[Kecamatan Ciemas merupakan daerah yang dikenal karena memiliki kekayaan geologi dengan terdapatnya batuan yang memiliki umur batuan tertua dan terluas di Pulau Jawa. Proses-proses geologi yang berlangsung memunculkan berbagai objek wisata alam yang menarik untuk dikunjungi. Tujuan dari penelitian ini adalah untuk mengetahui dan menganalisis keunikan geomorfologi sebagai potensi daya tarik wisata alam di Kecamatan Ciemas. Analisis dilakukan secara deskriptif dengan menggunakan pendekatan metode ideografik, korelasi kualitatif dan pembobotan terhadap variabel daya tarik wisata, aksesibilitas, dan fasilitas wisata pada unit analisis bantukan asal. Hasil yang diperoleh, yaitu bentukan asal struktural memiliki potensi tinggi dengan karateristik ketinggian 100-500 mdpl dan lereng yang curam.;Ciemas sub-district is an area known for its geological wealth, which lies the oldest and widest age of rocks on The Java Island. Geological processes that occurs in this area, led to many natural attractions worth visiting. The purpose of this study was to determine and analyze the unique of geomorphology as potential natural attractions in Ciemas Sub-District. The analysis was done descriptively by using ideographic approach method, qualitative correlation and weighted variables tourist attraction, accessibility, and tourist facilities on the analysis unit formed by origin. The result is formation of structural origin which have a high potential with a height of 100-500 meters above sea level characteristics and steep slopes., Ciemas sub-district is an area known for its geological wealth, which lies the oldest and widest age of rocks on The Java Island. Geological processes that occurs in this area, led to many natural attractions worth visiting. The purpose of this study was to determine and analyze the unique of geomorphology as potential natural attractions in Ciemas Sub-District. The analysis was done descriptively by using ideographic approach method, qualitative correlation and weighted variables tourist attraction, accessibility, and tourist facilities on the analysis unit formed by origin. The result is formation of structural origin which have a high potential with a height of 100-500 meters above sea level characteristics and steep slopes.]