Vote for your favorite mineral in #MinCup25! - Taenite vs. Nontronite
It's a mineral found mostly in the farthest reaches of space vs one so common an exhaustive list of localities is nigh impossible as alloy #taenite faces off against clay #nontronite.
Log InRegister
Quick Links : The Mindat ManualThe Rock H. Currier Digital LibraryMindat Newsletter [Free Download]
Home PageAbout MindatThe Mindat ManualHistory of MindatCopyright StatusWho We AreContact UsAdvertise on Mindat
Donate to MindatCorporate SponsorshipSponsor a PageSponsored PagesMindat AdvertisersAdvertise on Mindat
Learning CenterWhat is a mineral?The most common minerals on earthInformation for EducatorsMindat ArticlesThe ElementsThe Rock H. Currier Digital LibraryGeologic Time
Minerals by PropertiesMinerals by ChemistryAdvanced Locality SearchRandom MineralRandom LocalitySearch by minIDLocalities Near MeSearch ArticlesSearch GlossaryMore Search Options
Search For:
Mineral Name:
Locality Name:
Keyword(s):
 
The Mindat ManualAdd a New PhotoRate PhotosLocality Edit ReportCoordinate Completion ReportAdd Glossary Item
Mining CompaniesStatisticsUsersMineral MuseumsClubs & OrganizationsMineral Shows & EventsThe Mindat DirectoryDevice SettingsThe Mineral Quiz
Photo SearchPhoto GalleriesSearch by ColorNew Photos TodayNew Photos YesterdayMembers' Photo GalleriesPast Photo of the Day GalleryPhotography

Parsons, Anthony J., Wainwright, John, Brazier, Richard E., Powell, D. Mark (2008) Is sediment delivery a fallacy? Reply. Earth Surface Processes and Landforms, 33 (10) 1630-1631 doi:10.1002/esp.1627

Advanced
   -   Only viewable:
Reference TypeJournal (article/letter/editorial)
TitleIs sediment delivery a fallacy? Reply
JournalEarth Surface Processes and Landforms
AuthorsParsons, Anthony J.Author
Wainwright, JohnAuthor
Brazier, Richard E.Author
Powell, D. MarkAuthor
Year2008 (September)Volume33
Issue10
PublisherWiley
DOIdoi:10.1002/esp.1627Search in ResearchGate
Generate Citation Formats
Mindat Ref. ID14960063Long-form Identifiermindat:1:5:14960063:9
GUID0
Full ReferenceParsons, Anthony J., Wainwright, John, Brazier, Richard E., Powell, D. Mark (2008) Is sediment delivery a fallacy? Reply. Earth Surface Processes and Landforms, 33 (10) 1630-1631 doi:10.1002/esp.1627
Plain TextParsons, Anthony J., Wainwright, John, Brazier, Richard E., Powell, D. Mark (2008) Is sediment delivery a fallacy? Reply. Earth Surface Processes and Landforms, 33 (10) 1630-1631 doi:10.1002/esp.1627
In(2008, September) Earth Surface Processes and Landforms Vol. 33 (10) Wiley

See Also

These are possibly similar items as determined by title/reference text matching only.

Parsons, Anthony J., Wainwright, John, Brazier, Richard E., Powell, D. Mark (2006) Is sediment delivery a fallacy?. Earth Surface Processes and Landforms, 31 (10) 1325-1328 doi:10.1002/esp.1395
Parsons, Anthony J., Brazier, Richard E., Wainwright, John, Powell, D. Mark (2008) Scale relationships in hillslope runoff and erosion Reply. Earth Surface Processes and Landforms, 33 (10) 1637-1638 doi:10.1002/esp.1628
Parsons, Anthony J., Brazier, Richard E., Wainwright, John, Powell, D. Mark (2006) Scale relationships in hillslope runoff and erosion. Earth Surface Processes and Landforms, 31 (11) 1384-1393 doi:10.1002/esp.1345
Parsons, Anthony J., Wainwright, John, Mark Powell, D., Kaduk, Jörg, Brazier, Richard E. (2004) A conceptual model for determining soil erosion by water. Earth Surface Processes and Landforms, 29 (10) 1293-1302 doi:10.1002/esp.1096
Wainwright, John, Parsons, Anthony J., Müller, Eva N., Brazier, Richard E., Powell, D. Mark, Fenti, Bantigegne (2008) A transport-distance approach to scaling erosion rates: 1. Background and model development. Earth Surface Processes and Landforms, 33 (5) 813-826 doi:10.1002/esp.1624
Wainwright, John, Parsons, Anthony J., Müller, Eva N., Brazier, Richard E., Powell, D. Mark, Fenti, Bantigegne (2008) A transport-distance approach to scaling erosion rates: 3. Evaluating scaling characteristics ofMahleran. Earth Surface Processes and Landforms, 33 (7) 1113-1128 doi:10.1002/esp.1622
Wainwright, John, Parsons, Anthony J., Müller, Eva N., Brazier, Richard E., Powell, D. Mark, Fenti, Bantigegne (2008) A transport-distance approach to scaling erosion rates: 2. sensitivity and evaluation of Mahleran. Earth Surface Processes and Landforms, 33 (6) 962-984 doi:10.1002/esp.1623
Kinnell, P. I. A. (2008) Discussion: Misrepresentation of the USLE in ‘Is sediment delivery a fallacy?’. Earth Surface Processes and Landforms, 33 (10) 1627-1629 doi:10.1002/esp.1629
Parsons, Anthony John, Cooper, James, Wainwright, John (2015) What is suspended sediment?. Earth Surface Processes and Landforms, 40 (10) 1417-1420 doi:10.1002/esp.3730
Wainwright, John, Parsons, Anthony J., Müller, Eva N., Brazier, Richard E., Powell, D. Mark (2010) Standing proud: a response to ‘Soil-erosion models: where do we really stand?’ by Smith et al. Earth Surface Processes and Landforms, 35 (11) 1349-1356 doi:10.1002/esp.2047
Wainwright, John, Parsons, Anthony J., Müller, Eva N., Brazier, Richard E., Powell, D. Mark (2009) Response to Kinnell's ‘Comment on “A transport-distance approach to scaling erosion rates: III. Evaluating scaling characteristics of Mahleran”’. Earth Surface Processes and Landforms, 34 (9) 1320-1321 doi:10.1002/esp.1816
 
and/or  
Mindat.org is an outreach project of the Hudson Institute of Mineralogy, a 501(c)(3) not-for-profit organization.
Copyright © mindat.org and the Hudson Institute of Mineralogy 1993-2025, except where stated. Most political location boundaries are © OpenStreetMap contributors. Mindat.org relies on the contributions of thousands of members and supporters. Founded in 2000 by Jolyon Ralph.
To cite: Ralph, J., Von Bargen, D., Martynov, P., Zhang, J., Que, X., Prabhu, A., Morrison, S. M., Li, W., Chen, W., & Ma, X. (2025). Mindat.org: The open access mineralogy database to accelerate data-intensive geoscience research. American Mineralogist, 110(6), 833–844. doi:10.2138/am-2024-9486.
Privacy Policy - Terms & Conditions - Contact Us / DMCA issues - Report a bug/vulnerability Current server date and time: September 15, 2025 03:09:00
Go to top of page