969 resultados para 1800-tal.
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This layer is a georeferenced raster image of the historic paper map entitled: Africa. It was published by Calcogafia Vignozzi in 1800. Scale [ca. 1:30,000,000]. The image inside the map neatline is georeferenced to the surface of the earth and fit to a non-standard 'World Aitoff' projection with the central meridian at 20 degrees east. All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This map shows features such as drainage, cities and other human settlements, territorial boundaries, shoreline features, and more. Relief is shown pictorially.This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection and the Harvard University Library as part of the Open Collections Program at Harvard University project: Organizing Our World: Sponsored Exploration and Scientific Discovery in the Modern Age. Maps selected for the project correspond to various expeditions and represent a range of regions, originators, ground condition dates, scales, and purposes.
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This layer is a georeferenced raster image of the historic paper map entitled: A chart of the harbour of Boston : with soundings, sailing marks, &c. taken from Holland's survey's [sic], carefully revised and corrected by Osgood Carleton, Esqr. Republished and sold by W. Norman, book and chart-seller ca. 1800. Scale [ca. 1:25,500]. Covers Boston Harbor and adjacent lands. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Massachusetts State Plane Coordinate System, Mainland Zone (in Feet) (Fipszone 2001). All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, or other information associated with the principal map. This map shows coastal features such as rocks, channels, points, coves, islands, and more. Depths are shown by soundings and shading. It also shows land features such as roads, drainage, and more. Relief is shown pictorially and by hachures. This layer is part of a selection of digitally scanned and georeferenced historic maps of Massachusetts from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of regions, originators, ground condition dates (1755-1922), scales, and purposes. The digitized selection includes maps of: the state, Massachusetts counties, town surveys, coastal features, real property, parks, cemeteries, railroads, roads, public works projects, etc.
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An ijāzah issued by Aḥmad ibn ʻUbayd Allāh al-ʻAṭṭār to his student Muḥammad ibn Shafīʻ Sulṭān. The student's name is mentioned on fol. 1v; the master's name on fol. 6r. In the ijāzah al-ʻAṭṭār traces his authority back to al-Qasṭallānī's al-Mawāhib al-ladunnīyah, then to al-Shāfiʻī, and then gives his isnād of a musalsal ḥadīth.
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min muṣannafāt Aqā Mīrzā Ṣāliḥ al-maʻrūf bi-Dāmād.
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Tese de doutoramento, História (História Contemporânea), Universidade de Lisboa, Faculdade de Letras, 2016
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In recent years, interest in comtemporary conceptions and self-understandings of the social order has grown among historians, yet the field of an "intellectual history of society" is little expJored for modern Germany. This paper surveys the field and asks how Germans from the early modern era up to the present time of German reunification conceived of the social order they were building and living in, and it provides an overview of the developments of such major concepts as "estate" and "class," "community" and "society," "individual" and "mass," "state" and "nation." Three major points emerge as persistent and distinctive features of German social self-conception in the nineteenth cand twentieth centuries: the intellectual construction of dilemmas between social conformity and social fragmentation; the difficulties of conceiving of society as a plitical society; and the "futurization" of an idealized, utopian social roder of harmony that was hoped would one day replace the perceived social disintegration.
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Aim: Models project that climate warming will cause the tree line to move to higher elevations in alpine areas and more northerly latitudes in Arctic environments. We aimed to document changes or stability of the tree line in a sub-Arctic model area at different temporal and spatial scales, and particularly to clarify the ambiguity that currently exists about tree line dynamics and their causes. Location: The study was conducted in the Tornetrask area in northern Sweden where climate warmed by 2.5 °C between 1913 and 2006. Mountain birch (Betula pubescens ssp. czerepanovii) sets the alpine tree line. Methods: We used repeat photography, dendrochronological analysis, field observations along elevational transects and historical documents to study tree line dynamics. Results: Since 1912, only four out of eight tree line sites had advanced: on average the tree line had shifted 24 m upslope (+0.2 m/year assuming linear shifts). Maximum tree line advance was +145 m (+1.5 m/year in elevation and +2.7 m/year in actual distance), whereas maximum retreat was 120 m downslope. Counter-intuitively, tree line advance was most pronounced during the cooler late 1960s and 1970s. Tree establishment and tree line advance were significantly correlated with periods of low reindeer (Rangifer tarandus) population numbers. A decreased anthropozoogenic impact since the early 20th century was found to be the main factor shaping the current tree line ecotone and its dynamics. In addition, episodic disturbances by moth outbreaks and geomorphological processes resulted in descent and long-term stability of the tree line position, respectively. Main conclusions: In contrast to what is generally stated in the literature, this study shows that in a period of climate warming, disturbance may not only determine when tree line advance will occur but if tree line advance will occur at all. In the case of non-climatic climax tree lines, such as those in our study area, both climate-driven model projections of future tree line positions and the use of the tree line position for bioclimatic monitoring should be used with caution.
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Mode of access: Internet.