Future perspectives in astronomy and the earth sciences

Author(s):  
J. Michael T Thompson ◽  
Charles H.-T Wang

This article is an overview of the contributions to the Triennial Issue of Phil. Trans. R. Soc. A published in December, 2005, and also plays the role of a Preface. Devoted to the work of young scientists, the issue covers the fields of astronomy and earth science.

GSA Today ◽  
2003 ◽  
Vol 13 (3) ◽  
pp. 27
Author(s):  
W.G. Ernst ◽  
G. Heiken ◽  
Susan M. Landon ◽  
P. Patrick Leahy ◽  
Eldridge Moores
Keyword(s):  

Elements ◽  
2019 ◽  
Vol 15 (4) ◽  
pp. 229-234 ◽  
Author(s):  
Patrick J. Frings ◽  
Heather L. Buss

Weathering is the chemical and physical alteration of rock at the surface of the Earth, but its importance is felt well beyond the rock itself. The repercussions of weathering echo throughout the Earth sciences, from ecology to climatology, from geomorphology to geochemistry. This article outlines how weathering interacts with various geoscience disciplines across a huge range of scales, both spatial and temporal. It traces the evolution of scientific thinking about weathering and man's impact on weathering itself—for better and for worse. Future computational, conceptual and methodological advances are set to cement weathering's status as a central process in the Earth sciences.


2014 ◽  
Vol 51 (3) ◽  
pp. xvii-xxxi
Author(s):  
Gordon F. West ◽  
Ron M. Farquhar ◽  
George D. Garland ◽  
Henry C. Halls ◽  
Lawrence W. Morley ◽  
...  

Fifty years ago, the world’s Earth Scientists experienced the so-called “Revolution in the Earth Sciences”. In the decade from 1960 to 1970, a massive convergence took place from many diverse and contradictory theories about the tectonic processes operating on Earth (then loosely called “mountain building”) to a single widely accepted paradigm now called Plate Tectonics. A major player in leading the international “Revolution” was Canadian geophysicist J. Tuzo Wilson. This tribute reviews how he helped define and promote the Plate Tectonic paradigm, and also, from 1946 to 1967, how he led a rapid expansion of the role of geophysics in Canadian and international earth science. Wilson was a controversial figure before and during the “Revolution”, but his influence was large. It was not coincidental that earth science research in Canada grew by 1964 to the point where the National Research Council of Canada could add the Canadian Journal of Earth Sciences to its group of Canadian research journals.


Episodes ◽  
2000 ◽  
Vol 23 (3) ◽  
pp. 155-162 ◽  
Author(s):  
Umberto G. Cordani
Keyword(s):  

1983 ◽  
Vol 2 (1) ◽  
pp. 11-16 ◽  
Author(s):  
Ellen Drake ◽  
Paul Komar

Among his 17th century contemporaries Robert Hooke (1635-1703) was exceptional in his investigations of the terraqueous globe by experimentation and development of instrumentation for ocean exploration and in forming hypotheses concerning the origin of the earth's surface features. Most theories of the earth written at that time were concerned with bringing observations of nature into concordance with Biblical accounts of Creation, the Deluge, and the final Conflagration. In contrast, Hooke's hypotheses, published posthumously in 1705 in his Discourses of Earthquakes, were essentially unhampered by religious considerations or by other forms of Medievalism. Because he was a product of the 17th century and because these Discourses were presented over a period of 30 years, Hooke naturally made references to all-pervasive Biblical concepts and furthermore his ideas showed some changes as time went on. But his approach was generally scientific and is considered more sophisticated than purely Baconian. His system of the earth was not only unlike those of his contemporaries but in essence was the pre-continental-drift paradigm within which most present-day geologists over age 40 were reared; many of his insights were startlingly modern. Hooke's role was significant in the development of science and especially in the progress of earth science.


2000 ◽  
Vol 19 (1) ◽  
pp. 26-32 ◽  
Author(s):  
Tanya Levin ◽  
Ronald Doel

The Lamont-Doherty Earth Observatory (LDEO) celebrated its fiftieth anniversary in 1999. As part of" the effort to preserve the history of this important earth science research institute, senior Lamont administrators conceived an ambitious oral history project. Now complete, these oral histories present a useful resource for those studying the history of the earth sciences, environmental history, social and institutional history, disciplinary development, technological change, internationalism in the sciences, and patronage. This article summarizes certain preliminary conclusions reached during the course of this project.


1985 ◽  
Vol 4 (1) ◽  
pp. 69-71
Author(s):  
Louis Unfer

The history of Southeast Missouri State University parallels that of other teacher education institutions. It started as Southeast Missouri Normal School in 1873 and reached university status in 1972. A department of Geology and Geography was established in 1909, becoming the Geography Department in 1915. In 1924, the sciences were combined into the Science Department. In 1960, this became the Division of Science and Mathematics and the Department of Earth Sciences was formed. An earth science major began in 1937, with separate geology and geography majors established in 1958. Recently the Department has developed more specialized, job-oriented programs in mining geology and in cartography. Since 1983 the Department has also operated a field camp, headquartered on the campus of Dixie College, St. George, Utah.


1985 ◽  
Vol 4 (1) ◽  
pp. 72-74
Author(s):  
James Corgan

Austin Peay State University is a small school, founded 56 years ago. While geology has long been taught, major programs are less than a decade old. Despite small size and shallow historical roots, the earth science faculty have been able to participate in the evolution of American geology through publication and through work on NSF projects. Many small colleges have comparable histories.


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