<![CDATA[Abstrak:Penelitian ini dilakukan di daerah Pasarwajo, Desa Dongkala, Kecamatan Pasarwajo, Kabupaten Buton, Provinsi Sulawesi Tenggara. Penelitian ini bertujuan untuk mengetahui jenis batuan, variasi morfologi dan geomorfologi karst pada daerah penelitian. Metode pengumpulan data pada penelitian ini, terbagi atas tiga yaitu melalui observasi dan pengukuran langsung di lapangan menggunakan analisis petrologi dan analisis morfografi, melalui pengamatan di laboratorium menggunakan analisis petrografi serta melalui interpretasi peta citra satelit atau peta topografi menggunakan analisis morfometri. Hasil penelitian menunjukan bahwa terdapat 2 satuan bentanglahan yaitu satuan bentanglahan kars dan satuan bentanglahan marine. Variasi morfologi karst pada daerah penelitian secara umum terbagi atas tiga yaitu morfologi eksokarst,morfologi endokarst dan morfologi mikro dengan geomorfologi karst tipe Gunung sewu.. Untuk satuan bentanglahan marin bentuklahan pesisir yang ada di daerah penelitian dibentuk oleh hasil erosi laut yang terdiri dari ciff, wave-cut platform, gua laut, notch dan stumb dengan jenis batuan packstone, wackstone dan endapan alluvial. Kata Kunci : Geomorfologi karst, Eksokasrt, Endokasrt, Mikrokarst Abstrak: This research was conducted in the Pasarwajo area,Dongkal village, Pasarwajo District, Buton Regency, Southeast Sulawesi Province. This research to determine the rock type, morphological variations and the karst geomorphology of the research area. Data collection methods in this research, divided into three, through direct observation and measurements in the field, using petrological analysis and morphographic analysis, through laboratory observations using petrographic analysis, and through the interpretation of the satellite image map or topographic maps using morphometric analysis. The result of the study showed that there were two fields, those were karst field and marine field.. In general, the variation of karst morphology in the research area is divided into three, the exokarst morphology,the endokarst morphology and the minor karst with the karst geomorphology of the Sewu mountain type. For marine field, the shoreline field which is located in the area of the study, was shaped by the effect of erosion of the sea consisted of cliff, wave-cut plataform, sea cave,notch adan stumb, the type of lithologi packstone, wackstone and alluvial deposit. Keywords: Karst Geomorphology, Exokarst, Endokarst, Mikrokasrt]]>
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