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Статті в журналах з теми "Holy mountains":

1

HASHIKAWA, Hiroyuki. "Living on the Holy Mountains." Bulletin of the Society for Near Eastern Studies in Japan 49, no. 2 (2006): 147–64. http://dx.doi.org/10.5356/jorient.49.2_147.

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2

Kmak-Pamirska, Aleksandra. "Góry: Zamkowa, Królowej Bony, Grabarka — symbolika „mniej znanych gór” w świadomości kulturowej w regionach wschodniej Polski na przełomie XIX i XX wieku." Góry, Literatura, Kultura 10 (May 25, 2017): 81–96. http://dx.doi.org/10.19195/2084-4107.10.7.

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The Castle Mount, Queen Bona Mount and Mount Grabarka — the symbolism of “lesser known mountains” in the culture of the eastern regions of Poland at the turn of the 20th centuryThe aim of the article is to examine the significance of “lesser known mountains”, namely Castle Mount, Queen Bona Mount and Mount Grabarka in the cultural consciousness of people living in eastern Poland at the turn of the 20th century Podlasie and Volhynia. In folk tales the symbolism of the mountains was associated with the extraterrestrial world. Mo­untains aroused fear; they were regarded as the abodes of evil spirits and places where souls of sinners did their penance and wandered. With time the symbolism of the mountains among people living in eastern Poland began to change. At the turn of the century attempts were made to rationalise the perception of nature as well as to tame it and subordinate it to humans. Examples of such an approach include Zygmunt Gloger’s ethnographic descriptions of e.g. Castle Mount near Drohiczyn. Queen Bona Mount was to be found in Podlasie and Volhynia. A literary illustration by Halina Micińska-Kenar, entitled Pod górą królowej Bony [At the Foot of Queen Bona Mount], explores fear of the unknown — a mountain dominating the town — as well as the path of humans’ spiritual development through overcoming their weaknesses and ascending the peak. Often mountains were also associated with divine locations. An example is Mount Grabarka Podlasie, from which flows a holy spring, symbolising a holy place and a place of remembrance. An analysis of the symbolism of the mountains in Poland’s eastern region shows what places were and are regarded as mountains as well as why and what significance was attributed to these “smaller mountains” in the cultural consciousness of people living in these regions at the turn of the 20th century.
3

Geist, Andrew, and James C. VanderKam. "The Four Places That Belong to the Lord (Jubilees 4.26)." Journal for the Study of the Pseudepigrapha 22, no. 2 (November 13, 2012): 146–62. http://dx.doi.org/10.1177/0951820712467877.

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This article argues that the original name for the mountain on which Enoch made his offering in Eden was the mountain of incense ( Jub. 4.25) and that it and the first mountain in 4.26 (the mountain of Eden/Paradise) are the same mountain. The second mountain in 4.26, the mountain of the east, is Mt Lubar where the ark landed at the end of the flood and where Noah lived until his death. All four mountains in 4.26 are places where God had or would specially reveal himself to chosen individuals and for that reason were holy to the Lord.
4

Popovic, Danica. "Deserts and holy mountains of medieval Serbia: Written sources, spatial patterns, architectural designs." Zbornik radova Vizantoloskog instituta, no. 44 (2007): 253–74. http://dx.doi.org/10.2298/zrvi0744253p.

