993 resultados para East Church (Salem, Mass.)


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This layer is a georeferenced raster image of the historic paper map entitled: Map of the towns of Brookfield, North Brookfield, West Brookfield, Worcester County, Mass, surveyed & drawn by L. Fagan. It was published by Richard Clark in 1855. Scale [ca. 1:21,120]. Covers the towns of Brookfield, East Brookfield, North Brookfield, and West Brookfield, 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) 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, drainage, public buildings, schools, churches, cemeteries, industry locations (e.g. mills, factories, mines, etc.), selected private buildings with names of property owners, town boundaries, and more. Relief shown by hachures. Includes also town center insets and selected building illustrations.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.

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This layer is a georeferenced raster image of the historic paper map entitled: Lands of The Eastern Point Associates, East Gloucester, Mass., [by] William H. Foss, engr. and supt. It was published by Forbes Co., Mar. 1st, 1888. Scale [ca. 1:3,550]. Cadastral map showing roads, property lot numbers, dimensions, and areas. Covers Eastern Point and part of East Gloucester, Gloucester, Massachusetts. Relief is shown by hachures. It includes two vignettes. 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 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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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.

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From the Introduction. The refugee question is at the core of the conflict between Israel and the Palestinians. Palestinians were first displaced as a direct consequence of the 1948 war and its aftermath. Twenty years later, another wave of Palestinian refugees was created as a consequence of the war during which Israel occupied the West Bank and the Gaza Strip. The purpose of the present paper is to: • deliver a critical analysis of past approaches to deal with the refugee issue in the various attempts to resolve the conflict between Israel and the Palestinians; • discuss lessons to be learned from the settlement and its implementation mechanisms in Bosnia and Herzegovina; and • propose a direction for a long-term strategy for the international community that avoids past pitfalls and could ultimately lead both parties to an agreement.

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The eastern part of the Northern Caucasus (Dagestan, Chechnya and Ingushetia) is becoming an increasingly distinct region in cultural, civilisational and social terms when compared to the rest of the Russian Federation. The situation on the ground there bears greater resemblance to the Middle East than to Russia: Islam is the key factor organising socio-political life, and conflicts inside the Muslim community, often involving bloodshed, are the driving power of developments in the region. The conflict is between the two main branches of Islam in the Northern Caucasus: Sufism linked to the official clergy and government, and Salafism which is gaining more and more supporters among young people in the Caucasus. Tension, including clashes over mosques, attacks, mass detentions, etc. has been observed mainly in Dagestan and Ingushetia.

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Regional variations in abundance, morphology, and chemical composition of Fe-Mn nodules have a zonal character. Due to circumcontinental zonality of terrigenous sedimentation the main mass of the nodules occurs in the pelagic part of the ocean, in areas of minimal sedimentation rates. In spatial variations in morphology and chemical composition of the nodules the latitudinal zonality is very clear and associated with latitudinal changes in facial conditions of sedimentation. Elevated contents of Mn, Ni, and Cu and of Mn/Fe ratio occur in nodules from the radiolarian belt. Changes of chemical composition of the nodules with depth (vertical zonality of mineralization) are confirmed. Local variations in abundance, morphology and chemical composition of the nodules are caused by ruggedness of relief and depth variations, variations in sedimentation rate, age of ore formation, intensity of diagenetic redistribution of metals.