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ÁöÁú,ÁöÇü


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Á¦ÁÖµµÀÇ ÁöÁúÀº ÅðÀû¾ÏÃþ°ú Çö¹«¾Ï, Á¶¸éÁú¾È»ê¾Ï(ðØØüòõäÌߣäÛ), Á¶¸é¾Ï µîÀÇ È­»ê¾Ï·ù¿Í ±â»ýÈ­»ê¿¡¼­ ºÐÃâÇÑ È­»ê¼â¼³¾Ï(ûýߣáïàÚäÛ) µîÀ¸·Î ±¸¼ºµÇ¾î ÀÖÀ¸¸ç, ÀϺΠÁö¹æÀÇ Á¡»çÁú Åä¾çÀ» Á¦¿ÜÇÏ¸é ´ëºÎºÐÀÌ Èæ°¥»öÀÇ È­»êȸÅä·Î µ¤¿© ÀÖ´Ù. ±×¸®°í ÁöÇüÀº ÇѶó»êÀ» Áß½ÉÀ¸·Î µ¿¼­»ç¸éÀº 3µµ~5µµÀÇ ¸Å¿ì ¿Ï¸¸ÇÑ °æ»çÀ̸ç, ³²ºÏ»ç¸éÀº 5µµ Á¤µµ·Î ¾à°£ ±ÞÇÑ °æ»ç¸¦ ÀÌ·ç°í ÀÖ´Ù.

 

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Geological and geographical featurea : Geologically the island is basically
composed of volcanic material such as basalt and trachyte, mixed with sedimentary rock and some clay. Volcanic ash is evident in association with parasite cones dotting the island. The eastern and western slopes of Mt. Halla have a gentle incline of 3 to 5 degrees while the northern and southern faces are much steeper.

 

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