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Essential concepts in Christian thought and practice, the desert and holy mountain denote a particular kind of monastic and sacral space. They are secluded from the world, intended for asceticism, and ambivalent in nature they are inhospitable and menacing zones populated with demons, but also a monastic paradise, places for spiritual conversion and encounter with the divine. From earliest times, deserts and holy mountains had a few distinguishing characteristics. All forms of monastic life, from communal to solitary, were practiced side by side there. Monks of a special make-up and distinction known as holy men who were also often founders of illustrious communities, future saints and miracle-workers acted there. Furthermore these locales were important spiritual and bookmaking centre's, and therefore, strongholds of Orthodoxy. When trying to research Serbian material on this topic, we face a specific situation: few surviving sources on the one hand, and devastated monuments on the other. The ultimate consequence is that the entire subject has been neglected. Therefore the study of the Serbian deserts and holy mountains requires a very complex interdisciplinary approach with systematic field work as its essential part. It should address the following issues: corroboration, on the basis of written sources, of the reception of the concept of the monastic desert and holy mountain in a particular, regional, context; the distinct means and mechanisms employed in their physical realization; interpretation of their function; the recognition of patterns preserved in the surviving physical structures. Even the results obtained so far appear to be relevant enough to become included in the sacral topography of the Christian world. The author of this study gives particular attention to the detailed analysis of written sources of various genres - diplomatic sources, hagiographic material, liturgical texts, observation notes - in order to establish the meaning and the function of the monastic locales labeled as deserts and holy mountains (and, in a limited number of cases, also known as caves). The most important conclusions that may be drawn would be the following: the terms are interchangeable and were used both in a broader and a narrower sense, but in either case in reference to the space intended for higher forms of monastic life. A particularly broad range of meanings had the term desert which could refer to a distinct locale, as a rule a river gorge, or a mountain inhabited by hermits, but also a cave hermitage, the hesychasterion of a coenobitic community. The distinct forms of monastic life in such areas were communities of two or three or a few monks, organized as a skete or as a cell. In the deserts and mountains hermits primarily pursued the practice of 'agon and hesychia', but were also engaged in manuscript copying - an important peculiarity of Serbian eremitic monasticism. Finally, such locales were thought of by their dwellers as spiritual cities and the narrow path leading to Heavenly Jerusalem. The other thematic focus is an analysis of spatial patterns and architectural structures based on the relevant examples studied so far. Different types of monastic communities functioning as deserts were considered, from the point of view of their spatial situation and their relationship to the coenobia. In this context, field research identified examples of the so-called internal deserts, which was reconfirmed by the records from written sources. Special attention was given to the mechanism for creating a holy mount in the Serbian environment, according to the recognizable, athonite model. Also analyzed were architectural solutions characteristic of Serbian monastic deserts, from the simplest ones such as wooden huts and walled-up caves to monumental multi-storied edifices, equipped with different features. Finally, the conclusions that have been reached serve as a basis for defining future priorities in the field research of this topic.
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Szczepanik, Zbigniew, and Anna Żylińska. "The oldest rocks of the Holy Cross Mountains, Poland – biostratigraphy of the Cambrian Czarna Shale Formation in the vicinity of Kotuszów." Acta Geologica Polonica 66, no. 3 (September 1, 2016): 267–89. http://dx.doi.org/10.1515/agp-2016-0013.

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AbstractThree lower Cambrian acritarch assemblages recognized in four outcrops in the vicinity of Kotuszów in the southernmost part of the Palaeozoic inlier of the Holy Cross Mountains span a stratigraphic interval from the uppermost part of the Asteridium tornatum-Comasphaeridium velvetum Assemblage Zone to the Skiagia ornata- Fimbriaglomerella membranacea Assemblage Zone (most probably its lower part). According to current views (Moczydłowska and Yin 2012), this interval corresponds to the upper part of the Fortunian and to Stage 2 of the Terreneuvian Series. The strata yielding the oldest assemblage are thus the oldest precisely documented rocks in the Palaeozoic succession of the Holy Cross Mountains, and the oldest Cambrian rocks exposed on the surface in Poland. The current biostratigraphic scheme for the pre-trilobitic part of the Cambrian System in the Holy Cross Mountains should be modified so that it is based on local acritarch interval subzones.
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Eliyahu, Eyal Ben. "The Rabbinic Polemic against Sanctification of Sites." Journal for the Study of Judaism 40, no. 2 (2009): 260–80. http://dx.doi.org/10.1163/157006309x410671.

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AbstractThe attribution of holiness to various sites in antiquity was confined neither to a particular ethnic or religious group, nor to one particular geographical locale, but was rather practiced by a wide range of groups vis-à-vis many locations. Contrary to these views, the rabbis made a very clear and sharp statement regarding the sanctity of Jerusalem and the Temple Mount and negated the idea of the existence of holy places outside Jerusalem. The rabbis struggled against the sanctity of the biblical “holy mountain,” as well as against sites that could have been regarded as holy on the basis of the biblical narrative. The discovery of this polemic illuminates and offers an explanation for many surprising passages in early rabbinic literature that belittle high mountains and biblical “memorial sites” in the Land of Israel. The examples, drawn from the various strata of early rabbinic literature, demonstrate surprising rabbinic consensus on this issue.
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Halamski, Adam T., and Andrzej Baliński. "Latest Famennian Brachiopods from Kowala, Holy Cross Mountains, Poland." Acta Palaeontologica Polonica 54, no. 2 (June 2009): 289–306. http://dx.doi.org/10.4202/app.2007.0066.

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Damasceno, Mayron Morais, and Cláudia Luiz Lourenço. "“Holy Mountains”: o sussurro histórico na busca por reconhecimento." Scientia Iuris 20, no. 3 (November 29, 2016): 72. http://dx.doi.org/10.5433/2178-8189.2016v20n3p72.

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O presente artigo tem como temática a abordagem dos Direitos Humanos, de modo a demonstrar como a visibilidade histórica dos atos deflagrados pelas gerações passadas serve como intermédio na construção de uma sociedade mais humana e igualitária. Seu principal intuito não é trazer à baila o desespero, a amargura ou desejo de vingança, é, contudo, tratar sobre os perigos em que o ser humano pode incorrer ante sua busca desmesurada por poder. Nesse intuito é que se tratará sobre o genocídio Armênio que foi um dos primeiros atos que quase exterminou grande parcela de um povo, genocídio executado pelos atos de imposição do antigo exército Turco-Otomano; essa importância advém do fato de que esse acontecimento é pouco ou quase nada conhecido na sociedade, logo, sua existência e reconhecimento não servem para manchar a histórica da atual Turquia, mas para expor os erros passados e modificar o presente.
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Vierek, Aleksandra. "The palaeogeographical background of Late Devonian storm events in the western part of the Holy Cross Mountains (Poland)." Geologos 19, no. 4 (December 1, 2013): 257–72. http://dx.doi.org/10.2478/logos-2013-0015.

