Rajang River 2.5 热度 具体开放时间需咨询景区 实用攻略 Sarawak, Malaysia 地图·周边 暂无点评 快来发表第一条点评~ 写点评 暂无回答 不知道怎么玩?问问旅行达人 去提问 景点附近 景点 购物 Kapit Town Square 2.8 直线距离33.8km Kapit Sports Complex 2.1 直线距离33.3km Song Stadium ...
(also Rajung, Rejang), a river on the northwestern part of Kalimantan Island, in Sarawak (Malaysia). It is approximately 600 km long and drains an area of approximately 60,000 sq km. Originating on the slopes of the Iran Mountains, it flows primarily over a hilly plain and empties into...
1993 . Provenance and sediment dispersal in the Rajang River delta/coastal plain system, Sarawak, East Malaysia:. Sedimentary Geology 85: 191 – 201 .STAUB, J.R., AND ESTERLE, J.S., 1993, Provenance and sediment dispersal in the Rajang River delta/coastal plain system, Sarawak, East ...
Monitoring Trends of Land Use and Land Cover Changes in Rajang River Basin in land use and land cover (LULC) were evaluated from 1992 to 2015 for the Rajang River Basin (RRB) located in the Sarawak State of Malaysia. The... VK Oad,MRU Mustafa,HB Takaijudin,... 被引量: 0发表: 2021...
Despite this challenge, innovative developers such as Hock Peng Group has converted a useless sandbar off Lanang Road into Pulau Li Hua, a trendy up-market resort-like residential estate beside the Rajang River; and Soon Hup Group has developed its housing around a man-made lake which provides...
A. Seasonal sediment transport and deposition in the Rajang River delta, Sarawak, East Malaysia. Sediment Geol 133: 249-264, 2000.Staub, J. R., Among, H. L., & Gastaldo, R. A. (2000). Seasonal sediment transport and deposition in the Rajang River Delta, Sarawak, East Malaysia. ...
In this study, the spatiotemporal changes in land use and land cover (LULC) were evaluated from 1992 to 2015 for the Rajang River Basin (RRB) located in Sarawak State of Malaysia. The changes in water bodies, cropped lands, and forests were assessed based on the available remotely sensed ...
The Rajang River delta and coastal plain, Sarawak, East Malaysia, are covered in areally extensive, thick peat deposits that have attained at least a thickness of > 13 m in ombrogenous peat domes (Marudi, Baram River). Peat-swamp biomass began to accumulate over Pleistocene podzols when sea...
Paleocene river systems that flowed through the Malay Peninsula, transported large amounts of sediments to the marine basins including the deep-sea Rajang Group. A strong signal of sediment recycling for the Tatau Formation indicates uplift and denudation of lower Rajang Group in Late Eocene....