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- Base_level abstract "The base level of a river or stream is the lowest point to which it can flow, often referred to as the 'mouth of the river'. For large rivers, sea level is usually the base level, but a large river or lake is likewise the base level for tributary streams. All rivers and streams erode toward sea level, which is also known as the "ultimate base level." If a river is dammed, a new base level (the level of the reservoir) replaces the ultimate base level. As a result, the stream’s base level is raised. Consequently, this reduces the stream’s velocity, leads to deposition, and a reduction of the gradient upstream from the reservoir. A rather rare exception can be seen in the Jordan River, for which the base level is the Dead Sea, 417 m below modern sea level. Base level is also significant for subsurface drainage. A low base level is a prerequisite for the formation of karst topography, a network of sinkholes and caverns that can develop as slightly acidic groundwater enlarges joints (by solution) in limestone rock. Often this network of underground drainage feeds back to surface drainage along the edges of larger rivers, which are the effective base level.When the source of a stream is very high relative to its base level (high stream gradient), erosion proceeds rapidly due to the energy of the rapidly moving water and the topography becomes rugged, and it is considered a young stream (geologically speaking). When erosion has acted for a long geologic time, wearing down the high points and making a small difference between the source and the base level of a stream (low stream gradient), then the stream is called mature. Mature stream valleys have gentle slopes, rounded higher points and meandering courses.A very hard layer of rock can form a temporary base level, until it is cut through. For example, Lockport dolomite has created a temporary base level for the Niagara River. Eventually this will be cut through as Niagara Falls recedes, and Lake Erie will be drained to near the lower base level of Lake Ontario.Movements of land can greatly affect base levels. As an illustration, the uplift of the Colorado Plateau, combined with the opening of the Gulf of California to the sea, established sea level as the base level for the Colorado River and led to the (geologically) rapid erosion that resulted in the Grand Canyon.The many meanders of the Kentucky River show that it was a mature stream with little relief. Uplift of the central Kentucky area rejuvenated the stream, causing it to cut a deep canyon, but preserving the meanders that indicate the stream existed prior to the uplift.Other geologic processes can affect base levels. In the Finger Lakes of New York, Ice age glaciation greatly deepened the lake valleys and rejuvenated tributary streams. These streams have deep ravines and often waterfalls where hard rock layers slow erosion; they are said to be hanging valleys. Sea level can also change (primarily due to the formation or melting of continental ice sheets), and raise or lower the final base level for coastal rivers. Along the east coast of North America, river valleys extend out onto the continental shelf, indicating a time when erosion was possible due to the lower base level of a lower sea level in the past. Today many of these same rivers end in bays, indicating that sea level has risen in recent geologic time. This is referred to as a drowned coastline.".
- Base_level thumbnail Desembocadura_del_Ebro.jpg?width=300.
- Base_level wikiPageID "621549".
- Base_level wikiPageLength "4006".
- Base_level wikiPageOutDegree "35".
- Base_level wikiPageRevisionID "639700465".
- Base_level wikiPageWikiLink Bay.
- Base_level wikiPageWikiLink Category:Erosion.
- Base_level wikiPageWikiLink Category:Geomorphology.
- Base_level wikiPageWikiLink Cave.
- Base_level wikiPageWikiLink Cavern.
- Base_level wikiPageWikiLink Colorado_Plateau.
- Base_level wikiPageWikiLink Colorado_River.
- Base_level wikiPageWikiLink Continental_shelf.
- Base_level wikiPageWikiLink Dead_Sea.
- Base_level wikiPageWikiLink Drowned_coastline.
- Base_level wikiPageWikiLink Finger_Lakes.
- Base_level wikiPageWikiLink Glacier.
- Base_level wikiPageWikiLink Grand_Canyon.
- Base_level wikiPageWikiLink Gulf_of_California.
- Base_level wikiPageWikiLink Ice_age.
- Base_level wikiPageWikiLink Jordan_River.
- Base_level wikiPageWikiLink Karst.
- Base_level wikiPageWikiLink Karst_topography.
- Base_level wikiPageWikiLink Kentucky.
- Base_level wikiPageWikiLink Kentucky_River.
- Base_level wikiPageWikiLink Lake.
- Base_level wikiPageWikiLink Lake_Erie.
- Base_level wikiPageWikiLink Lake_Ontario.
- Base_level wikiPageWikiLink Limestone.
- Base_level wikiPageWikiLink Meander.
- Base_level wikiPageWikiLink New_York.
- Base_level wikiPageWikiLink Niagara_Falls.
- Base_level wikiPageWikiLink Niagara_River.
- Base_level wikiPageWikiLink North_America.
- Base_level wikiPageWikiLink River.
- Base_level wikiPageWikiLink River_mouth.
- Base_level wikiPageWikiLink Sea_level.
- Base_level wikiPageWikiLink Sinkhole.
- Base_level wikiPageWikiLink Solution.
- Base_level wikiPageWikiLink Stream.
- Base_level wikiPageWikiLink Stream_gradient.
- Base_level wikiPageWikiLink Submergent_coastline.
- Base_level wikiPageWikiLink File:Desembocadura_del_Ebro.jpg.
- Base_level wikiPageWikiLinkText "Base level".
- Base_level wikiPageWikiLinkText "River Mouth".
- Base_level wikiPageWikiLinkText "River mouth".
- Base_level wikiPageWikiLinkText "base level".
- Base_level wikiPageWikiLinkText "discharges into it".
- Base_level hasPhotoCollection Base_level.
- Base_level wikiPageUsesTemplate Template:Reflist.
- Base_level wikiPageUsesTemplate Template:River_morphology.
- Base_level subject Category:Erosion.
- Base_level subject Category:Geomorphology.
- Base_level hypernym Point.
- Base_level type Article.
- Base_level type Place.
- Base_level type Article.
- Base_level type Process.
- Base_level type Science.
- Base_level type Subfield.
- Base_level comment "The base level of a river or stream is the lowest point to which it can flow, often referred to as the 'mouth of the river'. For large rivers, sea level is usually the base level, but a large river or lake is likewise the base level for tributary streams. All rivers and streams erode toward sea level, which is also known as the "ultimate base level." If a river is dammed, a new base level (the level of the reservoir) replaces the ultimate base level.".
- Base_level label "Base level".
- Base_level sameAs Desembocadura.
- Base_level sameAs Desembocadura.
- Base_level sameAs Erosionsbasis.
- Base_level sameAs Desembocadura.
- Base_level sameAs Erosioonibaas.
- Base_level sameAs Bokale.
- Base_level sameAs سطح_مبنا.
- Base_level sameAs Niveau_de_base.
- Base_level sameAs בסיס_סחיפה.
- Base_level sameAs Livello_di_base.
- Base_level sameAs 侵食基準面.
- Base_level sameAs Foz.
- Base_level sameAs m.02xkrz.
- Base_level sameAs Q423794.
- Base_level sameAs Q423794.
- Base_level wasDerivedFrom Base_level?oldid=639700465.
- Base_level depiction Desembocadura_del_Ebro.jpg.
- Base_level isPrimaryTopicOf Base_level.