FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2610264902> ?p ?o ?g. }

• W2610264902 endingPage "526" @default.
• W2610264902 startingPage "497" @default.
• W2610264902 abstract "The availability of almost 180 cosmogenic-radionuclide (CRN) surface-exposure ages from moraine boulders and glacially polished bedrock surfaces makes possible an assessment of the timing and character of the local Last Glacial Maximum (LLGM) and subsequent deglaciation in the Colorado Rocky Mountains. A review of glacial chronologies and numerical modeling results indicates that although glaciers across Colorado responded broadly synchronously, apparent differences in the timing and magnitude of glacier retreat following the LLGM suggest that spatially variable regional forcing, possibly precipitation related, played a role in glacier behavior along with more spatially uniform hemispheric or global forcing. Glaciers in the five ranges examined reached their greatest LLGM extents before ~19.5 ka and abandoned their outermost LLGM moraines between ~23.5 and 19.5 ka. Detailed deglaciation chronologies are available for glaciers in four of the ranges. In the Sawatch Range and Sangre de Cristo Mountains, glaciers were near their LLGM extents at 17-16 ka, before retreating rapidly. In the San Juan Mountains and the Front Range, glaciers may have begun their post-LLGM recession earlier, although early deglaciation is indicated by only a few ages on polished bedrock that potentially contains pre-LLGM CRN inheritance, and thus may be too old. Regardless of the timing of the onset of deglaciation, the equilibrium-line rise associated with deglaciation was earlier and significantly larger in the San Juan Mountains than elsewhere in Colorado. This suggests that the San Juan Mountains, located well to the southwest of the other ranges, may have experienced enhanced precipitation during the LLGM, as did areas farther to the south and west, while LLGM conditions may have been drier in the northern and eastern Colorado ranges. A breakdown in this pattern after the LLGM, with precipitation decreasing in the south and west and increasing in the north and east, may have led to the range-to-range differences evident across Colorado. Deglaciation was nearly complete in all four ranges by 15-13 ka. While some proxy records indicate a later Younger Dryas-age cooling in the Colorado mountains, there is not clear moraine evidence of glacier readvance at that time." @default.
• W2610264902 created "2017-05-12" @default.
• W2610264902 creator A5012944806 @default.
• W2610264902 creator A5021072172 @default.
• W2610264902 creator A5030059133 @default.
• W2610264902 creator A5044491478 @default.
• W2610264902 creator A5067273143 @default.
• W2610264902 creator A5075213796 @default.
• W2610264902 date "2017-09-15" @default.
• W2610264902 modified "2023-10-15" @default.
• W2610264902 title "Deglaciation of the Colorado Rocky Mountains following the Last Glacial Maximum" @default.
• W2610264902 cites W1510748481 @default.
• W2610264902 cites W1527877883 @default.
• W2610264902 cites W1583628187 @default.
• W2610264902 cites W1812912021 @default.
• W2610264902 cites W1965426804 @default.
• W2610264902 cites W1966836679 @default.
• W2610264902 cites W1966928908 @default.
• W2610264902 cites W1969157568 @default.
• W2610264902 cites W1970872609 @default.
• W2610264902 cites W1971816180 @default.
• W2610264902 cites W1972895771 @default.
• W2610264902 cites W1976730890 @default.
• W2610264902 cites W1990237783 @default.
• W2610264902 cites W1992207643 @default.
• W2610264902 cites W1994358999 @default.
• W2610264902 cites W1996862213 @default.
• W2610264902 cites W2001072306 @default.
• W2610264902 cites W2005035365 @default.
• W2610264902 cites W2016446254 @default.
• W2610264902 cites W2026538666 @default.
• W2610264902 cites W2036280628 @default.
• W2610264902 cites W2036807810 @default.
• W2610264902 cites W2038577130 @default.
• W2610264902 cites W2040721671 @default.
• W2610264902 cites W2046343174 @default.
• W2610264902 cites W2047643658 @default.
• W2610264902 cites W2051826231 @default.
• W2610264902 cites W2054707461 @default.
• W2610264902 cites W2055136587 @default.
• W2610264902 cites W2057015756 @default.
• W2610264902 cites W2068401541 @default.
• W2610264902 cites W2071855417 @default.
• W2610264902 cites W2072476947 @default.
• W2610264902 cites W2078721910 @default.
• W2610264902 cites W2090386668 @default.
• W2610264902 cites W2111801219 @default.
• W2610264902 cites W2114319241 @default.
• W2610264902 cites W2125600063 @default.
• W2610264902 cites W2129040983 @default.
• W2610264902 cites W2132999078 @default.
• W2610264902 cites W2156208893 @default.
• W2610264902 cites W2160114818 @default.
• W2610264902 cites W2161699056 @default.
• W2610264902 cites W2162052046 @default.
• W2610264902 cites W2165563985 @default.
• W2610264902 cites W2168674057 @default.
• W2610264902 cites W2171420618 @default.
• W2610264902 cites W2171768006 @default.
• W2610264902 cites W2406136941 @default.
• W2610264902 cites W2520135012 @default.
• W2610264902 cites W2594505707 @default.
• W2610264902 cites W54453798 @default.
• W2610264902 cites W63635716 @default.
• W2610264902 doi "https://doi.org/10.18172/cig.3234" @default.
• W2610264902 hasPublicationYear "2017" @default.
• W2610264902 type Work @default.
• W2610264902 sameAs 2610264902 @default.
• W2610264902 citedByCount "13" @default.
• W2610264902 countsByYear W26102649022018 @default.
• W2610264902 countsByYear W26102649022019 @default.
• W2610264902 countsByYear W26102649022020 @default.
• W2610264902 countsByYear W26102649022022 @default.
• W2610264902 countsByYear W26102649022023 @default.
• W2610264902 crossrefType "journal-article" @default.
• W2610264902 hasAuthorship W2610264902A5012944806 @default.
• W2610264902 hasAuthorship W2610264902A5021072172 @default.
• W2610264902 hasAuthorship W2610264902A5030059133 @default.
• W2610264902 hasAuthorship W2610264902A5044491478 @default.
• W2610264902 hasAuthorship W2610264902A5067273143 @default.
• W2610264902 hasAuthorship W2610264902A5075213796 @default.
• W2610264902 hasBestOaLocation W26102649021 @default.
• W2610264902 hasConcept C100834320 @default.
• W2610264902 hasConcept C100970517 @default.
• W2610264902 hasConcept C114793014 @default.
• W2610264902 hasConcept C127313418 @default.
• W2610264902 hasConcept C137527640 @default.
• W2610264902 hasConcept C15739521 @default.
• W2610264902 hasConcept C15785411 @default.
• W2610264902 hasConcept C180705331 @default.
• W2610264902 hasConcept C188291805 @default.
• W2610264902 hasConcept C20116678 @default.
• W2610264902 hasConcept C205649164 @default.
• W2610264902 hasConceptScore W2610264902C100834320 @default.
• W2610264902 hasConceptScore W2610264902C100970517 @default.
• W2610264902 hasConceptScore W2610264902C114793014 @default.
• W2610264902 hasConceptScore W2610264902C127313418 @default.
• W2610264902 hasConceptScore W2610264902C137527640 @default.

• next