In geomorphology, drainage systems, also known as river systems, are the patterns formed by the streams, rivers, and lakes in a particular drainage basin.They are governed by the topography of land, whether a particular region is dominated by hard or soft rocks, and the gradient of the land. Geomorphologists and hydrologists often view streams as part of drainage basins (and sub …

WikiZero Özgür Ansiklopedi - Wikipedia Okumanın En Kolay Yolu . An antecedent stream is a stream that maintains its original course and pattern despite the changes in underlying rock topography. A stream with a dendritic drainage pattern, for example, can be subject to slow tectonic uplift.However, as the uplift occurs, the stream erodes through the rising ridge to form …

An antecedent stream is a stream that maintains its original course and pattern despite the changes in underlying rock topography. A stream with a dendritic drainage pattern, for example, can be subject to slow tectonic uplift.However, as the uplift occurs, the stream erodes through the rising ridge to form a steep-walled gorge.The stream thus keeps its dendritic pattern even …

An antecedent stream is a stream that maintains its original course and pattern despite the changes in underlying rock topography. A stream with a dendritic drainage pattern, for example, can be subject to slow tectonic uplift. However, as the uplift occurs, the stream erodes through the rising ridge to form a steep-walled gorge. The stream thus keeps its dendritic pattern even …

An antecedent stream is a stream that maintains its original course and pattern despite the changes in underlying rock topography. A stream with a dendritic drainage pattern, for example, can be subject to slow tectonic uplift.However, as the uplift occurs, the stream erodes through the rising ridge to form a steep-walled gorge.The stream thus keeps its dendritic pattern even …

Antecedent drainage stream and Meuse · See more » Paradox Valley. Paradox Valley is a basin located in Montrose County in the U.S. state of Colorado. New!!: Antecedent drainage stream and Paradox Valley · See more » Stream. A stream is a body of water with surface water flowing within the bed and banks of a channel. New!!:

Aliran anteseden adalah aliran yang mempertahankan arah dan pola aslinya meskipun ada perubahan topografi batuan yang mendasarinya. Sebuah sungai dengan pola drainase dendritik , misalnya, dapat mengalami pengangkatan tektonik lambat. Namun, saat pengangkatan terjadi, sungai terkikis melalui punggung bukit yang menanjak untuk membentuk ngarai berdinding …

A water gap is usually an indication of a river that is older than the current topography. The likely occurrence is that a river established its course when the landform was at a low elevation, or by a rift in a portion of the crust of the earth having a very low stream gradient and a thick layer of unconsolidated sediment.. In a hypothetical example, a river would have established its …

Az előzménypatak olyan patak, amely a mögöttes szikladomborzat változásai ellenére megtartja eredeti folyását és mintáját. Egy dendrites vízelvezető mintájú patak például lassú tektonikus emelkedésnek lehet kitéve. A kiemelkedés során azonban a patak az emelkedő gerincen keresztül erodálódik, és egy meredek falú szurdokot képez .