SLOPE STABILITY ANALYSIS OF THE PATHUK HILL FOR THE RESORTS DEVELOPMENT
Abstract
Pathuk Hill is located abouth 15km eastern from Yogyakarta City. Pathuk Hill is elongated
hill (escarpment) trending NE-SW stricking and formed the steep slopes to the north-west.
An average height of a Pathuk Hill between 200m-250m above sea level. This hill are
composed by interbadded tufaceous sandstone and tuff of Semilir Formation in the lower
part. Conformity above of Semilir Formation is volcanic breccia of a solid Nglanggran
Formation. In the top of the Pathuk Hill we can see the exotic view of Yogyakarta City in the
western, Merapi Vocano in the north-western and sunset in the western in the afternoon. In
the Pathuk Hill resort will be development of the big resort as the gateway to the Wonosari
City. This area would be developed as a torism object between Yogyakarta City and
Wonosari City.
Keywards : Pathuk Hill, slope tability, resort, view, torism object.
hill (escarpment) trending NE-SW stricking and formed the steep slopes to the north-west.
An average height of a Pathuk Hill between 200m-250m above sea level. This hill are
composed by interbadded tufaceous sandstone and tuff of Semilir Formation in the lower
part. Conformity above of Semilir Formation is volcanic breccia of a solid Nglanggran
Formation. In the top of the Pathuk Hill we can see the exotic view of Yogyakarta City in the
western, Merapi Vocano in the north-western and sunset in the western in the afternoon. In
the Pathuk Hill resort will be development of the big resort as the gateway to the Wonosari
City. This area would be developed as a torism object between Yogyakarta City and
Wonosari City.
Keywards : Pathuk Hill, slope tability, resort, view, torism object.
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