Glens Falls Research Articles

Hemorrhagic Proctosigmoiditis and Blastocystis hominis

Letters15 November 1996Hemorrhagic Proctosigmoiditis and Blastocystis hominisJoseph Carl Yarze, MDJoseph Carl Yarze, MDGastroenterology Associates of Northern New York, Glens Falls, NY 12801.Search for more papers by this authorAuthor, Article, and Disclosure Informationhttps://doi.org/10.7326/0003-4819-125-10-199611150-00021 SectionsAboutFull TextPDF ToolsAdd to favoritesDownload CitationsTrack CitationsPermissions ShareFacebookTwitterLinkedInRedditEmail TO THE EDITOR:Carrascosa and colleagues recently reported a case of hemorrhagic proctosigmoiditis in the setting of documented Blastocystis hominis infection [1]. They suggest that their case provides further evidence to support the pathogenicity of B. hominis and the idea that B. hominis should be considered a possible cause of hemorrhagic colitis in both immunocompetent and immunocompromised patients. Although I agree with their cautious conclusion, several points about the case merit comment.First, the authors mention that the patient's stool was not examined for Shiga-like toxins. I assume that they are alluding to the fact that enterohemorrhagic infection with Escherichia ...

Two Steps Forward. One Step Back.

Participants at a community health information network in Glens Falls, N.Y., have come face-to-face with obstacles that could have meant the end to this rural health network that the New York Department of Health and the John A. Hartford Foundation helped launch more than two years ago. Instead, John Laliberte, Glens Falls Hospital's director of information systems, and the rest of the IS team are recovering from some setbacks and preparing to increase the CHIN's capabilities.

5529190 Gas sparged hydrocyclone with foam separating vessel: Carlton Keith A; Doshi Mahendra; Salvato Todd A; Funk Erwin; Phillips Joseph R; Clum Scott M, Glens Falls, NY, United States assigned to Ahlstrom Machinery Inc

5529190 Gas sparged hydrocyclone with foam separating vessel: Carlton Keith A; Doshi Mahendra; Salvato Todd A; Funk Erwin; Phillips Joseph R; Clum Scott M, Glens Falls, NY, United States assigned to Ahlstrom Machinery Inc

Palynologie et paléoenvironnements des épisodes du Sable de Lotbinière et des Varves de Deschaillons (Pléistocène supérieur) de la vallée du Saint-Laurent

Lotbinière Sand and Deschaillons Varves are indicators of the drainage pattern of the St. Lawrence watershed, which presumably occurred during the Late Sangamonian (5c and 5c–5b transition?). The pollen content of the Lotbinière Sand suggests there was a Picea mariana – Betula – Pinus boreal forest in the valley. In the lowermost zone of the Deschaillons Varves, the pollen is very abundant: the boreal forest was progressively flooded by Lake Deschaillons. Above this zone, the vegetation seems to evolve toward a Picea and Betula open forest. The pollen of the upper contorted varves was presumably reworked from older material or transported from remote sources. The following paleoenvironmental sequence is reconstructed in the St. Lawrence Valley: (i) lowering of the relative drainage level, as indicated by the erosional disconformity in lower rythmites; this phase, of unknown duration, is ascribed to an eustatic lowering related to a global climatic cooling; (ii) an aggradation phase, as indicated by the Lotbinière Sand, before and at the beginning of a glacial damming in the middle estuary; (iii) progressive flooding of the valley and its boreal forest as ice caps are present on adjacent Laurentian and Appalachian highlands; (iv) expansion of Lake Deschaillons, limited by the Glens Falls sill, New York. The relative elevation of the lake was at least 56 m. Great Lakes and upper St. Lawrence River drainage system was probably deflected to the Hudson River. According to the number of varves, the regional ice caps preceded the general invasion by Laurentide Ice Sheet of approximatively 3800 years.

