A unique word-scanning facility for the Eureka full-text information retrieval system /

Thesis (M.S.)--University of Illinois at Urbana-Champaign.

Paleontology of the Eureka District /

Includes index.

Silver-lead deposits of Eureka, Nevada /

Includes index.

Climatological summary, Eureka, N. W. T., Canada.

Prepared in cooperation with the Meteorological Division of Canada.

Charter and revised ordinances of the city of Eureka,

Mode of access: Internet.

Paleontology of the Eureka district.

Mode of access: Internet.

Excellent Lincoln Highway Markers west of Eureka, Neb.

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

Freighters on the Lincoln Highway between Eureka and Austin, Nevada. June 14th.

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

Lady Eureka : or The mystery; a prophecy of the future /

Mode of access: Internet.

Diseño y estructuración de la estrategia de ventas de la empresa “Eureka Kids”

La estrategia de ventas es un pilar fundamental de la estrategia integral de una empresa, ya que en ella se definen las acciones que contribuirán a su crecimiento, a su posicionamiento en cada uno de los segmentos de mercado y a alcanzar la rentabilidad esperada. La compañía EUREKA KIDS era consciente que su departamento de ventas no estaba debidamente formado, direccionado y preparado para afrontar los retos que presenta el mercado de la puericultura en lo referente a los artículos de aseo y cosméticos, por tal motivo fue imperativo diseñar y estructurar una estrategia de ventas gerenciable, coherente y sostenible en el tiempo, que le permitiera a la empresa tener desde la selección de sus vendedores, un personal comprometido y competitivo a nivel profesional que le ayude a aumentar los niveles de ventas actuales y futuros. A través del método empírico – analítico, se pudo concluir que si la empresa agranda y profesionaliza su estructura comercial podrá lograr una mayor y mejor penetración del mercado actual, bajo los métodos y procesos de efectividad comercial propuestos a lo largo de la investigación, los cuales están fundamentados en las más recientes investigaciones realizadas a nivel mundial en estrategias de ventas.

XVI Conferência Interparlamentar EUREKA 2009

A realização, em Portugal, da XVI Conferência Interparlamentar EUREKA 2009 decorreu da decisão da Assembleia da República no sentido de se associar ao conjunto de iniciativas que concretizaram a presidência portuguesa da Iniciativa Eureka. O evento assumiu, como principal objetivo, proporcionar, a todas(os) as(os) deputadas(os) dos países membros deste ambicioso projeto, a reflexão e o debate de temas estratégicos e relevantes para a consolidação e o desenvolvimento do conceito e das práticas da Iniciativa Eureka. Nesta XVI Conferência Interparlamentar, as questões relacionadas com a Energia e a Sustentabilidade assumiram-se como tema central, em torno do qual se estruturou o respetivo programa. O desenho da conferência tentou sequenciar, através da organização de painés, as seguintes questões de partida: a. O que é a Iniciativa Eureka? b. A simbiose entre a Ciência, a Tecnologia e as Empresas: o caso português; c. Pesquisa e desenvolvimento na rede Eureka; d. A Ciência e a Tecnologia na União Europeia de 2020; e. Energia e Sustentabilidade. Cada painel teve o contribuo de especialistas na área objeto de reflexão e terminou com a realização de um pequeno debate. Os(as) parlamentares participantes na Conferência Interparlamentar Eureka tiveram também a oportunidade de se deslocar ao Alentejo. Aí, ocorreram um painel (na Universidade de Évora) e duas visitas de trabalho a unidades produtoras de energia elétrica a partir de fonte renovável (a Central Hidroelétrica do empreendimento do Alqueva e a Central Fotovoltaica da Amareleja). Neste último momento formal em que se encerra a XVI Conferência Interparlamentar Eureka 2009, com a publicação do livro da Conferência, esperamos que a mesma tenha sido um sério contributo para a Iniciativa Eureka e para a promoção, na Europa e no mundo, de um modelo de desenvolvimento energeticamente eficiente e compatível com uma adequada matriz de sustentabilidade humana, social e económica.

