Gotowe bibliografie tematyczne / Catskill Mountain House (Catskill, New York)

Gotowa bibliografia na temat „Catskill Mountain House (Catskill, New York)”

Autor: Grafiati

Data publikacji: 26 lipca 2024

Data aktualizacji: 27 lipca 2024

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Artykuły w czasopismach na temat "Catskill Mountain House (Catskill, New York)"

Ver Straeten, Charles. "The Devonian terrestrial system of New York". Bulletins of American Paleontology, nr 407 (lipiec 2023): 211–330. http://dx.doi.org/10.32857/bap.2023.407.05.

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Late 18th to early 19th century reports on the rocks of the Catskill Mountains in eastern New York were followed by over 180 years of geological and paleobiological studies of the Devonian terrestrial succession, in the state and up and down eastern North America. Yet, nearly 230 years later these estimated ca. 2.4 km- (1.5 mi-) thick, homogenous strata remain a largely unknown frontier in many ways. Studies of Devonian terrestrial strata in New York over the last century include two different stratigraphic frameworks. The first, by George Chadwick (1930s–1940s), focused on the Catskill Front to the vicinity of Slide Mountain, highest peak in the Catskills. The second, by Fletcher and Rickard in the 1960s to mid-1970s, attempted to create a broader, more geographically inclusive chronostratigraphic nomenclature throughout the entire Catskills outcrop belt. Recent work indicates that in the field this latter model, based on thick lithosomes of red and gray rocks and conglomerates, is problematic. It can be seen as representing a “second draft” stratigraphic framework, in need of additional work and refinement. At this time, however, too little is known as to how to better ground the existing stratigraphy, or to propose a sound alternate stratigraphic framework for the Catskills succession. Other major foci in the Devonian terrestrial of New York include paleobotany (1950s–today), petrography (1960s–1980s), fluvial systems (1970s–1990s), and terrestrial arthropods (1980s–2000s). Broader paleobiological studies, in part associated with the Red Hill site in northern Pennsylvania, burgeoned in the 1990s and continue today. Recent Catskills terrestrial research of impact is perhaps largely paleobiological and includes the first complete Eospermatopteris (“Gilboa”) tree, mapping of well- preserved forest floors, and increasing research on paleosols. Difficulties in research of Devonian terrestrial strata in New York include: the lateral discontinuity of terrestrial facies and the lack of documented, distinctive marker beds for correlation; little biostratigraphic and geochronologic control; extensive cover in sometimes rugged terrain; too few researchers, and a need for greater cross-disciplinary perspectives and communication. The purpose of recent and ongoing research by the author is multifold. First to systematically gather various data, such as event deposits, petrography, detrital zircon dating, and palynological biostratigraphy, top to bottom through the succession, initially in the classic Catskill Front to the vicinity of Slide Mountain, in the New York State Department of Conservation “Slide Mountain Wilderness” of the Catskill Park. Second within that succession, to better document depositional history, provenance, and biostratigraphy, and to know the succession more closely. Through this, the larger goal is to test the existing stratigraphic framework and try to ground that stratigraphy in the regional rock record better, or to develop a new stratigraphic framework. Key issues that remain largely unresolved in Devonian terrestrial strata of New York include: lack of a well-tested, viable, and correlatable stratigraphic framework; a general lack of chronostratigraphic data from palynological/microvertebrate biostratigraphy and radiometric ages from altered air fall volcanic tephra beds; and no systematic documentation of the vertical Catskill succession. Other future studies could include lateral, interstate/province comparisons of variations in provenance/drainage evolution along the Acadian (Acadian-Neoacadian) Foreland Basin and its subbasin known as the Appalachian Basin, via petrography, detrital mineral dating and other methods.

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Weathers, K. C., G. M. Lovett, G. E. Likens i R. Lathrop. "THE EFFECT OF LANDSCAPE FEATURES ON DEPOSITION TO HUNTER MOUNTAIN, CATSKILL MOUNTAINS, NEW YORK". Ecological Applications 10, nr 2 (kwiecień 2000): 528–40. http://dx.doi.org/10.1890/1051-0761(2000)010[0528:teolfo]2.0.co;2.

