Tokyo, Japan, 1860 (Image 1 of 4) (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Man'en kaisei O-Edo oezu, Takai Ranzan zu. It was published by Okadaya Kashichi in Man'en gannen in 1860. Scale [ca. 1:10,700]. This layer is image 1 of 4 total images of the four sheet source map, representing the northwest portion of the map. Covers Tokyo, Japan. Map in Japanese.The image inside the map neatline is georeferenced to the surface of the earth and fit to the Tokyo Universal Transverse Mercator (UTM) Zone 54N projected coordinate system. 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 roads, railroads and stations, drainage, built-up areas and selected buildings, names of landowners, parks, and more. Shows main temples, shrines, and points of interest pictorially.This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of originators, ground condition dates, scales, and map purposes.

Tokyo, Japan, 1860 (Image 3 of 4) (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Man'en kaisei O-Edo oezu, Takai Ranzan zu. It was published by Okadaya Kashichi in Man'en gannen in 1860. Scale [ca. 1:10,700]. This layer is image 3 of 4 total images of the four sheet source map, representing the northeast portion of the map. Covers Tokyo, Japan. Map in Japanese.The image inside the map neatline is georeferenced to the surface of the earth and fit to the Tokyo Universal Transverse Mercator (UTM) Zone 54N projected coordinate system. 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 roads, railroads and stations, drainage, built-up areas and selected buildings, names of landowners, parks, and more. Shows main temples, shrines, and points of interest pictorially.This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of originators, ground condition dates, scales, and map purposes.

Tokyo, Japan, 1860 (Image 4 of 4) (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Man'en kaisei O-Edo oezu, Takai Ranzan zu. It was published by Okadaya Kashichi in Man'en gannen in 1860. Scale [ca. 1:10,700]. This layer is image 4 of 4 total images of the four sheet source map, representing the southwest portion of the map. Covers Tokyo, Japan. Map in Japanese.The image inside the map neatline is georeferenced to the surface of the earth and fit to the Tokyo Universal Transverse Mercator (UTM) Zone 54N projected coordinate system. 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 roads, railroads and stations, drainage, built-up areas and selected buildings, names of landowners, parks, and more. Shows main temples, shrines, and points of interest pictorially.This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of originators, ground condition dates, scales, and map purposes.

East Bridgewater, Massachusetts, 1848 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Map of East Bridgewater, Mass., surveyed by M. Bates, Jr., 1848. It was published by J.H. Bufford's Lithography in 1848. Scale [1:19,800]. Covers also portions of Whitman and Brockton, Massachusetts. 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, index maps, legends, or other information associated with the principal map. This map shows features such as roads, railroads, drainage, public buildings, schools, churches, cemeteries, industry locations (e.g. mills, factories, mines, etc.), private buildings with names of property owners, town and district boundaries and more. Relief is shown by hachures.This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of originators, ground condition dates, scales, and map purposes.

San Francisco, California, 1863 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Map of the City & County of San Francisco : carefully compiled from recent surveys, including all new additions of cities, towns, and villas, delineating the lines of ranchos, private claims water works, railroads, &c. &c., drawn for the San Francisco News Letter and the Pacific Mining Journal by James Butler. It was published by Britton & Co. in 1863. Scale [1:15,840].The image inside the map neatline is georeferenced to the surface of the earth and fit to the California State Plane NAD 1983 coordinate system (Zone III) (in Feet) (Fipszone 0403). 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 roads, railroads, drainage, shoreline features, property lots, numbers and landowner names, reserved government properties, ranchos, city boundaries, cemeteries, water works, and more.This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of originators, ground condition dates, scales, and map purposes.

Duxbury, Massachusetts, 1833 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Map of Duxbury, Mass., surveyed by John Ford, Jr. It was published by Pendleton's Lithogy. in 1833. Scale [ca. 1:19,799]. 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, index maps, legends, or other information associated with the principal map. This map shows features such as roads, drainage, public buildings, schools, churches, cemeteries, industry locations (e.g. mills, factories, mines, etc.), private buildings with names of property owners, town boundaries and more. Relief shown by shading.This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of originators, ground condition dates, scales, and map purposes.

