Thesis (Ph.D.)--Victoria University (Melbourne, Vic.), 2008.

Thesis (Ph. D.)--University of Texas at Austin, 2002. / Vita. Includes bibliographical references. Available also from UMI Company.

Klamath Marsh is a wetland complex that lies in the rain shadow of the Cascade Range in the Williamson River sub-basin of the Klamath Basin. The marsh lies directly east of Crater Lake in an area inundated by pyroclastic-flow and -fall deposits from the Holocene eruptions of Mount Mazama. The physical characteristics of rocks of Pleistocene versus Pliocene age combined with NNW -striking fault systems divide the Williamson River basin into two distinct hydrogeologic regimes. The northwestern regime includes the east slope of the Cascades and consists of at least 150 m of interbedded sand, gravel, and stacks (15 to 45 m) of thin (3-5 m) and vesiculated basalt lava flows. Mean annual precipitation ranges from 150 cm near the crest of the Cascades to 50 cm near Klamath Marsh. Moderate to high yield (100 to 4000 gpm) water wells, springs and flowing wells suggest high permeability and ground water potential. The southeastern regime is underlain by Pliocene pyroclastic flows (∼ 40 m) and lava flows (>30 m). Mean annual precipitation ranges from 70 cm in the highlands to 50 cm in the lowlands. Low-yield (20-100 gpm) water wells and perched unconfined aquifers in Holocene pumice deposits suggest low permeability and low ground water potential in areas underlain by the pyroclastic flows. Volumetric analysis of inflows and outflows in Klamath Marsh for 2000 indicates approximately 86% of inflow is from groundwater and 14% from surface water, with nearly 200 x 10⁶ m³ of water removed by evapotranspiration

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This paper presents a zonation of the Austin chalk and the Burditt marl, divisions of the Austin group in the Jonah quadrangle, Williamson County, Texas. The Austin chalk consists of the Inoceramus subquadratus Schlüter faunizone, Gryphaea wratheri Stephenson faunizone, Inoceramus undulatoplicatus Roemer faunizone, Hemiaster texanus Roemer faunizone, Exogyra laeviuscula Roemer faunizone, and the Exogyra tigrina Stephenson epibole. The Burditt marl contains the Ostrea centerensis Stephenson faunizone. The Austin-Taylor contact has been traced from the southeastern to the northeastern corner of the area. The relations of the Taylor marl and some of the Terrace gravels are discussed. The outcrop, lithology, and paleontology of the Eagle Ford shale, which underlies the Austin group, are also included. / text

Thesis (M.A.)--Denver Conservative Baptist Seminary, 1994. / Includes bibliographical references (leaves [217]-231).

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Thesis (M.A.)--Youngstown State University, 2008. / Includes bibliographical references (leaves 125-127). Also available via the World Wide Web in PDF format.

Thesis (Ph. D.)--University of Sydney, 1996. / Title from title screen (viewed 27 March 2008). Submitted in fulfilment of the requirements for the degree of Doctor of Philosophy to the Dept. of English, Faculty of Arts. Includes bibliographical references. Also available in print form.

My thesis is a development and defence of the "Williamsonian" view of time, a temporalmetaphysical theory based on Timothy Williamson’s (1998, 1999, 2000, 2002) views concerning modality. As far as I am aware, the theory has never been developed or defended in print. The Williamsonian view is a version of the "a-theory" of time based on acceptance of the thesis of eternal existence, according to which always, everything always exists (i.e. everything exists eternally). I defend the Williamsonian view by showing that every other plausible temporal-metaphysical theory is subject to serious objections that cannot be raised against the Williamsonian view. I conclude that the Williamsonian view is the only plausible theory of time.