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Ernst, Anne G., Barry P. Baldigo, Christiane I. Mulvihill i Mark Vian. "Effects of Natural-Channel-Design Restoration on Habitat Quality in Catskill Mountain Streams, New York". Transactions of the American Fisheries Society 139, nr 2 (marzec 2010): 468–82. http://dx.doi.org/10.1577/t08-153.1.

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Anandhi, Aavudai, Mark S. Zion, Prasanna H. Gowda, Donald C. Pierson, David Lounsbury i Allan Frei. "Past and future changes in frost day indices in Catskill Mountain region of New York". Hydrological Processes 27, nr 21 (6.08.2013): 3094–104. http://dx.doi.org/10.1002/hyp.9937.

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Burns, Douglas A., Julian Klaus i Michael R. McHale. "Recent climate trends and implications for water resources in the Catskill Mountain region, New York, USA". Journal of Hydrology 336, nr 1-2 (marzec 2007): 155–70. http://dx.doi.org/10.1016/j.jhydrol.2006.12.019.

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Anandhi, Aavudai, Allan Frei, Soni M. Pradhanang, Mark S. Zion, Donald C. Pierson i Eliot M. Schneiderman. "AR4 climate model performance in simulating snow water equivalent over Catskill Mountain watersheds, New York, USA". Hydrological Processes 25, nr 21 (7.09.2011): 3302–11. http://dx.doi.org/10.1002/hyp.8230.

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Baldigo, B. P., i P. S. Murdoch. "Effect of stream acidification and inorganic aluminum on mortality of brook trout (Salvelinus fontinalis) in the Catskill Mountains, New York". Canadian Journal of Fisheries and Aquatic Sciences 54, nr 3 (1.03.1997): 603–15. http://dx.doi.org/10.1139/f96-314.

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Juvenile brook trout (Salvelinus fontinalis) were exposed in cages to fluctuating chemical conditions in four Catskill Mountain streams during the spring and fall of 1989 and the spring of 1990. Specific chemical constituents and characteristics of acidic episodes that correlated with increased fish mortality were identified. Mortality increased during acidic episodes in one poorly buffered stream when inorganic monomeric aluminum (Alim) concentrations increased; mortality was low in three other streams during acidic episodes of shorter duration and smaller magnitude than measured in the poorly buffered stream. Variation in mortality was attributed primarily to differences in concentrations of both Alim and dissolved organic carbon. Linear and logistic regression analyses indicate that either mean or median Alim concentrations could account for 73-99% of the variability in mortality. Regression analyses suggest that mortality was highly related (in order of importance) to Alim, pH, dissolved organic carbon, calcium, and chloride concentration. Brook trout mortality was also highly related to durations of exposure above 0.225 and 0.250 mg/L Alim during test periods. Characteristics of acidic-Alim episodes that are critical to mortality of caged brook trout appear to be (i) Alim concentrations of at least 0.225 ± 0.025 mg/L and (ii) exposure to these toxic Alim concentrations for at least 2 days.

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Baldigo, Barry P., Peter S. Murdoch i Douglas A. Burns. "Stream acidification and mortality of brook trout (Salvelinus fontinalis) in response to timber harvest in Catskill Mountain watersheds, New York, USA". Canadian Journal of Fisheries and Aquatic Sciences 62, nr 5 (1.05.2005): 1168–83. http://dx.doi.org/10.1139/f05-022.

