frsb.upm.edu.my · the pleistocene time. it is fully covered by recent quaternary river alluviums....

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Page 1: frsb.upm.edu.my · the Pleistocene time. It is fully covered by recent quaternary river alluviums. Marshland soil is characterized by continuous water presence, near or above the
Page 2: frsb.upm.edu.my · the Pleistocene time. It is fully covered by recent quaternary river alluviums. Marshland soil is characterized by continuous water presence, near or above the
Page 3: frsb.upm.edu.my · the Pleistocene time. It is fully covered by recent quaternary river alluviums. Marshland soil is characterized by continuous water presence, near or above the
Page 4: frsb.upm.edu.my · the Pleistocene time. It is fully covered by recent quaternary river alluviums. Marshland soil is characterized by continuous water presence, near or above the
Page 5: frsb.upm.edu.my · the Pleistocene time. It is fully covered by recent quaternary river alluviums. Marshland soil is characterized by continuous water presence, near or above the
Page 6: frsb.upm.edu.my · the Pleistocene time. It is fully covered by recent quaternary river alluviums. Marshland soil is characterized by continuous water presence, near or above the
Page 7: frsb.upm.edu.my · the Pleistocene time. It is fully covered by recent quaternary river alluviums. Marshland soil is characterized by continuous water presence, near or above the
Page 8: frsb.upm.edu.my · the Pleistocene time. It is fully covered by recent quaternary river alluviums. Marshland soil is characterized by continuous water presence, near or above the