North Carolina, 1808 (Image 3 of 3) (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: To David Stone and Peter Brown, Esq. : this first actual survey of the state of North Carolina taken by the subscribers is respectfully dedicated by their humble servants, Jona. Price and John Strother ; engraved by W. H. Harrison. It was printed by C.P. Harrison in 1808. Scale [ca. 1:506,880]. This layer is image 3 of 3 total images of the three sheet source map, representing the eastern portion of the map.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 Feet) (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, drainage, canals, cities and towns, selected public buildings (churches, inns), industry locations (e.g. mills, mines, etc.), selected private buildings with names of property owners, state and county boundaries, shoreline features, and more. Relief shown pictorially and 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.

Sandcastles of hope? Civil society organizations and the working conditions of migrant farmworkers in North America

This research explores whether civil society organizations (CSOs) can contribute to more effectively regulating the working conditions of temporary migrant farmworkers in North America. This dissertation unfolds in five parts. The first part of the dissertation sets out the background context. The context includes the political economy of agriculture and temporary migrant labour more broadly. It also includes the political economy of the legal regulations that govern immigration and work relations. The second part of the research builds an analytical model for studying the operation of CSOs active in working with the migrant farmworker population. The purpose of the analytical framework is to make sense of real-world examples by providing categories for analysis and a means to get at the channels of influence that CSOs utilize to achieve their aims. To this end, the model incorporates the insights from three significant bodies of literature—regulatory studies, labour studies, and economic sociology. The third part of the dissertation suggests some key strategic issues that CSOs should consider when intervening to assist migrant farmworkers, and also proposes a series of hypotheses about how CSOs can participate in the regulatory process. The fourth part probes and extends these hypotheses by empirically investigating the operation of three CSOs that are currently active in assisting migrant farm workers in North America: the Agricultural Workers Alliance (Canada), Global Workers’ Justice Alliance (USA), and the Coalition of Immokalee Workers (USA). The fifth and final part draws together lessons from the empirical work and concluded that CSOs can fill gaps left by the waning power of actors, such as trade unions and labour inspectorates, as well as act in ways that these traditional actors can not.

DEMOCRACY AND CITIZENSHIP IN NORTH AFRICA AFTER THE ARAB AWAKENING: CHALLENGES FOR EU AND US FOREIGN POLICY (EUSPRING). Arab Citizenship Review No. 1, Egypt, August 2013

This series of policy briefs provides a regular update of debates concerning key rights issues in three Arab states, Morocco, Egypt and Tunisia. In a first round of briefs on the three countries, we provide background on these debates since the beginning of the Arab spring

DEMOCRACY AND CITIZENSHIP IN NORTH AFRICA AFTER THE ARAB AWAKENING: CHALLENGES FOR EU AND US FOREIGN POLICY (EUSPRING). Arab Citizenship Review No. 2, Morocco, August 2013

This series of policy briefs provides a regular update of debates concerning key rights issues in three Arab states, Morocco, Egypt and Tunisia. In a first round of briefs on the three countries, we provide background on these debates since the beginning of the Arab spring.

DEMOCRACY AND CITIZENSHIP IN NORTH AFRICA AFTER THE ARAB AWAKENING: CHALLENGES FOR EU AND US FOREIGN POLICY (EUSPRING). Arab Citizenship Review No. 3, Tunisia, August 2013

This series of policy briefs provides a regular update of debates concerning key rights issues in three Arab states, Morocco, Egypt and Tunisia. In a first round of briefs on the three countries, we provide background on these debates since the beginning of the Arab spring.

DEMOCRACY AND CITIZENSHIP IN NORTH AFRICA AFTER THE ARAB AWAKENING: CHALLENGES FOR EU AND US FOREIGN POLICY (EUSPRING). Arab Citizenship Review No. 4, April 2014. Egypt. Egypt’s Transition in Crisis: The Decline of Citizenship Rights

This series of policy briefs provides a regular update of debates concerning key rights issues in three Arab states, Morocco, Egypt and Tunisia. In a first round of briefs on the three countries, we provide background on these debates since the beginning of the Arab spring.

