Relevant bibliographies by topics / The Hollow Mountains

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'The Hollow Mountains'

Author: Grafiati
Published: 4 June 2021
Last updated: 28 July 2025

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Journal articles on the topic "The Hollow Mountains"

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Zhang, Guoyi, Zhongshu Liu, and Qaunyu Zhang. "Systematics and biogeography of the genera Pseudiberus Ancey, 1887 and Platypetasus Pilsbry, 1895 (Stylommatophora: Camaenidae), with the description of Pseudiberus shanheicus n. sp." Journal of Conchology 45, no. 1 (2024): 77–90. http://dx.doi.org/10.61733/jconch/4510.

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Phylogenetic analyses based on morphological character and molecular data indicate that Platypetasus Pilsbry, 1895 should not be synonymized with Pseudiberus Ancey, 1887. These genera occur in different geographical areas; Pseudiberus species are distributed in the Qinling, Taihang, Yimeng, and Taishan mountains, and Platypetasus species occur in the Daxueshan, Qionglaishan, Minshan, and Dabashan mountains. Here we describe a new species, Pseudiberus shanheicus n. sp., from Henan Province, China. Its shell is distinguished by its ribless surface and hollow peripheral keel. The phylogenetic rel
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Zhang, Guoyi, Zhongshu Liu, Qi Feng, and Qaunyu Zhang. "Systematics and biogeography of the genera Pseudiberus Ancey, 1887 and Platypetasus Pilsbry, 1895 (Stylommatophora: Camaenidae), with the description of Pseudiberus shanheicus n. sp." Journal of Conchology 45, no. 1 (2024): 77–90. https://doi.org/10.61733/jconch/4510.

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Phylogenetic analyses based on morphological character and molecular data indicate that Platypetasus Pilsbry, 1895 should not be synonymized with Pseudiberus Ancey, 1887. These genera occur in different geographical areas; Pseudiberus species are distributed in the Qinling, Taihang, Yimeng, and Taishan mountains, and Platypetasus species occur in the Daxueshan, Qionglaishan, Minshan, and Dabashan mountains. Here we describe a new species, Pseudiberus shanheicus n. sp., from Henan Province, China. Its shell is distinguished by its ribless surface and hollow peripheral keel. The phylogenetic rel
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Gilliam, F. S., J. T. Sigmon, M. A. Reiter, and D. O. Krovetz. "Elevational and spatial variation in daytime ozone concentrations in the Virginia Blue Ridge Mountains: implications for forest exposure." Canadian Journal of Forest Research 19, no. 4 (1989): 422–26. http://dx.doi.org/10.1139/x89-066.

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Ozone (O3) concentrations before and during the early growing season were monitored continuously at two closely located areas in the Virginia Blue Ridge Mountains: a deciduous forest watershed (Shaver Hollow) and a predominantly open grassy meadow (Big Meadows). In addition, O3 concentrations and canopy development (percent leaf emergence) were measured simultaneously at three sites along the elevational gradient of the Shaver Hollow watershed. When the canopy at Shaver Hollow was leafless, patterns of O3 concentration were similar between the forest and meadow, increasing steadily toward earl
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Ratcliffe, Nicholas M., Anita G. Harris, and Gregory J. Walsh. "Tectonic and regional metamorphic implications of the discovery of Middle Ordovician conodonts in cover rocks east of the Green Mountain massif, Vermont." Canadian Journal of Earth Sciences 36, no. 3 (1999): 371–82. http://dx.doi.org/10.1139/e99-009.

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Middle Ordovician (late Arenigian - early Caradocian) conodonts were recovered from a dolostone lens in carbonaceous schist 30 m below the base of the Pinney Hollow Formation in the Eastern Cover sequence near West Bridgewater, Vermont. These are the first reported fossils from the metamorphic cover sequence rocks east of the Green Mountain, Berkshire, and Housatonic massifs of western New England. The conodonts are recrystallized, coated with graphitic matter, thermally altered to a color alteration index (CAI) of at least 5, and tectonically deformed. The faunule is nearly monospecific, cons
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VASSILIEVA, ANNA B., VITALY L. TROUNOV, NIKOLAY A. ,. JR POYARKOV, and EDUARD A. GALOYAN. "The phytotelm tadpoles of Microhyla arboricola (Anura: Microhylidae) from Vietnam, with comments on reproductive biology and development." Zootaxa 4247, no. 4 (2017): 413. http://dx.doi.org/10.11646/zootaxa.4247.4.4.