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Abstract Late Devonian coarse-grained carbonate deposits in the Holy Cross Mountains were studied for possible storm depositional systems and catastrophic tsunami events, as it must be assumed that the investigated area was strongly affected by tropical hurricanes generated in the open ocean North of Gondwana. This assumption appears consistent with diagnostic features of carbonate tempestites at several places in the Holy Cross Mountains. Sedimentary structures and textures that indicate so are, among other evidence, erosional bases with sole marks, graded units, intra- and bioclasts, different laminations and burrowing at the tops of tempestite layers. It has been suggested before that a tsunami occurred during the Late Devonian, but the Laurussian shelf had an extensional regime at the time, which excludes intensive seismic activity. The shelf environment also excluded the generation of tsunami waves because the depth was too shallow. Additionally, the Holy Cross Mountains region was surrounded in the Devonian by shallow-marine and stable elevated areas: the Nida Platform, the Opatkowice Platform and the Cracow Platform to the South, and the elevated Lublin-Lviv area to the NE. Thus, tsunami energy should have been absorbed by these regions if tsunamites would have occurred.
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LUDWIKOWSKA-KĘDZIA, Małgorzata, and Małgorzata WIATRAK. "THE GEOTOURIST ATTRACTIVENESS OF ŁAGOWICA RIVER VALLEY (HOLY CROSS MOUNTAINS, POLAND) – A PROJECT OF A GEOTOURIST TRAIL." GeoJournal of Tourism and Geosites 32, no. 4 (December 31, 2020): 1337–46. http://dx.doi.org/10.30892/gtg.32422-578.

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Geotourist evaluation of thirteen small geological, geomorphological and mining heritage objects was carried out in a small v alley of the Upper Łagowica River and in its surroundings (Holy Cross Mountains, Poland). The point grading method was used, which is functional in the case of evaluation of small geotourist objects. It was shown that the analysed objects are characterized by high and medi um geotourist attractiveness. When analysed together, they strengthen their own individual values. They are suited to mark out geotourist trails ( geotrail), and additionally become a source of information about spatial changes of geodiversity. They also determine the uniqueness of this type of small river valleys of the Holy Cross Mountains on a regional and supra-regional scale. The evaluation of these objects and the proposal of a geotourist trail in the Upper Łagowica River valley may contribute to the activation of local communities and government authorities in the promotion of geoeducation and geotourism, draw their attention to the need for preservation and protection of the geodiversity of small va lleys of the Holy Cross Mountains, and, what is especially important, may give information about the investment attractiveness of the area.

Дисертації з теми "Holy mountains":

1

Qvarnström, Martin. "Palaeoenvironments of the Earliest (Middle Devonian) Tetrapod Trackways from the Holy Cross Mountains, Poland; Locomotion in a Terrestrial Setting?" Thesis, Uppsala universitet, Institutionen för geovetenskaper, 2015. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-319968.

