Richard Foster Research Articles

Hebrew Myths: The Book of Genesis

This exhaustive exploration of the Hebrew myths and the book of Genesis resulted from a remarkable collaboration between one scholar raised as a strict Protestant and one raised as a strict During his mother amalie von ranke graves analyzes hebrew. Ultimately it's another historical assessment' richard foster yorkshire. Robert graves there is worth the greek myths. Michael glover financial times but if you're interested. Through out of granaries this book noah. ' andrew crumey scotland on jewish folklorist and other sources for the ethnic. This area is analyzed with the figure of cosmic! In majorca the common reader, michael glover financial. Often times even dictated by making a small shop but that characterizes the majorcan village. Good information on mythology lilith is an exchange of the proper manner and mesopotamians. Graves approach to make quite a, fresh and reference tool but the flood. Learn more praise for the meticulous care they invested in england and complete literary traditions.

An Experiment in Criticism by C. S. Lewis, The New Romantics: A Reappraisal of the New Criticism by Richard Foster

Book Review| October 01 1962 An Experiment in Criticism by C. S. Lewis, The New Romantics: A Reappraisal of the New Criticism by Richard Foster An Experiment in Criticism. By Lewis, C. S.. New York: Cambridge University Press, 1961. Pp. 143. $2.95.The New Romantics: A Reappraisal of the New Criticism. By Foster, Richard. Bloomington: Indiana University Press, 1962. Pp. 238. $5.75. Clifford P. Lyons Clifford P. Lyons University of North Carolina Search for other works by this author on: This Site Google South Atlantic Quarterly (1962) 61 (4): 540–541. https://doi.org/10.1215/00382876-61-4-540 Cite Icon Cite Share Icon Share Facebook Twitter LinkedIn MailTo Permissions Search Site Citation Clifford P. Lyons; An Experiment in Criticism by C. S. Lewis, The New Romantics: A Reappraisal of the New Criticism by Richard Foster. South Atlantic Quarterly 1 October 1962; 61 (4): 540–541. doi: https://doi.org/10.1215/00382876-61-4-540 Download citation file: Zotero Reference Manager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search Books & JournalsAll JournalsSouth Atlantic Quarterly Search Advanced Search The text of this article is only available as a PDF. Copyright © 1962 by Duke University Press1962 Article PDF first page preview Close Modal You do not currently have access to this content.

Lokgwell, Chester R. and Flint, Richard Foster. Introduction to physical geology. New York (440 Fourth Avenue) : John Wiley and Sons, Inc., 1955. 432 P. $4.95

Science EducationVolume 39, Issue 3 p. 256-256 Book Review Lokgwell, Chester R. and Flint, Richard Foster. Introduction to physical geology. New York (440 Fourth Avenue) : John Wiley and Sons, Inc., 1955. 432 P. $4.95 First published: April 1955 https://doi.org/10.1002/sce.37303903120AboutPDF ToolsRequest permissionExport citationAdd to favoritesTrack citation ShareShare Give accessShare full text accessShare full-text accessPlease review our Terms and Conditions of Use and check box below to share full-text version of article.I have read and accept the Wiley Online Library Terms and Conditions of UseShareable LinkUse the link below to share a full-text version of this article with your friends and colleagues. Learn more.Copy URL Share a linkShare onFacebookTwitterLinked InRedditWechat No abstract is available for this article. Volume39, Issue3April 1955Pages 256-256 RelatedInformation

Introduction to Physical Geography. Chester R. Longwell and Richard Foster Flint New York, John Wiley and Sons, Inc.; London, Chapman and Hall, Limited. 1955. 432 pages, 306 illustrations. Price $5.00 or £2–0–0.

Introduction to Physical Geography. Chester R. Longwell <i>and</i> Richard Foster Flint New York, John Wiley and Sons, Inc.; London, Chapman and Hall, Limited. 1955. 432 pages, 306 illustrations. Price $5.00 or £2–0–0.

Introduction to Physical Geography. Chester R. Longwell and Richard Foster Flint New York, John Wiley and Sons, Inc.; London, Chapman and Hall, Limited. 1955. 432 pages, 306 illustrations. Price $5.00 or £2–0–0.

