Earth

지진계와 관성의 법칙 Seismometer and Inertia

Seismometer and Inertia

Inertia Inertia is the resistance, of any physical object, to any change in its velocity. Examples of Inertia Shaking a bottle of ketchup. When bringing the bottom down, the suddenly stopping it,…
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지진파 Seismic Wave

Seismic Wave

Earthquake Investigation inside earth The most obvious way to see the inside of the earth is to drill directly into the earth. However, as you enter the Earth, the temperature and pressure…
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조륙운동 Epeirogeny

Epeirogenic movement

Epeirogenic movement(Epeirogeny) It is a phenomenon that the crust is slowly rising or sinking over a wide range. The crust is floating on a dense mantle and forms an equilibrium of force.…
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여러 모양 지층 만들기 Stratum Making

Stratum Making

Limestone Shale Sandstone Conglomerate Erosion Fold Normal Fault Reverse Fault Reset About this simulation, When you press the button, you can see the corresponding strata. Combining the layer, you can create variety…
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이슬이 생기는 원리 Dew

Dew

Could the cup’s water leak out? From the conclusion, the water on the surface of the cup is derived from the air. In very dry desert, dew does not occur. If you…
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코리올리 효과 Coriolis Effect

Coriolis Effect

Path Speed Reset Run Coriolis effect The French mathematician Coriolis first explained that the direction of fluid movement on the Earth’s surface is slightly warped. You can observe this effect in all…
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건습구습도계 Psychrometer(hygrometry)

Psychrometer(hygrometer)

A hygrometer consisting of a dry-bulb thermometer and a wet-bulb thermometer. Dry-bulb is a ordinary thermometer. And wet-bulb is the thermometer with wet sock. Thus, wet-bulb measured a little lower due to…
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화성암 Igneous Rock

Classification of igneous rocks

Igneous rocks are rocks formed from molten magma. The material is made liquid by the heat inside the Earth’s mantle. Igneous rock occurs in two ways. Slow cooling : Igneous rock formed…
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