P-waves travel at speeds between 5 to 8 km/s, as such a P-wave may take between 812 and 1300 seconds (13 and 22 minutes respectively) to travel 6500 km.
Please see the related question on P-wave velocity.
Epicentre.
There are two types of seismic body waves that travel through the earth when an earthquake occurs. P-waves and S-waves. When an earthquake occurs it has been observed that there is a zone at the opposite side of the earth where P-waves are detected but S-waves are not. S-waves are not able to travel through liquids where as P-waves can and as such it is believed that the shadow zone is caused by the presence of a liquid outer core.
arrival time-travel time
Earthquake generated waves are called seismic waves. These are waves of energy that travel through the Earth's layers. Their velocity depends on the elasticity and density of the medium that they travel through.
hg
Epicentre.
1737 miles, 2795 kilometers
P-waves travel at speeds between 5 to 8 km/s, as such a P-wave may take between 812 and 1300 seconds (13 and 22 minutes respectively) to travel 6500 km. Please see the related question on P-wave velocity.
Approximately 300,000 Km/s
420 km/(79 km/h) = 5.3165 h = 5 h 19 minutes (approximately)
P-waves travel between 5-8 km/s. As such the epicentre could be anywhere between 1200 and 1920 km away.
To travel from Bendigo, Victoria, Australia to Melbourne, Victoria, Australia is about 152 kilometers. It will take approximately one hour and forty five minutes to travel.
Approximately 291 kilometers, with an estimated travel time of 3 hours, 15 minutes.
earthquake waves travel through the earths crust.
Approximately 66.4 hours
Earthquake P-waves don't travel in straight lines, they travel in like a circle after the earthquake has struck. These P-waves arrive first during an earthquake.
Approximately 24 thousand light years or 2.27E17 kilometers (227,000,000,000,000,000 kilometers).