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Çѱ¹Áö¹Ý°øÇÐȸ / v.26, no.5, 2010³â, pp.49-55
¼³¾Ç»ê±¹¸³°ø¿ø õºÒµ¿ °è°î¿¡¼­ ¹ß»ýµÈ ³«¼® °Åµ¿ºÐ¼®
( Analysis for Behavior of Rockfall Movement by Cheonbuldong Valley of Seoraksan National Park )
Á¶¿ë¼º;±èÀ¯¼º; ±¹¸³°ø¿ø°ü¸®°ø´Ü ±¹¸³°ø¿ø¿¬±¸¿ø;ÀüºÏ´ëÇб³ °ø°ú´ëÇÐ Åä¸ñ°øÇаú;
 
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2007³â 2¿ù 22ÀÏ ¼³¾Ç»ê±¹¸³°ø¿ø õºÒµ¿°è°î º´Ç³±³ ºÎ±Ù¿¡¼­ ´ë±Ô¸ð ³«¼®ÀÌ ¹ß»ýÇÏ¿´°í, ޹æ·Î°¡ Çѵ¿¾È Æó¼âµÇ¾ú¾ú´Ù. ¼³¾Ç»ê±¹¸³°ø¿ø³»¿¡¼­´Â ±âÈĺ¯È­·Î ÀÎÇÑ ¾Ï¹ÝÀÇ Àý¸®, dzȭ¿Í ÁöÇ¥¼ö µîÀÇ ±Þ°ÝÇÑ º¯È­·Î À¯»çÇÑ ³«¼®»ç°í ºóµµ°¡ Àæ¾ÆÁö°í ÀÖ´Ù. ÀÌ ¿¬±¸¿¡¼­´Â °è°î¹Ù´Ú¿¡¼­ ³ôÀÌ 80m ºÎ±Ù¿¡¼­ ¹ß»ýÇÑ ´ë±Ô¸ð ³«¼®ÀÇ Á¤¹ÐÁ¶»ç¿¡ ±Ù°ÅÇÏ¿© ³«¼®ÀÇ °Åµ¿À» ºÐ¼®ÇÏ¿´°í, ³«¼®¿¡³ÊÁö¸¦ »êÁ¤ÇÏ¿´´Ù. ºÐ¼®°á°ú·ÎºÎÅÍ ¼³¾Ç»ê±¹¸³°ø¿ø³»ÀÇ ÀÚ¿¬È¯°æÀ» ÈѼÕÇÏÁö ¾Ê°í, À§Çè¿ä¼Ò¸¦ ÃÖ¼ÒÈ­ÇÒ ¼ö ÀÖ´Â È¿°úÀûÀÎ ³«¼®°ü¸®¹æ¹ýÀ» Á¦¾ÈÇÏ¿´´Ù.
The large scale rock falling had occurred on 22nd February, 2007 in the Cheongbuldong valley area of Seoraksan National Park, and the visiting pass had been closed for a while. Similar cases of rock falling have occurred in the latest years according to a great variety of crack, joint, weathering of solid rock and surface water caused by a recent climatic change in the Seoraksan National Park. In this study, rock falling energy was estimated and the movement of rockslide was analysed based on detailed investigation on large scale rockslides occurring at the spot 80 m high from the bottom of the valley. From analysing results, the effective management method for rock falling was proposed. The method could minimized the dangerous factors with no change of natural environment of the National Park.
 
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Cheonbuldong valley;Joint;Rock fall;Seoraksan National Park;
 
Çѱ¹Áö¹Ý°øÇÐȸ³í¹®Áý / v.26, no.5, 2010³â, pp.49-55
Çѱ¹Áö¹Ý°øÇÐȸ
ISSN : 1229-2427
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO201023064629497)
¾ð¾î : Çѱ¹¾î
³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø
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