FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2152510867> ?p ?o ?g. }

• W2152510867 endingPage "1202" @default.
• W2152510867 startingPage "1189" @default.
• W2152510867 abstract "Effective river management strategies require an understanding of how fluvial processes vary both spatially and temporally. Here, we examine the natural range of variability in the Conejos River Valley, southern Colorado, through documentation of terrace morphostratigraphic and sedimentological characteristics as well as through investigation of sediment contributions from headwaters, hillslopes and tributary streams. Additionally, soil development and radiocarbon ages, together with local and regional paleoclimate reconstructions, were used to infer the range of processes acting in this system. Since de-glaciation, the Conejos River has fluctuated between episodes of bedrock strath formation, aggradation and vertical incision. Morphostratigraphic relationships, soil development and radiocarbon ages enable us to propose a chronology for periods of alluvial deposition (around 8·9–7·6 ka, 5·5 ka and from 3·5 to 1·1 ka), separated by intervals of fluvial incision. We infer potential forcing mechanisms by utilizing multiple working hypotheses. Specifically, we discuss the potential for increases in sediment supply during periods of (1) para-glacial adjustment, (2) climatic cooling, (3) increased frequency of climate change and (4) increased fire frequency or severity. We also consider the effects of changes in stream discharge and extreme storm occurrence. We conclude that combinations of these processes, operating at different times, have contributed to sediment mobilization since de-glaciation. Stream and landform morphology also varies longitudinally due to the influence of remnant glacial topography. In particular, valley bottom overdeepening at tributary junctions has resulted in incision and strath formation into unlithified glacial deposits (i.e. fill-cut terraces) rather than bedrock in some reaches. Overall, the Conejos fluvial system has varied significantly both temporally and spatially since de-glaciation and appears to be sensitive to changes in sediment supply related to Holocene scale climate fluctuations. This natural range of variability must therefore be a key consideration in any future stream management policies. Copyright © 2012 John Wiley & Sons, Ltd." @default.
• W2152510867 created "2016-06-24" @default.
• W2152510867 creator A5002461123 @default.
• W2152510867 creator A5069215556 @default.
• W2152510867 creator A5069727428 @default.
• W2152510867 creator A5082155833 @default.
• W2152510867 date "2012-06-19" @default.
• W2152510867 modified "2023-10-06" @default.
• W2152510867 title "Post-glacial range of variability in the Conejos River Valley, southern Colorado, USA: fluvial response to climate change and sediment supply" @default.
• W2152510867 cites W1594043601 @default.
• W2152510867 cites W1963521198 @default.
• W2152510867 cites W1971880530 @default.
• W2152510867 cites W1983807604 @default.
• W2152510867 cites W1985887943 @default.
• W2152510867 cites W1986673020 @default.
• W2152510867 cites W1989697444 @default.
• W2152510867 cites W1993737188 @default.
• W2152510867 cites W1998456714 @default.
• W2152510867 cites W1998783802 @default.
• W2152510867 cites W2020489173 @default.
• W2152510867 cites W2026259333 @default.
• W2152510867 cites W20277813 @default.
• W2152510867 cites W2036740201 @default.
• W2152510867 cites W2036807810 @default.
• W2152510867 cites W2042339500 @default.
• W2152510867 cites W2044910655 @default.
• W2152510867 cites W2045419467 @default.
• W2152510867 cites W2052495616 @default.
• W2152510867 cites W2056084716 @default.
• W2152510867 cites W2062547535 @default.
• W2152510867 cites W2067541303 @default.
• W2152510867 cites W2072380362 @default.
• W2152510867 cites W2080042998 @default.
• W2152510867 cites W2082562613 @default.
• W2152510867 cites W2087747927 @default.
• W2152510867 cites W2087828802 @default.
• W2152510867 cites W2088884065 @default.
• W2152510867 cites W2103737089 @default.
• W2152510867 cites W2107642448 @default.
• W2152510867 cites W2111204986 @default.
• W2152510867 cites W2120637384 @default.
• W2152510867 cites W2121357375 @default.
• W2152510867 cites W2125217075 @default.
• W2152510867 cites W2145313784 @default.
• W2152510867 cites W2154225016 @default.
• W2152510867 cites W2155970950 @default.
• W2152510867 cites W2160358468 @default.
• W2152510867 cites W2164161076 @default.
• W2152510867 cites W2319440775 @default.
• W2152510867 cites W2326637401 @default.
• W2152510867 cites W2329027129 @default.
• W2152510867 cites W2524104916 @default.
• W2152510867 cites W4210964572 @default.
• W2152510867 cites W4233058348 @default.
• W2152510867 cites W4242329307 @default.
• W2152510867 cites W4367435926 @default.
• W2152510867 doi "https://doi.org/10.1002/esp.3253" @default.
• W2152510867 hasPublicationYear "2012" @default.
• W2152510867 type Work @default.
• W2152510867 sameAs 2152510867 @default.
• W2152510867 citedByCount "15" @default.
• W2152510867 countsByYear W21525108672012 @default.
• W2152510867 countsByYear W21525108672013 @default.
• W2152510867 countsByYear W21525108672014 @default.
• W2152510867 countsByYear W21525108672015 @default.
• W2152510867 countsByYear W21525108672017 @default.
• W2152510867 countsByYear W21525108672019 @default.
• W2152510867 countsByYear W21525108672023 @default.
• W2152510867 crossrefType "journal-article" @default.
• W2152510867 hasAuthorship W2152510867A5002461123 @default.
• W2152510867 hasAuthorship W2152510867A5069215556 @default.
• W2152510867 hasAuthorship W2152510867A5069727428 @default.
• W2152510867 hasAuthorship W2152510867A5082155833 @default.
• W2152510867 hasConcept C100134115 @default.
• W2152510867 hasConcept C100834320 @default.
• W2152510867 hasConcept C100970517 @default.
• W2152510867 hasConcept C109007969 @default.
• W2152510867 hasConcept C111368507 @default.
• W2152510867 hasConcept C112959462 @default.
• W2152510867 hasConcept C114793014 @default.
• W2152510867 hasConcept C127313418 @default.
• W2152510867 hasConcept C132651083 @default.
• W2152510867 hasConcept C137527640 @default.
• W2152510867 hasConcept C142614818 @default.
• W2152510867 hasConcept C151730666 @default.
• W2152510867 hasConcept C15739521 @default.
• W2152510867 hasConcept C166390339 @default.
• W2152510867 hasConcept C16828302 @default.
• W2152510867 hasConcept C187320778 @default.
• W2152510867 hasConcept C205649164 @default.
• W2152510867 hasConcept C206137718 @default.
• W2152510867 hasConcept C2816523 @default.
• W2152510867 hasConcept C32552466 @default.
• W2152510867 hasConcept C58640448 @default.
• W2152510867 hasConcept C6494504 @default.
• W2152510867 hasConcept C65589250 @default.
• W2152510867 hasConcept C69823785 @default.
• W2152510867 hasConcept C76886044 @default.

• next