Posthumous works of the Rev. Henry B. Bascom /

Each volume has also separate title-page.

Frederick the Great and the seven years' war /

Series title also at head of title page.

A Homiletic and illustrative treasury of religious thought : or twenty thousand choice extracts, selected from the works of all the great writers, ancient and modern with copious indices /

Includes indexes.

The genteel A. B. /

Mode of access: Internet.

The great seven--the greater nine; a story for the people,

Mode of access: Internet.

Canada; the country, its people, religions, politics, rulers, and its apparent future, being a compendium of travel from the Atlantic to the Pacific, the Great Lakes, Manitoba, the North-West, and British Columbia, with a description of their resources, trade, statistics, together with the legends of the Ottawa, the lower St. Lawrence, and the coast. With 40 illustrations, rapids of the St. Lawrence, &c.

"Copyright Washington, D.C., 1881. Ottawa, 1882. Stationers' Hall, London, Eng., 1882.

The Pleistocene of Indiana and Michigan and the history of the Great Lakes.

Some plates printed on both sides of leaves.

An historical account of the ancient town and port of Wisbech, in the Isle of Ely, in the county of Cambridge, and of the circumjacent towns and villages, the drainage of the great level of the fens, the origin of the royal franchise of the Isle of Ely &c. ...

Mode of access: Internet.

A history of the civil war, 1861-65, and the causes that led up to the great conflict,

Published in 16 parts.

Life and public services of Gen. Grant; being a complete life of the great hero ...

Mode of access: Internet.

Ancient Greece : a sketch of its art literature and philosophy viewed in connection with its external history from earliest times to the age of Alexander the Great.

Mode of access: Internet.

March ... for the organ [in B flat major]

Mode of access: Internet.

The source of the Great Dyke, Zimbabwe, and its tectonic significance: Evidence from Re-Os isotopes

Re-Os data for chromite separates from 10 massive chromitite seams sampled along the 550-km length of the 2.58-Ga Great Dyke layered igneous complex, Zimbabwe, record initial 187Os/188Os ratios in the relatively narrow range between 0.1106 and 0.1126. This range of initial 187Os/188Os values is only slightly higher than the value for the coeval primitive upper mantle (0.1107) as modeled from the Re-Os evolution of chondrites and data of modern mantle melts and mantle derived xenoliths. Analyses of Archean granitoid and gneiss samples from the Zimbabwe Craton show extremely low Os concentrations (3-9 ppt) with surprisingly unradiogenic present-day 187Os/188Os signatures between 0.167 and 0.297. Only one sample yields an elevated 187Os/188Os ratio of 1.008. Using these data, the range of crustal contamination of the Great Dyke magma would be minimally 0%-33% if the magma source was the primitive upper mantle, whereas the range estimated from Nd and Pb isotope systematics is 5%-25%. If it is assumed that the primary Great Dyke magma derived from an enriched deep mantle reservoir (via a plume), a better agreement can be obtained. A significant contribution from a long-lived subcontinental lithospheric mantle (SCLM) reservoir with subchondritic Re/Os to the Great Dyke melts cannot be reconciled with the Os isotope results at all. However, Os isotope data on pre-Great Dyke ultramafic complexes of the Zimbabwe Craton and thermal modeling show that such an SCLM existed below the Zimbabwe Craton at the time of the Great Dyke intrusion. It is therefore concluded that large melt volumes such as that giving rise to the Great Dyke were able to pass lithospheric mantle keels without significant contamination in the late Archean. Because the ultramafic-mafic melts forming the Great Dyke must have originated below the SCLM (which extends to at least a 200-km depth ), the absence of an SCLM signature precludes a subduction-related magma-generation process.

Establishing representative no-take areas in the Great Barrier Reef : Large scale implementation of theory on marine protected areas

The Great Barrier Reef Marine Park, an area almost the size , of Japan, has a new network of no-take areas that significantly improves the protection of biodiversity. The new marine park zoning implements, in a quantitative manner, many of the theoretical design principles discussed in the literature. For example, the new network of no-take areas has at least 20% protection per bioregion, minimum levels of protection for all known habitats and special or unique features, and minimum sizes for no-take areas of at least 10 or 20 kat across at the smallest diameter Overall, more than 33% of the Great Barrier Reef Marine Park is now in no-take areas (previously 4.5%). The steps taken leading to this outcome were to clarify to the interested public why the existing level of protection wets inadequate; detail the conservation objectives of establishing new no-take areas; work with relevant and independent experts to define, and contribute to, the best scientific process to deliver on the objectives; describe the biodiversity (e.g., map bioregions); define operational principles needed to achieve the objectives; invite community input on all of The above; gather and layer the data gathered in round-table discussions; report the degree of achievement of principles for various options of no-take areas; and determine how to address negative impacts. Some of the key success factors in this case have global relevance and include focusing initial communication on the problem to be addressed; applying the precautionary principle; using independent experts; facilitating input to decision making; conducting extensive and participatory consultation; having an existing marine park that encompassed much of the ecosystem; having legislative power under federal law; developing high-level support; ensuring agency Priority and ownership; and being able to address the issue of displaced fishers.