The tallest waves on Earth are typically found at locations known as "wave hotspots," such as the coast of Hawaii, particularly at Jaws (Peahi) and the North Shore of Oahu, as well as in the Southern Ocean near Antarctica. These massive waves are primarily generated by powerful storms and strong winds that create swells across vast ocean distances. The unique underwater topography and coastal features of these areas can further amplify wave heights, resulting in some of the tallest and most notorious surfable waves in the world.
The tallest waves on Earth are typically generated by a combination of strong winds, long fetch (the distance over which the wind blows across the water), and deep ocean waters. These conditions often occur during powerful storms or hurricanes, where sustained winds can create massive swells. Additionally, the interaction of ocean currents and underwater topography, such as underwater ridges, can amplify wave heights as they approach the shore. The tallest recorded waves, reaching over 100 feet, are often associated with these extreme weather events.
they are usally found in the ocean the most and hen when the waves come on the surface they stay on the shell for people to collect.
Seismic waves travel through Earth's interior primarily as body waves, which include P-waves (primary waves) and S-waves (secondary waves). These waves can also travel along the Earth's surface as surface waves, such as Love waves and Rayleigh waves.
Earthquakes transmit seismic waves, which are vibrations that travel through the Earth's crust and are responsible for the shaking felt during an earthquake. There are two main types of seismic waves: body waves (P-waves and S-waves) that travel through the Earth's interior, and surface waves that travel along the Earth's surface.
Earthquakes dont move the friction in tectonical plates makes the ground vibrate (shake)They move by the shifting and movement of the tectonic plates that are moving in the first place that is causing the earthquake.
The tallest waves on Earth are typically generated by a combination of strong winds, long fetch (the distance over which the wind blows across the water), and deep ocean waters. These conditions often occur during powerful storms or hurricanes, where sustained winds can create massive swells. Additionally, the interaction of ocean currents and underwater topography, such as underwater ridges, can amplify wave heights as they approach the shore. The tallest recorded waves, reaching over 100 feet, are often associated with these extreme weather events.
yeah it makes waves
the wind or earthquakes or the earth itself
Longitudinal waves can be found in mediums such as air, water, and solids. They are commonly observed in sound waves traveling through air and seismic waves traveling through the Earth's crust.
Compressional waves can be found in various mediums, such as solids, liquids, and gases. They are commonly observed in earthquakes, sound waves in air or water, and seismic waves in the Earth's crust.
The Radio waves are reflected back to Earth in the Ionosphere.
A pond or a small stream may have water that makes very small waves due to wind or disturbance. These small waves are often gentle and subtle compared to waves found in larger bodies of water like oceans.
Seismic waves travel through the Earth's interior as a form of mechanical energy. They can travel through solid rock, liquid magma, and other materials found beneath the Earth's surface.
they are usally found in the ocean the most and hen when the waves come on the surface they stay on the shell for people to collect.
The three electromagnetic waves that make up most of the energy that Earth receives from the sun are infrared radiation, visible light, and ultraviolet radiation. These waves carry different amounts of energy and play key roles in sustaining life on Earth.
yes, the Earth's core is liquid.Scientists have found this out by seismic waves. They are unable to pass through liquid and whilst tracking them, scientists found that they avoid the center, telling us that the center of the earth is liquid.
Seismic waves travel through Earth's interior primarily as body waves, which include P-waves (primary waves) and S-waves (secondary waves). These waves can also travel along the Earth's surface as surface waves, such as Love waves and Rayleigh waves.