Transvaal & Orange Free State Regions, South Africa, ca. 1899 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Bacon's large-print map of the Transvaal and Orange Free State. It was published by G.W. Bacon & Co. ca. 1899. Scale [ca. 1:1,900,000]. Covers also Swaziland, Lesotho, and portions of Botswana, Zimbabwe, and Mozambique.The image inside the map neatline is georeferenced to the surface of the earth and fit to the Africa Sinusoidal 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 drainage, cities and other human settlements, territorial and administrative boundaries, roads, railroads, shoreline features, and more. Relief shown by shading and spot heights. Includes also insets: "Map showing the routes from England and India to South Africa", "Environs of Cape Town", "Lorenço Marquez [and vicinity]", 'South Africa" and "Durban and Port Natal".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.

New England and Eastern New York Railroads, 1849 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Railroad map of New England & eastern New York : compiled from the most authentic sources, by J.H. Goldthwait. It was published in 1849 by Redding & Co. and Clark, Austin, & Co. Scale [ca. 1:700,000]. Covers Massachusetts, Rhode Island, Connecticut, and portions of New York, Vermont, New Hampshire, and Maine. The image inside the map neatline is georeferenced to the surface of the earth and fit to the USA Contiguous Albers Equal Area Conic projection (Meters). 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 features such as railroads completed and in progress, drainage, state, county, and town boundaries, and more. Includes inset: Boston & vicinity showing the Grand Junction R.R. Scale [ca. 1:170,000]. This layer is part of a selection of digitally scanned and georeferenced historic maps of New England 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, scales, and purposes.

European and North American Railway, New England and Eastern Canada, 1850 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Map of the European and North American Railway : showing its connection with the railways of the United States & Canada, [by] A.C. Morton, engineer. It was published in 1850 by Bowen & Co. Scale [ca. 1:1,625,000]. Covers New England, eastern New York, and the Maritime Provinces. The image inside the map neatline is georeferenced to the surface of the earth and fit to the USA Contiguous Albers Equal Area Conic projection (Meters). 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 features such as completed, in progress, and proposed railroads, selected towns, drainage, state boundaries, and more. Includes inset: Map showing the plan for shortening the transit between New York & London. This layer is part of a selection of digitally scanned and georeferenced historic maps of New England 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, scales, and purposes.

Sherbrooke, Eastern Townships and Kennebec Railway, New England, 1874 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Map of the Sherbrooke, Eastern Townships and Kennebec Railway : with connections, prepared by G.W. & C.B. Colton & Co. It was published in 1874. Scale [ca. 1:1,267,200]. Covers New Hampshire, Vermont, Massachusetts, Connecticut, Rhode Island, and portions of New Jersey, Pennsylvania, New York, Maine, and the province of Quebec, Canada. The image inside the map neatline is georeferenced to the surface of the earth and fit to the USA Contiguous Albers Equal Area Conic projection (Meters). 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 features such as railroads, railroad connections and stations, drainage, state and county boundaries, and more. Includes inset: [Sherbrooke, Eastern Townships and Kennebec Railway in province of Québec]. Scale [ca. 1:921,600]. This layer is part of a selection of digitally scanned and georeferenced historic maps of New England 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, scales, and purposes.

Eastern Point, East Gloucester, Massachusetts, 1888 (Raster Image)

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.

The Impact of Visa Liberalisation in Eastern Partnership Countries, Russia and Turkey on Trans-Border Mobility. CEPS Liberty and Security in Europe No. 63, March 2014

Schengen Visa liberalisation in the Eastern Partnership countries, Russia and Turkey has proven to have a huge transformative potential across the justice, liberty and security policies of the countries where it has been deployed. Far-reaching technical reforms in the fields of document security, irregular migration and border management, public order security and fundamental rights have to be implemented so that visa-free travel can be allowed. Evidence provided by visa applications data reveals that visa liberalisation is a logical step, provided that the technical reforms are adopted and implemented. This study analyses the current state of play of the implementation of the EU visa policy instruments and assesses the positive impact of visa-free travel on trans-border mobility according to current visa application statistics.

