there is no core on Venus causing there to be no earthquakes on Venus
There is not accurate data that gives precise, but it is estimated that there are hundreds of thousands of earthquakes happening per second. Almost all of this earthquakes are classified as Mini-Earthquakes and are usually unnoticable.
what country did the zero symbol originate from?
Geometry did not originate in India.
Even though you probably don't realize that there are over 100 earthquakes a week around the globe, Earthquakes can vary from small to big. Simply meaning, locations closer to the equator line are affected with larger and much more disastorous Earthquakes. So depending where you live, you wont be able to feel earthquakes, without some kind of crazy science stuff
Convergent
tsunami
It is unpredictable, however statistics show that a tsunami as result is incredibly unlikely.
Tidal waves originate deep within the ocean and end once they reach the coast. They are typically caused by large earthquakes which send shock waves outward from the epicenter.
The Hypocenter
Earthquakes are internal forces of change caused by tectonic plate movement and stress release along faults within the Earth's crust. They are not considered external forces as they originate from within the Earth.
Shallow-focus earthquakes cause more damage than deep-focus earthquakes. This is because shallow-focus earthquakes originate closer to the Earth's surface, which allows the energy to be more concentrated and lead to stronger shaking and more destruction of structures. Deep-focus earthquakes, occurring deeper underground, tend to have their energy dissipate before reaching the surface.
Earthquakes at convergent boundaries occur at greater depths because of the intense pressure from the overriding tectonic plates, which drives the descending plate deeper into the mantle where it eventually triggers seismic activity. In contrast, earthquakes at divergent boundaries are generally shallower due to the tensional forces pulling the plates apart, causing them to fracture closer to the surface.
Earthquakes are most likely to originate along tectonic plate boundaries, where the movement and interaction of plates create stress that is eventually released as an earthquake. The most seismically active areas include the Pacific Ring of Fire, which encircles the Pacific Ocean, and the boundaries of the Eurasian, North American, South American, African, Indian, Australian, and Antarctic plates.
Earthquakes are most likely to originate at tectonic plate boundaries, where the Earth's plates interact. This is because the movement of these plates can create stress and pressure that eventually leads to the release of energy in the form of an earthquake. Some of the most seismically active regions in the world are the Ring of Fire around the Pacific Ocean and the Himalayan region.
asthenosphere.
Most destructive waves, such as tsunamis, originate from underwater seismic activity, like earthquakes, volcanic eruptions, or landslides. When these events displace a large volume of water, it sets off a series of powerful waves that can travel great distances across the ocean.