FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W24303325> ?p ?o ?g. }

• W24303325 abstract "The cluster of glaciated stratovolcanoes called the Three Sisters—South Sister, Middle Sister, and North Sister—forms a spectacular 20-km-long reach along the crest of the Cascade Range in Oregon. The three eponymous stratocones, though contiguous and conventionally lumped sororally, could hardly display less family resemblance. North Sister (10,085 ft), a monotonously mafic edifice at least as old as 120 ka, is a glacially ravaged stratocone that consists of hundreds of thin rubbly lava flows and intercalated falls that dip radially and steeply; remnants of two thick lava flows cap its summit. Middle Sister (10,047 ft), an andesite-basalt-dacite cone built between 48 and 14 ka, is capped by a thick stack of radially dipping, dark-gray, thin mafic lava flows; asymmetrically glaciated, its nearly intact west flank contrasts sharply with its steep east face. Snow and ice-filled South Sister is a bimodal rhyolitic-intermediate edifice that was constructed between 50 ka and 2 ka; its crater (rim at 10,358 ft) was created between 30 and 22 ka, during the most recent of several explosive summit eruptions; the thin oxidized agglutinate that mantles its current crater rim protects a 150-m-thick pyroclastic sequence that helped fill a much larger crater. For each of the three, the eruptive volume is likely to have been in the range of 15 to 25 km³, but such estimates are fairly uncertain, owing to glacial erosion. The map area consists exclusively of Quaternary volcanic rocks and derivative surficial deposits. Although most of the area has been modified by glaciation, the volcanoes are young enough that the landforms remain largely constructional. Furthermore, twelve of the 145 eruptive units on the map are postglacial, younger than the deglaciation that was underway by about 17 ka. The most recent eruptions were of rhyolite near South Sister, about 2,000 years ago, and of mafic magma near McKenzie Pass, about 1,500 years ago. As observed by trailblazing volcanologist, Howel Williams, For magnificence of glacial scenery, for wealth of recent lavas, and for graphic examples of dissected volcanoes, no part of this range surpasses the area embracing the Sisters and McKenzie Pass. Scientific and journalistic interest in the Three Sisters volcanic cluster was aroused a few years ago when ongoing uplift centered about 5 km west of South Sister was identified, first recognized by satellite imagery in 2001. Subsequent geodetic measurements and continuing satellite imagery analysis confirmed 3 to 4 cm/yr uplift during the interval from 1997 to 2004; the uplift has been modelled as inflation thought to be caused by an intracrustal intrusion, largely aseismic and plausibly involving mafic magma." @default.
• W24303325 created "2016-06-24" @default.
• W24303325 creator A5005161882 @default.
• W24303325 creator A5075369838 @default.
• W24303325 creator A5090222248 @default.
• W24303325 date "2012-01-01" @default.
• W24303325 modified "2023-09-26" @default.
• W24303325 title "Geologic map of Three Sisters volcanic cluster, Cascade Range, Oregon" @default.
• W24303325 cites W1481120636 @default.
• W24303325 cites W1497511897 @default.
• W24303325 cites W1499050487 @default.
• W24303325 cites W1524319733 @default.
• W24303325 cites W1559444043 @default.
• W24303325 cites W1566382610 @default.
• W24303325 cites W1681228281 @default.
• W24303325 cites W1969225785 @default.
• W24303325 cites W1973487037 @default.
• W24303325 cites W1973609684 @default.
• W24303325 cites W1979350315 @default.
• W24303325 cites W1982075335 @default.
• W24303325 cites W1989328364 @default.
• W24303325 cites W1995843132 @default.
• W24303325 cites W1998146565 @default.
• W24303325 cites W199830191 @default.
• W24303325 cites W1998322169 @default.
• W24303325 cites W1999546014 @default.
• W24303325 cites W2004293503 @default.
• W24303325 cites W2005438659 @default.
• W24303325 cites W200613990 @default.
• W24303325 cites W2019032388 @default.
• W24303325 cites W2024953052 @default.
• W24303325 cites W2033927110 @default.
• W24303325 cites W2039869455 @default.
• W24303325 cites W203987590 @default.
• W24303325 cites W2040659190 @default.
• W24303325 cites W2050622444 @default.
• W24303325 cites W2053544840 @default.
• W24303325 cites W2054920148 @default.
• W24303325 cites W2057660381 @default.
• W24303325 cites W2064499777 @default.
• W24303325 cites W2065050814 @default.
• W24303325 cites W2067076206 @default.
• W24303325 cites W2071946564 @default.
• W24303325 cites W2072206013 @default.
• W24303325 cites W2072392240 @default.
• W24303325 cites W2073980485 @default.
• W24303325 cites W2075343818 @default.
• W24303325 cites W2085480633 @default.
• W24303325 cites W2098429927 @default.
• W24303325 cites W2103976459 @default.
• W24303325 cites W2113660406 @default.
• W24303325 cites W2117979886 @default.
• W24303325 cites W2118437744 @default.
• W24303325 cites W2123803462 @default.
• W24303325 cites W2124315063 @default.
• W24303325 cites W2125350032 @default.
• W24303325 cites W2132531596 @default.
• W24303325 cites W2138973655 @default.
• W24303325 cites W2138987072 @default.
• W24303325 cites W2144677198 @default.
• W24303325 cites W2153312858 @default.
• W24303325 cites W2154965338 @default.
• W24303325 cites W2155628626 @default.
• W24303325 cites W2157099954 @default.
• W24303325 cites W2169897697 @default.
• W24303325 cites W218328447 @default.
• W24303325 cites W2260310939 @default.
• W24303325 cites W2325019720 @default.
• W24303325 cites W2469673062 @default.
• W24303325 cites W2470156641 @default.
• W24303325 cites W2621541130 @default.
• W24303325 cites W2914082243 @default.
• W24303325 cites W382451578 @default.
• W24303325 cites W48246389 @default.
• W24303325 cites W781665547 @default.
• W24303325 cites W86462072 @default.
• W24303325 doi "https://doi.org/10.3133/sim3186" @default.
• W24303325 hasPublicationYear "2012" @default.
• W24303325 type Work @default.
• W24303325 sameAs 24303325 @default.
• W24303325 citedByCount "7" @default.
• W24303325 countsByYear W243033252014 @default.
• W24303325 countsByYear W243033252018 @default.
• W24303325 countsByYear W243033252020 @default.
• W24303325 countsByYear W243033252021 @default.
• W24303325 crossrefType "journal-article" @default.
• W24303325 hasAuthorship W24303325A5005161882 @default.
• W24303325 hasAuthorship W24303325A5075369838 @default.
• W24303325 hasAuthorship W24303325A5090222248 @default.
• W24303325 hasBestOaLocation W243033251 @default.
• W24303325 hasConcept C107504934 @default.
• W24303325 hasConcept C113754120 @default.
• W24303325 hasConcept C114793014 @default.
• W24303325 hasConcept C120806208 @default.
• W24303325 hasConcept C121332964 @default.
• W24303325 hasConcept C127313418 @default.
• W24303325 hasConcept C1276947 @default.
• W24303325 hasConcept C146348940 @default.
• W24303325 hasConcept C151730666 @default.
• W24303325 hasConcept C167284885 @default.

• next