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  • 1
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    Higher Education Revolutions in the Gulf (2021)
    Taylor & Francis | Routledge
    Details
    Publication Date: 2024-03-29
    Description: Over the past quarter century, the people of the Arabian Peninsula have witnessed a revolutionary transformation in higher education. In 1990, there were fewer than ten public universities that offered their Arabic-language curricula in sex-segregated settings to national citizens only. In 2015, there are more than one hundred public, semi-public, and private colleges and universities. Most of these institutions are open to expatriates and national citizens; a few offer gender integrated instruction; and the language of instruction is much more likely to be in English than Arabic. Higher Education Revolutions in the Gulf explores the reasons behind this dramatic growth. It examines the causes of the sharp shift in educational practices and analyses how these new systems of higher education are regulated, evaluating the extent to which the new universities and colleges are improving quality. Questioning whether these educational changes can be sustained, the book explores how the new curricula and language policies are aligned with official visions of the future. Written by leading scholars in the field, it draws upon their considerable experiences of teaching and doing research in the Arabian Gulf, as well as their different disciplinary backgrounds (linguistics and economics), to provide a holistic and historically informed account of the emergence and viability of the Arabian Peninsula’s higher education revolutions. Offering a comprehensive, critical assessment of education in the Gulf Arab states, this book represents a significant contribution to the field and will be of interest to students and scholars of Middle East and Gulf Studies, and essential for those focused on higher education.
    Keywords: arab ; arabic ; development ; human ; modern ; reform ; report ; standard ; university ; zayed ; bic Book Industry Communication::J Society & social sciences::JN Education::JNM Higher & further education, tertiary education ; bic Book Industry Communication::G Reference, information & interdisciplinary subjects::GT Interdisciplinary studies::GTB Regional studies ; thema EDItEUR::J Society and Social Sciences::JN Education::JNM Higher education, tertiary education ; thema EDItEUR::G Reference, Information and Interdisciplinary subjects::GT Interdisciplinary studies::GTM Regional / International studies
    Language: English
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  • 2
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    Focused Fluid Flow along the Nootka Fault Zone and Continental slope, Explorer‐Juan de Fuca Plate Boundary (2020)
    AGU (American Geophysical Union) | Wiley
    Details
    Publication Date: 2023-02-08
    Description: Key Points: - Fluid flow is focused along Nootka Fault traces resulting in shallow bright spots - Two seafloor mounds are the result of basaltic intrusions in the Nootka Fault zone - Gas hydrates occur at the Nootka Slope and are imaged seismically as bottom- simulating reflectors suggesting a regional heat-flow of ~80 mW/m2 along the slope Abstract Geophysical and geochemical data indicate there is abundant fluid expulsion in the Nootka fault zone (NFZ) between the Juan de Fuca and Explorer plates and the Nootka continental slope. Here we combine observations from 〉 20 years of investigations to demonstrate the nature of fluid‐flow along the NFZ, which is the seismically most active region off Vancouver Island. Seismicity reaching down to the upper mantle is linked to near‐seafloor manifestation of fluid flow through a network of faults. Along the two main fault traces, seismic reflection data imaged bright spots 100 – 300 m below seafloor that lie above changes in basement topography. The bright spots are conformable to sediment layering, show opposite‐to‐seafloor reflection polarity, and are associated with frequency‐reduction and velocity push‐down indicating the presence of gas in the sediments. Two seafloor mounds ~15 km seaward of the Nootka slope are underlain by deep, non‐conformable high amplitude reflective zones. Measurements in the water column above one mound revealed a plume of warm water, and bottom‐video observations imaged hydrothermal vent system biota. Pore fluids from a core at this mound contain predominately microbial methane (C1) with a high proportion of ethane (C2) yielding C1/C2 ratios 〈 500 indicating a possible slight contribution from a deep source. We infer the reflective zones beneath the two mounds are basaltic intrusions that create hydrothermal circulation within the overlying sediments. Across the Nootka continental slope, gas hydrate related bottom‐simulating reflectors are widespread and occur at depths indicating heat‐flow values of 80 – 90 mW/m2.
    Type: Article , PeerReviewed
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    PAPER (OCEANREP)
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