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.
12.
"' 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.
13.
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 ).
14.
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.
15.
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.
16.
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 ."
17.
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.
18.
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.
19.
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.
20.
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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