In a state of necessity. How has Orban changed Hungary. OSW Point of View Number 41, April 2014

Viktor Orban’s sweeping victory in the 2010 election ensured his party, Fidesz, a constitutional two-thirds majority in parliament. The party took over the rule of the country from the discredited political left when Hungary was plunged in political and economic crisis. Claiming that the circumstances were unusual and that it had a strong electoral mandate, Fidesz introduced radical changes in the country and thus challenged the previous economic and political order. These changes have led to an unprecedented concentration of power and provoked a discussion on the limits of democracy and the rule of law in the European Union. The state’s economic role has strengthened. The Orban government has been unable to overcome economic stagnation but it has managed to stabilise Hungary’s budget situation, which needs to deal with the high debt. Hungary’s relations with most partners in the EU and NATO have cooled due to controversial moves made by its government. As regards foreign policy and economic co-operation, Orban has granted high priority to the ‘Eastern opening’, where Russia has assumed the leading role.

European Neighbourhood Policy Package - Conclusions for the Eastern Partners. OSW Commentary No. 78, 2012-05-25

In 2011 the European Union began a process aimed at reforming its policy on the Eastern and Southern Neighbourhood. The change in circumstances in neighbouring countries following the Arab Spring, along with the lack of significant progress regarding Eastern Europe’s integration with the EU, formed the main driving force behind this process. The prime objective of the changes to the European Neighbourhood Policy (ENP) was the need to introduce new incentives for partner countries to modernise and integrate more closely with the EU Another aim was to increase the flexibility of EU instruments (by adapting them to the specific context of each partner state). One year later, on 15 May 2012, the European Commission and the EU High Representative for Foreign Affairs and Security Policy published the European Neighbourhood Policy Package which reported on the progress made in the implementation of the ENP over the preceding year and set out the aims and Action Plans for 20131. An analysis of the outcomes of changes made to the EU policy towards Eastern Europe and the South Caucasus suggests that the aim of the revision was aimed more at addressing the changing political landscape in the region rather than at the implementation of a substantial reform of the neighbourhood policy. The ENP is largely based on bureaucratic procedures (the negotiation of bilateral agreements, the implementation of support programmes). These have only a limited capacity to bring about lasting change in the region, as has been exemplified by the deterioration of democratic standards in a number of countries; this was highlighted in EU’s own reports. This problem is particularly clear in the case of Ukraine; until recently it was seen as the leader of European integration but is now raising much concern due to a deterioration in the state of democracy there. EU instruments have a limited influence on the situation in Eastern Partnership countries and the region’s significance on the EU’s agenda is falling (the priority is now given to counteracting the economic crisis, and prominence in the neighbourhood policy has been given to the Southern Mediterranean). In response to this EU policy on Eastern Europe will focus to a larger extent on technical and sectoral cooperation.

Ending the State-Building Impasse: What Can Be Learned from Previous EU Enlargements that Might Offer Solutions for Bosnia and Herzegovina. ACES Working Paper No. 10, 2007

On the basis of the success of the two previous waves of European Union enlargement to post-communist states, EU accession is the international community's solution for ending the state-building impasse in Bosnia and Herzegovina. Through a literature review of analysis of the recent EU enlargements, this paper compares those countries' experiences with the current situation in Bosnia, and raises questions about the ability of the EU to address state-building issues through the accession process. The paper concludes that the previous enlargements do not provide a model for state-building in Bosnia. Because the EU's attempts to help along the process of state building in Bosnia is a new type of policy project, the paper proposes how the enlargement process might be adapted to address the specific problems in Bosnia, particularly in terms using human rights norms to compel Bosnian leaders to adopt necessary reforms.

Social Investment and State Capacity. CEPS Working Document No. 419/February 2016

This paper looks at the difference between the levels and nature of social policy expenditure in northern and northwest European countries and the countries of southern, central, and eastern Europe, and examines the relationship between social investment and state capacity in these country groupings. The authors show that southern and eastern countries have a much greater preference for ‘compensating’ rather than ‘capacitating’ social policy spending. Furthermore, the state capacity in these countries is lower, which generates less state revenue. Based on these observations they conclude that low state capacity and low state revenue go hand in hand with the preference for capacitating social policies, as these policies involve less delegation and discretion than social investment policies. This paper shows that high state capacity is probably a necessary precondition for effective social investment policies, although some limited alternative paths do exist.