DEMOCRACY AND CITIZENSHIP IN NORTH AFRICA AFTER THE ARAB AWAKENING: CHALLENGES FOR EU AND US FOREIGN POLICY (EUSPRING). Arab Citizenship Review No. 5, May 2014. TUNISIA. The New Tunisian Constitution and Citizenship Rights

This series of policy briefs provides a regular update of debates concerning key rights issues in three Arab states, Morocco, Egypt and Tunisia. In a first round of briefs on the three countries, we provide background on these debates since the beginning of the Arab spring.

North Caucasus: the Russian Gordian knot. The key problems and conflicts in the region and the effect thereof on the future of Russia; Putin after re-election: The Kremlin's policy in Vladimir Putin's second term. OSW Study 16/2004

North Caucasus: North Caucasus is the most instable part of the Russian Federation: since the early 90's, there has been going on the military conflict in Chechnya, which is gradually spilling over into the other republics of the region, terrorism seems to have occupied its regular position in the political life of Caucasus, organized crime is flourishing, the tension persists there and military incidents and attacks are breaking out every now and again. During the recent year, the destabilization of the region, which affects many fields of Russian political and social life, has grown to an alarming size. Putin after re-election: Vladimir Putin's first term as President was a period of submitting political, regional and economic lobbies to the Kremlin. The actions Putin has taken since being re-elected are aimed at consolidating the Kremlin's control over the political, economic and social spheres. Further liquidation of political and informational pluralism, an increase of the ruling group's control over state and private property, and an intensification of state propaganda aimed at generating social support for the Kremlin's initiatives have all proceeded apace. These processes reinforce authoritarian tendencies and strengthen the emerging monocentric political system, with the President's strong domination over political, economic and social life.

Spatially explicit estimates of length and biomass of Micromesistius poutassou (Blue Whiting) from acoustic and trawl surveys in the North-East Atlantic in May 2012

Acoustic estimates of herring and blue whiting abundance were obtained during the surveys using the Simrad ER60 scientific echosounder. The allocation of NASC-values to herring, blue whiting and other acoustic targets were based on the composition of the trawl catches and the appearance of echo recordings. To estimate the abundance, the allocated NASC -values were averaged for ICES-squares (0.5° latitude by 1° longitude). For each statistical square, the unit area density of fish (rA) in number per square nautical mile (N*nm-2) was calculated using standard equations (Foote et al., 1987; Toresen et al., 1998). To estimate the total abundance of fish, the unit area abundance for each statistical square was multiplied by the number of square nautical miles in each statistical square and then summed for all the statistical squares within defined subareas and over the total area. Biomass estimation was calculated by multiplying abundance in numbers by the average weight of the fish in each statistical square then summing all squares within defined subareas and over the total area. The Norwegian BEAM soft-ware (Totland and Godø 2001) was used to make estimates of total biomass.

Age models of sediment cores from the North-West African continental margin

A statistical analysis ol 15 deep sea cores in the eastern North Atlantic off NW Africa revealed the typical fluctuation pattern of distinct species proups as has been described from various parts of the world ocean. Only the "WBF-group" appears to be correlated with global climatic changes, i.e. warmer periods as the Eemian and the Atlanticum. A partly antagonistic "High Productivity group" (HPR-group) is in general not linked with global changes but times of increased fertility in the surface water and the resulting flux of organic matter reaching the bottom. The groups were extracted from cluster analysis of more than 150 surface samples (HPR-group) and a factor analysis of selected cores (WBF-group). In contrast to previous studies the observed fluctuations can not be explained by drastic changes in bottom water masses, but by the pulsation of a distinct "High Productivity Patch" in space and time. At present, this patch is located below the well known upwelling area between 22° and 12° northern latitude. It shifted to the north (up to 27 °N) during the latest glacial period ( 18 ky), indicating an equivalent shift of upwelling productivity caused by advection of nutrient rich upwelling SACW-waters, probably during most of isotopic stages 2 and 3.

