Search results
Results from the WOW.Com Content Network
The thalweg of a river. In geography, hydrography, and fluvial geomorphology, a thalweg or talweg (/ ˈ t ɑː l v ɛ ɡ /) is the line or curve of lowest elevation within a valley or watercourse. [1] Its vertical position in maps is the nadir (greatest depth, sounding) in the stream profile.
The thalweg legal principle states that if the border between two political entities is stated to be a waterway without further description (e.g. a median line, right bank, eastern shore, low tide line, etc.), the boundary follows the thalweg of that watercourse; in particular, the boundary follows the center of the principal navigable channel ...
Grassed waterway in Velm, Belgium, during a sunny day. A grassed waterway is a 2-metre (6.6 ft) to 48-metre-wide (157 ft) native grassland strip of green belt.It is generally installed in the thalweg, the deepest continuous line along a valley or watercourse, of a cultivated dry valley in order to control erosion.
The line of maximum depth, or channel, is the thalweg or thalweg line. It is typically designated the borderline when rivers are used as political borders. The thalweg hugs the outer banks and returns to center over the riffles. The meander arc length is the distance along the thalweg over one meander. The river length is the length along the ...
A wide variety of river and stream channel types exist in limnology, the study of inland waters.All these can be divided into two groups by using the water-flow gradient as either low gradient channels for streams or rivers with less than two percent (2%) flow gradient, or high gradient channels for those with greater than a 2% gradient.
Retrieved from "https://en.wikipedia.org/w/index.php?title=Thalweg_Doctrine&oldid=352893489"This page was last edited on 30 March 2010, at 04:50 (UTC). (UTC).
The parties had agreed that the state line was the thalweg, or steamboat channel, of the Mississippi River as it flows west and southward between the states.Nordbye heard evidence and was presented exhibits and maps which showed that the migration of the Mississippi River northward and west continued until about 1912.
Experimental verifications of the Onsager reciprocal relations were collected and analyzed by D. G. Miller [2] for many classes of irreversible processes, namely for thermoelectricity, electrokinetics, transference in electrolytic solutions, diffusion, conduction of heat and electricity in anisotropic solids, thermomagnetism and galvanomagnetism.