Adirondack Mountains Region, New York, 1883 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Map of the Adirondack wilderness, compiled by S.R. Stoddard. 4th rev. ed. It was published by S.R. Stoddard in 1883. Scale [ca. 1:255,000]. Covers the Adirondack Mountains Region, New York, including portions of St. Lawrence, Franklin, Clinton, Lewis, Herkimer, Hamilton, Essex, Warren, and Saratoga Counties. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Universal Transverse Mercator (UTM) Zone 18N NAD83 projection. 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 natural features, drainage, railroads, important roads, ordinary roads, carries and trails, and township and county boundaries, and more. "Distances are given in Figures on Roads and Trails. Air-Line Distances from Mount Marcy are indicated by Circles, 10 miles apart." Relief is shown by hachures and spot heights. This layer is part of a selection of digitally scanned and georeferenced historic maps from The Harvard Map Collection as part of the Imaging the Urban Environment project. Maps selected for this project represent major urban areas and cities of the world, at various time periods. These maps typically portray both natural and manmade features at a large scale. The selection represents a range of regions, originators, ground condition dates, scales, and purposes.

Wilmington and Topsail Sound Region, North Carolina, 1865 (Raster Image)

This layer is a georeferenced raster image of the historic, paper manuscript map entitled: Map of country between the N.E. Cape-Fear River and Topsail sound, made under the direction of Capt. Wm. H. James, Chf. Engineer, by B.L. Blackford, Top. Engrs. It was drawn in 1865. Scale 1:40,000. The image inside the map neatline is georeferenced to the surface of the earth and fit to the North Carolina State Plane NAD 1983 coordinate system (in Meters) (Fipszone 3200). 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, bridges, drainage, troop camps, lines of defense, selected buildings with names of landowners, mills and salt works, ground cover, swamps, and more. Relief shown by hachures. Includes also ill. of Confederate soldier with a plane table and Confederate flag, at left within margin. This layer is part of a selection of digitally scanned and georeferenced historic maps of the Civil War from the Harvard Map Collection. Many items from this selection are from a collection of maps deposited by the Military Order of the Loyal Legion of the United States Commandery of the State of Massachusetts (MOLLUS) in the Harvard Map Collection in 1938. These maps typically portray both natural and manmade features, in particular showing places of military importance. The selection represents a range of regions, originators, ground condition dates, scales, and purposes.

Jefferson County, Kentucky, 1910 (Raster Image)

This layer is a georeferenced raster image of the historic, topographic paper map entitled: Topography of Jefferson County, Kentucky : from U.S. Geological Survey topographic atlas sheets surveyed in 1904-1910, U.S. Geological Survey ; in cooperation with Kentucky Geological Survey, C. J. Norwood, director. It was published by U.S. Geological Survey in 1912. Scale 1:62,500. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Kentucky North State Plane NAD 1983 coordinate system (in Feet) (Fipszone 1601). 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 is a typical topographic map portraying both natural and manmade features. It shows and names works of nature, such as mountains, valleys, lakes, rivers, vegetation, etc. It also identify the principal works of humans, such as roads, railroads, boundaries, transmission lines, major buildings, etc. Relief is shown with standard contour intervals of 20 feet and spot heights. This layer is part of a selection of digitally scanned and georeferenced historic maps from The Harvard Map Collection as part of the Imaging the Urban Environment project. Maps selected for this project represent major urban areas and cities of the world, at various time periods. These maps typically portray both natural and manmade features at a large scale. The selection represents a range of regions, originators, ground condition dates, scales, and purposes.

Land Use Map, Cincinnati Region, Ohio, 1975 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: OKI regional land use : 1975. It was published by OKI Regional Planning Authority in 1975. Scale [ca. 1:5,000]. Covers Cincinnati Region, Ohio including Butler, Clermont, Hamilton, Warren counties, Ohio; Boone, Campbell, and Kenton counties, Kentucky; and Dearborn and Ohio counties, Indiana. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Ohio South State Plane NAD 1983 coordinate system (in Feet) (Fipszone 3402). 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 is colored to show land use categories: Urban residential ; Suburban residential ; Commercial ; Institutional/Service ; Utilities ; Industrial ; Resource extraction ; Recreational/Open space ; Cropland ; Grassland ; Woodland ; Water. It also shows features as major roads, drainage, administrative and political boundaries, and more. This layer is part of a selection of digitally scanned and georeferenced historic maps from The Harvard Map Collection as part of the Imaging the Urban Environment project. Maps selected for this project represent major urban areas and cities of the world, at various time periods. These maps typically portray both natural and manmade features at a large scale. The selection represents a range of regions, originators, ground condition dates, scales, and purposes.