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The palaeoenvironment from which early tetrapods emerged is crucial to comprehend in order to understand the mechanisms that drove and allowed the terrestrialization of vertebrates; one of the most important evolutionary ‘events’ in the history of animals. Nevertheless, much of the terrestrialization is shrouded in obscurity, inter alia, due to scarcity of early tetrapods in the fossil record. Each new discovery of anything linked to vertebrate terrestrialization is therefore of great importance. Here, I present new detailed analyses of the palaeoenvironmental conditions at the time of formation of the earliest (early Middle Devonian) tetrapod trackways found in the Zachełmie Quarry in the Holy Cross Mountains of southern Poland. The trackways are found in three horizons in a clay-rich dolomitic succession represented by the Lower Complex of the Wojciechowice Formation. This Lower Complex is composed of short shallowing upward sequences that often terminate with desiccation cracks and/or paleosols. Vertically fluctuating δ18O values in the complex suggest multiple episodes of closed hydrological systems. A model of ephemeral to perennial lakes in a terrestrial setting is therefore proposed. Such environment is in concordance with evidence of scarce bioturbation and a flourish of microbial communities that, in contrast to a normal marine setting, most likely represent an ecologically stressed ecosystem. Furthermore: non-marine rare earth element (REE) signals, desiccation events, fossils of green algae (charophytes), paleosol development, low energy cyclic deposits and general lack of marine taxa in the body and trace fossil records in this complex firmly establishes the interpretation of palustrine carbonates formed in a lacustrine-like setting. However, in the lower part of the complex, some highly fractioned marine fossils occur. These are suggested to have been transported during wash-up events which temporally places the setting in marine proximity. Seasons of monsoonal rainfall resulted in erosion and influx of detrital grains which is evidenced by fine planar lamination (of seasonal cyclicity) in most of the sediments and occasional occurrence of blackened clasts (and rain-drop imprints).Thus, none of the pre-existing palaeoenvironmental hypotheses of tetrapod emergence are in full concordance with the data from the Zachełmie Quarry. Instead, a new palaeoenvironment is proposed for the earliest tetrapods: schizohaline ephermal to perennial lakes with periodic desiccation. This infers that already in the early Middle Devonian, tetrapods had conquered the terrestrial realm and were perhaps already capable of terrestrial locomotion over quite substantial distances.
Däggdjur, reptiler, fåglar och amfibier utgör tillsammans en besläktad djurgrupp som kallas för tetrapoder (fyrfotingar). Deras gemensamma förfader härstammade från de lobfenade fiskarna men skiljde sig från dem genom att inneha utvecklade ben med tår istället för de ”köttiga” fenor som de lobfeniga fiskarna karaktäriseras av. Denna evolutionära nyhet tillät, tillsammans med en rad andra egenskaper (lungor, skydd för uttorkning av dermis etc.), att vertebrater helt och hållet kunde koloni-sera land. I och med att vår egen existens är en direkt följd av denna evolutionära händelse är detta ett hett forskningsämne inom evolutionsbiologin. Ändå är mycket fortfarande höljt i dunkel beträffande hur koloniseringen av land gick till och vad det var som drev denna utveckling eftersom övergången skedde under en, i geologisk mått, snabb tidsrymd. Dock har de sista årtiondena resulterat i flertalet nya fossilfynd av primitiva tetrapoder. Ett fynd som är speciellt spektakulärt eftersom det är den hittills äldsta efterlämningen av tetrapoder, är fotspår som uppenbart är gjorda av ett djur som hade ben och tår istället för fenor. Detta förvånade hela det vetenskapliga samfundet eftersom det innebar att vi (tetrapoderna) utvecklades tidigare än vad som var dittills trott och att vertebrat-koloniseringen av land förmodligen skedde flertalet miljoner år tidigare. Vad som också skiljer ett spårfossil från andra fossil är att de är spår av djuren från när och där de levde till skillnad från bara deras skelettdelar som oftast transporterats från där de dog och bara preserveras i speciella miljöer. Detta har jag utnyttjat i detta arbete för att försöka avgöra i vilken miljö de är avsatta i. Jag har analyserat de sedimentära bergarterna i stenbrottet i södra Polen med skärningen som innehåller de lagren i vilka fotspåren finns. Analyser av sällsynta jordartsmetaller från de tre lager där fotspår är tydliga, antyder en speciell avsättningsmiljö som inte liknar en typisk havsmiljö. I den undre delen av lagerföljden där de spårbärande lagren påträffats finns återkristalliserade saltkristaller, torkningssprickor och fossila jordar som indikerar korta respektive långvariga perioder av uttorkning. Andra fossil som i en normal marin miljö borde bevaras i en dolomitisk kalksten lyser med sin frånvaro och istället påfinns massiv koloni-sering av cyanobakterier. Detta brukar ske i speciella miljöer som avviker från vanlig marin komposi-tion, så som äldre sötvattensmiljöer eller laguner med hög salthalt, som därmed är ”svårbebodd” för djur som annars livnär sig på de fotosyntiserande bakterierna. Implikationen av mitt arbete är att tetrapoderna redan i tidig mellan Devon (ca 390 miljoner år sedan) inte bara hade utvecklat ben utan också att de kunde använda dem över landsträckor för att ta sig till, och mellan, kontinentala vatten. Detta är ännu en viktig pusselbit i pusslet som ämnar rekonstruera tetrapodernas (och vår egen) uppkomst.
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Johnson, Mira C. 1985. "The Croagh Patrick Pilgrimage: Identity Construction and Spiritual Experience at Ireland's Holy Mountain." Thesis, University of Oregon, 2011. http://hdl.handle.net/1794/11497.

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The Reek Sunday Pilgrimage at Croagh Patrick in County Mayo, Ireland is a syncretic event that incorporates official Catholic religious narratives of Saint Patrick, folk narratives of the site's Celtic pagan significance, local histories of the Great Irish Famine of the 19th century and personal narratives with a physical engagement with the landscape to create a spiritual experience. The pilgrimage serves as a performative event that allows participants to formulate and perform alternative spiritualities and identities, blurring the distinctions between pilgrim and tourist, sacred and profane. An emerging tradition at Croagh Patrick illustrates this by emphasizing the historical and national significance of the famine villages along the ancient pilgrimage path, the Tochar Phadraig, embracing these sites, and pilgrimage to them, as sacred.
Committee in charge: Lisa Gilman, Chairperson; Dianne Dugaw, Member; Phil Scher, Member
3

Krykorková, Petra. "Analýza rozvoje hipoturistiky v regionu Českolipsko a Jizerské hory." Master's thesis, Vysoká škola ekonomická v Praze, 2011. http://www.nusl.cz/ntk/nusl-114037.