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Effects of clear-cut and timber-stand improvement (TSI) harvests on water chemistry and mortality of caged brook trout (Salvelinus fontinalis) were evaluated in a study of three Catskill Mountain streams, 19942000. Harvests removed 73% of tree basal area (BA) from a clearcut subbasin, 5% BA from a TSI subbasin, and 14% BA at a site below the confluence of both streams. A fourth nonharvested site served as a control. Water quality and trout mortality were affected only in the clearcut stream. Acidity and concentrations of nitrate and inorganic monomeric aluminum (Alim) increased sharply during high flows after the first growing season (fall 1997). AcidAlim episodes were severe during this period and decreased steadily in magnitude and duration thereafter. All trout at this site died within 7 days during spring 1998 and 85% died during spring 1999. Only background mortality was observed in other years at this site and at the other three sites during all tests. The absence of mortality in TSI watersheds indicates that limited harvests should not harm brook trout populations in acid-sensitive streams. Effects of tree harvests on fish communities are of concern, however, because many stream-dwelling species are more sensitive to acidified waters than brook trout.

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Hanavan, R. P., J. Pontius i R. Hallett. "A 10-Year Assessment of Hemlock Decline in the Catskill Mountain Region of New York State Using Hyperspectral Remote Sensing Techniques". Journal of Economic Entomology 108, nr 1 (21.01.2015): 339–49. http://dx.doi.org/10.1093/jee/tou015.

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Yeo, Myeong‐Ho, Allan Frei, Rakesh K. Gelda i Emmet M. Owens. "A stochastic weather model for generating daily precipitation series at ungauged locations in the Catskill Mountain region of New York state". International Journal of Climatology 40, nr 2 (25.07.2019): 687–705. http://dx.doi.org/10.1002/joc.6230.

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Rozprawy doktorskie na temat "Catskill Mountain House (Catskill, New York)"

Scheer, Virginia. "Farmhouses That Became Boarding Houses in the Catskill Mountains of New York State". TopSCHOLAR®, 1999. http://digitalcommons.wku.edu/theses/755.

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In this thesis the author uses oral histories to study vernacular architecture, analyzing the changes in the way people in the Catskills have used buildings, specifically farm dwellings, to make a living, first as farmers and then as proprietors of boarding houses. The Catskills region in upstate New York is well known for its dairy farms and also for its resorts, but little has been researched to trace continuities and discrepancies between the rural residents and urban visitors. Boarding on farms in the late nineteenth and early twentieth centuries showed continuity between the two groups: recent immigrants who lived in New York City and rural families, whether long-established or recently arrived. The two groups used their living spaces in similar ways, one to achieve a healthful family vacation and the other to earn a living for the family on the farm. They made generalized use of unitary spaces (rooms), accommodating multiple activities and numbers of people in ways that were antithetical to the suburban middle-class' prescriptions for individual privacy, family privacy, and the specialization of spaces. Using oral histories and other primary sources, the author describes these similarities in space utilization as a commonality between urban and rural people in the Catskills, demonstrating that neither group is a passive consumer of architecture. Instead, they not only modify the rooms in the farmhouse but also continue to use or actively revive ways of using space that meet their goals, within the material resource at hand. Vernacular architecture is sometimes inaccurately equated with buildings that lack style. For architecture that may not seem to meet the criteria of the historians of style, people's words are the most eloquent interpretation of buildings and of the lives they sheltered.

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Książki na temat "Catskill Mountain House (Catskill, New York)"

Ratzer, Philip. Bungalow kid: A Catskill Mountain summer. Albany: Excelsior Editions/State University of New York Press, 2010.

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Evers, Alf. In Catskill country: Collected essays on mountain history, life, and lore. Woodstock, N.Y: Overlook Press, 1995.

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Stradling, David. Making mountains: New York City and the Catskills. Seattle: University of Washington Press, 2007.

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George, Jean Craighead. My side of the mountain. New York: Puffin Books, 1991.

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George, Jean Craighead. My side of the mountain. London: Red Fox, 1994.

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George, Jean Craighead. My side of the mountain. Waterville, Me: Thorndike Press, 2005.

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George, Jean Craighead. My side of the mountain. S.l: Thorndike Press, 2005.

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George, Jean Craighead. Mi rincón en la montaña. New York: Scholastic, 1997.

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To Know You: A Catskill Mountain House Summer. Outskirts Press, Incorporated, 2012.

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Steven Holl: Stretto House, Dallas, Texas, U.S.A.,1989-92 : "Y" House Catskill Mountains, New York, U.S.A., 1997-99. Tōkyō: Ē Dī Ē Edita Tōkyō, 2010.

