never have an earthquake or have a volcano in Texas since Texas is very far away from the tectonic plate, and the volcanoes are mostly in California.
Volcanoes are not usually found in the interior of tectonic plates, such as in the middle of continents like in the interior of Australia. These areas are called intraplate regions and typically have less tectonic activity compared to plate boundaries where volcanoes are commonly found.
Volcanoes occur along the plates of the Earth. Volcanoes can remain dormant, active, or in inactive states. Active volcanoes occur in particular regions of the world due to the movement of the plates in the Earth.
Japan has earthquakes, tsunami's, volcanoes, snow avalanches and many other hazards.
No only middle and big magnitude earthquakes do.
The Middle East is typically considered to be part of three continents: Asia, Europe, and Africa. These continents converge at the Middle East due to its geographical location connecting the three landmasses.
Plains