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The reproductive biology of Microhyla arboricola (Microhylidae) was studied in two regions of the southern Annamite Mountains in Vietnam. M. arboricola is an obligate phytotelm-breeder that reproduces in water-filled tree hollows in montane evergreen forests. Clutches are attached above the water level in the hollows and contain 5–37 pigmented, relatively large eggs. Larvae hatch at markedly advanced stages and develop in water until metamorphosis is completed. The developing tadpoles are obligately oophagous and feed on conspecific eggs and embryos. M. arboricola tadpoles differ from tadpoles
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Gao, Zihui, Nicholas D. Perez, Brent Miller, and Michael C. Pope. "Competing sediment sources during Paleozoic closure of the Marathon-Ouachita remnant ocean basin." GSA Bulletin 132, no. 1-2 (2019): 3–16. http://dx.doi.org/10.1130/b35201.1.

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Abstract The Paleozoic construction of Pangea advanced southwestward from the Appalachian system to the Marathon fold-and-thrust belt in west Texas and progressively closed a remnant ocean basin between Laurentia and Gondwana. The resulting collisional orogen was a potential driver of Ancestral Rocky Mountain tectonism and impacted continental-scale sediment routing. New detrital zircon U-Pb geochronologic and heavy mineral provenance data from Ordovician–Pennsylvanian strata in the Marathon fold-and-thrust belt, and Permian strata in the Guadalupe Mountains of west Texas record changes in sed
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Lu, Zhang. "Design Technology of Irrigation and Drainage Engineering in Hollow Villages in Hilly Mountains." International Journal of ICT-aided Architecture and Civil Engineering 7, no. 1 (2020): 1–8. http://dx.doi.org/10.21742/ijiace.2020.7.1.01.

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Davis, P. Thompson. "Cirques of the Presidential Range, New Hampshire, and surrounding alpine areas in the northeastern United States." Géographie physique et Quaternaire 53, no. 1 (2002): 25–45. http://dx.doi.org/10.7202/004784ar.

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Abstract Evidence for rejuvenation of cirque glaciers following wastage of continental ice remains elusive for the Presidential Range and Mount Moosilauke of New Hampshire, Mount Katahdin and the Longfellow Mountains of Maine, and the Adirondack Mountains of New York. At Ritterbush Pond in the northern Green Mountains of Vermont, radiocarbon ages from lake sediment cores suggest that a low-altitude valley head, located up- valley of a series of cross-valley moraines, was ice-free by 11,940 14 C yrs BP (Bierman et al. , 1997). Although some workers argue that these moraines in Vermont are evide
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Mykitchak, T. I. "ГІЛЛЯСТОВУСІ (CLADOCERA) Й ВЕСЛОНОГІ (COPEPODA: CALANOIDA, CYCLOPOIDA) РАКОПОДІБНІ МАРМАРОСЬКИХ ГІР (УКРАЇНСЬКІ КАРПАТИ)". Scientific Issue Ternopil Volodymyr Hnatiuk National Pedagogical University. Series: Biology 82, № 1-2 (2022): 26–31. http://dx.doi.org/10.25128/2078-2357.22.1-2.4.

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There are noted 11 species of plankton crustaceans (7 – Cladocera and 4 – Copepoda (Calanoida and Cyclopoida)) from the reservoirs of the Ukrainian part of the Marmarosh Mountains. 
 The high mountain glacial lake Kryvave, the forest lake of the overflow type (landslide) Shchevora, small swamp and some of the puddles are investigated. Lake Kryvave is located at an altitude of 1620 m above sea level in the glacial crust of Mt. Pip Ivan Marmarosky within the subalpine vegetation. Its size is 38.8 by 19.4 m, the maximum depth is 0.5 m. Lake Shchevora is located at an altitude of 1209 m above
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MIYAMOTO, Masayuki. "Distribution of Shattered Clasts at a Nivation Hollow in Mt. Koizumidake, the Daisetsu Mountains." Geographical Review of Japa,. Ser. A, Chirigaku Hyoron 73, no. 5 (2000): 448–58. http://dx.doi.org/10.4157/grj1984a.73.5_448.

