A model for discharge in spring‐dominated streams and implications for the transmissivity and recharge of quaternary volcanics in the Oregon Cascades
- 1 August 1997
- journal article
- Published by American Geophysical Union (AGU) in Water Resources Research
- Vol. 33 (8), 1813-1822
- https://doi.org/10.1029/97wr01339
Abstract
No abstract availableKeywords
This publication has 15 references indexed in Scilit:
- Floods, channel change, and the hyporheic zoneWater Resources Research, 1999
- Comment [on “Rates and patterns of groundwater flow in the Cascade Range volcanic arc and the effect on subsurface temperatures” by S. E. Ingebritsen, D. R. Sherrod, and R. H. Mariner]Journal of Geophysical Research: Solid Earth, 1996
- Reply [to “Comment on ‘Rates and patterns of groundwater flow in the Cascade Range volcanic arc and the effect on subsurface temperatures’ by S. E. Ingebritsen, D. R. Sherrod, and R. H. Mariner”]Journal of Geophysical Research: Solid Earth, 1996
- Hydrology of Spring‐Dominated Streams in the Oregon CascadesWater Resources Research, 1996
- Scale effects in transmissivityJournal of Hydrology, 1996
- Isotope hydrology of voluminous cold springs in fractured rock from an active volcanic region, northeastern CaliforniaJournal of Hydrology, 1996
- Modélisation d'un aquifère basaltique fracturé tenant compte de données géologiques, climatiques et hydrauliques: cas des basaltes perchés de Garni (Arménie)Journal of Hydrology, 1996
- Estimates of Evapotranspiration or Effective Moisture in Rocky Mountain Watersheds from Chloride Ion Concentrations in Stream BaseflowWater Resources Research, 1996
- The hydrology and form of spring-dominated channelsGeomorphology, 1995
- Changing ideas in hydrology — The case of physically-based modelsJournal of Hydrology, 1989