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II. SOILS OF THE BINTULU COASTAL AREA
The sub-mature landscape of the country rock (Miocene fine sandstones and shales) along the coast north of Bintulu gives rise under a mean annual rainfall of 150 in. to highly leached yellow soils, comparable to Kellogg's Red-Yellow Latosols, associated with lowland Dipterocarp rain forest. Areas of level or nearly level coarse-textured marine or estuarine deposits marking successive stages of the fall in sea-level during the Pleistocene are associated with ground-water podzols supporting various forms of the characteristic kerangas forest, which give rise to ‘blackwater’ streams
Citing Literature
For further details log on website :
http://onlinelibrary.wiley.com/doi/10.1111/j.1365-2389.1961.tb00912.x/full
Author
II. SOILS OF THE BINTULU COASTAL AREA
The sub-mature landscape of the country rock (Miocene fine sandstones and shales) along the coast north of Bintulu gives rise under a mean annual rainfall of 150 in. to highly leached yellow soils, comparable to Kellogg's Red-Yellow Latosols, associated with lowland Dipterocarp rain forest. Areas of level or nearly level coarse-textured marine or estuarine deposits marking successive stages of the fall in sea-level during the Pleistocene are associated with ground-water podzols supporting various forms of the characteristic kerangas forest, which give rise to ‘blackwater’ streams
Citing Literature
For further details log on website :
http://onlinelibrary.wiley.com/doi/10.1111/j.1365-2389.1961.tb00912.x/full
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