To be or not to be an EU member state – A question for the Balkan aspirants as well? EPC Commentary, 13 July 2016

Last month, a majority of British voters decided that the UK should leave the European Union (EU). In the wake of the Brexit result, anti-EU politicians in a host of member states began to float the idea of putting the same ‘in-out’ option to electorates in their own countries. As the economic and political fallout of the UK’s choice to withdraw from the EU continues to unfold, an acute sense of uncertainty gathers steam and ripples not just through the remaining member states but also their EU-hopeful neighbours in the Balkans. What will the departure of the UK from the EU mean for the Balkan enlargement process?

Polyaromatic hydrocarbons in sediments from the Barents and White Seas

Polycyclic aromatic hydrocarbons (PAHs) are common environmental contaminants which can be derived from anthropogenic sources, such as combustion and discharges from extraction and transport, and natural processes, including leakage and erosion of fossil carbon. Natural PAH sources contribute, along with biological activities and terrestrial run-off, to the organic carbon content in sediments.The Barents Sea region is far from many anthropogenic sources of PAH, but production and trans-shipment of hydrocarbons is increasing. We present data for polycyclic aromatic hydrocarbon (PAH) concentrations in bottom sediments from 510 stations in the Barents and White Seas, and along the northern coast of Norway.

Geochemistry and sedimentation rates of ODP Leg 199 sites and of surface sediments in the eastern Pacific ocean

We present the first high-resolution organic carbon mass accumulation rate (MAR) data set for the Eocene equatorial Pacific upwelling region, from Sites 1218 and 1219 of the Ocean Drilling Program. A maximum Corg MAR anomaly appears at 41 Ma and corresponds to a high carbonate accumulation event (CAE). Independent evidence suggests that this event (CAE-3) was a time of rapid cooling. Throughout the Eocene, organic carbon burial fluxes were an order of magnitude lower than fluxes recorded for the Holocene. In contrast, the expected organic carbon flux, calculated from the biogenic barium concentrations for these sites, is roughly equal to modern. A sedimentation anomaly appears at 41 Ma, when both the measured and the expected organic carbon MAR increases by a factor of two-three relative to the background Eocene fluxes. The rain of estimated Corg and barium from the euphotic zone to the sediments increased by factors of three and six, respectively. We suggest that the discrepancy between the expected and measured Corg in the sediments is a direct consequence of the increased metabolic rates of all organisms throughout the Eocene oceans and sediments. This hypothesis is supported by recent work in ecology and biochemical kinetics that recognizes the fundamental basis of ecology as following from the laws of thermodynamics. This dependence is now elucidated as the Universal Temperature Dependence (UTD) "law" of metabolism and can be applied to all organisms over their biologically relevant temperature range. The general pattern of organic carbon and barium deposition throughout the Eocene is consistent with the UTD theory. In particular, the anomaly at 41 Ma (CAE-3) is associated with rapid cooling, an event that triggered slower metabolic rates for all organisms, slower recycling of organic carbon in the water and sediment column, and, consequently, higher deposition of organic carbon in the sediments. This "metabolism-based" scenario is consistent with the sedimentation patterns we observe for both Sites 1218 and 1219.

Late pleistocene and holocene sedimentation in the central and eastern Persian Gulf