Managerial Barriers to the Internationalization of U.S. Property and Liability Insurers: Theory and Perspectives

Managerial Barriers to Internationalization of U.S. Property and Liability Insurers: Theory and Perspectives Trade Barriers to International Property and Liability Operations Government Trade Barriers Numerous articles in insurance trade literature document instances where governmentally imposed trade barriers may have prevented entry into specific foreign markets [National Underwriter (1985), Risk Management (1980), McIntyre (1984), Nutter (1981)]. Academic attention has also been given to documenting existence of trade barriers and their economic consequences [Organization for Economic Cooperation and Development (1983), Carter and Dickinson (1977), Detwiler (1983), Pfeffer (1976), Skipper (1987)]. However, importance of foreign trade barriers as an explanation for lack of international involvement of U.S. property and liability insurers is not known [Fisher (1982), Ripol (1983), Skipper (1987)]. The purpose of this article is to examine, in a theoretical context, foreign market entry patterns of U.S. property and liability insurers. The results of a survey of industry executives' attitudes toward foreign operations are analyzed. An explanation for that behavior which is consistent with theory is also proposed. An Information Gap One of most serious obstacles to foreign operations of U.S. insurers is lack of market information. That information gap may actually be a greater barrier to entry into foreign markets than are governmental trade barriers. According to Skipper (1987, p. 63), the most impotant practical problems relating to [trade in] services revolve around data inadequacy. Pfeffer (1978) also speaks to problem of obtaining data necessary for foreign market operations. Despite trade barriers and lack of information, a few U.S. property and liability companies have entered foreign markets. CIGNA Corp., American International Group, continental Insurance, Allendate Mutual and others have been exceptionally active abroad. However, majority of U.S. insurers have made no attempt to enter foreign markets. With so many insurers in United States, why have so few chosen to engage in international operations? Why have those who have chosen to do so become so active? The answer to these questions may, in part, lie in nature and cost of foreign market information available in United States. In turn, source of this information barrier may be result of historical pattern of international operations of U.S. companies. The Modern History of International Activities of U.S. Property and Liability Companies By beginning of World War II, number of U.S. property and liability insurers operating in Europe had declined from a high of 21 immediately following World War I to only a dozen [Glass (1960)]. During World War II, industry responded by providing international coverages, especially war risk coverage. But post-war era of domestic prosperity again saw industry turn it back on international operations. The European business of U.S. companies immediately following war was, at best, negligible. Writing in late 1950s, Glass notes that only seven U.S. companies, excluding American and Foreign Insurance Association (AFIA) and American International Underwriters (AIU), had substantially rebuilt their European business after World War II [Glass (1960)]. They were: The Insurance Company of North America of Philadelphia, American Home Insurance Company of New York, Glens Falls Insurance Company of Hartford, Great American Insurance Company of New York, Hanover Fire Insurance Company of New York, Home Insurance Company of New York, and National Union Fire Insurance Company of Pittsburgh. In addition, Allstate Insurance Company had entered European market on a broad scale after World War II. …

Adirondack Pilgrimage. By Paul Jamieson. Glens Falls, New York: Adirondack Mountain Club, 1986. vi + 238 pp. Adirondack Portraits: A Piece of Time. By Jeanne Robert Foster. Edited by Noel Riedinger-Johnson. Syracuse, New York: Syracuse University Press, 1986

Previous articleNext article No AccessBook ReviewsAdirondack Pilgrimage. By Paul Jamieson. Glens Falls, New York: Adirondack Mountain Club, 1986. vi + 238 pp. Adirondack Portraits: A Piece of Time. By Jeanne Robert Foster. Edited by Noel Riedinger-Johnson. Syracuse, New York: Syracuse University Press, 1986Philip G. TerriePhilip G. Terrie Search for more articles by this author PDFPDF PLUS Add to favoritesDownload CitationTrack CitationsPermissionsReprints Share onFacebookTwitterLinkedInRedditEmail SectionsMoreDetailsFiguresReferencesCited by Volume 32, Number 2April 1988 Published for the American Society for Environmental History and the Forest History Society Article DOIhttps://doi.org/10.2307/4005079 Journal History This article was published in the Journal of Forest History (1974-1989), which was continued by Forest & Conservation History (1990-1995). © 1988 Forest History Society, Inc. All rights reserved.PDF download Crossref reports no articles citing this article.