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Dissertations / Theses on the topic "The Hollow Mountains"

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Merricks, Timothy Chad. "Ecotoxicological Evaluation of Hollow Fill Drainages in Low Order Streams in the Appalachian Mountains of Virginia and West Virginia." Thesis, Virginia Tech, 2003. http://hdl.handle.net/10919/32977.

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Hollow fills are composed of excess spoil and debris produced from surface coal mining that is not returned to the original mined site. Hollow fills are often constructed in the head of hollows nearby or adjacent to the mined land area, which may be the origins of headwater streams or drain into low order systems. Eleven hollow fills were utilized in evaluating the influence fill drainages had on low order streams in Virginia and West Virginia. The study was conducted in six watersheds including; Five Mile Creek in Mingo County, West Virginia, Trace Fork in Mingo County, West Virginia, Lave
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Hangartner, Garth Jerod. "IN DARK MOUNTAIN HOLLOWS." University of Cincinnati / OhioLINK, 2001. http://rave.ohiolink.edu/etdc/view?acc_num=ucin991308403.

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Helmke, Elizabeth Ashley. "Structural analysis of cleavage at Sandy Hollow, McCartney Mountain fold-and-thrust salient, Southwest Montana." Thesis, Montana State University, 2008. http://etd.lib.montana.edu/etd/2008/helmke/HelmkeE1208.pdf.

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The McCartney Mountain salient is a distinct convex-east segment of the Sevier fold-and-thrust belt in southwest Montana, lying east of the Pioneer batholith and west of basement-cored Laramide uplifts. Prominent features of the central part of the salient include the in-sequence Sandy Hollow thrust fault (displacing Permian over Lower Cretaceous strata), and hanging wall and footwall syncline-anticline pairs that display complex intra-formational duplexes and parasitic detachment folds at all scales. Cleavage occurs in the argillaceous carbonate members of the Cretaceous Kootenai and Triassic
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Bačina, Jan. "Horský penzion." Master's thesis, Vysoké učení technické v Brně. Fakulta stavební, 2016. http://www.nusl.cz/ntk/nusl-240038.

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This diploma thesis solves the project of four-storey, partly cellared mountain pension situated in the plant number 645/2 in the cadastral area in Deštné in Orlické hory. The building has a capacity of 44 seats to accommodate 72 persons in the restaurant and 57 persons in the wellness center. There is a wellness center with fitness room and engine room of air-conditioning system in the basement. There is an entrance hall with hotel base, restaurant, sanitary facilities and utility room with boiler room on the first floor. The second and third floor is designed for accommodation. There is an o
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Books on the topic "The Hollow Mountains"

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Viggiani. Hollow mountains. Epimetheus Press, 1986.

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Gleiter, Jan. The legend of Sleepy Hollow. Raintree Childrens Books, 1985.

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Gleiter, Jan. The legend of Sleepy Hollow. Torstar Books, 1986.

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ill, Tibbles Jean-Paul, ed. Midnight in Lonesome Hollow: A Kit mystery. Pleasant, 2007.

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Washington, Irving. The legend of Sleepy Hollow, and Rip Van Winkle. ABDO Pub., 2002.

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Sebanc, Mark. Flight to Hollow Mountain. W.B. Eerdmans Pub., 1996.

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Cullen, Seán. Hamish X and the Hollow Mountain. Puffin Canada, 2007.

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8

Stepp, Lin. Tell me about Orchard Hollow. Canterbury House Pub., 2010.

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Stepp, Lin. Tell me about Orchard Hollow. Canterbury House Pub., 2010.

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Horning, Audrey J. In the shadow of Ragged Mountain: Historical archaeology of Nicholson, Corbin, & Weakley Hollows. Shenandoah National Park Association, 2004.

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Book chapters on the topic "The Hollow Mountains"

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"Meng Wall Hollow." In Laughing Lost in the Mountains. University Press of New England, 2023. http://dx.doi.org/10.2307/jj.2840649.43.

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"Preface: The Haynes Family of Haynes Hollow." In Making Mountains. University of Washington Press, 2009. https://doi.org/10.1515/9780295989891-002.

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Radcliffe, Ann. "Chapter V." In A Sicilian Romance. Oxford University Press, 2008. http://dx.doi.org/10.1093/owc/9780199537396.003.0006.

