Geomorphology and soils of Apid Island, Inopacan, Leyte, Philippines
Jan Grenz | Sandra Zukunft | Victor B. Asio
Abstract:
Grenz J.,S. Zukunff and V.B. Asio. 1999. Geomorphology and soils of Apid Island, Inopacan, Leyte,
Philippines. Ann. Trop. Res. 21:1-8.
The island of Apid was most probably formed during the Upper Pleistocene as a
barrier reef resting on volcanic rock. Two main types of soil can be found there: Rendzic
Leptosols in the rocky interior and Arenosols on the sandy beach. Soil samples taken
on the island showed low nutrient contents and a very low capacity to store plantavailable water. Therefore, conditions for agricultural land-use are not very favorable.
References:
- BUREAU OF MINES. 1950. Geologic Map Series, Manila Philippines.
- FAO. 1994. Soil Map of the World. World Soil Resources Report 60. Rome, Italy.
- KADOMURA H. 1995. Palaeontological & palaeohydrological changes in the humid tropics during the last 20,000 years with reference to equatorial Africa. In: Global Continental Palaeohydrology (Gregory, K.J., et al., eds). John Wiley & Sons, Chichester.
- MARESH W. and O. MODENBACH. 1987. Gesteine. Mosaik Verlag, Muenchen.
- RAMMLMAIR D. 1993. The evolution of the Philippine archipelago in time and space: A plate tectonic model. Geologisches Jahrbuch, Reihe B. Heft 81E. Schweizerbartsche Verlagsbuchhandlung, Stuttgart.
- SCHLICHTING E., H.P. BLUME and K. STAHR. 1995. Bodenkundliches Praktikum (2nd ed.). Blackwell, Berlin.
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