Informasi Detil Paper |
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| Judul: | Geomorfologi - Tanah Gunung Wungkal Kecamatan Seyegan dan Kecamatan Godean Kabupaten Sleman - Yogyakarta |
| Penulis: | Steeves W. J. Louhenapessy || email: info@mail.unpatti.ac.id |
| Jurnal: | Logika Vol. 9 no. 1 - hal. 88-93 Tahun 2011 [ IPTEK ] |
| Keywords: | Geomorphology, Pedogeomorphology, Soil Development. |
| Abstract: | This research is aimed at studying correlation between geomorphology and soil of Gunung Wungkal describe in three objectives of the study, those are: to know the geomorphology features of the investigated region; to know the characteristic of the soil and to classify the category of USDA (1998) soil series; and to know correlation between geomorphology condition and the rate of soil development in the research area. The method used in this inquiry was a field survey conducted by observing the studied object based on the made land units. This was helped by means of working maps, which then result a pedogeomorphologic map depicting correlation between geomorphologic condition and soil in the research area. The results were analyzed by means of spatial descriptive approach. The result show that the research area has 11 land units formulated based on the form of the landform (denudation origin), parent material (diorite, sandstone, and andesite formation), and land use (secondary forest, desert, and housing). The geomorphologic process occurred in the research area involve various forms of erosion, mass move, and sedimentation. Soil characteristics in the research area are generally reflected from the rate of soil development. Soil development is influenced by geomophologic process working in every land unit. The more intensive the morphologic process is, the lower the rate of soil development will be, as in the contrary. The rate of soil development in the research area is in the category of developed, developing, and has not developed. |
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