Results 171 to 180 of about 1,480 (183)

Quantifying form resistance is essential for estimating summer low and bankfull flow from stream survey channel morphology. [PDF]

Geomorphology (Amst)
Kaufmann PR, Carlisle DM, Faustini JM, Weber MH, Herlihy AT, Hill RA, Kasprak A, Paulsen SG.   +7 more
europepmc   +1 more source

Interpretable machine learning for predicting rating curve parameters using channel geometry and hydrological attributes across the United States. [PDF]

Sci Rep
Baruah A, Zarrabi R, Cohen S, Johnson JM, McDermott R.   +4 more
europepmc   +1 more source

InSAR characterization of short-term deformation in a Late Quaternary landslide complex in the lower Rio Grande Gorge, New Mexico, U.S.A. [PDF]

Sci Rep
Das R, Wegmann KW.
europepmc   +1 more source

Mapping the groundwater potential zones in mountainous areas of Southern China using GIS, AHP, and fuzzy AHP. [PDF]

Sci Rep
Chen M, Zhang S, Liu S, Li M, Zhang T, Wu T, Bu X.   +6 more
europepmc   +1 more source

Urbanization and Suspended Sediment Transport Dynamics: A Comparative Study of Watersheds with Varying Degree of Urbanization Using Concentration-Discharge Hysteresis. [PDF]

ACS ES T Water
Safdar S, Jefferson AJ, Costello DM, Blinn A.   +3 more
europepmc   +1 more source

Geomorphology of Jeddah Governate, with Emphasis on Drainage Systems

Journal of King Abdulaziz University-Earth Sciences, 2009
Jeddah Governate comprises three distinct geomorphological zones; the Red Sea and shore features, the coastal plain, and coastal hills and pediments. The last zone lies east of the municipal Jeddah city and consists of low lying hills, and an elongated N-S oriented depression, forming a basin that lies within the coastal hills.
Mohammed H. Qari
openalex   +2 more sources

Basin geomorphology and drainage morphometry parameters used as indicators for groundwater prospect: Insight from geographical information system (GIS) technique

Journal of Earth Science, 2014
Influence of structural and lithological controls of various drainage patterns and their stream orientations (for 2nd, 3rd and 4th order steams) were identified to evaluate the direction and controlling factors of drainage network. To investigate the prospect of groundwater, hydrogeomorphological features of river basin viz.
Avinash Kumar, B. Deepika, K. S. Jayappa
  +4 more sources

Three-dimensional seismic geomorphology and analysis of the Ordovician paleokarst drainage system in the central Tabei Uplift, northern Tarim Basin, western China

AAPG Bulletin, 2011
High-quality three-dimensional seismic data acquired in the central Tabei Uplift, Tarim Basin, western China, provide a rare opportunity to characterize in exceptional detail the three-dimensional geomorphology of a deeply buried (5500–6500 m [18,045–21,325 ft]) Ordovician unconformity and the related paleokarst drainage system.
Hongliu Zeng, Robert G. Loucks, Xavier Janson, Guizhong Wang, Yiping Xia, Bingheng Yuan, Ligui Xu   +6 more
openalex   +3 more sources

Structural control on drainage network and catchment area geomorphology in the Dead Sea area: an evaluation using remote sensing and geographic information systems in the Wadi Zerka Ma’in catchment area (Jordan)

Environmental Earth Sciences, 2016
The geology of Jordan is characterized by fault systems with three major trends: (1) NW–SE, the oldest, (2) WNW–ESE, and (3) NNW–SSE, the youngest. The drainage network of the Wadi Zerka Ma’in catchment area, located in the middle of the Dead Sea rift, parallels these structural orientations.
Taleb Odeh, Richard Gloaguen, Alsharifa Hind Mohammad, Mario Schirmer   +3 more
openalex   +3 more sources

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Geomorphological analysis of paleo drainage systems and their environmental implications in the desert of Kuwait

Environmental Geology, 1997
A well-developed drainage network is carved in the hard calcretized and gypcretized gravelly sand of the Pleistocene Dibdibba Formation in northern Kuwait. The present-day aridity suggests that these drainages were developed during pluvial episodes that took place in the post-Pleistocene time and, therefore, are considered as paleo-drainage.
J. Al-Sulaimi, F. J. Khalaf, A. Mukhopadhyay   +2 more
openaire   +1 more source