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- Q1069618 subject Q6926752.
- Q1069618 subject Q6965877.
- Q1069618 subject Q8663676.
- Q1069618 abstract "Fluvial terraces are elongated terraces that flank the sides of floodplains and fluvial valleys all over the world. They consist of a relatively level strip of land, called a “tread,” separated from either an adjacent floodplain, other fluvial terraces, or uplands by distinctly steeper strips of land called “risers.” These terraces lie parallel to and above the river channel and its floodplain. Because of the manner in which they form, fluvial terraces are underlain by fluvial sediments of highly variable thickness.Fluvial terraces are the remnants of earlier floodplains that existed at a time when either a stream or river was flowing at a higher elevation before its channel downcut to create a new floodplain at a lower elevation. 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. For example, downcutting by a river can lead to increased velocity of a tributary, causing that tributary to erode toward its headwaters. Terraces can also be left behind when the volume of the fluvial flow declines due to changes in climate, typical of areas which were covered by ice during periods of glaciation, and their adjacent drainage basins.".
- Q1069618 thumbnail Kanab_Creek_fill_terrace_1939.jpg?width=300.
- Q1069618 wikiPageWikiLink Q11465.
- Q1069618 wikiPageWikiLink Q1434465.
- Q1069618 wikiPageWikiLink Q166620.
- Q1069618 wikiPageWikiLink Q180184.
- Q1069618 wikiPageWikiLink Q193110.
- Q1069618 wikiPageWikiLink Q1987070.
- Q1069618 wikiPageWikiLink Q23392.
- Q1069618 wikiPageWikiLink Q2616063.
- Q1069618 wikiPageWikiLink Q271669.
- Q1069618 wikiPageWikiLink Q39816.
- Q1069618 wikiPageWikiLink Q4022.
- Q1069618 wikiPageWikiLink Q4478339.
- Q1069618 wikiPageWikiLink Q47521.
- Q1069618 wikiPageWikiLink Q5303078.
- Q1069618 wikiPageWikiLink Q602963.
- Q1069618 wikiPageWikiLink Q6185405.
- Q1069618 wikiPageWikiLink Q6926752.
- Q1069618 wikiPageWikiLink Q6965877.
- Q1069618 wikiPageWikiLink Q7310579.
- Q1069618 wikiPageWikiLink Q7622670.
- Q1069618 wikiPageWikiLink Q7937.
- Q1069618 wikiPageWikiLink Q80026.
- Q1069618 wikiPageWikiLink Q828581.
- Q1069618 wikiPageWikiLink Q8663676.
- Q1069618 wikiPageWikiLink Q889515.
- Q1069618 comment "Fluvial terraces are elongated terraces that flank the sides of floodplains and fluvial valleys all over the world. They consist of a relatively level strip of land, called a “tread,” separated from either an adjacent floodplain, other fluvial terraces, or uplands by distinctly steeper strips of land called “risers.” These terraces lie parallel to and above the river channel and its floodplain.".
- Q1069618 label "Fluvial terrace".
- Q1069618 depiction Kanab_Creek_fill_terrace_1939.jpg.