Grain size analysis on core plugs of sediment core CRP-1 (Table 1, 2)

Twenty four core samples from CRP-1, seven from Quaternary strata (20-43.55 meters below sea floor or mbsf) and seventeen from early Miocene strata (43.55 to 147.69 mbsf), have been analysed for their grain-size distribution using standard sieve and Sedigraph techniques. The results are in good agreement with estimates of texture made as part of the visual core description for the 1 :20 core logs for CRP-1 (Cape Roberts Science Team, 1998). Interpretation of the analyses presented here takes into account the likely setting of the site in Quaternary times as it is today, with CRP-1 high on the landward flank of a well-defined submarine ridge rising several hundred metres above basins on either side. In contrast, seismic geometries for strata deposited in early Miocene times indicate a generally planar sea floor dipping gently seaward. Fossils from these strata indicate shallow water depths (< 100 m), indicating the possibility that waves and tidal currents may have influenced sea floor sediments. The sediments analysed here are considered in terms of 3 textural facies: diamict, mud (silt and clay) and sand. Most of the Quaternary section but only 30% of the early Miocene section is diamict, a poorly sorted mixture of sand and mud with scattered clasts, indicating little wave or current influence on its texture. Although not definitive, diamict textures and other features suggest that the sediment originated as basal glacial debris but has been subsequently modified by minor winnowing, consistent with the field interpretation of this facies as ice-proximal and distal glaciomarine sediment. Sediments deposited directly from glacier ice appear to be lacking. Mud facies sediments, which comprise only 10% of the Quaternary section but a third of the early Miocene section, were deposited below wave base and largely from suspension, and show features (described elsewhere in this volume) indicative of the influence of both glacial and sediment gravity flow processes. Sand facies sediments have a considerable proportion of mud, normally more than 20%, but a well-sorted fine-very fine sand fraction. In the context of the early Miocene coastal setting we interpret these sediments as shoreface sands close to wave base.

Clay mineralogy and shear strength of subglacial and glaciomarine sediments in the southern Bellingshausen Sea

The Belgica Trough and the adjacent Belgica Trough Mouth Fan in the southern Bellingshausen Sea (Pacific sector of the Southern Ocean) mark the location of a major outlet for the West Antarctic Ice Sheet during the Late Quaternary. The drainage basin of an ice stream that advanced through Belgica Trough across the shelf during the last glacial period comprised an area exceeding 200,000 km**2 in the West Antarctic hinterland. Previous studies, mainly based on marine-geophysical data from the continental shelf and slope, focused on the bathymetry and seafloor bedforms, and the reconstruction of associated depositional processes and ice- drainage patterns. In contrast, there was only sparse information from seabed sediments recovered by coring. In this paper, we present lithological and clay mineralogical data of 21 sediment cores collected from the shelf and slope of the southern Bellingshausen Sea. Most cores recovered three lithological units, which can be attributed to facies types deposited under glacial, transitional and seasonally open-marine conditions. The clay mineral assemblages document coinciding changes in provenance. The relationship between the clay mineral assemblages in the subglacial and proglacial sediments on the shelf and the glacial diamictons on the slope confirms that a grounded ice stream advanced through Belgica Trough to the shelf break during the past, thereby depositing detritus eroded in the West Antarctic hinterland as soft till on the shelf and as glaciogenic debris flows on the slope. The thinness of the transitional and seasonally open-marine sediments in the cores suggests that this ice advance occurred during the last glacial period. Clay mineralogical, acoustic sub-bottom and seismic data furthermore demonstrate that the palaeo-ice stream probably reworked old sedimentary strata, including older tills, on the shelf and incorporated this debris into its till bed. The geographical heterogeneity of the clay mineral assemblages in the sub- and proglacial diamictons and gravelly deposits indicates that they were eroded from underlying sedimentary strata of different ages. These strata may have been deposited during either different phases of the last glacial period or different glacial and interglacial periods. Additionally, the clay mineralogical heterogeneity of the soft tills recovered on the shelf suggests that the drainage area of the palaeo-ice stream flowing through Belgica Trough changed through time.

Shell preservation of Limacina inflata in surface sediments of the Central and South Atlantic

