They speed up
A seismograph works by detecting and recording seismic waves caused by earthquakes. It consists of a mass suspended on a spring inside a casing, which moves when seismic waves hit it. The movement of the mass is converted into an electrical signal that is recorded on paper or digitally to measure the intensity and duration of the earthquake.
True. A seismograph is a device that records the intensity and duration of seismic waves during an earthquake. When seismic waves hit, a small needle attached to a mass moves across a graph paper, creating a seismogram that shows the amplitude and frequency of the waves. The farther the needle moves, the more powerful the seismic wave is.
When electromagnetic waves hit an object, they can be absorbed, transmitted, reflected, or scattered. The interaction between the waves and the object will depend on the material properties of the object and the frequency of the electromagnetic waves.
When waves hit the shoreline, they slow down and their energy is transferred to the coast. This can cause erosion of the shoreline, as the waves carry sediment away. The waves can also break, creating turbulence and causing sediment to be deposited on the beach.
When sound waves hit a smooth surface, they bounce off the surface at an equal angle at which they hit it, a phenomenon known as reflection. With light waves, they can either be reflected, absorbed, or transmitted through the surface, depending on the material and angle of incidence.
It sends a ratio active wave in the aiqr
Seismic waves can be reflected, refracted, or diffracted when they encounter a fault. The behavior of the waves depends on the orientation and properties of the fault. Additionally, seismic waves can generate new waves when they interact with a fault, contributing to complex wave patterns in the Earth's subsurface.
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.
The first waves to hit are primary waves. Primary waves are seismic waves that compress and stretch the ground. P waves, or primary waves, can wreck buildings and can move straightforward through solids and liquids.
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.
The Tectonic Plates Shook And Hit each other Forming Seismic Waves.........Mkay
P-waves hit, followed by S-waves, followed by surface waves.
A seismograph works by detecting and recording seismic waves caused by earthquakes. It consists of a mass suspended on a spring inside a casing, which moves when seismic waves hit it. The movement of the mass is converted into an electrical signal that is recorded on paper or digitally to measure the intensity and duration of the earthquake.