Ephemeral landform development following rapid coastal uplift in the southern orogen of Taiwan

2021 ◽  
Author(s):  
Slawomir Jack Giletycz ◽  
Andrew Tien‐Shun Lin ◽  
Katsura Yamada ◽  
Liang‐Chi Wang ◽  
Chih‐Wei Chien ◽  
...  
Keyword(s):  
Landform Development ◽  
Coastal Uplift

Archaeological Evidence for Modern Coastal Uplift at Diu, Saurashtra Peninsula, India

2016 ◽  
Vol 31 (5) ◽  
pp. 376-387 ◽  
Author(s):  
Miklós Kázmér ◽  
Nilesh Bhatt ◽  
Vishal Ukey ◽  
Siddharth Prizomwala ◽  
Danko Taboroši ◽  
...  
Keyword(s):  
Archaeological Evidence ◽  
Coastal Uplift

scholarly journals Annual variation of coastal uplift in Greenland as an indicator of variable and accelerating ice mass loss

2013 ◽  
Vol 14 (5) ◽  
pp. 1569-1589 ◽  
Author(s):  
Qian Yang ◽  
Shimon Wdowinski ◽  
Timothy H. Dixon
Keyword(s):  
Mass Loss ◽  
Annual Variation ◽  
Coastal Uplift

scholarly journals Relationship between Landform Development and Lake Water Recharge in the Badain Jaran Desert, China

Water ◽  
2019 ◽  
Vol 11 (10) ◽  
pp. 1999
Author(s):  
Da-Peng Yue ◽  
Jing-Bo Zhao ◽  
Yan-Dong Ma ◽  
Xiao-Gang Huang ◽  
Tian-Jie Shao ◽  
...  
Keyword(s):  
Water Film ◽  
Adsorbed Water ◽  
Water Source ◽  
Infiltration Rate ◽  
High Water ◽  
Badain Jaran Desert ◽  
Multi Stage ◽  
Water Recharge ◽  
Landform Development ◽  
Precipitation Events

Four distinctive but poorly documented landforms in the Badain Jaran megadunes were studied: arcuate steps, multi-stage fans, depressions formed by runoff erosion, and groundwater overflow zones around lakes. The development of these four landform types indicates the following: (1) The hydrological balance in the sand layers of the megadune areas is positive; (2) After evaporation and transpiration, precipitation is able to infiltrate the deep sand layers; (3) Precipitation is a source for the groundwater and for many of the lakes of the area. The groundwater recharge mechanism is characterized by intense precipitation events that provide a water source, high infiltration rate, shallow evaporation depth, and low water retention. These factors together enable the precipitation to be transformed into groundwater. The energy of gravity water and the high water film pressure of adsorbed water together provide the forces necessary for effective water recharge.

Soil–landform development of a part of the fold belt along the eastern coast of Bangladesh

Geomorphology ◽  
2005 ◽  
Vol 71 (3-4) ◽  
pp. 310-327 ◽  
Author(s):  
Md. Sharif Hossain Khan ◽  
B. Parkash ◽  
Sudhir Kumar
Keyword(s):  
Eastern Coast ◽  
Fold Belt ◽  
Landform Development
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