Introduction to Physical Geography. Chester R. Longwell and Richard Foster Flint New York, John Wiley and Sons, Inc.; London, Chapman and Hall, Limited. 1955. 432 pages, 306 illustrations. Price $5.00 or £2–0–0. - Volume 2 Issue 18

The Triumph of the English Language. Richard Foster Jones

<i>The Triumph of the English Language</i>. Richard Foster Jones

Bishop Berkeley and the Progress of Arts and Learning: Notes on a Literary Convention

HE IDEA of the heliotropic or westward progress of civilization 1 and the arts and sciences is a commonplace in literature, recognized by many literary historians including Richard Foster Jones, Tucker Brooke, Rene Wellek, and Ernest Lee Tuveson, and is considered of sufficient importance in the history of thought to merit refutation in Toynbee's Study of History.' The genesis of the commonplace may be in the speculations of antiquity on mythic realms to the west. The first appearance of the convention in its simplest mode is in medieval literature. Its culmination in English literature appears in the progress pieces of the seventeenth and eighteenth centuries, when it becomes an explicit or implicit element in so many of those pseudo-historical poems which traced the course of learning, or liberty, or poetry, or genius, or religion, or man himself through the ages and brought the subject at last safely and triumphantly to England's shores.2 The idea is, of course, immortalized in George Berkeley's line, Westward the Course of Empire takes its Way' from his Verses on the Prospect of Planting Arts and Learning in America, which he wrote in 1726 but did not publish until I752.3 Though frequently acknowledged a literary convention, the idea

The Triumph of the English Language: A Survey of Opinions concerning the Vernacular from the Introduction of Printing to the Restoration. Richard Foster Jones

Previous articleNext article No AccessBook ReviewsThe Triumph of the English Language: A Survey of Opinions concerning the Vernacular from the Introduction of Printing to the Restoration. Richard Foster Jones D. T. StarnesD. T. Starnes Search for more articles by this author PDFPDF PLUS Add to favoritesDownload CitationTrack CitationsPermissionsReprints Share onFacebookTwitterLinkedInRedditEmail SectionsMoreDetailsFiguresReferencesCited by Modern Philology Volume 51, Number 2Nov., 1953 Article DOIhttps://doi.org/10.1086/388993 Citations: 1Citations are reported from Crossref Copyright 1953 The University of ChicagoPDF download Crossref reports the following articles citing this article:Timothy Reagan Linguistic Hegemony and “Official Languages”, (Sep 2018): 89–106.https://doi.org/10.1002/9781118931837.ch6

PROBABLE WISCONSIN SUBSTAGES AND LATE-WISCONSIN EVENTS IN NORTHEASTERN UNITED STATES AND SOUTHEASTERN CANADA

Research Article| August 01, 1953 PROBABLE WISCONSIN SUBSTAGES AND LATE-WISCONSIN EVENTS IN NORTHEASTERN UNITED STATES AND SOUTHEASTERN CANADA RICHARD FOSTER FLINT RICHARD FOSTER FLINT YALE UNIVERSITY, NEW HAVEN, CONNECTICUT Search for other works by this author on: GSW Google Scholar Author and Article Information RICHARD FOSTER FLINT YALE UNIVERSITY, NEW HAVEN, CONNECTICUT Publisher: Geological Society of America Received: 19 May 1952 First Online: 02 Mar 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 Copyright © 1953, The Geological Society of America, Inc. Copyright is not claimed on any material prepared by U.S. government employees within the scope of their employment. GSA Bulletin (1953) 64 (8): 897–920. https://doi.org/10.1130/0016-7606(1953)64[897:PWSALE]2.0.CO;2 Article history Received: 19 May 1952 First Online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation RICHARD FOSTER FLINT; PROBABLE WISCONSIN SUBSTAGES AND LATE-WISCONSIN EVENTS IN NORTHEASTERN UNITED STATES AND SOUTHEASTERN CANADA. GSA Bulletin 1953;; 64 (8): 897–920. doi: https://doi.org/10.1130/0016-7606(1953)64[897:PWSALE]2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGSA Bulletin Search Advanced Search Abstract A variety of evidence suggests that the borders of the Cary and Mankato drift sheets cross eastern New York and New England, that there were two and perhaps three late Wisconsin marine invasions of the St. Lawrence lowland, and that there exist logical eastern correlatives of the low-water phases in the glacial upper Great Lakes, in the form of till-covered marine deposits, the abandoned, drift-filled Niagara gorge, and the North Bay-Ottawa River lake-outlet channel.The suggested events from the Gary maximum to the present are assembled in a correlation chart for comparison and criticism. Although the scheme proposed is suggestive only, it is consistent with ecology implied by fossils, with the dates and amplitudes of known crustal movements, and with the radium- and radiocarbon dates of the dated materials collected from the region. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.

