The tectonic plates move at about the same speed your finger nails grow. The gap the plates create when they move apart is constantly being closed up by magma moving up from the mantle.
Tectonic plates move at a rate of approximately 1 to 10 centimeters per year on average. This movement can cause earthquakes, volcanic activity, and the formation of mountain ranges as the plates interact with each other.
the average speed of a tectonic plate is 2-5 cm per year. the average of 3.5 cm / yr x 200 mil years= 700 million centimeters (7 million meters or 7,000 km)
Well, if the plates drift 5-10 cm per year, that means the plates would've shifted about 5-10 km which isn't a massive change, to be honest. The big changes would only be seen after millions of years.
When Earth's plates spread apart, it creates a divergent boundary where new oceanic crust is formed as magma rises from the mantle and solidifies. This process leads to the creation of features like mid-ocean ridges and rift valleys.
An active continental margin will have tectonic activity like earthquakes and volcanic eruptions due to the collision of tectonic plates. In contrast, a passive margin generally does not have such tectonic activity because it is far from plate boundaries and lacks the forces that drive tectonic movements.
the tectonic platesthe tectonic plates can be move to be far and near to each other
Continental drift is influenced by tectonic plate movement. Over 200 million years, the continents may continue to drift apart as tectonic plates move at a rate of a few centimeters per year.Exact distances are difficult to predict due to uncertainties in plate movement and geological processes.
When the plates move apart they will more than likley create a large creak, Depending on how far they move apart. It would be a small creek.
As far as I know the result is an earthquake.
As the tectonic plates “stretched” the crust, the valley’s basin continuously slipped downwards. This process is far from over, as where tectonic plates move, so is Death Valley gains in size.
The movement of tectonic plates, which make up the Earth's outer shell, caused the continents to drift apart over millions of years in a process called continental drift. This movement is driven by forces in the Earth's mantle, leading to the current positions of the continents.
Earthquakes are less likely to occur at the center of tectonic plates because these regions are generally characterized by stable, older crust that experiences less stress compared to plate boundaries. Most seismic activity is concentrated at the edges of plates, where tectonic forces cause them to interact, either colliding, sliding past each other, or pulling apart. The center of plates lacks the significant geological activity and fault lines that typically generate earthquakes. Thus, while earthquakes can technically occur anywhere, they are far less frequent in the central regions of tectonic plates.
The state of matter in which molecules are generally far apart and moving randomly is known as the gaseous state. Steam is an example of a gas.
Tectonic plates move at a rate of approximately 1 to 10 centimeters per year on average. This movement can cause earthquakes, volcanic activity, and the formation of mountain ranges as the plates interact with each other.
the average speed of a tectonic plate is 2-5 cm per year. the average of 3.5 cm / yr x 200 mil years= 700 million centimeters (7 million meters or 7,000 km)
That's my answer
Earthquake normally happen at or near the boundaries of tectonic plates. Particularly those where two plates are sliding past each other (a transform boundary) or are colliding (a convergent boundary). They can also occur away from the boundaries of tectonic plates but these tend to be far rarer and of much smaller magnitude.