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Części książek na temat "Catskill Mountain House (Catskill, New York)"

Rusch, Frederik L. "The Northeast". W A Jean Toomer Reader, 219–32. Oxford University PressNew York, NY, 1993. http://dx.doi.org/10.1093/oso/9780195083293.003.0018.

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Rusch, Frederik L. "The South". W A Jean Toomer Reader, 233–34. Oxford University PressNew York, NY, 1993. http://dx.doi.org/10.1093/oso/9780195083293.003.0019.

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Abstract Some miles northwest of New York, perhaps a hundred and fifty as the crow flies, there is a valley flanked by the southern spur-ends of the Catskill mountains. The valley is well watered. In summer, the natural grass and agricultural growths spread out in rich green waves and solid ractangles. Looked down upon from the mountain top, when the sun is shining, this carpet of the valley is amazingly fresh and brilliant. Towns, valley villages, irregular in form, houses for people and barns for cattle, belonging there, are clustered and scattered over the verdant lawn. The house[s] are white; some dulled to grey and greyish brown by long weathering. Most of them, built years ago, were built to stay and be homes. They are honest. The barns are red. The old red barns, among the finest forms of the American landscape. Peace, an active repose rests on this valley, wells up from it as dawn and twilight rise upward from horizons. When bands of cloud hang over it or drift slowly like great airships, the scene is magical. Particularly is it so if looked down upon from a mountain top when the sun rises and strikes these clouds, causing them to lift, turning them to mist and iridescence.

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Ettensohn, Frank R., D. Clay Seckinger, David P. Moecher i Cortland F. Eble. "Paleoenvironmental and tectonic implications of an Upper Devonian glaciogenic succession from east-central West Virginia, USA". W Field Excursions to the Appalachian Plateaus and the Valley and Ridge for GSA Connects 2023, 1–27. Geological Society of America, 2023. http://dx.doi.org/10.1130/2023.0066(01).

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ABSTRACT Glaciogenic rocks are rare in the Appalachian area and occur only locally as parts of Upper Precambrian and Upper Devonian successions. This trip examines a relatively recent exposure of Upper Devonian glaciogenic diamictites and laminites along Corridor H (U.S. Highway 48) in east-central West Virginia, USA. The diamictites occur in the Rockwell Member of the Price Formation, in transition with the underlying redbeds of the Upper Devonian Hampshire Formation. Palynology indicates that all parts of the Rockwell Member exposed at the locality are present in the Retispora lepidophyta – Verrucosisporites nitidus (LN) Miospore Biozone and are, therefore, of Late Devonian, but not latest Devonian, age. This biozone occurrence indicates correlation with parts of the Oswayo Member of the Price Formation, the Finzel tongue of the Rockwell Formation, and with dropstone-bearing parts of the Cleveland Shale Member of the Ohio Shale in northeastern Kentucky. Much previous work supports a glaciogenic origin for the diamictites and associated sediments, which occur as parts of a shallow-marine incursion that ended the Hampshire/Catskill alluvial-plain/deltaic complex across much of the Central Appalachian area. The glaciogenic succession is part of nearshore, marginal-marine strata that accumulated in an embayment during the Cleveland-Oswayo-Finzel transgression, which represents a global eustatic sea-level rise and foreland subsidence related to Acadian/Neoacadian deformational loading in the adjacent orogen. Detrital-zircon-provenance data from the diamictites indicate Ordovician plutonic sources as well as reworked Neoproterozoic to Ordovician sedimentary sources that can only have been derived from nearby Inner Piedmont sources like the Potomac terrane. This provenance suggests that Acadian/Neoacadian convergence of the exotic Carolina terrane with the New York and Virginia promontories along the southeastern margin of Laurussia not only uplifted Inner Piedmont source areas into a high mountain range capable of supporting glaciation in a subtropical setting, but also, through deformational loading, enhanced regional subsidence and the incursion of shallow seas that allowed alpine glaciers access to the open sea.

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