973 resultados para Hale, Nathan, 1755-1776
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Premio Extraordinario de Doctorado. Rama de Artes y Humanidades. Tesis Mención con Doctorado Europeo
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La tesi indaga il significato del concetto di “preesistenze ambientali” nel pensiero teorico dell’architetto Ernesto Nathan Rogers. Il tema è scelto come punto di vista privilegiato per indagare il contributo di Rogers al dibattito sull’eredità del Movimento Moderno in un momento, il secondo dopoguerra, in cui si intensifica la necessità di soffermare l’attenzione delle riflessioni teoriche sulle relazioni tra ambiente e progetto. Il problema fu inteso come la ricerca di un linguaggio adeguato all’era macchinista e di un ordine formale per lo sviluppo urbano recente da costruire in funzione del suo rapporto con la città consolidata. Esso fu sviluppato, all’interno dell’opera teorica rogersiana, come riflessione sulla dialettica contrapposizione tra intuizione e trasmissione del sapere, contingenza e universalità. La tesi mostra le ricche connessioni culturali tramite cui tale dialettica è capace di animare un discorso unitario che va dall’insegnamento del Movimento Moderno alle ricerche tipologiche e urbane della cultura italiana degli anni Sessanta. Riportando il concetto di preesistenze ambientali alla sua accezione originale, da un lato attraverso la ricostruzione delle relazioni intellettuali instaurate da Rogers con il Movimento Moderno e i CIAM, dall’altro mediante l’approfondimento del progetto editoriale costruito durante la direzione della rivista “Casabella continuità”, la tesi intende conferire alla nozione il valore di un contributo importante alla teoria della progettazione architettonica urbana. Il concetto di preesistenze ambientali diventa così la chiave analitica per indagare, in particolare, l’influenza del dibattito dell’VIII CIAM su Il Cuore della città e della partecipazione di Rogers al lavoro di redazione dell’Estudio del Plan di Buenos Aires nel 1948-1949 nella maturazione del progetto editoriale di “Casabella continuità” (1954-1965) attraverso l’attribuzione di un preciso valore all’archetipo, alla fenomenologia e alla tradizione nella definizione del rapporto architettura e storia.
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This thesis assesses relationships between vegetation and topography and the impact of human tree-cutting on the vegetation of Union County during the early historical era (1755-1855). I use early warrant maps and forestry maps from the Pennsylvania historical archives and a warrantee map from the Union County courthouse depicting the distribution of witness trees and non-tree surveyed markers (posts and stones) in early European settlement land surveys to reconstruct the vegetation and compare vegetation by broad scale (mountains and valleys) and local scale (topographic classes with mountains and valleys) topography. I calculated marker density based on 2 km x 2 km grid cells to assess tree-cutting impacts. Valleys were mostly forests dominated by white oak (Quercus alba) with abundant hickory (Carya spp.), pine (Pinus spp.), and black oak (Quercus velutina), while pine dominated what were mostly pine-oak forests in the mountains. Within the valleys, pine was strongly associated with hilltops, eastern hemlock (Tsuga canadensis) was abundant on north slopes, hickory was associated with south slopes, and riparian zones had high frequencies of ash (Fraxinus spp.) and hickory. In the mountains, white oak was infrequent on south slopes, chestnut (Castanea dentata) was more abundant on south slopes and ridgetops than north slopes and mountain coves, and white oak and maple (Acer spp.) were common in riparian zones. Marker density analysis suggests that trees were still common over most of the landscape by 1855. The findings suggest there were large differences in vegetation between valleys and mountains due in part to differences in elevation, and vegetation differed more by topographic classes in the valleys than in the mountains. Possible areas of tree-cutting were evenly distributed by topographic classes, suggesting Europeans settlers were clearing land and harvesting timber in most areas of Union County.
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We use various data sets, including images from the High Resolution Imaging Science Experiment camera (HiRISE), to examine the ejecta of the generally fresh-looking Hale crater that occurs in the rugged mountain terrain of Nereidum Montes in the northern rim materials of the Argyre impact structure on Mars. Our investigation reveals that the distal parts of the Hale crater ejecta and other basin deposits behave like viscous flows, which we attribute to the secondary flow of ejecta mixed with water–ice-rich basin materials. Consistent with water-enrichment of the basin materials, our mapping further reveals occasionally deformed surfaces, including highly conspicuous features such as mounds and fractured plateaus that we interpret to be a result of periglacial modification, subsequent (including possibly present-day) to the transient localized melting and fluvial erosion caused by Hale-impact-generated heating. In particular, our morphometric analysis of a well-defined valley system west of Hale crater suggests that it may have been formed through hydrologic/glacial activity prior to the Hale impact, with additional modification resulting from the impact and subsequent geologic and hydrologic phenomena including glacial and periglacial activity.
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von H. de Grousilliers