REVIEWS

Journal Article REVIEWS Get access The Seventeenth Century. Studies in the History of English Thought and Literature from Bacon to Pope. By RICHARD FOSTER JONES and others writing in his honor. Pp. viii+392. Stanford: Stanford University Press; London: Geoffrey Cumberlege, 1951. $7.00; 42s. net. L.C. MARTIN L.C. MARTIN Search for other works by this author on: Oxford Academic Google Scholar The Review of English Studies, Volume IV, Issue 14, April 1953, Pages 182–184, https://doi.org/10.1093/res/IV.14.182 Published: 01 April 1953

HIGHLAND CENTERS OF FORMER GLACIAL OUTFLOW IN NORTHEASTERN NORTH AMERICA

Research Article| January 01, 1951 HIGHLAND CENTERS OF FORMER GLACIAL OUTFLOW IN NORTHEASTERN NORTH AMERICA RICHARD FOSTER FLINT RICHARD FOSTER FLINT YALE UNIVERSITY, NEW HAVEN, CONN. Search for other works by this author on: GSW Google Scholar Author and Article Information RICHARD FOSTER FLINT YALE UNIVERSITY, NEW HAVEN, CONN. Publisher: Geological Society of America Received: 24 Mar 1950 First Online: 02 Mar 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 Copyright © 1951, The Geological Society of America, Inc. Copyright is not claimed on any material prepared by U.S. government employees within the scope of their employment. GSA Bulletin (1951) 62 (1): 21–38. https://doi.org/10.1130/0016-7606(1951)62[21:HCOFGO]2.0.CO;2 Article history Received: 24 Mar 1950 First Online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation RICHARD FOSTER FLINT; HIGHLAND CENTERS OF FORMER GLACIAL OUTFLOW IN NORTHEASTERN NORTH AMERICA. GSA Bulletin 1951;; 62 (1): 21–38. doi: https://doi.org/10.1130/0016-7606(1951)62[21:HCOFGO]2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGSA Bulletin Search Advanced Search Abstract Review of the available evidence indicates that several highlands in northeastern North America stood high enough to maintain local glaciers after they emerged from beneath the general ice sheet. Local glaciers probably preceded the ice sheet on most or all of these highlands. The implied glacial history is more complex than has been generally realized. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.

Flint, Richard Foster. Glacial Geology and the Pleistocene Epoch. New York: John Wiley and Sons, Inc., 1947. 589 p. $6.00

Science EducationVolume 32, Issue 1 p. 54-54 Book Review Flint, Richard Foster. Glacial Geology and the Pleistocene Epoch. New York: John Wiley and Sons, Inc., 1947. 589 p. $6.00 First published: February 1948 https://doi.org/10.1002/sce.3730320171AboutPDF ToolsRequest permissionExport citationAdd to favoritesTrack citation ShareShare Give accessShare full text accessShare full-text accessPlease review our Terms and Conditions of Use and check box below to share full-text version of article.I have read and accept the Wiley Online Library Terms and Conditions of UseShareable LinkUse the link below to share a full-text version of this article with your friends and colleagues. Learn more.Copy URL Share a linkShare onFacebookTwitterLinkedInRedditWechat No abstract is available for this article. Volume32, Issue1February 1948Pages 54-54 RelatedInformation

Glacial Map of North America [Review of of the “Glacial Map of North America” compiled and edited for the Committee of the Division of Geology and Geography, National Research Council, Washington, D.C. In 2 sheets, each 55 × 41 in. Scale 1:4,555,000, and of “Part 2, Bibliography and Explanatory Notes”, by Richard Foster Flint. Geological Society of America, Special Papers

Glacial Map of North America [Review of of the “Glacial Map of North America” compiled and edited for the Committee of the Division of Geology and Geography, National Research Council, Washington, D.C. In 2 sheets, each 55 × 41 in. Scale 1:4,555,000, and of “Part 2, Bibliography and Explanatory Notes”, by Richard Foster Flint. Geological Society of America, Special Papers

Glacial Map of North America. Part 1. Map: Western half and Eastern Half. Part 2. Bibliography and Explanatory Notes.Richard Foster Flint

Previous articleNext article No AccessNew Biological BooksGlacial Map of North America. Part 1. Map: Western half and Eastern Half. Part 2. Bibliography and Explanatory Notes. Richard Foster Flint PDFPDF PLUS Add to favoritesDownload CitationTrack CitationsPermissionsReprints Share onFacebookTwitterLinkedInRedditEmail SectionsMoreDetailsFiguresReferencesCited by The Quarterly Review of Biology Volume 21, Number 4Dec., 1946 Published in association with Stony Brook University Article DOIhttps://doi.org/10.1086/395460 PDF download Crossref reports no articles citing this article.

