What is the Role of Universities in High-tech Economic Development? The Case of Portland, Oregon, and Washington, DC

This paper focuses on two regions in the United States that have emerged as high-technology regions in the absence of major research universities. The case of Portland's Silicon Forest is compared to Washington, DC. In both regions, high-technology economies grew because of industrial restructuring processes. The paper argues that in both regions other actors—such as firms and government laboratories—spurred the development of knowledge-based economies and catalysed the engagement of higher education institutions in economic development. The paper confirms and advances the triple helix model of university–government–industry relationships and posits that future studies have to examine degrees of university-region engagement.

Anträge der Erlanger Gewerbtreibenden bei dem Gewerbs-Congresse zu Frankfurt: Die sämmtlichen Wahlmänner für einen Abgeordneten zum Gewerbscongresse nach Frankfurt, welcher am 15. d. Mt. eröffnet werden soll, authorisiren und bevollmächtigen ihren Vertrauensmann: Herrn Tünchermeister Andreas Schmidtill ...

Welsch (Projektbearbeiter): Bekanntgabe der Mandatierung des Tünchermeisters Schmidtill als Vertreter der Erlanger Gewerbetreibenden auf dem 'Deutschen Handwerker- und Gewerbe-Congreß' zu Frankfurt/Main

Washington Irving's sämmtliche Werke

In Fraktur

John Rziha, Perfecting human actions: St. Thomas Aquinas on human participation in eternal law, Catholic University of America Press, Washington, 2009; 300 p., ISBN 978-0-8132-1672-0.

Fil: Peretó Rivas, Rubén.

Paleomagnetism at DSDP Sites 86-576 and 86-578

The upper sections of Deep Sea Drilling Project Sites 576 (32°21.4'N, 164°16.5'E) and 578 (33°55.6'N, 151°37.7'E) both have stable detrital remanence that can be correlated with the standard reversal stratigraphy. Site 576 contains all reversals above the base of the Gilbert Epoch (5 m.y.) at about 25 m, whereas Site 578 contains a remarkable section of about 60 reversals extending to Anomaly 5B (15 m.y.) at about 150 m sub-bottom depth. In both cases, the paleomagnetic stratigraphy breaks down when accumulation rates drop below 2 m/m.y. At both sites, authigenic manganiferous clays deposited from 70 to 16 m.y. ago accumulated at about 0.4 m/m.y. Similarly, at both sites, the Pleistocene pulse of eolian debris increased accumulation rates by about 6 m/m.y.**2. From 16 to 2 m.y. ago, however, sediment accumulated at Site 578 about five times as rapidly as at Site 576, apparently because of augmented input to the western site by bottom currents.