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The night grew stormy. The hollow winds swept over the mountains, and blew bleak and cold around; the clouds were driven swiftly over the face of the moon, and the duke and his people were frequently involved in total darkness. They had travelled on...
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Lane, Belden C. "Traveling Light: Gunstock Hollow and Dag Hammarskjöld." In Backpacking with the Saints. Oxford University Press, 2015. http://dx.doi.org/10.1093/oso/9780199927814.003.0016.

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It was new to me. Backpacker magazine had listed Gunstock Hollow as the “best Southern hollow in America,” and I was curious. The dog and I set out one weekend, hiking the middle fork of the Ozark Trail into this hollow nestled between two ridges. Three days remained in deer hunting season that year, so I tied a red bandana around Desert’s neck and wore a bright orange vest myself. With a name like Gunstock Hollow we figured we ought to be careful. Gunstock Hollow is typical of a lot of closed-in wilderness sites in the Ozarks. Thickets of densely growing trees give it a secluded and mysteriou
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John, David A. "Day One Road Log." In Geology and Ore Deposits of the Oquirrh and Wasatch Mountains, Utah. Society of Economic Geologists, 1998. http://dx.doi.org/10.5382/gb.29.05.

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Abstract Today's field trip examines late Eocene and Oligocene granitoid intrusions, cogenetic volcanic rocks (Keetley Volcanics), and associated hydrothermally altered and mineralized rocks in the central Wasatch Mountains. Because of late Cenozoic tilting related to Basin and Range extension, a continuum of mid-Tertiary paleodepths is exposed that ranges from about 11 km on the west side of the Little Cottonwood stock to the actual paleosurface on the east side of the range (Fig. 1; John, 1989a). Consequently, we will see a wide variety of textures and styles of emplacement in the intrusive
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Tam, Evan, Laura E. Webb, Cheyne Aiken, Jonathan Kim, and Keith Klepeis. "Formation of the Green Mountain anticlinorium in northern Vermont at ca. 420 Ma." In Laurentia: Turning Points in the Evolution of a Continent. Geological Society of America, 2022. http://dx.doi.org/10.1130/2022.1220(27).

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ABSTRACT The Appalachian Mountains in northern Vermont host a complex rock record of the tectonic evolution of eastern Laurentia, from the opening of the Iapetus Ocean to the subsequent formation of a convergent Paleozoic margin involving multiple phases of orogenesis. Prior 40Ar/39Ar studies in Vermont and northern Massachusetts have generally interpreted two major events associated with a dominantly Ordovician Taconic orogeny and a Devonian Acadian orogeny; intermediate ages were considered to reflect Taconic metamorphism and/or deformation that was “partially reset” during the Acadian oroge
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Lane, Belden C. "Community: Lower Rock Creek and Teilhard de Chardin." In Backpacking with the Saints. Oxford University Press, 2015. http://dx.doi.org/10.1093/oso/9780199927814.003.0024.

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I’m up for vigils, but the monks are still asleep. They were noisy last night at compline. The peepers were nearly as loud as the bullfrogs. The whole choir chanted like mad as stars came out over the creek. When I first set up camp along this quiet Ozark stream, I hadn’t realized I’d entered a cloister full of exuberant frogs cheered by yesterday’s rain. Their enthusiastic interpretation of the Psalms made me think of the deep-throated chanting of Tibetan Buddhist monks. The sound echoed off the steep rock walls where Cathedral Canyon narrows at this point. Its acoustical effect seemed to tak
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"mountain holly, n." In Oxford English Dictionary, 3rd ed. Oxford University Press, 2023. http://dx.doi.org/10.1093/oed/2154940007.

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Lane, Belden C. "Mindfulness: Moonshine Hollow and Thich Nhat Hanh." In Backpacking with the Saints. Oxford University Press, 2015. http://dx.doi.org/10.1093/oso/9780199927814.003.0017.

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The locals call it Moonshine Hollow, or Mooner’s Hollow, partly because of the haunting character of the moonlight in this small, isolated valley. It forces you to pay attention to the thousand shades of shadow and light you’d never thought to distinguish before. The phenomenon has something to do with the curvature of the ravine here, as light reflects off stone cliffs above and the lithe, white limbs of sycamore trees below. Whatever accounts for it, Moonshine Hollow is well named. Up from Coonville Creek in St. Francois State Park in southeast Missouri, it lies along the eleven-mile Pike Ru
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Colvin, Stephen. "Literary Texts." In A Historical Greek Reader. Oxford University PressOxford, 2007. http://dx.doi.org/10.1093/oso/9780199226597.003.0060.

