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  • Zuckerrübenanbau im Red-River-Valley (Culture de la betterave sucrière dans la Red river Valley)
  • Agriculture ; Betterave à sucre ; Etats-Unis ; Géographie de l'Amérique ; Marché intérieur ; North Dakota ; Produit agricole ; Red river valley ; Région agricole ; Régulation du marché ; Sucre ; Variété hybride
  • Water in the Red River valley of the North
  • ; Irrigation ; Lutte contre les crues ; Manitoba ; Minnesota ; North Dakota ; Red River ; Ressources en eau ; Régularisation ; Sol irrigable ; Vallée
  • The Red River valley is a homogeneous physical region that is partitioned between two countries and among two states and one province. Problems of water surpluses and water deficits are common to the valley. Flood protection is better developed
  • in the Canadian portion than in the American portion of the valley. State and provincial governments have promoted, with varying degree of success, an integrated approach to local water management.
  • Spatial and temporal variation of runoff of Red River Basin in Yunnan
  • China ; Climatic change ; Climatic data ; Evaporation ; Geographical information system ; Mountain ; Precipitation ; Runoff ; Spatial variation ; Stream ; Temperature ; Valley ; Watershed ; Yunnan
  • This paper studies the variation of runoff of Red River Basin and discusses the influence of corridor-barrier functions of valleys and mountains on variation of runoff by using GIS and statistic methods based on the monthly precipitation
  • , temperature and evaporation data from 1960 to 2000 at 32 meteorological stations in Red River Basin, and the annual runoff data of Yuanjiang River, Lixian River and Panlong River from 1956 to 2000. These 3 river basins are contrasted. Results and discussion.
  • [b1] Asian International Rivers Center, Yunnan University, Kunming, Chine
  • Monitoring the 1997 flood in the Red River Valley using hydrologic regimes and RADARSAT imagery
  • Canada ; Cartographie ; Cours d'eau ; Crue ; Date 1997 ; Image sar ; Inondation ; Manitoba ; Mesure de terrain ; Red River ; Régime hydrologique ; Télédétection
  • Magnetostratigraphy, biostratigraphy and geochronology of Cretaceous-Tertiary boundary sediments, Red Deer Valley
  • Alberta ; Biostratigraphie ; Canada ; Datation K-Ar ; Ere secondaire ; Ere tertiaire ; Géochronologie ; Géographie physique ; Limite stratigraphique ; Magnétostratigraphie ; Paléogéographie ; Red Deer Valley ; Stratigraphie
  • Valleys and river benches from the viewpoint of morphotectonics
  • Concept ; Fluvial processes ; Hydrogeology ; Valley
  • The geomorphological concepts on the formation of valleys and river benches applied until now have been based upon the viewpoints of dynamic and climatic geomorphology. This exogenous interpretation should be abandoned and an endogenous concept
  • The Late Wisconsinan savanna terrace in tributaries to the upper Mississippi River
  • The Savanna Terrace, composed of alternating red and gray clayey sediments of late Wisconsinan age, is the highest glaciofluvial-lacustrine deposit without a loess cover in the upper Mississippi valley. Chemical, physical, and mineralogical data
  • show that two different sources provided sediment. Radiocarbon dates obtained from the lower Illinois valley indicate that the terrace sediments were deposited sometime between about 13,100 and 9 500 years ago. Soils developed on the terrace
  • Aspects du bilan d'énergie de surface les plus importants pour le développement d'une fonte rapide des neiges au cours du printemps 1997 dans la Red River Valley du Dakota du Nord et du Minnesota. La fonte rapide des neiges d'un amas
  • The evolution of the Vistula river valley between Cracow and Niepołomice in late Vistulian and Holocene times
  • Evolution of the Vistula river valley during the last 15 000 years, part IV
  • Alluvium ; Climatic variation ; Drainage network ; Fluvial processes ; Holocene ; Human impact ; Poland ; Quaternary ; Sedimentology ; Valley ; Valley floor evolution ; Wisła
  • This is a new synthesis of the evolution of the section of the Vistula river valley. There are changes in the channel patterns and parameters, sedimentological characteristics of the different alluvial deposits of different ages, the reflection
  • of both climatic fluctuation and human activity in the valley floor morphology and in alluvia. - (DG)
  • Variability of the morphometric characteristics of valley networks caused by variations in a scale
  • Drainage network ; Fractals ; Geomorphometry ; Spatial scale ; Valley
  • Escala espacial ; Fractal ; Geomorfometría ; Red de drenaje ; Valle
  • This article indicates the quantitative tools, with assistance of which it is possible to characterize the morphology (shape) of the valley network and determine their variability caused by the scale change. The monitored morphometric
  • characteristics (quantitative tools) have been applied to the paradigmatic examples of the schematic valley networks and have been analyzed in three scales. In order to analyze the valley networks, the most suitable are “valley junction angles” and “homogeneity
  • of various order valleys”, where the relevant values dropped while increasing the scale, but the normal (Gauss) distribution of values was preserved. - (EN)
  • Development and chronology of the lower Vistula River valley, North Poland
  • The lower Colorado River valley : a Pleistocene desert
  • Colorado River Valley ; Domaine aride ; Etats-Unis ; Géographie de l'Amérique ; Histoire de la végétation ; Pléistocène supérieur ; Quaternaire zone chaude ; Végétation ; Zone subtropicale
  • A chronological sequence of plant macrofossil assemblages from twenty-five pack rat middens provides a record of desert scrub vegetation for most of the last 13,380 yr BP from a hyperarid portion of the lower Colorado River Valley.
