http://www.teara.govt.nz/EarthSeaAndSky/NaturalHazardsAndDisasters/Earthquakes/1/ENZ-Resources/Standard/4/en GO THERE! Great example
Primary waves (P-waves) and secondary waves (S-waves) are both types of seismic waves that travel through the Earth's interior during an earthquake. They are both body waves that move through the Earth's interior. Additionally, both P-waves and S-waves play a crucial role in helping seismologists understand the structure of the Earth's interior.
Primary occupations are those occupations which depend directly on nature. For example: agriculture, fishing, lumbering, mining, gathering forest products and so on. Occupations in which production of finished useful commodities by processing raw materials obtained from nature is involved are called secondary occupations. For example: various types of industries.
The objectives of teaching geography at primary level are to develop basic spatial awareness and understanding of the world around us. At the secondary level, the objectives include deeper exploration of physical and human geography concepts, critical thinking skills, and understanding global interconnections. Geography education at both levels aims to foster appreciation for diverse cultures and environments.
Iron mining is considered a primary economic activity because it involves the extraction of raw materials directly from the Earth. Secondary economic activities typically involve processing or manufacturing raw materials into goods.
No, islands do not move but they may shift over time due to factors like erosion, tectonic plate movement, or volcanic activity. While the landmass itself remains stationary, the position of islands can change on a geological scale.
There are three types of vibrations:- Primary waves, Secondary waves and long waves. Primary waves can move through solid and liquid. Secondary waves move through only solids and long waves can only move along the surface of the earth's crust.
Primary waves (P-waves) move outward from the focus of an earthquake, while secondary waves (S-waves) also move outward from the focus. Both types of waves are seismic body waves that travel through the Earth's interior.
Yes, both primary (P-waves) and secondary (S-waves) waves move outward from the earthquake's epicenter. P-waves are faster and move through solid and liquid materials, while S-waves are slower and only travel through solid materials.
Secondary waves, also known as S-waves, are seismic waves that arrive after primary waves (P-waves) during an earthquake. They are slower than P-waves and travel through the Earth by causing particles to move in a perpendicular motion to the direction of wave propagation.
Primary seismic waves travel the fastest.
These waves are called secondary waves, or S-waves. They travel at slower speeds than primary waves and move the ground side-to-side, causing shaking and structural damage to buildings. S-waves are more destructive than P-waves and are usually felt after the initial P-wave motion during an earthquake.
Secondary waves.
Primary waves, Secondary waves, and Seismic waves
P-Waves (Primary Waves) S-Waves (Secondary Waves) Surface Waves
The three main types of seismic waves are P-waves (primary waves), S-waves (secondary waves), and surface waves. P-waves are compressional waves that travel the fastest and can move through both solids and liquids. S-waves are shear waves that move more slowly and only travel through solids. Surface waves are the slowest and travel along the surface of the Earth, causing the most damage during an earthquake.
Primary Waves, Secondary Waves, and Surface Waves.
P waves (primary waves) and S waves (secondary waves).