✦ LIBER ✦

Flood and vortex scour of the channel bed of the Prosna river, and their depth range

✍ Scribed by Zygmunt Młynarczyk; Karol Rotnicki

Publisher: John Wiley and Sons
Year: 1989
Tongue: English
Weight: 615 KB
Volume: 14
Category: Article
ISSN: 0360-1269
DOI: 10.1002/esp.3290140502

No coin nor oath required. For personal study only.

📜 SIMILAR VOLUMES

Channel form and processes of the flood-

Channel form and processes of the flood-dominated Narmada River, India

✍ S. N. Rajaguru; Avijit Gupta; V. S. Kale; Sheila Mishra; R. K. Ganjoo; L. L. Ely 📂 Article 📅 1995 🏛 John Wiley and Sons 🌐 English ⚖ 1020 KB

Channel change and the significance of f

Channel change and the significance of floodplain stratigraphy: 1990 flood event, lower river Tay, Scotland

✍ D. J. Gilvear; D. J. Harrison 📂 Article 📅 1991 🏛 John Wiley and Sons 🌐 English ⚖ 858 KB

Flood and Megaflood Processes and Deposi

Flood and Megaflood Processes and Deposits || Use of Remote Sensing in Monitoring River Floods and their Effects on the Landscape

✍ Martini, I. Peter; Baker, Victor R.; Garzn, Guillermina 📂 Article 📅 2002 🏛 Blackwell Publishing Ltd. 🌐 English ⚖ 652 KB

The objective of this study is to establish a procedure for estimating the effects of river floods in large areas utilizing remote sensing satellite data. Floods usually occur unexpectedly and generally last a short time. Satellite image data can show floods instantaneously over tens of thousands of

CHANGES IN THE MAGNITUDE AND TRANSFORMAT

CHANGES IN THE MAGNITUDE AND TRANSFORMATION OF FLOOD WAVES SUBSEQUENT TO THE CHANNELIZATION OF THE RABA RIVER, POLISH CARPATHIANS

✍ WYZGA, BARTLOMIEJ 📂 Article 📅 1996 🏛 John Wiley and Sons 🌐 English ⚖ 1019 KB

Alterations in flood flows of the Raba River are examined to determine the influence exerted on flood waves by changing morphological conditions. With stable vertical channel position, the river increased its sinuosity during the 1920s to 1940s, and the change was accompanied by a growing tendency t

Persistence of the surface texture of a

Persistence of the surface texture of a gravel-bed river during a large flood

✍ Jordan A. Clayton; John Pitlick 📂 Article 📅 2008 🏛 John Wiley and Sons 🌐 English ⚖ 742 KB

The distribution and residence time of s

The distribution and residence time of suspended sediment stored within the channel margins of a gravel-bed bedrock river

✍ Katherine Skalak; James Pizzuto 📂 Article 📅 2010 🏛 John Wiley and Sons 🌐 English ⚖ 285 KB 👁 1 views

## Abstract Previously undocumented deposits are described that store suspended sediment in gravel‐bedded rivers, termed ‘fine‐grained channel margin’ (FGCM) deposits. FGCM deposits consist of sand, silt, clay, and organic matter that accumulate behind large woody debris (LWD) along the margins of