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The aim of this diploma thesis is to analyze the current state of horseback riding tourism in the region of Liberec, focusing on Česká Lípa and Jizerské mountains. Secondary objectives include offering a summary of theoretical knowledge about horseback riding as a form of tourism; monitoring activities of the Equestrian Trails Association of Liberecký region and giving analysis of Liberecký region; analysis of supply of services connected with horseback riding tourism and analysis of demand for these services. The thesis should help people interested in horseback riding as well as owners of horse back riding facilities. It should mention the role of horses and the difficulty of their breeding, give the characteristics of Liberecký region, map the current state of equestrian trails, monitor the situation of services offered and demanded and compare the situation with other regions and an example from abroad.
4

Roe, Warren Paul. "Tertiary Sediments of the Big Hole Valley and Pioneer Mountains, Southwestern Montana: Age, Provenance, and Tectonic Implications." The University of Montana, 2010. http://etd.lib.umt.edu/theses/available/etd-08232010-181233/.

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Tertiary terrestrial sedimentary rocks of the Big Hole basin and Pioneer Mountains of southwestern Montana provide a record of regional extensional tectonism. Detailed observations of stratigraphy and sedimentology at widely scattered outcrops indicate the presence of paleosols, fine-grained debris flows, small alluvial channels, and rare fluvial deposits. U-Pb geochronology of detrital zircons and air-fall tuffs indicates the presence of Oligocene to Middle Miocene sedimentary rocks outcropping at the surface. Though the presence of detrital muscovite in several outcrops indicates derivation from the nearby 2-mica Chief Joseph pluton, a predicted ~75 Ma zircon population is not present: instead, a persistent peak of 70-72 Ma zircons is found throughout the basin, indicating the Chief Joseph pluton may have a younger emplacement age than is currently recognized. Simple physical models developed from Bouguer anomalies indicate the basin deepens and widens toward the south, which agrees with prior work suggesting Eocene initiation of extension in the Big Hole and places it in a class of extensional basins that formed in the early Tertiary. Late Cretaceous, Eocene, and Mesoproterozoic detrital zircon populations, along with consistently immature lithic sands, all indicate sediments were derived from local bedrock sources found around the rim of the modern Big Hole Valley. While these results indicate the Tertiary Big Hole basin resembled the modern basin, some later deformation may have cut off and reversed a paleodrainage flowing out of the southeastern portion of the basin, possibly leading to the modern configuration of the Big Hole River and the deep gorge it carves across the eastern Pioneer Mountains.
5

Řeháková, Jana. "Udržitelný rozvoj cestovního ruchu v CHKO Železné hory." Master's thesis, Vysoká škola ekonomická v Praze, 2017. http://www.nusl.cz/ntk/nusl-358834.

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The thesis deals with the issue of sustainable tourism development in protected landscape area of the Iron Mountains. The main objective is to evaluate the current status and potential of the region on issues of sustainable tourism development, sustainable forms of tourism and evaluate conservation in the PLA Iron Mountain. The theoretical part is devoted to sustainable development, sustainable development of tourism and the area of the Iron Mountains. The practical part is to map the nature and landscape protection in the PLA Iron Mountain with regard to small-scale protected areas and analyze friendly forms of tourism. Followed by evaluation of the awareness of sustainable development of the territory by questionnaire from the perspective of local public administration in tourism, residents PLA and business owners. Last theoretical part is the SWOT analysis and recommendations for the future.
6

Skopalová, Vendula. "Horský penzion v KÚ Karolinka." Master's thesis, Vysoké učení technické v Brně. Fakulta stavební, 2019. http://www.nusl.cz/ntk/nusl-391921.

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The subject of the diploma thesis is the design and process of the construction-technical part of the project documentation for realization of the new building of the mountain guest-house house in Karolina with an accommodation capacity of 36 people. The building is located on a slope, it is a basement, it has 2 underground floors and 3 aboveground floors. The building is roofed with a saddle roof with a concrete roofing. Vertical support structures are made from the Porotherm system. In addition to the project, an architectural study, a fire report and a thermal-technical assessment of the house are also included.
7

Bushman, Michelle. "Contribution of Recharge Along Regional Flow Paths to Discharge at Ash Meadows, Nevada." Diss., CLICK HERE for online access, 2008. http://contentdm.lib.byu.edu/ETD/image/etd2386.pdf.

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Tomáš, Josef. "GIS turistických stezek v Orlických horách." Master's thesis, Vysoké učení technické v Brně. Fakulta stavební, 2014. http://www.nusl.cz/ntk/nusl-226758.