Newbury, West Newbury, & Newburyport, Massachusetts, 1830 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Map of the original town of Newbury, now divided into Newbury, Newburyport, and West Newbury, surveyed & drawn by Philan[de]r Anderson for Moses Petangell in 1830. It was published by Pendleton's Lithography in 1830. Scale [1:19,800]. 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, index maps, legends, or other information associated with the principal map. This map shows features such as roads, drainage, public buildings, schools, churches, cemeteries, industry locations (e.g. mills, factories, mines, etc.), private buildings with names of property owners, town boundaries and more. Relief shown by shading.This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of originators, ground condition dates, scales, and map purposes.

Tokyo, Japan, 1859 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: O-Edo ezu. It was published by Suharaya Mohe zohan in Ansei 6 [1859]. Scale [ca. 1:14,000]. Covers Tokyo, Japan. Map in Japanese.The image inside the map neatline is georeferenced to the surface of the earth and fit to the Tokyo Universal Transverse Mercator (UTM) Zone 54N projected coordinate system. 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 roads, railroads and stations, drainage, built-up areas and selected buildings, names of landowners, parks, and more. Shows main shrines and temples pictorially. This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of originators, ground condition dates, scales, and map purposes.

Framingham, Massachusetts, 1832 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Map of Framingham : from actual surveys taken by Jonas Clayes & Warren Nixon in the years 1830 and 1831, drawn by Warren Nixon. It was published by Pendleton's Lithography in 1832. Scale [19,800]. Covers also a portion of Ashland, Massachusetts. 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, index maps, legends, or other information associated with the principal map. This map shows features such as roads, drainage, public buildings, schools, churches, cemeteries, industry locations (e.g. mills, factories, mines, etc.), private buildings with names of property owners, town boundaries and more. Relief shown by shading.This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of originators, ground condition dates, scales, and map purposes.

The Empirical Content of the Present Value Model: A survey of the instrumental uses of farmland prices. Factor Markets Working Document No. 53, June 2013

After reviewing the Present Value Model (PVM), in its basic form and with its major extensions, the authors carried out a literature review on the instrumental uses of farm land prices; namely what land prices may reveal in the framework of the PVM. Urban influence, non-market goods and climate change are topics where the PVM used with applied data may reveal farmers’ or landowners’ beliefs or subjective values, which are discussed in this paper. There is also extensive discussion of the topic of public regulations, and how they may affect land price directly, or through its present value.

Empirical Evidence of the Distributional Effects of the CAP in the New EU Member States. Factor Markets Working Document No. 58, August 2013

This study, carried out in the context of the Factor Markets research project, investigates the impact of the SAPS (Single Area Payment Scheme) on farmland rental rates in the new EU member states. Using a unique set of farm level panel data with 20,930 observations for 2004 and 2005 we are able to control for important sources of endogeneity. According to our results, the SAPS has a positive and statistically significant impact on land rents in the EU. However, the estimated incidence is smaller than predicted theoretically. Land rents capture only 19 cents of the marginal SAPS euro, and around 10% of the SAPS benefit non-farming landowners through higher farmland rental prices. As the share of rented land is higher in corporate farms than individual ones, family farms benefit more from the SAPS than corporate farms do.

Violencia e invisibilidad indígena : La cuestión de los pueblos originarios durante el primer peronismo

