headward erosion वाक्य
उदाहरण वाक्य
मोबाइल
- Instead headward erosion has excavated large hoodoos that are up to high.
- The blocks will eventually erode, but will cause headward erosion of the river while it exists.
- Headward erosion and mass wasting helped to erode cliffs back into their fault-bounded plateaus, widening the basins in-between.
- Headward erosion of one of those tributaries, the Paria River, eroded north-northwestward toward what is now Paria Amphitheater.
- Dhansari river along with Kapili by headward erosion has completely isolated the Mikir hills from the Peninsular plateau.
- It has been observed at least since 1990 that a ravine of Arana Gulch appeared to indicate headward erosion due to concentration of surface runoff.
- Headward erosion is a fluvial process of erosion that lengthens a stream, a valley or a gully at its capture drainage that previously flowed to another stream.
- The current resurgence is located close to the base of the Dolomitic Conglomerate at the head of a short gorge formed by headward erosion with subsequent cavern collapse.
- Through a process called headward erosion, it gradually moved eastward, gobbling up the land around its headwaters in Pac-Man fashion, until it met up with the ancestral upper Colorado.
- Alternatively, a water gap may be formed through headward erosion of two streams on opposite sides of a ridge, ultimately resulting in the capture of one stream by the other.
- These domes intrude the glacially eroded core of the stratovolcano and headward erosion has further modified the Level Mountain shield by incising youthful V-shaped stream canyons into the lava plateau margin.
- "' Headward erosion "'is erosion at the origin of a stream channel, which causes the origin to move back away from the direction of the stream flow, and so causes the stream channel to lengthen.
- The flow reversal in lower Cedar Creek was probably accelerated by the downcutting of the St . Joseph River, which increased the velocity of its tributaries, causing them to erode toward their headwaters ( headward erosion ).
- The meta-sedimentary rock along with the granite batholith that forms Black Mountain are remnants of what laid hidden beneath a sea and underground, that are now exposed by headward erosion that continues northward today into Arizona s Transition Zone.
- Headward erosion creates three major kinds of drainage patterns : " trellis patterns " and " rectangular and angular patterns " . "'Dendritic patterns "'form in homogenous landforms where the underlying bedrock has no structural control over where the water flows.
- While additional deep testing may reveal other information, at this time the most appropriate hypothesis is to regard all of these adjacent landforms as non-cultural portions of the higher soils, dissected by centuries [ if not millennia ] of natural headward erosion and downslope weathering ."
- Changes in elevation can be due to changes in the base level ( elevation of the lowest point in the fluvial system, usually the drainage basin ) of the fluvial system, which leads to headward erosion along the length of either a stream or river, gradually lowering its elevation.
- Three kinds of streams are formed by headward erosion : " insequent streams ", " subsequent streams ", and " obsequent and resequent streams " ( " See Fluvial landforms of streams " . ) "'Insequent streams "'form by random headward erosion, usually from sheetflow of water over the landform surface.
- Three kinds of streams are formed by headward erosion : " insequent streams ", " subsequent streams ", and " obsequent and resequent streams " ( " See Fluvial landforms of streams " . ) "'Insequent streams "'form by random headward erosion, usually from sheetflow of water over the landform surface.
- The water collects in channels where the velocity and erosional power increase, cutting into and extending the heads of gullies . "'Subsequent streams "'form by selective headward erosion by cutting away at less resistive rocks in the terrain . "'Obsequent and resequent streams "'form after time in an area of insequent or subsequent streams.
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