Louisville and Vicinity, Kentucky, 1955 (Raster Image)

This layer is a georeferenced raster image of the historic, topographic paper map entitled: Louisville and vicinity : prepared in cooperation with city, county, and state agencies, mapped by the Geological Survey and the Army Map Service. It was edited and published by the Geological Survey in 1957. Ed. of 1955. Scale 1:24,000. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Kentucky North State Plane NAD 1927 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 10 feet (with 5 foot supplementary intervals). 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.

Louisville and Vicinity, Kentucky, 1907 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Louisville Title Co.'s revised map of Louisville, Ky. and environs, compiled & drawn by Wm. B. Hunter. It was published by Louisville Title Co. in 1907. Scale [ca. 1:36,000]. Covers Louisville, Kentucky and vicinity. Portions of source paper map have outer edges torn, and some title and index information is lacking. 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 map shows features such as roads, railroads and stations, drainage, selected buildings and names of landowners, property areas and/or dimensions, parks, cemeteries, and more. Includes index. 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.

Chicago and vicinity, Illinois, 1953 (Image 1 of 3) (Raster Image)

This layer is a georeferenced raster image of the historic, topographic paper map entitled: Chicago and vicinity, Ill.-Ind. : sheet no. 1 of 3 (Evanston), 1953, mapped, edited, and published by the Geological Survey. It was published in 1957. Scale 1:24,000. The source map was compiled from 1:24,000 scale maps of Evanston, Park Ridge, Arlington Heights, Elmhurst, River Forest, and Chicago Loop, 1953 7.5 minute quadrangles. Hydrography from U.S. Lake Survey Charts 75 (1:120,000), 751 (1:60,000), and 752 (1:15,000). This layer is image 1 of 3 total images of the three sheet source map. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Illinois East State Plane Coordinate System NAD27 (in Feet) (Fipszone 1201). 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 5 feet. Depths shown by isolines and soundings. 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.

Russia goes on the offensive ahead of the Eastern Partnership summit in Vilnius. OSW Commentary No. 115, 30.09.2013

In recent weeks, Russia has stepped up its efforts to prevent a group of former Soviet republics from tightening their relations with the European Union. The intensification of these efforts comes ahead of the upcoming Eastern Partnership summit, scheduled to take place in Vilnius on 28-29 November. It is expected that during the summit Kiev will sign the EU-Ukraine Association Agreement (AA) initialled in March 2012, including an agreement for a Deep and Comprehensive Free Trade Area (DCFTA). Meanwhile, Moldova, Armenia and Georgia are expected to initial similar documents, effectively accepting their terms and conditions, and paving the way for their official signing in the near future. Moscow has always viewed the relations between the EU and the post-Soviet states as a threat to its own influence in the region. Consequently, any attempts to tighten these relations have been actively opposed by Russia. The EU’s Eastern Partnership programme, launched in 2009, has posed a particular challenge to Moscow’s policies in the region.. Russia responded by rolling out a Eurasian integration project, which began in 2010 with the establishment of the Customs Union of Russia, Kazakhstan and Belarus, and is expected to culminate in the establishment of the Eurasian Economic Union by 2015. Moscow’s overarching objective has been to persuade the countries in the region, especially Ukraine, to adopt an unambiguously pro-Russian geopolitical stance and to join the integration project proposed by the Kremlin. The Russian government hopes that this would permanently place these states in Moscow’s sphere of influence and at the same time prevent them from developing closer relations with Brussels. Russia has regularly taken actions aimed at showcasing the benefits of integration with the Customs Union (particularly, by promising preferential pricing of Russian energy resources) and at the same time it has adopted measures highlighting the pitfalls of retaining a pro-European orientation (mainly by imposing occasional trade sanctions). The upcoming summit in Vilnius, during which Ukraine, Moldova, Armenia and Georgia could lock themselves on to a pro-European course, has spurred Moscow to intensify its efforts to torpedo a successful outcome of the Vilnius meeting, with a view to slowing down or even blocking the possibility of closer cooperation between the EU and the former Soviet republics.

Ukraine and the European Union: Time for a Re-Think. ACES Working Papers, 2011

There are two reasons for the virtual nature of the West’s dialogue with Ukraine. The first is institutional as the EU has until now only been willing to use ‘carrots’ and ‘sticks’ in ‘enlargement-heavy’ (i.e. full membership) whereas it has only used ‘carrots,’ but never ‘sticks’, in ‘enlargement-light’ (i.e. the DCFTA). European Council Foreign Relations Senior Fellows Nicu Popescu and Andrew Wilson argue that the EU should be more willing to use both carrots and sticks; that is integrating its soft and hard power. The second is a disconnection between the West and Kyiv over definitions of democracy. The Ukrainian authorities have until now wanted to have their cake and eat it, too; rolling back democracy in Kyiv while claiming to sign up to ‘European values’ in Brussels.