The sandfraction of the sediment was analysed in five cores, taken from 65 m water depth in the central and eastern part of the Persian Gulf. The holocene marls are underlayn by aragonite muds, which are probably 10-11,000 years old. 1. The cores could be subdivided into coarse grained and fine grained layers. Sorting is demonstrated by the following criteria: With increasing median values of the sandfraction - the fine grained fraction decreases within each core; - the median of each biogenic component, benthonic as well as planktonic, increases; - the median of the relict sediment, which in core 1179 was carried upward into the marl by bioturbation, increases; - the percentages of pelecypods, gastropods, decapods and serpulid worms in the sandfraction increase, the percentages of foraminifera and ostracods decrease; - the ratios of pelecypods to foraminifera and of decapods to ostracods increase; - the ratios of benthonic molluscs to planktonic molluscs (pteropods) and of benthonic foraminifera to planktonic foraminifera increase (except in core 1056 and 1179); - the ratio of planktonic molluscs (pteropods) to planktonic foraminifera increases; - the globigerinas without orbulinas increase, the orbulinas decrease in core 1056. Different settling velocities of these biogenic particles help in better understanding the results : the settling velocities, hence the equivalent hydrodynamic diameters, of orbulinas are smaller than those of other globigerinas, those of planktonic foraminifera are smaller than those of planktonic molluscs, those of planktonic molluscs are smaller than those of benthonic molluscs, those of pelecypods are smaller than those of gastropods. Bioturbation could not entirely distroy this "grain-size-stratification". Sorting has been stronger in the coarse layers than in the finer ones. As a cause variations in the supply of terrigenous material at constant strength of tidal currents is suggested. When much terrigenous material is supplied (large contents of fine grained fraction) the sedimentation rates are high: the respective sediment surface is soon covered and removed from the influence of tidal currents. When, however, the supply of terrigenous material is small, more sandy material is taken away in all locations within the influence of terrigenous supply. Thus the biogenic particles in the sediment do not only reflect the organic production, but also the influence of currents. 2. There is no parameter present in all cores that is independently variable from grain size and can be used for stratigraphic correlation. The two cores from the Strait of Hormus were correlated by their sequences of coarse and fine grained layers. 3. The sedimentation rates of terrigenous material, of total planktonic and benthonic organisms and of molluscs, foraminifera, echinoids and ophiuroids are shown in table 1 (total sediment 6.3-75.5 cm/1000 yr, biogenic carbonate 1.9-3.6 cm/1000 yr). The sedimentation rates of benthonic organisms are nearly the same in the cores of the Strait of Hormus, whereas near the Central Swell they are smaller. In the upper parts of the two cores of the Strait of Hormus sedimentation rates are higher than in the deeper parts, where higher median values point to stronger reworking. 4. The sequence of coarse and fine grained intervals in the two cores of the Hormus Strait, attributed to variations in climate, as well as the increase of terrigenous supply from the deeper to the upper parts of the cores, agrees with the descriptions in the literature of the post Pleistocene climate as becoming more humid. The rise of sea level is sedimentologically not measurable in the marly sediments - except perhaps for the higher content of echinoids in the lower part of core 1056. These may be attributed to the influence of a migrating wave-base. 5. The late Pleistocene aragonite mud is very fine grained (> 50%< 2 p) and poor in fossils (0.5-1.8%) biogenic particles of total sediment. The sand fraction consists almost entirely of white clumps, c. 0.1 mm in diameter (1177), composed of aragonite needles and of detrital minerals with the same size (1201). The argonite mud was probably not formed in situ, because the water depth at time of formation was at most 35 m at least 12 m. The sorting of the sediment (predominance of the fine grained sand), the absence of larger biogenic components and of pellets, c. 0.2-0.5 mm in diameter, which are typical for Recent and Pleistocene locations of aragonite formation, as well as the sedimentological conditions near the sampling points, indicate rather a transport of aragonite mud from an area of formation in very shallow waters. Sorting as well as lenticular fabric in core 1201 point to sedimentation within the influence of currents. During alternating sedimentation - and reworking processes the aragonitic matrix was separated from the silt - and sand-sized minerals. The lenses grade into touches because of bioturbation. 6. In core 1056 D2 from Hormus Bay the percentages of organic carbon, total nitrogen and total carbonate were determined. With increasing amounts of smaller grain sizes the content of organic matter increases, whereas the amount of carbonate decreases. The amounts of organic carbon and of nitrogen decrease with increasing depth, probably due to early-diagenetic decomposition processes. Most of the total nitrogen is of organic origin, only about 10% may well be inorganically fixed as ammonium-nitrogen. In the upper part of the core the C/N-ratio increases with increasing depth. This may be connected with a stronger decomposition of nitrogen-containing organic compounds. The general decrease of the C/N-ratios in the lower part of the core may be explained by the relative increase of inorganically fixed ammonium-nitrogen with decreasing content of organic matter.

The National Highway Traffic Safety Administration 1980-1981 workshops on alcohol and occupant restraints - eastern series. Final report.

National Highway Traffic Safety Administration, Washington, D.C.