9   Artículos

 
en línea
Scott M. White, Erin Smoak, Andrew L. Leier and Alicia M. Wilson    
The spatial variations in Quaternary sediments on the inner continental shelf are produced by the progression of depositional environments during the latest sea-level rise, and this sedimentary architecture plays a fundamental role in controlling groundw... ver más
Revista: Geosciences    Formato: Electrónico

 
en línea
Md Rizwanul Hasan, Daniel Larsen, Scott Schoefernacker and Brian Waldron    
Electrical resistivity and borehole data are applied to delineate lithostratigraphic boundaries and image the geometry of confining-unit breaches in Eocene coastal-plain deposits to evaluate inter-aquifer exchange pathways. Eight dipole?dipole array surv... ver más
Revista: Water    Formato: Electrónico

 
en línea
Estela García-Botella and Alfredo Ramón-Morte    
Many ephemeral Mediterranean watercourses are affected by the growth of tourism and the demand for holiday homes. Calculating the runoff threshold in these small basins is vital for understanding the impact generated by urban growth and its incidence on ... ver más
Revista: Geosciences    Formato: Electrónico

 
en línea
Quinn Buzzard, Jeff B. Langman, David Behrens and James G. Moberly    
The heterogeneity of the fractured-basalt and interbedded-sediment aquifer along the eastern margin of the Columbia Plateau Regional Aquifer System has presented challenges to resource managers in quantifying recharge and estimating sustainable withdrawa... ver más
Revista: Geosciences    Formato: Electrónico

 
en línea
Philippe Paillou, Sylvia Lopez, Eugene Marais and Klaus Scipal    
The Kuiseb River is one of the major ephemeral rivers of Western Namibia, setting the northern limit of the Namib Sand Sea and outflowing in the Atlantic Ocean at Walvis Bay. Such ephemeral rivers are of the highest importance for the country since they ... ver más
Revista: Water    Formato: Electrónico

 
en línea
Rita De la Cruz,Manuel Suarez     Pág. 3 - 24
RESUMEN. Durante el Jurasico, en el sector occidental de la cuenca de Neuquen (region de Lonquimay, Chile, entre los paralelos 38 y 39°S), se acumularon depositos sedimentarios marinos y volcanicos marinos y subaereos. Estos constituyen la Formacion Naci... ver más
Revista: Andean Geology    Formato: Electrónico

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