Surface water is known to shape the formation and growth of valleys and channels. However, in some geologic settings, groundwater seeping upwards is important for the development of channel networks.
This is a preview of subscription content, access via your institution
Access options
Subscribe to this journal
Receive 12 print issues and online access
$259.00 per year
only $21.58 per issue
Buy this article
- Purchase on Springer Link
- Instant access to full article PDF
Prices may be subject to local taxes which are calculated during checkout
FLORIDA DEPARTMENT OF REVENUE
References
Abrams, D. M. et al. Nature Geosci. 2, 193–196 (2009).
Lamb, M. P. et al. J. Geophys. Res. 111, E07002 (2005).
Lamb, M. P. et al. Science 320, 1067–1070 (2008).
Schumm, S. A., Boyd, K. F., Wolff, C. G. & Spitz, W. J. Geomorphology 12, 281–297 (1995).
Schorghofer, N., Jensen, B., Kudrolli, A. & Rothman, D. H. J. Fluid Mech. 503, 357–374 (2004).
Lobkovsky, A. E., Jensen, W., Kudrolli, A. & Rothman, D. H. J. Geophys. Res. 109, F04019 (2004).
Lobkovsky, A. E., Smith, B. E., Kudrolli, A., Mohrig, D. C. & Rothman, D. H. J. Geophys. Res. 112, F03S12 (2007).
Howard, A. D. Geomorphology 12, 187–214 (1995).
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Howard, A. Forming valleys from below. Nature Geosci 2, 165–166 (2009). https://doi.org/10.1038/ngeo447
Issue Date:
DOI: https://doi.org/10.1038/ngeo447