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Abstract EPIC As a snake in the mountains waits for a man by its den, having fed on poisonous herbs, and a terrible anger has entered it: dreadfully its eyes glitter as it twists around its den. So Hektor, full of unquenchable fierceness, did not give ground, but leant his bright shield against a projecting battlement. With turbulent feelings he addressed his mighty spirit: ‘Ah me, if I enter within the gates and the wall, (100) Polydamas will be the first to lay reproach upon me: he was the man who bade me lead the Trojans to the city during this fatal night when glorious Achilles roused hims
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Conference papers on the topic "The Hollow Mountains"

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Barliba, Luminita Livia, C. Barliba, Adina Horablaga, I. Samfira, and G. Popescu. "TOPOGRAPHICAL TECHNIQUES APPLIED IN THE CRISUL ALB BASIN AS THE BASIS OF COMPLEX HYDROLOGICAL STUDIES." In 22nd International Multidisciplinary Scientific GeoConference 2022. STEF92 Technology, 2022. http://dx.doi.org/10.5593/sgem2022v/3.2/s12.26.

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The Cri?ul-Alb River springs from the Apuseni mountains, and its course crosses many rural and urban towns. In the Cri?ul Alb hollow, there are several tributaries that have a significant contribution to the volume and water flow of the Cri?ul Alb River. Due to the abundant precipitation combined with the melting of the snow during the spring period, high levels of water flow are created, endangering human settlements and other goods isolated by their flooding. The aim of the paper was to present a topographic study that would be the basis for the subsequent preparation of a complex hydrologic
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Chase, Alyssa, and Mark D. Schmitz. "A NEW AGE CONSTRAINT ON LATE JURASSIC MAGMATISM AND SEDIMENTATION IN THE COON HOLLOW FORMATION (WALLOWA TERRANE)." In 68th Annual Rocky Mountain GSA Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016rm-276274.

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Gaylord, David R., Paul K. Link, Tammy M. Rittenour, Caleb A. Grant, and Angela J. Coleman. "SEDIMENTOLOGY, STRATIGRAPHY, GEOMORPHOLOGY AND PALEOCLIMATE IN MID-LATE PLEISTOCENE GHOST DUNE HOLLOWS, EASTERN SNAKE RIVER PLAIN, IDAHO." In 68th Annual Rocky Mountain GSA Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016rm-275935.

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Goetz, Silas, and Simone Runyon. "PUMPKIN HOLLOW DEPOSIT, YERINGTON DISTRICT, NV: INSIGHTS ON MINERALIZATION BASED ON ASSOCIATED ALTERATION AND COMPOSITION OF EPIDOTE GROUP MINERALS." In Joint 118th Annual Cordilleran/72nd Annual Rocky Mountain Section Meeting - 2022. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022cd-373639.

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Scott, W. A., and W. R. Guice. "Completion Effectiveness in the Shannon Formation of the Jepson Draw and Holler Draw Fields, Powder River Basin, Wyoming." In SPE Rocky Mountain Petroleum Technology Conference. Society of Petroleum Engineers, 2001. http://dx.doi.org/10.2118/71071-ms.

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Şlapac, Mariana. "Kilia fortress of Stephen the Great." In Conferința științifică internațională Patrimoniul cultural: cercetare, valorificare, promovare. Ediția XIV. Institute of Cultural Heritage, Republic of Moldova, 2022. http://dx.doi.org/10.52603/pc22.08.

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Th e stone fortress of Kilia was erected on the banks of the Danube in the summer of 1479 on the initiative led by Stephen the Great. An inner wall separated it, following the example of the Cetatea Alba, into two distinct parts: the Outer Fortress, which corresponded to the “civil court”, and the Middle Fortress, to which conformed to the “middle court” corresponded. It was joined by the third courtyard, the “garrison courtyard”, which surrounded the old stone citadel. Th e inner citadel corresponded to the “middle court” and the “garrison court”. Th e fourth court, the “court of the citadel”
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Reports on the topic "The Hollow Mountains"

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Geologic map of the Nevershine Hollow area, eastern Black Mountains, southern Tushar Mountains and northern Markagunt Plateau, Beaver and Iron counties, Utah. US Geological Survey, 1990. http://dx.doi.org/10.3133/i1999.

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