El presente trabajo busca profundizar en el análisis de los vínculos existentes entre el primer gobierno peronista y la cuestión indígena, centrándose en las políticas gubernamentales desarrolladas por el gobierno de Perón frente a dos fuertes conflictos violentos que tuvieron lugar entre 1946 y 1947: el "Malón de la paz", la movilización indígena llevada a cabo entre mayo y agosto de 1947, cuando 174 kollas caminaron 2000 kilómetros desde la Puna y el valle de Orán hasta la Capital Federal para reclamar por la titularidad de sus tierras, en manos de terratenientes y en denuncia de las condiciones de explotación en las que trabajaban; y "Masacre de Rincón Bomba", el conflicto desarrollado en una pequeña localidad de Formosa, cuando indígenas de comunidades wichi, tobas y principalmente pilagás fueron masacradas por la Gendarmería Nacional en un confuso episodio, que sale a la luz hace pocos años. El objetivo en ambos puntos es doble: por un lado analizar la relación entre los intereses e intenciones del gobierno de Juan Domingo Perón para con las comunidades originarias, visibilizando su existencia y sus condiciones de vida en tanto sujetos de derechos históricamente vulnerados. Por otro, abrir el debate historiográfico sobre el quehacer de los historiadores respecto de una temática que ha sido silenciada durante décadas, negando la existencia y la identidad de los pueblos originarios

Sedimentology of core PS2564-3 and GeoB2110-4

In the South Atlantic and adjoining Southern Ocean the kaolinite/chlorite-ratio in Late Quaternary sediments are an alternative deep water proxy to benthic foraminiferal proxies and carbonate preservation indices that is even suitable in regions with poor carbonate preservation. This paper shows the relationship between modern abyssal circulation and the kaolinite/chloriteratio and presents reconstructions of deep and bottom water advection based on the kaolinite/ chlorite proxy. We also discuss the limitations and future perspectives of the kaolinite/chlorite proxy. Latitudinal and water depth-related patterns of the kaolinite/chlorite-ratio in surface sediments correspond to the modern deep and bottom water mass distribution. Kaolinite originates from lowlatitudes and traces North Atlantic Deep Water (northern-source deep water) advection to the south. Chlorite from the southern high-latitudes is exported via northward advecting Antarctic Bottom Water and Circumpolar Deep Water (southern-source deep and bottom water). Deep-sea sedimentation in regions underlying the Antarctic Circumpolar Current was current-dominated throughout the Late Quaternary. Temporal variations of the kaolinite/chlorite-ratio in response to glacial-interglacial cycles reflect changing deep water mass configurations, suggesting a shallowing and northward retreat of northern-source deep water and accordingly wider expansion of southernsource deep and bottom water masses during glacial times relative to interglacial times. Submarine topography influenced the spatial and temporal patterns of deep water mass distribution.

Sedimentology of surface samples from the Weddell Sea, Antarctica

Mineralogical and granulometric properties of glacial-marine surface sediments of the Weddell Sea and adjoining areas were studied in order to decipher spatial variations of provenance and transport paths of terrigenous detritus from Antarctic sources. The silt fraction shows marked spatial differences in quartz contents. In the sand fractions heavy-mineral assemblages display low mineralogical maturity and are dominated by garnet, green hornblende, and various types of clinopyroxene. Cluster analysis yields distinct heavy-mineral assemblages, which can be attributed to specific source rocks of the Antarctic hinterland. The configuration of modern mineralogical provinces in the near-shore regions reflects the geological variety of the adjacent hinterland. In the distal parts of the study area, sand-sized heavy minerals are good tracers of ice-rafting. Granulometric characteristics and the distribution of heavy-mineral provinces reflect maxima of relative and absolute accumulation of ice-rafted detritus in accordance with major iceberg drift tracks in the course of the Weddell Gyre. Fine-grained and coarse-grained sediment fractions may have different origins. In the central Weddell Sea, coarse ice-rafted detritus basically derives from East Antarctic sources, while the fine-fraction is discharged from weak permanent bottom currents and/or episodic turbidity currents and shows affinities to southern Weddell Sea sources. Winnowing of quartz-rich sediments through intense bottom water formation in the southern Weddell Sea provides muddy suspensions enriched in quartz. The influence of quartz-rich suspensions moving within the Weddell Gyre contour current can be traced as far as the continental slope in the northwestern Weddell Sea. In general, the focusing of mud by currents significantly exceeds the relative and absolute contribution of ice-rafted detritus beyond the shelves of the study area.