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Earthquake(ÁöÁø)´Â Áö±¸ ³»ºÎ¿¡ store(ÃàÀû)µÈ elastic strain energy(ź¼º º¯Çü ¿¡³ÊÁö)°¡ ¼ø°£ÀûÀ¸·Î release(¹æÃâ)µÇ¾î earth¡¯s crust(Áö°¢)°¡ °¥¶óÁö°í Èçµé¸®´Â phenomenon(Çö»ó)ÀÌ´Ù. Earthquake´Â fault(´ÜÃþ)¸¦ µû¶ó ÀϾ ¶§°¡ ¸¹´Ù. Áö±¸ ³»ºÎ¿¡¼ force(Èû)°¡ ÃàÀûµÇ¸é faultÀÇ ¾çÂÊ rock mass(¾Ï¹Ý, ¾Ï¼®)°¡ bend(ÈÖ´Ù)ÇÑ´Ù. À̶§ rock mass°¡ ½ÉÇÏ°Ô bendµÇ¸é snap(²÷¾îÁö´Ù)ÇÏ¸é¼ earth surface(ÁöÇ¥¸é)°¡ Èçµé¸®±â ¶§¹®¿¡ earthquake°¡ ¹ß»ýÇÏ´Â °ÍÀÌ´Ù. Earth¡¯s crust¿Í upper mantle(»óºÎ ¸ÇƲ)Àº elasticity(ź¼º)°¡ ÀÖ´Â rock(¾Ï¼®)À¸·Î ÀÌ·ç¾îÁ® ÀÖ´Ù. µû¶ó¼ elasticity limit(ź¼º Çѵµ) À̳»¿¡¼ strain(¾Ð·Â)ÀÌ ¿À¸é earth¡¯s crust´Â plate glass(ÆÇÀ¯¸®)ó·³ ¾î´À Çѵµ±îÁö´Â bendµÆ´Ù°¡ force°¡ ¾ø¾îÁö¸é ¿ø·¡´ë·Î µÇµ¹¾Æ°£´Ù. ±×·¯³ª elasticity limit¸¦ ³ÑÀ¸¸é rockÀº ²÷¾îÁö°í À̶§ ¹ß»ýÇÑ tremor(Áøµ¿)°¡ Àü´ÞµÇ¾î earth¡¯s crust°¡ Èçµé¸®°Ô µÇ´Âµ¥ À̰ÍÀÌ ¹Ù·Î earthquakeÀÌ´Ù. _º»¹® 116-117ÂÊ basic concept Áß¿¡¼
An earthquake is a naturally induced shaking and vibration of the Earth¡¯s surface. The Earth¡¯s crust is made up of several large pieces called plates. Earthquakes happen when these plates suddenly slip past one another. The area where these plates meet is called the fault line. When the plates move or slip along the fault line, tension is released and an earthquake occurs. Earthquakes can also be caused by volcanic activity. _º»¹® 121ÂÊ reading earth science Áß¿¡¼
Example 2¡¡Fill in the blanks with the right answers.
a. The scale representing the gross energy released when earthquakes occur is ( ).
b. What determines the degree of influence (or how destructive it is) by earthquake to other regions is ( ).
_º»¹® 129ÂÊ problem solving Áß¿¡¼
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