  • Late Holocene valley-bottom aggradation and erosion in the South Loup River Valley, Nebraska
  • The chronology of aggradation and erosion is developed from ten radiocarbon ages. After discussing fluvial erosion and floodplain aggradation in the South Loup River Valley, the paper reconstructs the late Holocene alluvial records of the North
  • and Middle Loup River Valleys from published reports and articles.
  • for major logjams and rafts on Red, Atchafalaya, and Colorado Rivers on the Gulf Coast, which blocked navigation from tens to hundreds of kilometers in the 1800s. Results from Hurricane Rita suggest that blowdown into channels alone - not withstanding
  • blowdown elsewhere in the river valleys or along tributaries which could deliver large woody debris to the river - is sufficient to completely block channels, thus providing a plausible mechanism for initiating such (pre)historic log rafts.
  • Hurricane Rita which struck the US Gulf Coast near the Louisiana/Texas border in 2005, did not cause extensive river flooding. However, the storm did result in extensive forest damage and tree blowdown. High-resolution post-storm aerial photography
  • allowed an inventory of river bank trees blown into the channel along the lower Neches and Sabine Rivers of southeast Texas and southwest Louisiana. The Rita blowdown inventory also allowed an assessment of whether similar blowdown events could account
  • Holocene development of the River Lippe valley, Germany : a case study of anthropogenic influence
  • Channel geometry ; Fluvial terrace ; Germany ; Holocene ; Human impact ; Hydraulic works ; Meander ; Model ; North Rhine Westfalia ; Palaeohydrology ; River bed ; Stream
  • This article describes the Inselterrasse and Aue in detail and explains the Holocene development of the Lippe valley floor morphology, which is atypical for a central European river. It is shown that morphological evolution of the Lippe valley floor
  • is a special case of anthropogenic influence that might be an interesting addition to previous studies of human impacts on palaeohydrology, channel change and valley floor development (Gregory, 1995; Brown, 1996; Kalicki,1996).
  • Outlines of the late Quaternary history of the Drentsche Aa Valley (Drente, The Neteherlands)
  • An outline is given of the geomorphology and Late Quaternary history of the Drentsche Aa valley. The valley sediments are subdivided in fluvial, slope and aeolian sediments on lithological arguments. The vertical succession of the river valley
  • sediments demonstrates a decreasing fluvial activity during the Weichselian. Tentatively four erosion phases are distinguished in the valley system.
  • River valleys as elements of the system of protected areas in the Lublin administrative district
  • Environment ; Lublin ; Nature conservation ; Poland ; Protected area ; Stream ; Valley
  • This article presents results of the research on the protection of the river valleys of Lublin Voivodeship. To determine the degree of protection of the river valleys cartometric methods based on the available maps and the Ministry of Environment
  • the protected areas, there are 70% of the length of the river. In this system of protection, fragmentation of the valleys is significant. None of the major rivers of the region, including the Vistula and the Bug, is not protected throughout in their length
  • and Office of Spatial Planning in Lublin data are used. The results of researches made that the protected landscape areas are element of the system of protected areas, which includes the highest percentage of river length in region (over 13%). Outside
  • Calle ; Casco urbano ; Esfahan ; Irán ; Khuzestan ; Red urbana ; Relieve ; Suburbio ; Yazd
  • This article shows that landforms have significant effects on the city shape and street patterns of the fast-growing Iranian cities of Dezful (a river) and Khorramabad (mountains and valleys), but no clear effects on the cities of Yazd and Nain
  • Influence of logjam-formed hard points on the formation of valley-bottom landforms in an old-growth forest valley, Queets River, Washington, USA
  • Floodplain ; Fluvial landform ; Forest ; Impact ; Terrace ; United States of America ; Valley ; Washington State
  • Des enquêtes de terrain et la datation au carbone 14 des logjams fossiles dans une vieille forêt de vallée démontrent la formation de points durs résistants à l'érosion dans la plaine d'inondation de Queets River, Washington.
  • Análisis de regresión ; Balance sedimentario ; Campo árido ; Cuenca hidrográfica ; Erosión de las riberas ; Geomorfometría ; Hidrología ; Hipsometría ; Jordania ; Oued ; Red de drenaje
  • This study addresses the morphometric variables that determine the sediment yield in Wadi Al-Arja through the analysis of the impact of different morphometric characteristics along the course of the valley on its sediment yield, as well
  • as the analysis of spatial and formal dimensions and morphologies of the basin and its relationship to the sediment yield. The study also addresses the size of variation in the volume of sediment yield of the river tributaries that make up the water network
  • of the valley under the differences of its morphometric and hydrological characteristics. The results of the step-wise regression analysis confirmed the importance of the morphometric and hydrological variables, and plant coverage in interpreting the variation
  • in the size of the sediment yield of the river tributaries of different stream order in Wadi Al-Arja basin.