"Mammoth Shakes and Monster Waves" is a children's book by Barbara J. Davis that explores the themes of natural disasters, specifically earthquakes and tsunamis. The story combines vivid illustrations and engaging narratives to explain how these powerful phenomena occur and their impacts on the environment and communities. It aims to educate young readers about the science behind these events while instilling a sense of preparedness and resilience. Overall, the book serves as both an informative resource and an engaging tale for children.
surface waves
seismic waves thta shakes particles at right angles to the dircetion that they travel
When a baby shakes a rattle, the mechanical energy from their hand movement is converted into sound energy as the rattle vibrates and generates sound waves.
You click your monsters hand and it thumbs up or waves
because since the earthquake shakes up the ground so much some extra waves come up which are called after shocks
The S-wave is the secondary seismic wave.
Margaret A. Sabol has written: '1993 annual climatic summary for the Network for Engineering Monitoring of the Ocean' -- subject(s): Statistics, Wind waves, Ocean waves, Water waves
The surface wave that shakes the ground in a rolling elliptical shape is called the Rayleigh wave. Rayleigh waves travel along the surface of solids and cause both vertical and horizontal ground movement, resulting in a rolling motion that resembles ocean waves. They are typically the most destructive type of seismic wave during an earthquake.
Shear waves can travel through solids, but they cannot travel through liquids. Shear waves are a type of seismic wave that shakes particles perpendicular to the direction of wave propagation. This makes them unable to propagate through liquids, which do not have the necessary shear strength to transmit these waves.
Seismic waves called "S waves" shake the ground up and down as they move through the Earth. S waves are a type of shear wave that travels through the Earth's interior and are responsible for the side-to-side or up-and-down motion felt during an earthquake.
Typically, at least three seismometers are needed to accurately determine the location and magnitude of an earthquake. By measuring the arrival times of earthquake waves at different locations, seismologists can triangulate the epicenter and assess the seismic activity more effectively.
During an earthquake, the Earth's surface shakes hardest at the epicenter, which is the point on the surface directly above where the earthquake originated. The seismic waves radiate outwards from this point, causing the most intense shaking near the epicenter.