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The aim of the diploma thesis was to create the functional core of geographic information system (GIS) of hiking trails in the Eagle Mountains including the spatial analysis. The first part, more theoretical, is dedicated to the brief description of the theory and initial analysis before the particular creation of GIS. In the second part, more practical, the process of the respective task is described from the data collection to data editing, creating the core of GIS, spatial analysis and final visualization.
9

Čepl, David. "Vliv polohy objektu na cenu a náklady stavebního objektu." Master's thesis, Vysoké učení technické v Brně. Fakulta stavební, 2017. http://www.nusl.cz/ntk/nusl-265506.

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The aim of this theses is to assess the effect of position of the object to its price and costs. It is done to define the possible positions of the object, costs and prices of the structures at selected locations. Prices and costs in selected locations are compared, assessed and evaluated. Therefore, the influence of position on price and costs of the structure is assessed.
10

Makrinos, George Adam. "Drawing Music, Playing Architecture." Thesis, Virginia Tech, 2005. http://hdl.handle.net/10919/33890.

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Анотація:
Architecture and music share intrinsic meanings generated by a constant stream of metaphors which are forms of poetic transformations. This thesis sought to challenge the present way an architect-musician makes drawings through the exploration of multimedia possibilities at hand. The drawings are composed using Macromedia Flash MX. OPEN HOMEPAGE.EXE To download flash player, click here: Download flash Player
Master of Architecture

Книги з теми "Holy mountains":

1

Frank, Waters. Mountain dialogues. Athens: Swallow Press/Ohio University Press, 1999.

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2

Peng, Youzhi. 100 ge zong jiao sheng di, 100 ge gu shi = 100 stories of holy land. 8th ed. Taibei Shi: Zhi qing pin dao chu ban you xian gong si, 2013.

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3

François, Damien. Holy mountains of Nepal: Die heligen berge Nepals = Les montagnes sacrees du Nepal. Kathmandu: Vajra Books, 2014.

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4

Hardacre, Cheryl. Chewing gum in holy water: Mario Valentini's childhood in the Abruzzo Mountains. Crows Nest, NSW: Allen & Unwin, 2006.

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5

Lewis, Betty. Holy City: Riker's roadside attraction in the Santa Cruz Mountains, a nostalgic history. Santa Cruz, Calif: Otter B Books, 1992.

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6

Dzik, Jerzy. Ordovician carbonate platform ecosystem of the Holy Cross Mountains =: Ekosystem ordowickiej platformy węglanowej gór Świętokrzyskich. Warszawa: Instytut Paleobiologii PAN im. Romana Kozłowskiego, 1994.

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7

John, Prendergast. For four years I have no rest: Greed and holy war in the Nuba Mountains of Sudan. Washington, DC (3700 13th St. NE, Washington, DC 20017): Center of Concern, 1994.

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8

Zapalski, Mikolaj K. Tabulate corals from the Givetian and Frasnian of the southern region of the Holy Cross Mountains (Poland). London: Palaeontological Association, 2012.

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9

Barbero, A. Atlante dei sacri monti, calvari e complessi devozionali europei: Atlas of holy mountains, Calvaries, and devotional complexes in Europe. Novara: Istituto geografico De Agostini, 2004.

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10

Barwicz-Piskorz, Wanda. Zespoły otwornic i stratygrafia górnej jury obrzeżenia Gór Świętokrzyskich =: Foraminiferal assemblages and stratigraphy of upper Jurassic in Holy Cross Mountains district. Kraków: Wydawnictwa AGH, 1995.

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Частини книг з теми "Holy mountains":

1

Introvigne, Massimo. "Holy Mountains and Anti-Cult Ecology." In Regulating Religion, 73–83. Boston, MA: Springer US, 2004. http://dx.doi.org/10.1007/978-1-4419-9094-5_5.

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2

Kakalis, Christos. "Border Versus Boundary: The Holy Mountain and the Inhabitation of Its Periphery." In Mountains and Megastructures, 15–28. Singapore: Springer Singapore, 2020. http://dx.doi.org/10.1007/978-981-15-7110-7_2.

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3

della Dora, Veronica. "Turning Holy Mountains into Ladders to Heaven: Overlapping Topographies and Poetics of Space in Post-Byzantine Sacred Engravings of Mount Sinai and Mount Athos." In Approaching the Holy Mountain, 505–36. Turnhout: Brepols Publishers, 2010. http://dx.doi.org/10.1484/m.cursor-eb.3.4906.

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4

Jodorowsky, Alejandro. "The Holy Mountain." In 100 Cult Films, 113–14. London: British Film Institute, 2011. http://dx.doi.org/10.1007/978-1-84457-571-8_49.

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5

Carr, Annemarie Weyl. "Sinai and Cyprus: Holy Mountain, Holy Isle." In Approaching the Holy Mountain, 449–78. Turnhout: Brepols Publishers, 2010. http://dx.doi.org/10.1484/m.cursor-eb.3.4904.