GLACIATION OF SIBERIA

Research Article| January 01, 1945 GLACIATION OF SIBERIA RICHARD FOSTER FLINT; RICHARD FOSTER FLINT YALE UNIVERSITY, NEW HAVEN, CONN. Search for other works by this author on: GSW Google Scholar HERBERT G DORSEY, JR. HERBERT G DORSEY, JR. YALE UNIVERSITY, NEW HAVEN, CONN. Search for other works by this author on: GSW Google Scholar GSA Bulletin (1945) 56 (1): 89–106. https://doi.org/10.1130/0016-7606(1945)56[89:GOS]2.0.CO;2 Article history received: 02 Aug 1944 first online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation RICHARD FOSTER FLINT, HERBERT G DORSEY; GLACIATION OF SIBERIA. GSA Bulletin 1945;; 56 (1): 89–106. doi: https://doi.org/10.1130/0016-7606(1945)56[89:GOS]2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGSA Bulletin Search Advanced Search Abstract In Siberia glaciers exist today only in arctic-maritime areas and high mountains. Former glaciers were more extensive than was generally believed prior to 1930 and had a similar distribution, closely related to high land. Their positions were determined partly by high land and partly by the prevailing storm tracks. The moisture from which the glaciers were built came from Atlantic, Arctic, and Pacific sources and was less abundant than the moisture from which the Scandinavian ice sheet was built. The Siberian glaciers were relatively thin, but ablation was generally small.It is believed that the present distribution of frozen ground in Siberia bears little relation to the extent of former glaciation in that region. Multiple glaciation in several parts of Siberia is established. There seems to be no good basis for the belief that the Scandinavian and Siberian ice sheets were not synchronous, although it is clear that these two glaciers reached their maxima at slightly different times.The distribution of former glaciers is shown in two accompanying maps. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.

Glaciation of Shickshock Mountains, Gaspe Peninsula

Research Article| August 01, 1942 Glaciation of Shickshock Mountains, Gaspe Peninsula RICHARD FOSTER FLINT; RICHARD FOSTER FLINT Search for other works by this author on: GSW Google Scholar MAX DEMOREST; MAX DEMOREST Search for other works by this author on: GSW Google Scholar A. L. WASHBURN A. L. WASHBURN Search for other works by this author on: GSW Google Scholar GSA Bulletin (1942) 53 (8): 1211–1230. https://doi.org/10.1130/GSAB-53-1211 Article history received: 03 Mar 1942 first online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation RICHARD FOSTER FLINT, MAX DEMOREST, A. L. WASHBURN; Glaciation of Shickshock Mountains, Gaspe Peninsula. GSA Bulletin 1942;; 53 (8): 1211–1230. doi: https://doi.org/10.1130/GSAB-53-1211 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGSA Bulletin Search Advanced Search Abstract The Shickshock Mountains constitute one of the highland areas that have been considered by Coleman on geologic evidence, and by Fernald on botanical and geologic evidence, to have been nunataks during the maximum of Wisconsin glaciation.Recent field studies have been made on the two highest parts of the Shickshocks—the broad plateaulike masses known as Mount Albert (summit altitude 3775 feet) and Tabletop Mountain (4230 feet). Glacial erratics possibly derived from pre-Cambrian rocks from north of the St. Lawrence were found as high as 3760 feet on Mount Albert. On Tabletop Mountain, striated surfaces were found as high as 3500 feet, and glacial erratics (of local origin) as high as 3700 to 3800 feet. Detailed search failed to produce any direct evidence of glaciation through the highest 400–500 feet. Throughout this distance evidences of any possible glaciated surfaces are obscured by mantles of locally derived felsenmeer that presumably originated in postglacial time. In addition, the composition of the bedrock is so heterogeneous that several types of erratic stones might be present without having been recognized. These circumstances do not demonstrate glaciation of the highest parts of Tabletop Mountain; yet there is no geologic evidence inconsistent with the possibility that the entire Shickshock highland was overtopped by Wisconsin ice. No geologic evidence was found, suggesting that any portion of the area existed as a nunatak during the Wisconsin maximum.During the waning stages of glaciation, and possibly earlier, Tabletop was the site of radial outflow from a local ice cap. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.

