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Cited by 55 publications
(41 citation statements)
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“…Staub and Esterle (1994) estimated that prior to anthropogenic development the Rajang River drainage basin provided about 30 million MT of sediment annually to the delta. This estimate was corroborated by the work of Farrant et al (1995). Volumetric analysis of varved delta front and prodelta sediments in this study indicates that about 80% (roughly 24 million MT) of this amount is supplied to the delta front and prodelta in an average year.…”
Section: Seasonal Sediment Transport and Delta Front Sedimentationsupporting
confidence: 76%
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“…Staub and Esterle (1994) estimated that prior to anthropogenic development the Rajang River drainage basin provided about 30 million MT of sediment annually to the delta. This estimate was corroborated by the work of Farrant et al (1995). Volumetric analysis of varved delta front and prodelta sediments in this study indicates that about 80% (roughly 24 million MT) of this amount is supplied to the delta front and prodelta in an average year.…”
Section: Seasonal Sediment Transport and Delta Front Sedimentationsupporting
confidence: 76%
“…During the Quaternary, base-level lowering/epirogenic uplift of the Central Borneo Massif is estimated at 0.15-0.22 m/ka (Farrant et al, 1995) and, as a result, siliciclastic sediment production from the upland drainage basin is substantial. Staub and Esterle (1994) estimated that before anthropogenic development, the Rajang River drainage basin provided ഡ30 million MT of sediment annually to the delta.…”
Section: Physiographic Setting Climate and Previous Workmentioning
confidence: 99%
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“…If the level of 238 the sediment fill is stable, lateral incision will generate vadose alluvial notches coincident with the top 239 of the fill. As meanders grow, their outer bends incise farther back into the walls, resulting in low, 240 wide arcuate notches which may extend for tens to hundreds of metres down a passage, and in some 241 cases kilometres (Farrant et al, 1995). Such vadose alluvial notches are invariably sub-horizontal, 242 because their formation is linked directly to sediment accumulation below a free water surface ( Figure 243 5a,b).…”
Section: Effects Of Sediment Influx In a Vadose Setting 234mentioning
confidence: 99%
“…Heights above river level can thus give a useful indication of age (e.g. Farrant et al, 1995), one that can frequently be calibrated with reference to datable spe leothem.…”
Section: Bulgariamentioning
confidence: 99%