Dublin Region, Ireland, 1853 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: The environs of Dublin, drawn and engraved by B.R. Davies. It was published under the superindentance of the Society for the Diffusion of Useful Knowledge [by] George Cox Jan[y] 1st 1853. Scale [ca. 1:15,250]. Covers the Dublin Region, Ireland, including portions of County Kildare and County Meath. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Irish National Grid 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, built-up areas and selected buildings, parks, 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 as part of the Imaging the Urban Environment project. Maps selected for this project represent major urban areas and cities of the world, at various time periods. These maps typically portray both natural and manmade features at a large scale. The selection represents a range of regions, originators, ground condition dates, scales, and purposes.

Indus River Region, India, Pakistan, and Afghanistan, 1816 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Sindetic Hindoostan or the countries occupied by the Sinde or Indus and its branches, by John Cary. It was published by J. Cary June 1, 1816. Scale [ca. 1:7,000,000]. Covers the Indus River region including portions of Northwest India, Pakistan, Afghanistan and Kashmir. The image inside the map neatline is georeferenced to the surface of the earth and fit to a modified 'Asia North Lambert Conformal Conic' projection with a central meridian of 72 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, roads, territorial boundaries, shoreline features, and more. Relief shown by hachures. This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection as part of the Open Collections Program at Harvard University project: Islamic Heritage Project. Maps selected for the project represent a range of regions, originators, ground condition dates, scales, and purposes. The Islamic Heritage Project consists of over 100,000 digitized pages from Harvard's collections of Islamic manuscripts and published materials. Supported by Prince Alwaleed Bin Talal and developed in association with the Prince Alwaleed Bin Talal Islamic Studies Program at Harvard University.

Long Island, New York & Connecticut, 1863 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Map of Long Island and the southern part of Connecticut. It was published by J.H. Colton in 1863. Scale [ca. 1:165,000]. The image inside the map neatline is georeferenced to the surface of the earth and fit to the North American Datum 1983, Universal Transverse Mercator (UTM) Zone 18N 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, shoreline features, roads, railroads, canals, post offices, churches, mills and factories, township and county boundaries, and more. Relief shown by hachures. Depths shown by soundings. Includes also inset of Greater New York.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.

Migration and asylum: The movement of people in the Mediterranean Region - Future scenarios and the EU response. Jean Monnet Occasional Paper No. 11/2014

Introduction. In recent years, the global discussion on migration and asylum has evolved from polarization of perspectives and mistrust, to improving partnerships and fostering cooperation between countries and regions. The paradigm has shifted from control and security exclusively to an increased awareness of the ramifications of migration in development and labour markets, the increasing demographic gap1 and the dangers of exclusion faced by migrant workers (regular or irregular). Eastern Europe will suffer the biggest population decline in the coming years, and Nigeria’s population will reach one billion by 2100. In Europe, the work replacement ratio will be two pensioners for one active worker. It has become clear that these facts cannot be ignored and that there is a need for greater convergence of policies (migration/mobility, fundamental rights, and economic growth), with a migrant-centred approach.2. The assumption that Europe will remain a geopolitical and economic hub that attracts immigrants at all skill levels might not hold water in the long run. The evolving demographic and economic changes have made it evident that the competitiveness of the EU (Europe 2020 Strategy) is also at stake, particularly if an adaptable workforce with the necessary skills is not secured in view of shortfalls in skill levels and because of serious labour mismatches. Therefore, it is the right moment to develop more strategic and long-term migration policies that take into account the evolving position of Europe and its neighbours in the world. By the same token, labour market strategies that meet needs and promote integration of regular migrants are still a pending task for the Member States (MS) in terms of the free movement of people, but also in relation with neighbouring and partner countries.

