This is a hard question to answer, as the depth of a focus depends upon the type of fault or formation that is being discussed. North America has a range of these, so it varies greatly across the continent.
The Mexico City 1985 earthquake occurred due to friction between the Cocos and North American tectonic plates. Specifically, on the southern coast of Mexico, at a depth of 15 kilometers below the sea level. (Coordinates: 18.42, -102.38)
The top of the mantle is defined by a sudden increase in seismic velocity, which was first noted by Andrija Mohorovičić in 1909; this boundary is now referred to as the "Mohorovicic discontinuity" or "Moho". Its depth ranges from about 5 km beneath the ocean floor to about 35 km below the continent, although it may reach 60 km or more under some mountain ranges.
For Lincoln County, Wyoming, in particular the Bedford area, Recommended foundation depth is 36 inches. Recommended Snow load, live, roof, is 80 lbs per sq. ft., ground is 90 lbs per sq. ft. Seismic Zone is D2. Window Exposure 3 sec. Max Wind mph is 85 B. Nathan Harding
The depth? That must be the length inside: 60 meters.
false, the temperature increases with depth
220 km
North America because i said so!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! North America because i said so!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!
Generally increase with depth, occasionally making abrupt jumps termed seismic-velocity discontinuities.
L waves
A large crack in the ground made by a river or series of earthquakes is known as a fissure. Fissures can range in size and depth depending on the force and duration of the geological activity that caused them. They can be found in various landscapes, including along riverbanks or in regions prone to seismic activity.
The results of the Loch Ness Bathymetric and Seismic Survey in 1991 found the maximum depth to be 745ft (226.96m). It was recorded 1km south of Urquhart Castle.
When seismic waves hit a fault, the waves are reflected off the fault.Seismograph can detect these reflected seismic waves.Geologists then use these data to map the fault's length and depth.
When seismic waves hit a fault, the waves are reflected off the fault.Seismograph can detect these reflected seismic waves.Geologists then use these data to map the fault's length and depth.
When seismic waves hit a fault, the waves are reflected off the fault.Seismograph can detect these reflected seismic waves.Geologists then use these data to map the fault's length and depth.
Geologists use the data from the movements of seismic waves to determine earthquake risk for an area by analyzing the magnitude, location, and depth of the earthquake. They also study historical seismic activity in the region and compare it to current data to identify patterns and potential fault lines. This information helps geologists assess the likelihood and potential impact of future earthquakes in the area.
When seismic waves hit a fault, the waves are reflected off the fault.Seismograph can detect these reflected seismic waves.Geologists then use these data to map the fault's length and depth.
When seismic waves hit a fault, the waves are reflected off the fault.Seismograph can detect these reflected seismic waves.Geologists then use these data to map the fault's length and depth.