Properties of granular analogue model materials: A community wide survey

We report the material properties of 26 granular analogue materials used in 14 analogue modelling laboratories. We determined physical characteristics such as bulk density, grain size distribution, and grain shape, and performed ring shear tests to determine friction angles and cohesion, and uniaxial compression tests to evaluate the compaction behaviour. Mean grain size of the materials varied between c. 100 and 400 μm. Analysis of grain shape factors shows that the four different classes of granular materials (14 quartz sands, 5 dyed quartz sands, 4 heavy mineral sands and 3 size fractions of glass beads) can be broadly divided into two groups consisting of 12 angular and 14 rounded materials. Grain shape has an influence on friction angles, with most angular materials having higher internal friction angles (between c. 35° and 40°) than rounded materials, whereas well-rounded glass beads have the lowest internal friction angles (between c. 25° and 30°). We interpret this as an effect of intergranular sliding versus rolling. Most angular materials have also higher basal friction angles (tested for a specific foil) than more rounded materials, suggesting that angular grains scratch and wear the foil. Most materials have an internal cohesion in the order of 20–100 Pa except for well-rounded glass beads, which show a trend towards a quasi-cohesionless (C < 20 Pa) Coulomb-type material. The uniaxial confined compression tests reveal that rounded grains generally show less compaction than angular grains. We interpret this to be related to the initial packing density after sifting, which is higher for rounded grains than for angular grains. Ring-shear test data show that angular grains undergo a longer strain-hardening phase than more rounded materials. This might explain why analogue models consisting of angular grains accommodate deformation in a more distributed manner prior to strain localisation than models consisting of rounded grains.

(Table 1) Paleomagnetic of reoriented core pieces of IODP Hole 304-U1309D

Oceanic core complexes expose lower crustal and upper mantle rocks on the seafloor by tectonic unroofing in the footwalls of large-slip detachment faults. The common occurrence of these structures in slow and ultra-slow spread oceanic crust suggests that they accommodate a significant component of plate divergence. However, the subsurface geometry of detachment faults in oceanic core complexes remains unclear. Competing models involve either: (a) displacement on planar, low-angle faults with little tectonic rotation; or (b) progressive shallowing by rotation of initially steeply dipping faults as a result of flexural unloading (the "rolling-hinge" model). We address this debate using palaeomagnetic remanences as markers for tectonic rotation within a unique 1.4 km long footwall section of gabbroic rocks recovered by Integrated Ocean Drilling Program (IODP) sampling at Atlantis Massif oceanic core complex on the Mid-Atlantic Ridge (MAR). These rocks contain a complex record of multipolarity magnetizations that are unrelated to alteration and igneous stratigraphy in the sampled section and are inferred to result from progressive cooling of the footwall section over geomagnetic polarity chrons C1r.2r, C1r.1n (Jaramillo) and C1r.1r. For the first time we have independently reoriented drill-core samples of lower crustal gabbros, that were initially azimuthally unconstrained, to a true geographic reference frame by correlating structures in individual core pieces with those identified from oriented imagery of the borehole wall. This allows reorientation of the palaeomagnetic data, placing far more rigorous constraints on the tectonic history than those possible using only palaeomagnetic inclination data. Analysis of the reoriented high temperature reversed component of magnetization indicates a 46° ± 6° anticlockwise rotation of the footwall around a MAR-parallel horizontal axis trending 011° ± 6°. Reoriented lower temperature components of normal and reversed polarity suggest that much of this rotation occurred after the end of the Jaramillo chron (0.99 Ma). The data provide unequivocal confirmation of the key prediction of flexural, rolling-hinge models for oceanic core complexes, whereby oceanic detachment faults initiate at higher dips and rotate to their present day low-angle geometries as displacement increases.

Runaway truck arresting schemes. Final report.

North Carolina Department of Transportation, Raleigh

Mechanics of pneumatic tires.

Mode of access: Internet.

Tire treadwear validation. Volume 1: technical report. Final report.

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

Das illustrirte Mississippithal : dargestellt in 80 nach der Natur aufgenommenen Ansichten vom Wasserfalle zu St. Anthony an bis zum Golf von Mexico (eine Entfernung von ungefähr 2300 englischen Meilen) /

Cf. Sabin 40807.

Augmentation of research and analysis capabilities for timely support of automotive fuel economy activities. Volume II: appendices A through C. Final report.

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

Augmentation of research and analysis capabilities for timely support of automotive fuel economy activities. Volume III: appendix D. Final report.

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

The skidding of vehicles - a dynamic analysis. Progress report for the period September 1967-September 1968.

National Highway Safety Bureau, Washington, D.C.

Harmonization of braking regulations - report number 6: testing to address surface friction and vehicle braking efficiency comments to the SNPRM. Interim report.

Mode of access: Internet.