Item talk:Q239512
From geokb
{
"USGS Publications Warehouse": { "@context": "https://schema.org", "@type": "Article", "additionalType": "Journal Article", "name": "Dating of river terraces along Lefthand Creek, western High Plains, Colorado, reveals punctuated incision", "identifier": [ { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "70189792", "url": "https://pubs.usgs.gov/publication/70189792" }, { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 70189792 }, { "@type": "PropertyValue", "propertyID": "DOI", "value": "10.1016/j.geomorph.2017.04.044", "url": "https://doi.org/10.1016/j.geomorph.2017.04.044" } ], "journal": { "@type": "Periodical", "name": "Geomorphology", "volumeNumber": "295", "issueNumber": null }, "bookEdition": "295", "inLanguage": "en", "isPartOf": [ { "@type": "CreativeWorkSeries", "name": "Geomorphology" } ], "datePublished": "2017", "dateModified": "2017-07-25", "abstract": "The response of erosional landscapes to Quaternary climate oscillations is recorded in fluvial terraces whose quantitative interpretation requires numerical ages. We investigate gravel-capped strath terraces along the western edge of Colorado's High Plains to constrain the incision history of this shale-dominated landscape. We use \u00b9\u2070Be and \u00b2\u2076Al cosmogenic radionuclides (CRNs), optically stimulated luminescence (OSL), and thermally transferred OSL (TT-OSL) to date three strath terraces, all beveled in shale bedrock and then deposited upon by Lefthand Creek, which drains the crystalline core of the Front Range. Our study reveals: (i) a long history (hundreds of thousands of years) of fluvial occupation of the second highest terrace, T2 (Table Mountain), with fluvial abandonment at 92 \u00b1 3 ka; (ii) a brief occupation of a narrow and spatially confined terrace, T3, at 98 \u00b1 7 ka; and (iii) a 10\u201325 thousand year period of cutting and fluvial occupation of a lower terrace, T4, marked by the deposition of a lower alluvial unit between 59 and 68 ka, followed by deposition of an upper alluvial package at 40 \u00b1 3 ka. In conjunction with other recent CRN studies of strath terraces along the Colorado Front Range (Riihimaki et al., 2006; D\u00fchnforth et al., 2012), our data reveal that long periods of lateral planation and fluvial occupation of strath terraces, sometimes lasting several glacial-interglacial cycles, are punctuated by brief episodes of rapid vertical bedrock incision. These data call into question what a singular terrace age represents, as the strath may be cut at one time (its cutting-age) and the terrace surface may be abandoned at a much later time (its abandonment age), and challenge models of strath terraces that appeal to simple pacing by the glacial-interglacial cycles.", "description": "15 p.", "publisher": { "@type": "Organization", "name": "Elsevier" }, "author": [ { "@type": "Person", "name": "Mahan, Shannon A. smahan@usgs.gov", "givenName": "Shannon A.", "familyName": "Mahan", "email": "smahan@usgs.gov", "identifier": { "@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0001-5214-7774", "url": "https://orcid.org/0000-0001-5214-7774" }, "affiliation": [ { "@type": "Organization", "name": "Geosciences and Environmental Change Science Center", "url": "https://www.usgs.gov/centers/geosciences-and-environmental-change-science-center" } ] }, { "@type": "Person", "name": "Foster, Melissa A.", "givenName": "Melissa A.", 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