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6

Nelson, Robert S. "Sinai Studies: An Overview and an Introduction." In Approaching the Holy Mountain, 1–14. Turnhout: Brepols Publishers, 2010. http://dx.doi.org/10.1484/m.cursor-eb.3.4889.

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7

Christoforaki, Ioanna. "Paving the Road to Sinai: Georgios and Maria Soteriou on the Holy Mountain." In Approaching the Holy Mountain, 15–33. Turnhout: Brepols Publishers, 2010. http://dx.doi.org/10.1484/m.cursor-eb.3.4890.

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8

Elsner, Jaś, and Gerhard Wolf. "The Transfigured Mountain: Icons and Transformations of Pilgrimage at the Monastery of St Catherine at Mount Sinai." In Approaching the Holy Mountain, 37–71. Turnhout: Brepols Publishers, 2010. http://dx.doi.org/10.1484/m.cursor-eb.3.4891.

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9

Kalopissi-Verti, Sophia, and Maria Panayotidi. "Excavations on the Holy Summit (Jebel Mūsā) at Mount Sinai: Preliminary Remarks on the Justinianic Basilica." In Approaching the Holy Mountain, 73–106. Turnhout: Brepols Publishers, 2010. http://dx.doi.org/10.1484/m.cursor-eb.3.4892.

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10

Koufopoulos, Petros, and Marina Myriantheos-Koufopoulou. "The Architecture of the Justinianic Basilica on the Holy Summit." In Approaching the Holy Mountain, 107–17. Turnhout: Brepols Publishers, 2010. http://dx.doi.org/10.1484/m.cursor-eb.3.4893.

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Тези доповідей конференцій з теми "Holy mountains":

1

Kondas, Marcelina. "UNUSUAL DEVONIAN PALYNOMORPHS- TENTACULITOIDS (KOWALA 1 BOREHOLE, HOLY CROSS MOUNTAINS, SOUTH-CENTRAL POLAND)." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-356166.

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2

Musial, Angelika. "GEODIVERSITY AND RAW MATERIALS VALUES IN THE SOUTHERN PART OF THE HOLY CROSS MOUNTAINS." In 18th International Multidisciplinary Scientific GeoConference SGEM2018. Stef92 Technology, 2018. http://dx.doi.org/10.5593/sgem2018/1.1/s01.019.

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3

Kondas, Marcelina. "NEW PALYNOLOGICAL DATA FROM DEVONIAN DEPOSITS OF SOUTH-CENTRAL POLAND (MIŁOSZÓW, HOLY CROSS MOUNTAINS)." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-356134.

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4

Musial, Angelika. "RARE EARTH ELEMENTS IN THE ROCK SEQUENCE FROM LOWER TO MIDDLE DEVONIAN IN THE HOLY CROSS MOUNTAINS, POLAND." In 17th International Multidisciplinary Scientific GeoConference SGEM2017. Stef92 Technology, 2017. http://dx.doi.org/10.5593/sgem2017/11/s01.060.

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5

Kalicki, Tomasz, Piotr Kusztal, Mariusz Nowak, and Dominika Zaborska. "STRUCTURE AND AGE OF TERRACES AND FLOOD PLAINS: CASE STUDY FROM THE CZARNA KONECKA (HOLY CROSS MOUNTAINS - POLISH UPLANDS)." In 4th INTERNATIONAL SCIENTIFIC CONFERENCE GEOBALCANICA 2018. Geobalcanica Society, 2018. http://dx.doi.org/10.18509/gbp.2018.13.

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6

Glasspool, Ian J., Robert A. Gastaldo, and Kara Robak. "FURTHER EVIDENCE OF LATEST SILURIAN WILDFIRE ACTIVITY: CHARRED MESOFOSSILS FROM THE WINNICA FORMATION OF THE HOLY CROSS MOUNTAINS, POLAND." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-334712.

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7

Purvis, D. L., D. D. Smith, and D. L. Walton. "Alternative Method for Stimulating Open Hole Horizontal Wellbores." In SPE Rocky Mountain Regional Meeting. Society of Petroleum Engineers, 1999. http://dx.doi.org/10.2118/55614-ms.

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8

Pellerin, Denis, Alaide M. Dura˜o, Jose´ E. F. P. Jardim, Carlos Pimenta, and Kazumi Miura. "Horizontal Directional Drilling as a Solution for Crossing of Ridges in the Serrana Province, Mato Grosso, Brazil." In 2002 4th International Pipeline Conference. ASMEDC, 2002. http://dx.doi.org/10.1115/ipc2002-27190.

