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∙ 14y agoField is square ===> full perimeter travel time is 4 x (one side travel time) = 4 x 40 = 160sec = 2min 40sec 2min 20sec is 20sec short of the full perimeter = 1/2 of one-side travel time = 5 meters' travel time
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∙ 14y agoWiki User
∙ 15y agoThe simplest way to find his speed, in meters/second.
10m per 40s, reduce the 10 and 40, 1/4 m/s. Find how many seconds there are in 2min 20 sec, 140s. 1/4 m/s after 140s. 1/4*140=35m.
Yes. All known earthquakes of magnitude 9.0 or greater have occurred at subduction boundaries.
Hsien K. Cheng has written: 'The shock layer concept and three-dimensional hypersonic boundary layers' 'Boundary-layer displacement and leading-edge bluntness effects in high temperature hypersonic flow'
D. S. McGhee has written: 'The effect of acceleration versus displacement methods on steady-state boundary forces'
Britain is effected by earthquakes. However because Britain is not near a tectonic plate boundary, the earthquakes that occur tend to be low in magnitude.
Use a enforced displacement boundary condition. Use a lot of substeps and force/moment reaction probes to know when you're at the load(s) you want. A free body diagram should tell you that.
When a wave hits a boundary and bounces back, it undergoes a process called reflection. The wave's direction is reversed but its properties such as frequency and wavelength remain the same. The angle of incidence is equal to the angle of reflection, following the law of reflection.
Well it is technically a vector because it has a magnitude and a direction on zero degrees. Reactive power will have a direction of either + or - 90 degrees and apparent power will be the vector sum of the real and reactive power.
You would most likely find a reverse fault at a convergent tectonic boundary, where two tectonic plates are colliding and one plate is being forced up and over the other. Reverse faults are characterized by vertical displacement and compression.
Convergent boundaries typically have the most earthquakes with high magnitudes because they involve the collision of tectonic plates, leading to intense pressure and stress that can be released in the form of large earthquakes. Examples of convergent boundaries with high-magnitude earthquakes include the Ring of Fire around the Pacific Plate.
A boundary is marked on the ground during the stage called "construction staking." This process involves locating and marking the exact positions of structures, roads, or utilities as shown in the construction plans.
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.
The plate boundary at which plates collide or come together is called a convergent boundary. At convergent boundaries, one plate is typically forced beneath the other in a process known as subduction. This collision can lead to the formation of mountain ranges, deep ocean trenches, and volcanic activity.