Over 300 surface sediment samples from the Central and South Atlantic Ocean and the Caribbean Sea were investigated for the preservation state of the aragonitic test of Limacina inflata. Results are displayed in spatial distribution maps and are plotted against cross-sections of vertical water mass configurations, illustrating the relationship between preservation state, saturation state of the overlying waters, and overall water mass distribution. The microscopic investigation of L. inflata (adults) yielded the Limacina dissolution index (LDX), and revealed three regional dissolution patterns. In the western Atlantic Ocean, sedimentary preservation states correspond to saturation states in the overlying waters. Poor preservation is found within intermediate water masses of southern origin (i.e. Antarctic intermediate water (AAIW), upper circumpolar water (UCDW)), which are distinctly aragonite-corrosive, whereas good preservation is observed within the surface waters above and within the upper North Atlantic deep water (UNADW) beneath the AAIW. In the eastern Atlantic Ocean, in particular along the African continental margin, the LDX fails in most cases (i.e. less than 10 tests of L. inflata per sample were found). This is most probably due to extensive "metabolic" aragonite dissolution at the sediment-water interface combined with a reduced abundance of L. inflata in the surface waters. In the Caribbean Sea, a more complex preservation pattern is observed because of the interaction between different water masses, which invade the Caribbean basins through several channels, and varying input of bank-derived fine aragonite and magnesian calcite material. The solubility of aragonite increases with increasing pressure, but aragonite dissolution in the sediments does not simply increase with water depth. Worse preservation is found in intermediate water depths following an S-shaped curve. As a result, two aragonite lysoclines are observed, one above the other. In four depth transects, we show that the western Atlantic and Caribbean LDX records resemble surficial calcium carbonate data and delta13C and carbonate ion concentration profiles in the water column. Moreover, preservation of L. inflata within AAIW and UCDW improves significantly to the north, whereas carbonate corrosiveness diminishes due to increased mixing of AAIW and UNADW. The close relationship between LDX values and aragonite contents in the sediments shows much promise for the quantification of the aragonite loss under the influence of different water masses. LDX failure and uncertainties may be attributed to (1) aragonite dissolution due to bottom water corrosiveness, (2) aragonite dissolution due to additional CO2 release into the bottom water by the degradation of organic matter based on an enhanced supply of organic matter into the sediment, (3) variations in the distribution of L. inflata and hence a lack of supply into the sediment, (4) dilution of the sediments and hence a lack of tests of L. inflata, or (5) redeposition of sediment particles.

Annual statement exhibiting the condition of the state banks, savings banks, institutions for savings, and trust companies.

Includes also, 1902-1907 statements of building and loan associations, 1901-1906 (Domestic and foreign building and loan associations, 1901-1904; Domestic building and loan associations, 1905-1906)

Pen pictures of British battles,

The victory of the Falkland islands, by R. Wilson.--The battle of the Marne, by Sir A.C. Doyle.--A glimpse of Canada in Flanders, by Lord Beaverbrook.--The second battle of Ypres, by J. Buchan.--The battle of Jutland Bank, by H.W. Wilson.--The charge at Loos of the London Irish.--The landing at V beach, near Sedd-el-Bahr, by J. Masefield.--The Coldstream guards at the battle of the Some, by 0P. Gibbs.--The moonlight battle for Baghdad, by E. Candler.--The battle of Arras, by P. Gibbs.--Warfare under water, by R. Kipling.

Annual report of the Board of Commissioners of Savings Banks : part I, savings banks, institutions for savings, and safe deposit, loan and trust companies.

Mode of access: Internet.

Annual report of the Commissioner of Banking of state and mutual savings banks of Wisconsin.

Description based on: 9th (1903).

The story of the great war ...

Another issue in 8 vols. has title: The story of the great war, the complete historical records of events to date. Illustrated with drawings, maps and photographs by Francis J. Reynolds ... Allen L. Churchill ... Francis Trevelyan Miller ...

Views on the corn bill of 1827 : and other measures of government ; together with a further exposition of certain principles on corn and crurency before published /

With this are bound: Muschet, R. An attempt to explain from facts the effect of the issues of the Bank of England...1826; Attwood, T. The Schotch banker. 1828.

Annual report of the Superintendent of the Banking Department of the State of New York.

Vols. for <, 1881, 1887,1926, 1928, 1931, 1934, 1936-38> issued also without Detailed statement.

Leaving Lodge Pole, Nebr., June 7th

Horses pulling automobile out of mud. Photo album title: Detroit to San Francisco over Lincoln Highway. May 27-June 18, 1915. Henry B. Joy; A.F. Bement; E. Eisenhut

The meaning of money.

Introductory.- Coined cash.- Paper cash.- The bill of exchange.- The manufacture of money.- London, the world's monetary clearing house.- The cheque-paying banks.- The bill-brokers and discount houses.- The accepting houses and foreign banks.- The foreign exchanges.- The bank of England.- Bank rate and market rate.- The bank return.- The gold reserve.- Other reserves.- Summary and conclusion.- Index.

An evaluation of results and effectiveness of job banks /

"Contract no. 83-06-72-01."

Views from Hamburg : the Juno Trader case or how to make sense of the coastal State's rights in the light of its duty of prompt release

Special edition: The United Nations and international legal order - the case of the Juno Trader - on 18 December 2004, the International Tribunal for the Law of the Sea ordered the prompt release of a refrigerated cargo vessel and its cargo for fisheries violations in an exclusive economic zone - Tribunal unanimously decided that the vessel and cargo be released, upon posting of a bond in the form of a bank guarantee - crew should be free to leave without conditions - in this case, on prompt release, the Tribunal made valuable contributions to existing case law on the issue - shows that specialised tribunals may perform a decentralised application of the international rule of law - crystallises international fundamental standards of fairness and human rights.