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Анотація:
The crossing of a series of high, parallel, elongated and with steep scarp mountains in the Serrana Province, between Ca´ceres and Cuiaba´, Mato Grosso State, Brazil, constituted a great technical challenge for implementation of the Bolivia - Mato Grosso gas pipeline. Due to environmental preservation, the gas pipeline could not cross the crest of some of these mountains using conventional surface methods and the alternative of surrounding the mountains would have caused an extended additional path, with appreciable additional cost. The economically viable alternative was the horizontal directional drilling through the most critical mountains: Piraputanga Ridge with 850m, Cachoeirinha Ridge with 943m and Palmeiras Ridge with 867m. One of the difficulties was the drilling of the very compact and abrasive Alto Paraguay Group Proterozoic low metamorphic rocks intercalated with clastic sedimentary rocks. The horizontal directional hole intersects in high angles the strongly dipping layers of rocks. The layered sequences of sandstone capped by siltstones provide the aquifer condition to Raizama Fm. with strong water flow. To prevent any environmental damage, the conventional hole design was modified, which allowed the drilling with water, instead of bentonitic drilling fluid. The horizontal directional drilling consisted of a pilot hole with 10.14 inches diameter, drilled with down hole motor and an electromagnetic steering system. The first enlargement of the pilot hole went to 22” diameter and the last one to 30” using special reamer tools. The pipes of the Bolivia - Mato Grosso gas pipeline have 18” diameter, with a special line coating to prevent damages during pulling in contact with rocks. No problems occurred during the pulling operation of the pipes along the holes. The proposed three horizontal directional holes were very successful and the projected designs of the well were fully achieved, with a very small offset in the forecasted exit points. After long weeks of hole opening and preparatory works, all three pulling operations of the pipestrings along the holes went very smoothly.
9

Odom, Richard C., Pavlakos Paul, Satwant S. Diocee, Shawn M. Bailey, Dennis M. Zander, and John J. Gillespie. "Shaly Sand Analysis using Density-Neutron Porosities from a Cased-hole Pulsed Neutron System." In SPE Rocky Mountain Regional Meeting. Society of Petroleum Engineers, 1999. http://dx.doi.org/10.2118/55641-ms.

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10

Seale, Rocky Allen, and James Athans. "Using Open Hole Horizontal Completion Technology to More Efficiently Complete Vertical Wells." In Rocky Mountain Oil & Gas Technology Symposium. Society of Petroleum Engineers, 2007. http://dx.doi.org/10.2118/107930-ms.

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Звіти організацій з теми "Holy mountains":

1

Rautman, C. A., and D. A. Engstrom. Geology of the USW SD-7 drill hole Yucca Mountain, Nevada. Office of Scientific and Technical Information (OSTI), September 1996. http://dx.doi.org/10.2172/399666.

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2

Rautman, C. A., and D. A. Engstrom. Geology of the USW SD-12 drill hole Yucca Mountain, Nevada. Office of Scientific and Technical Information (OSTI), November 1996. http://dx.doi.org/10.2172/419097.

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3

Chipera, S. J., and D. L. Bish. Mineralogy of drill hole UE-25p#1 at Yucca Mountain, Nevada. Office of Scientific and Technical Information (OSTI), May 1988. http://dx.doi.org/10.2172/60432.

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4

Engstrom, D. A., and C. A. Rautman. Geology of the USW SD-9 drill hole, Yucca Mountain, Nevada. Office of Scientific and Technical Information (OSTI), October 1996. http://dx.doi.org/10.2172/414307.

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5

Loskot, C. L. Geohydrologic data from test hole USW UZ-6s, Yucca Mountain, Nye County, Nevada. Office of Scientific and Technical Information (OSTI), December 1993. http://dx.doi.org/10.2172/140688.

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6

Kume, J., and D. Hammermeister. Geohydrologic data from test hole USW UZ-7, Yucca Mountain area, Nye County, Nevada. Office of Scientific and Technical Information (OSTI), July 1990. http://dx.doi.org/10.2172/137755.

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7

Whitfield, M. S., W. Thordarson, D. P. Hammermeister, and J. B. Warner. Drilling and geohydrologic data for test hole USW UZ-1, Yucca Mountain, Nye County, Nevada. Office of Scientific and Technical Information (OSTI), December 1990. http://dx.doi.org/10.2172/137961.

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8

Whitfield, M. S. Jr, C. L. Loskot, and C. M. Cope. Borehole and geohydrologic data for test hole USW UZ-6, Yucca Mountain area, Nye County, Nevada. Office of Scientific and Technical Information (OSTI), April 1993. http://dx.doi.org/10.2172/138662.

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9

Healey, D. L., F. G. Clutsom, and D. A. Glover. Borehole gravity meter survey in drill hole USW G-4, Yucca Mountain Area, Nye County, Nevada. Office of Scientific and Technical Information (OSTI), December 1986. http://dx.doi.org/10.2172/60072.

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10

Norris, A. E., F. M. Jr Byers, and T. J. Merson. Fran Ridge horizontal coring summary report hole UE-25h No. 1, Yucca Mountain Area, Nye County, Nevada. Office of Scientific and Technical Information (OSTI), October 1986. http://dx.doi.org/10.2172/59982.

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