Vic Slater during the Youth Campaign against Conscription, Brisbane, Australia

Vic Slater and police during the Youth Campaign against Conscription, Brisbane, Australia in 1965. Victor Charles Slater (now retired) was born in Queensland in March 1944 the only child of Jim and Joyce Slater, card carrying members of the Communist Party of Australia. Vic's mother, Joyce, joined up in Great Britain. Vic too joined the party in 1962 after a stint as president of the Eureka Youth League. He stayed with the more broad left CPA when it split from the hardline Stalinists after the Soviet invasion of Czechoslovakia in 1968. Vic joined the Waterside Workers' Federation before his 21st birthday in January 1965, one of 300 casual workers recruited to the Port of Brisbane that year. On the wharves he soon earned the nickname 'the Professor' arriving on the job each day bespectacled and carrying a briefcase heavy with reading matter on world politics and economics - a walking encyclopaedia of information. [information kindly provided by Peter Gray]

Poracanthodid acanthodian from the Upper Silurian (Pridoli) of Nevada

Dissociated remains of the acanthodian Poracanthodes punctatus are described from Upper Silurian (Pridoli) limestones of the Roberts Mountains Formation at Pete Hanson Creek, Eureka County, Nevada. The vertebrate microremains in sample residues comprise scales, a dentigerous jaw bone fragment, and a fin spine fragment assigned to P. punctatus, plus one possible acanthothoracid placoderm scale. Some macroremains from the same locality are also assigned to P. punctatus. This taxon has been nominated as, a zone fossil for the Silurian vertebrate biozonal scheme, and its presence has been recorded throughout the circum-Arctic region. Identification of the taxon in Nevada extends its known geographic range.

Critical reappraisal of Late Mesozoic-Cenozoic Central and North Atlantic, Caribbean and Mediterranean evolution

(l) The Pacific basin (Pacific area) may be regarded as moving eastwards like a double zip fastener relative to the continents and their respective plates (Pangaea area): opening in the East and closing in the West. This movement is tracked by a continuous mountain belt, the collision ages of which increase westwards. (2) The relative movements between the Pacific area and the Pangaea area in the W-EfE-W direction are generated by tidal forces (principle of hypocycloid gearing), whereby the lower mantle and the Pacific basin or area (Pacific crust = roof of the lower mantle?) rotate somewhat faster eastwards around the Earth's spin axis relative to the upper mantle/crust system with the continents and their respective plates (Pangaea area) (differential rotation). (3) These relative West to East/East to West displacements produce a perpetually existing sequence of distinct styles of opening and closing oeean basins, exemplified by the present East to West arrangement of ocean basins around the globe (Oceanic or Wilson Cycle: Rift/Red Sea style; Atlantic style; Mediterranean/Caribbean style as eastwards propagating tongue of the Pacific basin; Pacific style; Collision/Himalayas style). This sequence of ocean styles, of which the Pacific ocean is a part, moves eastwards with the lower mantle relative to the continents and the upper-mantle/crust of the Pangaea area. (4) Similarly, the collisional mountain belt extending westwards from the equator to the West of the Pacific and representing a chronological sequence of collision zones (sequential collisions) in the wake of the passing of the Pacific basin double zip fastener, may also be described as recording the history of oceans and their continental margins in the form of successive Wilson Cycles. (5) Every 200 to 250 m.y. the Pacific basin double zip fastener, the sequence of ocean styles of the Wilson Cycle and the eastwards growing collisional mountain belt in their wake complete one lap around the Earth. Two East drift lappings of 400 to 500 m.y. produce a two-lap collisional mountain belt spiral around a supercontinent in one hemisphere (North or South Pangaea). The Earth's history is subdivided into alternating North Pangaea growth/South Pangaea breakup eras and South Pangaea growth/North Pangaea breakup eras. Older North and South Pangaeas and their collisional mountain belt spirals may be reconstructed by rotating back the continents and orogenic fragments of a broken spiral (e.g. South Pangaea, Gondwana) to their previous Pangaea growth era orientations. In the resulting collisional mountain belt spiral, pieced together from orogenic segments and fragments, the collision ages have to increase successively towards the West. (6) With its current western margin orientated in a West-East direction North America must have collided during the Late Cretaceous Laramide orogeny with the northern margin of South America (Caribbean Andes) at the equator to the West of the Late Mesozoic Pacific. During post-Laramide times it must have rotated clockwise into its present orientation. The eastern margin of North America has never been attached to the western margin of North Africa but only to the western margin of Europe. (7) Due to migration eastwards of the sequence of ocean styles of the Wilson Cycle, relative to a distinct plate tectonic setting of an ocean, a continent or continental margin, a future or later evolutionary style at the Earth's surface is always depicted in a setting simultaneously developed further to the West and a past or earlier style in a setting simultaneously occurring further to the East. In consequence, ahigh probability exists that up to the Early Tertiary, Greenland (the ArabiaofSouth America?) occupied a plate tectonic setting which is comparable to the current setting of Arabia (the Greenland of Africa?). The Late Cretaceous/Early Tertiary Eureka collision zone (Eureka orogeny) at the northern margin of the Greenland Plate and on some of the Canadian Arctic Islands is comparable with the Middle to Late Tertiary Taurus-Bitlis-Zagros collision zone at the northern margin of the Arabian Plate.