The gas target model for the Visegard 4 Region: conceptual analysis. OSW Report, May 2013

The similarity of issues and geographical proximity have led the Visegrad 4 countries (V4) to undertake closer collaboration in natural gas policy, notably by agreeing on a common security of supply strategy, including regional emergency planning, and a common implementation of the Gas Target Model (GTM) that European regulators have proposed for the medium-long term design of the EU gas market, and which has been endorsed by the Madrid Regulatory Forum. As a contribution to this collaboration, the present paper will analyse how the GTM may be implemented in the V4 region, with a view to maximize the benefits that arise from joint implementation. A most relevant conclusion of the GTM is that markets should be large enough to attract market players and investments, so that sufficient diversity of sources may be reached and market power indicators are kept below dangerous levels. In most cases, this requires physical and/or virtual interconnection of present markets, which is also useful to achieve the required security of supply standards, as envisaged in the Regulation 994/2010/EC.

The EU Strategy for the Baltic Sea Region from Germany’s perspective. OSW Commentary No. 69, 2011-01-10

Germany is one of the eight EU member states which participate in the EU Strategy for the Baltic Sea Region along with Denmark, Estonia, Finland, Latvia, Lithuania, Poland and Sweden. Germany had a positive approach to the EUSBSR strategy (see Appendix 1) right from planning stage. This project contributed to the continuation of Germany’s co-operation with the countries in this region, which has been conducted since the mid 1980s mainly by German federal states. Germany is playing a major role as part of this strategy because it is the coordinator of its three priority areas.However, the German federal government sees the EUSBSR as a project to be implemented at the level of federal states. This has been proven by the great activity of three German federal states participating in the strategy (Hamburg, Mecklenburg-Vorpommern and Schleswig-Holstein) and at the same time the low level of engagement from the Bundestag, the federal government and expert circles. Furthermore, federal states more often formulate evaluations of the effects of co-operation achieved so far as part of the EUSBSR. Still, the relatively low level of Berlin’s engagement does not mean that it is not interested in co-operation in the Baltic region as such. Germany actively participates in the work of such bodies as the Council of the Baltic Sea States or the Baltic Marine Environment Protection Commission (HELCOM). All German entities engaged in the strategy make its future attractiveness and the success of individual projects as part of it dependent on including Russia in the EUSBSR. As long as Germany has the opportunity of regional co-operation with Russia at other forums (for example, the Council of the Baltic Sea States), it is unlikely to become more engaged in developing the strategy and enhancing co-operation as part of this project.

Latest Cretaceous to Late Paleocene radiolarian biostratigraphy from the New Zealand region

The scarcity of records of Early Paleocene radiolarians has meant that while radiolarian biostratigraphy is firmly established as an important tool for correlation, there has been a long-standing gap between established zonations for the Cretaceous and from latest Paleocene to Recent. It has also led to considerable speculation over the level of faunal change across the Cretaceous/Tertiary (K/T) boundary. Consequently, the discovery of rich and diverse radiolarian assemblages in well-delineated K/T boundary sections within siliceous limestones of the Amuri Limestone Group in eastern Marlborough, New Zealand, is of great significance for biostratigraphy and K/T boundary research. This initial report is restricted to introducing a new latest Cretaceous to mid Late Paleocene zonation based on the radiolarian succession at four of these sections and a re-examination of faunas from coeval sediments at DSDP Site 208 (Lord Howe Rise). Three new Paleocene species are described: Amphisphaera aotea, Amphisphaera kina and Stichomitra wero. Six new interval zones are defined by the first appearances of the nominate species. In ascending order these are: Lithomelissa? hoplites Foreman (Zone RK9, Cretaceous), Amphisphaera aotea n. sp. (Zone RP1, Paleocene), Amphisphaera kina n. sp. (RP2), Stichomitra granulata Petrushevskaya (RP3), Buryellaforemanae petrushevskaya (RP4) and Buryella tetradica (RP5). Good age control from foraminifera and calcareous nannofossils permits close correlation with established microfossil zonations. Where age control is less reliable, radiolarian events are used to substantially improve correlation between the sections. No evidence is found for mass extinction of radiolarians at the end of the Cretaceous. However, the K/T boundary does mark a change from nassellarian to spumellarian dominance, due to a sudden influx of actinommids, which effectively reduces the relative abundance of many Cretaceous survivors. An accompanying influx of diatoms in the basal Paleocene of Marlborough, together with evidence for an increase of total radiolarian abundance, suggests siliceous plankton productivity increased across the K/T boundary. Possible causes for this apparently localised phenomenon are briefly discussed.