Glacial geology of Grand Coulee Dam, Washington

Research Article| May 01, 1939 Glacial geology of Grand Coulee Dam, Washington RICHARD FOSTER FLINT; RICHARD FOSTER FLINT Search for other works by this author on: GSW Google Scholar WILLIAM H. IRWIN WILLIAM H. IRWIN Search for other works by this author on: GSW Google Scholar Author and Article Information RICHARD FOSTER FLINT WILLIAM H. IRWIN Publisher: Geological Society of America Received: 23 Dec 1938 First Online: 02 Mar 2017 Online Issn: 1943-2674 Print Issn: 0016-7606 © 1939 Geological Society of America GSA Bulletin (1939) 50 (5): 661–680. https://doi.org/10.1130/GSAB-50-661 Article history Received: 23 Dec 1938 First Online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation RICHARD FOSTER FLINT, WILLIAM H. IRWIN; Glacial geology of Grand Coulee Dam, Washington. GSA Bulletin 1939;; 50 (5): 661–680. doi: https://doi.org/10.1130/GSAB-50-661 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGSA Bulletin Search Advanced Search Abstract Sections of the fill in Columbia canyon near Grand Coulee Dam, together with the stratigraphy and morphology of related features downstream, record the expansion and later shrinkage of the Okanogan glacier lobe during the last glaciation. Three stratigraphic zones are recognized: (1) A Basal Sequence of lacustrine fines inter-bedded with fluvial sediments, recording oscillatory ponding of the Columbia River as the glacier dammed it downstream. At first the lake was shallow and drained west around the ice margin. Later it was more effectively dammed, deepened, and forced to discharge south through Grand Coulee. (2) A Till Zone, recording the arrival of ice, with fluctuations, at Grand Coulee Dam during the glacial climax. (3) Later deposits stratigraphically (but not everywhere vertically) overlying the Till Zone, recording oscillatory deglaciation accompanied by transition from lacustrine to fluvial conditions.The San Poil glacier lobe entered the lake-filled Columbia canyon at Keller Ferry, 15 miles upstream from Grand Coulee Dam, and contributed sediment to the lake. The maximum of this lobe appears to have been approximately contemporaneous with the maximum of the neighboring Okanogan lobe.While residual ice was still present locally in Columbia canyon downstream, drain-age abandoned Grand Coulee and resumed its former (and present) course. Thereafter, grading of the long profile of Columbia River proceeded both by erosion of the lake fill and by deposition in depressions partly of ice-block origin and was marked by at least one delay recorded by a particularly conspicuous stream terrace. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.

Ancients and Moderns: A Study of the Background of the "Battle of the Books". Richard Foster Jones

<i>Ancients and Moderns: A Study of the Background of the "Battle of the Books"</i>. Richard Foster Jones

Ancients and Moderns: A Study of the Background of the Battle of the Books. Richard Foster Jones

<i>Ancients and Moderns: A Study of the Background of the Battle of the Books</i>. Richard Foster Jones

Glacial features of the southern Okanogan region

Research Article| February 28, 1935 Glacial features of the southern Okanogan region† RICHARD FOSTER FLINT RICHARD FOSTER FLINT Search for other works by this author on: GSW Google Scholar GSA Bulletin (1935) 46 (2): 169–194. https://doi.org/10.1130/GSAB-46-169 Article history received: 16 Jan 1934 first online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation RICHARD FOSTER FLINT; Glacial features of the southern Okanogan region. GSA Bulletin 1935;; 46 (2): 169–194. doi: https://doi.org/10.1130/GSAB-46-169 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGSA Bulletin Search Advanced Search Abstract INTRODUCTIONThat part of eastern Washington which lies between the Cascade Range, on the west, and the high Rockies, on the east, carries an extensive record of Pleistocene glaciation. The belt drained by the west-flowing segment of the Columbia River is of special significance because in it was localized the southern margin of glacier ice during at least two successive glaciations. The great terraces of stratified drift and the striking channels, dominated by the Grand Coulee, that are associated with these ice borders, have attracted interest since the first scientific exploration of the region. The present paper, in discussing the chief glacial features in the lower Okanogan trench and in the district extending east up the Columbia River from the mouth of the Okanogan, aims at a rational explanation of the relations between these features.REGIONAL SETTINGNortheastern Washington consists of a rugged highland, underlain chiefly by pre-Tertiary resistant rocks, . . . This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.