Characteristics of acoustic recordings of narwhals (Monodon monoceros) north of Disko Island, April 2007 and 2009

A total of 1,690 individual narwhal nonecholocation sounds were recorded over 5 h in 2007 and 2009. Each sound was classified as either tonal (FM) or pulsed (amplitude modulated). Omnipresent in all the recordings were the songs of bearded seals, Erignathus barbatus, which were often so loud and numerous that the lower frequency ranges of narwhal sounds could not be distinguished.

New calibration of Neogene radiolarian events in the North Pacific

New age models for twelve Deep Sea Drilling Project sites in the North Pacific have been produced, based on (in order of importance in our dataset) a recompilation of previously published diatom, calcareous nannofossil and foraminifer first and last occurrences, and magnetostratigraphy. The projected ages of radiolarian first and last occurrences derived from the line of correlation of the age/depth plots have been computed from these sites, and 28 radiolarian events have thereby been newly cross calibrated to North Pacific diatom and other stratigraphy. Several of the North Pacific radiolarian events are older than in previously published equatorial Pacific calibrations, and some may be diachronous within the North Pacific. These patterns may be due to complex latitudinal patterns of clinal variation in morphotypes within lineages, or to migration events from the North Pacific towards the Equator.

Composition of airborne material from yellow snow fallen in the Russian North

Large amounts of dust responsible for bright colors of atmospheric precipitation in the temperate, subpolar and polar zones of the northern hemisphere have been rarely observed. In the twentieth century and in the beginning of the twenty first century in the Northern European Russia such events were not registered up to March 25-26, 2008. At that time in some parts of the Arkhangel'sk region, Komi Republic, and Nenets Autonomous Area atmospheric precipitation as sleet and rain responsible for sand- and saffron colors of ice crust formation on the snow surface was observed. During detailed mineralogical, geochemical, pollen, diatom and meteorological investigations it was established that semidesert and steppe regions of the Northwest Kazakhstan, Volgograd and Astrakhan' regions, and Kalmykia are the main sources of the yellow dust.

Integrated stratigraphy of the Messinian across the North Atlantic Ocean

The Messinian was a time of major climatic and paleoceanographic change during the late Cenozoic. It is well known around the Mediterranean region because of the giant anhydritelgypsum sequence and the suggested desiccation of the Mediterranean Sea. However, this interval is less constrained outside the Mediterranean region, where several paleoceanographic changes could have taken place because of the desiccation. Hence, we present an integrated stratigraphic framework for future Messinian paleoceanographic studies, determination of the effect of the Mediterranean desiccation on deep-water paleoceanography, and comparison of intra-Mediterranean paleoceanographic changes with those in the open oceans during the Messinian Stage. Four DSDP/ODP Holes (552A, 646B, 608, and 547A) from the North Atlantic Ocean and one land borehole from Morocco have been studied to integrate bio-, magneto-, and stable isotope Messinian stratigraphy with high resolution sampling. Our results produce the best assessment of the Tortonian/Messinian boundaries in all holes because they do not rely on any one signal. In paleomagnetic Subchronozone C3An1r in the Sale borehole and DSDP Site 609, a S/D coiling direction change of Neogloboquadrina pachyderma/acostaensis appears to indicate PMOW entering the northeastern Atlantic Ocean, at least reaching 50°N. Diachrony and synchrony of some important Messinian planktic foraminifera from these Atlantic DSDP/ODP holes and the Sale borehole, such as the LO of Gq. dehiscens, the LO of Gt. Eenguaensis, the FO and LO of Ct. conomiozea, the FO of Gt. margaritae s.s., the FO of Gt. puncticutata, and the FO of Gt. crassaformis are discussed for understanding some of the paleoceanographic changes. This integrated stratigraphic framework presented here allows much better North Atlantic correlations at this critical point in Messinian geologic history.