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�썝      臾� ● 제주의 지맥

제주풍수의 모체는 한라산이며, 모체인 한라산과 오름은 체용(體用)의 관계이다. 한라산을 빼어놓고  풍수를 논할 수 없고, 오름을 빼어놓고 제주의 풍수를 논할 수 없다. 사방에 산포한 오름과 관련하여 한라산의 산세를 알 수 있고 오름마다에 생기를 타는 길지(吉地)가 있으며 그곳엔 제주민의 애환과 이상이 서려있다. 제주의 선조들은 한라산과 오름의 상호 유기적인 지맥을 이용하여 양택과 음택을 가리고 그들이 지향하는 삶의 안녕과 번영을 꿈꾸었다. 또한 오름은 제주인의 삶속에 복합적인 문화를 형성하는 요인이 되었으며 오름마다 우마를 방목하였고 지역을 구분하는데 오름이나 물길이 이용되었으며 최후의 안식처로써 제주인들의 뼈를 묻는 묘역 또한 오름을 중심으로 형성되었다
제주의 지맥은 예로부터 한라산을 종산으로 삼아 첫 번째 맥은 동쪽의 사라악을 중심으로 성판악으로 이어져 궤팽이오름·거문오름·붉은오름·소록산·대록산·따라비·모지악·영주산으로 이어져 천민천을 만나 일시 멈추었다가 남산봉에 이른다. 원맥은 계속하여 은월봉·두산봉·지미봉·식산봉·소수산봉·대수산봉을 거느리며 성산일충봉을 거쳐 우도까지 뻗어 나갔다고 본다. 동쪽의 주맥인 성판악에서 우도로 이어지는 본맥의 중심선에서 다시 좌우 두 줄기로 크게 나누어져 한 줄기는 동남쪽 남원읍 수망리를 거쳐 반득이왓으로 흘러 내리고 또 한줄기는 동북쪽의 조천읍 교래리에 있는 조인납으로 흘러내린다. 두 번째 맥은 서쪽의 영실로 뻗어나가 그 중 한 갈래가 법정악, 녹하지오름, 왕이메를 거쳐 군산, 월라산, 산방산으로 이어지고 또 한 갈래는 족은대비오름·왕이메·원물오름·거린오름으로 이어져 지맥이 덕수 방향으로 잠시 약해졌다가 물을 만나 지세를 회복하고 산방산에 임하여 잠시 멈추었다가 단산·금산이오름·송악산·가파도·마라도로 흘러내리고 또 한 갈래는 한 대오름·빈네오름·폭낭오름·괴오름을 거쳐 어음방면인 새별오름·이달오름·정물오름·금악·가마오름·새신오름·저지악 등으로 이어져 한림과 한경 방면인 고산의 당오름·수월봉을 거쳐 차귀도로 내려가고 다시 한 갈래는 어승생 서쪽으로 삼형제오름·노루오름·바리메·노꼬메·과오름·알오름으로 이어져 애월 납읍, 고내 방면과 금덕, 하귀 쪽으로 내려가고 한 갈래는 어승생 서쪽 삼형제오름으로 흘러 내려 붉은오름·천아오름·산세미오름을 거쳐 애월 광령쪽으로 이어진다고 보는데 남성대 위쪽 어승생 방향으로 떨어진 용세를 고려하여 서쪽은 크게 세갈래의 지맥을 중심으로 크고 작은 지맥이 주변으로 이어 내려간다고 보는 설이 지배적이다.
제주의 지맥을 구성하는 중요한 것은 오름과 오름을 사이로 크고 작은 하천을 경계로 한라산의 용맥이 실핏줄처럼 서로 교응하면서 산천의 조화를 이루며 이어졌다는 것이다. 특히 오름을 중심으로 지맥이 연결되어 마을마다 하나의 의지처로써 마을을 호위하고 지켜주는 진산으로 삼았으며 정신적인 지주이자 살아서는 생업의 젓줄이었고 생을 마치면 돌아가 뼈를 묻을 영원의 쉼터였으니 오름은 바로 독특한 제주의 풍수관을 이룬 모체가 되었으며 오름을 통하여 자연스럽게 배어 나온 그들의 삶의 방식이자 제주만의 독특한 역사성 위에서 길들여진 절대적 가치를 중시한 풍수신앙이었다고 볼 수 있다. 
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