Stable hydrogen and carbon isotope records and concentration data for four long chain n-alkanes from core GIK16160-3 derived from the Zambezi delta in the Mozambique Channel during the last 37,000 years

Hydrogen isotope values (dD) of sedimentary terrestrial leaf wax such as n-alkanes or n-acids have been used to map and understand past changes in rainfall amount in the tropics because dD of precipitation is commonly assumed as the first order controlling factor of leaf wax dD. Plant functional types and their photosynthetic pathways can also affect leaf wax dD but these biological effects are rarely taken into account in paleo studies relying on this rainfall proxy. To investigate how biological effects may influence dD values we here present a 37,000-year old record of dD and stable carbon isotopes (d13C) measured on four n-alkanes (n-C27, n-C29, n-C31, n-C33) from a marine sediment core collected off the Zambezi River mouth. Our paleo d13C records suggest that each individual n-alkanes had different C3/C4 proportional contributions. n-C29 was mostly derived from a C3 dicots (trees, shrubs and forbs) dominant vegetation throughout the entire record. In contrast, the longer chain n-C33 and n-C31 were mostly contributed by C4 grasses during the Glacial period but shifted to a mixture of C4 grasses and C3 dicots during the Holocene. Strong correlations between dD and d13C values of n-C33 (correlation coefficient R2 = 0.75, n = 58) and n-C31 (R2 = 0.48, n = 58) suggest that their dD values were strongly influenced by changes in the relative contributions of C3/C4 plant types in contrast to n-C29 (R2 = 0.07, n = 58). Within regions with variable C3/C4 input, we conclude that dD values of n-C29 are the most reliable and unbiased indicator for past changes in rainfall, and that dD and d13C values of n-C31 and n-C33 are sensitive to C3/C4 vegetation changes. Our results demonstrate that a robust interpretation of palaeohydrological data using n-alkane dD requires additional knowledge of regional vegetation changes from which nalkanes are synthesized, and that the combination of dD and d13C values of multiple n-alkanes can help to differentiate biological effects from those related to the hydrological cycle.

(Table 1) Crystal sizes of measured samples from the Bush Hill region in the Gulf of Mexico and from ODP Leg 204 at the Hydrate Ridge offshore Oregon

The grain sizes of gas hydrate crystallites are largely unknown in natural samples. Single grains are hardly detectable with electron or optical microscopy. For the first time, we have used high-energy synchrotron diffraction to determine grain sizes of six natural gas hydrates retrieved from the Bush Hill region in the Gulf of Mexico and from ODP Leg 204 at the Hydrate Ridge offshore Oregon from varying depth between 1 and 101 metres below seafloor. High-energy synchrotron radiation provides high photon fluxes as well as high penetration depth and thus allows for investigation of bulk sediment samples. Gas hydrate grain sizes were measured at the Beam Line BW 5 at the HASYLAB/Hamburg. A 'moving area detector method', originally developed for material science applications, was used to obtain both spatial and orientation information about gas hydrate grains within the sample. The gas hydrate crystal sizes appeared to be (log-)normally distributed in the natural samples. All mean grain sizes lay in the range from 300 to 600 µm with a tendency for bigger grains to occur in greater depth. Laboratory-produced methane hydrate, aged for 3 weeks, showed half a log-normal curve with a mean grain size value of c. 40 µm. The grains appeared to be globular shaped.

Benthic fauna of an offshore borrow area in Broward County, Florida /

Benthic fauna from two stations within a 5-year-old borrow area and two control stations off Hillsboro Beach (Broward County), Florida, were sampled quarterly from June 1977 to March 1978 to evaluate the long-term impact of offshore dredging. Generally enhanced productivities occurred within the borrow area, although there was much seasonal variation among stations. Species diversities were usually higher at the borrow stations than at the control stations. The single exception was due to a high concentration of the bivalve E. nitens at one of the control stations in June. Although faunal similarity analysis revealed a qualitative change in the fauna of the borrow area, this change is not considered detrimental. Conspicuous patterns of heterogeneous faunal distributions were evident in this study, particularly for the bivalve E. nitens. No lasting detrimental effects, in terms of numbers of species, faunal densities, or species diversity, resulted from the dredging operation. (Author).