FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1988698844> ?p ?o ?g. }

• W1988698844 endingPage "1773" @default.
• W1988698844 startingPage "1753" @default.
• W1988698844 abstract "Bridge Glacier is a prominent eastward-flowing valley glacier located on the east side of the Pacific Ranges within the southern British Columbia Coast Mountains. The terminus of Bridge Glacier has retreated at rates up to 125 m/year over the last 50 years and currently calves into proglacial Bridge Lake. Field investigations of the recently deglaciated terrain and moraines led to the discovery of detrital boles and glacially sheared stumps. Dendroglaciological analyses of this subfossil wood produced five radiocarbon-controlled floating tree-ring chronologies. The relative age and stratigraphic location of these samples revealed that Bridge Glacier experienced at least four periods of significant advance during the late Holocene: a Tiedemann-aged advance ca. 3000 14 C years BP, an unattributed advance ca. 1900 14 C years BP, a first millennium advance ca. 1500 14 C years BP, and a Little Ice Age advance beginning ca. 700 14 C years BP. Lichenometric investigations at eight terminal and lateral moraine complexes identified early Little Ice Age moraine stabilization during the late 13th to early 14th centuries, with subsequent ice-front oscillations ending in the middle 15th, early 16th, middle to late 17th, early 18th, middle to late 19th, and early 20th centuries. These investigations build upon previous research and compliment recent geobotanical evidence emerging from other glaciers in this region that describe multiple late Holocene glacier advances. The discovery of a glacially sheared whitebark pine stump dating to 1500 ± 50 14 C years BP provides irrevocable proof for an advance of Bridge Glacier during a time when glaciers throughout Pacific North America were also expanding." @default.
• W1988698844 created "2016-06-24" @default.
• W1988698844 creator A5010655864 @default.
• W1988698844 creator A5071709984 @default.
• W1988698844 date "2007-12-01" @default.
• W1988698844 modified "2023-10-18" @default.
• W1988698844 title "Late Holocene glacial activity of Bridge Glacier, British Columbia Coast Mountains" @default.
• W1988698844 cites W1881638488 @default.
• W1988698844 cites W1927648166 @default.
• W1988698844 cites W2001242932 @default.
• W1988698844 cites W2002068414 @default.
• W1988698844 cites W2018126594 @default.
• W1988698844 cites W2020066000 @default.
• W1988698844 cites W2026432050 @default.
• W1988698844 cites W2036806968 @default.
• W1988698844 cites W20633688 @default.
• W1988698844 cites W2070308957 @default.
• W1988698844 cites W2072030233 @default.
• W1988698844 cites W2084474243 @default.
• W1988698844 cites W2085437517 @default.
• W1988698844 cites W2088785500 @default.
• W1988698844 cites W2091146354 @default.
• W1988698844 cites W2104842070 @default.
• W1988698844 cites W2108030225 @default.
• W1988698844 cites W2108283405 @default.
• W1988698844 cites W2121886152 @default.
• W1988698844 cites W2129016148 @default.
• W1988698844 cites W2149238852 @default.
• W1988698844 cites W2153966666 @default.
• W1988698844 cites W2154276443 @default.
• W1988698844 cites W2156288258 @default.
• W1988698844 cites W2161925367 @default.
• W1988698844 cites W2167335879 @default.
• W1988698844 cites W2168678027 @default.
• W1988698844 cites W2180558051 @default.
• W1988698844 cites W2280624662 @default.
• W1988698844 cites W2475122422 @default.
• W1988698844 cites W2509202485 @default.
• W1988698844 cites W2795622292 @default.
• W1988698844 doi "https://doi.org/10.1139/e07-059" @default.
• W1988698844 hasPublicationYear "2007" @default.
• W1988698844 type Work @default.
• W1988698844 sameAs 1988698844 @default.
• W1988698844 citedByCount "40" @default.
• W1988698844 countsByYear W19886988442012 @default.
• W1988698844 countsByYear W19886988442013 @default.
• W1988698844 countsByYear W19886988442014 @default.
• W1988698844 countsByYear W19886988442015 @default.
• W1988698844 countsByYear W19886988442016 @default.
• W1988698844 countsByYear W19886988442018 @default.
• W1988698844 countsByYear W19886988442019 @default.
• W1988698844 countsByYear W19886988442020 @default.
• W1988698844 countsByYear W19886988442021 @default.
• W1988698844 countsByYear W19886988442022 @default.
• W1988698844 crossrefType "journal-article" @default.
• W1988698844 hasAuthorship W1988698844A5010655864 @default.
• W1988698844 hasAuthorship W1988698844A5071709984 @default.
• W1988698844 hasConcept C100134115 @default.
• W1988698844 hasConcept C100834320 @default.
• W1988698844 hasConcept C100970517 @default.
• W1988698844 hasConcept C104932425 @default.
• W1988698844 hasConcept C111368507 @default.
• W1988698844 hasConcept C117935615 @default.
• W1988698844 hasConcept C127313418 @default.
• W1988698844 hasConcept C136894858 @default.
• W1988698844 hasConcept C140345934 @default.
• W1988698844 hasConcept C151730666 @default.
• W1988698844 hasConcept C15739521 @default.
• W1988698844 hasConcept C15785411 @default.
• W1988698844 hasConcept C166957645 @default.
• W1988698844 hasConcept C17241749 @default.
• W1988698844 hasConcept C174110039 @default.
• W1988698844 hasConcept C197435368 @default.
• W1988698844 hasConcept C205649164 @default.
• W1988698844 hasConcept C81820708 @default.
• W1988698844 hasConceptScore W1988698844C100134115 @default.
• W1988698844 hasConceptScore W1988698844C100834320 @default.
• W1988698844 hasConceptScore W1988698844C100970517 @default.
• W1988698844 hasConceptScore W1988698844C104932425 @default.
• W1988698844 hasConceptScore W1988698844C111368507 @default.
• W1988698844 hasConceptScore W1988698844C117935615 @default.
• W1988698844 hasConceptScore W1988698844C127313418 @default.
• W1988698844 hasConceptScore W1988698844C136894858 @default.
• W1988698844 hasConceptScore W1988698844C140345934 @default.
• W1988698844 hasConceptScore W1988698844C151730666 @default.
• W1988698844 hasConceptScore W1988698844C15739521 @default.
• W1988698844 hasConceptScore W1988698844C15785411 @default.
• W1988698844 hasConceptScore W1988698844C166957645 @default.
• W1988698844 hasConceptScore W1988698844C17241749 @default.
• W1988698844 hasConceptScore W1988698844C174110039 @default.
• W1988698844 hasConceptScore W1988698844C197435368 @default.
• W1988698844 hasConceptScore W1988698844C205649164 @default.
• W1988698844 hasConceptScore W1988698844C81820708 @default.
• W1988698844 hasIssue "12" @default.
• W1988698844 hasLocation W19886988441 @default.
• W1988698844 hasOpenAccess W1988698844 @default.
• W1988698844 hasPrimaryLocation W19886988441 @default.
• W1988698844 hasRelatedWork W1988698844 @default.

• next