Our home planet is a shifting, moving, groaning, spitting ball of rock. We need to build solid, unmoving, long-lasting structureson it. To bring about this feat of construction, builders need to consult an expert in geotechnical engineering. The geotechnical engineer has studied the shifting and moving of our rock ball and gained the knowledge to give advice on how to anchor the structures or build them to accommodate what happens underneath.
Earthquakes are among the most common and widespread of potential problems that builders must anticipate. Earthquakes can cause many different types of damage, and none can be ignored. The first type of damage that we think of when we hear of an earthquake occurrence is surface rupture. An earthquake occurs when the earth at a fault line moves in reaction to deep underground pressures that build up as the tectonic plates grind up against each other. When the pressure is released through an earthquake, the land on one or both sides of the fault line moves a little or a lot. This movement can take many forms. A crack may split the earth as the two sides separate. The shift might be in the plane of the surface, which might shift a road so that it becomes misaligned. There might be a vertical change, with one side of the fault becoming higher or lower than the other side.
Another possible effect of an earthquake might be a landslide. If it occurs in an area of hills or cliffs, the land under the hill or cliff crumble and be dislodged and, succumbing to gravity's pull, come tumbling to the lower elevation. Unfortunately, objects at the brink, whether trees or houses, will most likely also come tumbling down with it.
Still another result of the quake might be subsidence. This effect may occur when the path of the earthquake takes a bend or steps over the land. When this happens, there is tension in the land, and a land area can settle very suddenly. If the quake occurs on a waterfront area, a section of the land may quickly sink under water.
An even larger danger in an earthquake near the water's edge can be liquefaction. This type of damage is most common near a port or a dam. Liquefaction is the process of the soil breaking up and being invaded by the nearby water. The result is a sort of soupy mixture that can swallow up roadways and sink harbors. As the land slides into the water, it can also open up other cracks in adjoining areas. This shifting of the earth can then collapse any other structures that were built there.
For many reasons, humanity sees these earthquake-prone areas as the most attractive places to settle. Consider the most popular and admired State in the United States-California. On the other side of the Pacific Rim is Japan, also densely populated. Is it the dramatic scenery that came about as a result of this shifting falling landscape? Probably.
Earthquakes are among the most common and widespread of potential problems that builders must anticipate. Earthquakes can cause many different types of damage, and none can be ignored. The first type of damage that we think of when we hear of an earthquake occurrence is surface rupture. An earthquake occurs when the earth at a fault line moves in reaction to deep underground pressures that build up as the tectonic plates grind up against each other. When the pressure is released through an earthquake, the land on one or both sides of the fault line moves a little or a lot. This movement can take many forms. A crack may split the earth as the two sides separate. The shift might be in the plane of the surface, which might shift a road so that it becomes misaligned. There might be a vertical change, with one side of the fault becoming higher or lower than the other side.
Another possible effect of an earthquake might be a landslide. If it occurs in an area of hills or cliffs, the land under the hill or cliff crumble and be dislodged and, succumbing to gravity's pull, come tumbling to the lower elevation. Unfortunately, objects at the brink, whether trees or houses, will most likely also come tumbling down with it.
Still another result of the quake might be subsidence. This effect may occur when the path of the earthquake takes a bend or steps over the land. When this happens, there is tension in the land, and a land area can settle very suddenly. If the quake occurs on a waterfront area, a section of the land may quickly sink under water.
An even larger danger in an earthquake near the water's edge can be liquefaction. This type of damage is most common near a port or a dam. Liquefaction is the process of the soil breaking up and being invaded by the nearby water. The result is a sort of soupy mixture that can swallow up roadways and sink harbors. As the land slides into the water, it can also open up other cracks in adjoining areas. This shifting of the earth can then collapse any other structures that were built there.
For many reasons, humanity sees these earthquake-prone areas as the most attractive places to settle. Consider the most popular and admired State in the United States-California. On the other side of the Pacific Rim is Japan, also densely populated. Is it the dramatic scenery that came about as a result of this shifting falling landscape? Probably.
About the Author:
Connor R. Sullivan recently met with a skilled geotechnical engineer for an engineering project he is working on. He hired a geotechnical engineering firm for a road construction project.
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