Seat belt use law enforcement and publicity in Elmira, New York: a reminder campaign.

A three-week belt use law publicity and enforcement campaign in Elmira, New York, in November 1985, increased use from 49 per cent to 77 per cent; four months later belt use was 66 per cent. A reminder program, in April 1986, increased belt use to 80 per cent; use declined to 69 per cent four months later and to 60 per cent eight months later. Throughout these periods, belt use in Glens Falls, a comparison community, remained stable at just over 40 per cent.

Results of a seat belt use law enforcement and publicity campaign in Elmira, New York

In New York and other states in which seat belt use laws went into effect in the mid-1980s, belt use rates surged initially, then declined. This pattern of belt use also occurred in Canadian provinces that enacted laws in the mid-1970s; special enforcement programs reversed this trend. In late 1985 a three-week enforcement and publicity program was conducted in Elmira, New York. Belt use rates in Elmira were 49 percent before the program, 77 percent right after, and 66 percent two months later. In Glens Falls, a comparison city without a program, belt use declined from 43 percent to 37 percent during this interval. In a telephone survey after the campaign, Elmira respondents were more likely to say the belt use law was being strictly enforced and were more favorable toward it, compared to Glens Falls respondents. These data indicate that enforcement/publicity programs are an important and feasible method for increasing compliance with belt use laws.

Foreland Fold and Thrust Belt Deformation Chronology, Trenton Group Limestones and Overlying Shales, Northwestern Vermont: ABSTRACT

Outcrops of Trenton and younger limestones and shales between Plattsburgh, New York, and Malletts Bay, Vermont, show eastwardly increasing progressive deformation fabric in the foreland fold and thrust belt of northwestern Vermont. The deformation sequence within the calcareous Stony Point and Ibervillle shales is: (1) bed-parallel slip, marked by grooved calcite-covered surfaces; (2) folding accompanied by pressure solution cleavage; (3) overturned folds with frequent faulting along overturned limbs; fault surfaces, marked by calcite slickensides, at high angles to calcite-filled extension fractures; cleavage frequency increases and is rotated into a lower angle with bedding; (4) late-stage features 2-3 km (1.2-1.9 mi) from the Champlain thrust include high-angle faults and pervasive shearing of early fabric. Less than 1 km (0.6 mi) from the Champlain thrust (Malletts Bay area), fold hinges are sheared out and closely spaced cleavage is folded. The Cumberland Head Argillite (transitional between the Trenton Glens Falls Limestones and the younger Stony Point Shale) contains medium to thick micrite beams in a calcareous shale matrix. Deformation in the beams occurs by brittle failure and minor thrusting up ramps in the beams. The surrounding shale deforms by bed-plane slip and pressure-solution cleavage. Glens Falls Limestone in the study area consists of medium to thick beds of fossiliferous micrite. A widely spaced pressure solution cleavage is intensified and rotated in ramp-and-fold zones. The cleavage is crosscut by late high-angle faults. A progressive increase in deformation fabric from west to east across the Ordovician limestones and shales of the northern Champlain Valley allows the fold and thrust chronology to be determined for the different lithologies. End_of_Article - Last_Page 1923------------

The Adirondack Reader. Edited by Paul F. Jamieson (Glens Falls, New York: The Adirondack Mountain Club, Inc., 1983; 2nd. ed. 544 pp. $29.50, cloth; $18.50, paper.)

Previous articleNext article No AccessReviewsThe Adirondack Reader. Edited by Paul F. Jamieson (Glens Falls, New York: The Adirondack Mountain Club, Inc., 1983; 2nd. ed. 544 pp. $29.50, cloth; $18.50, paper.)Neal S. BurdickNeal S. Burdick St. Lawrence University Search for more articles by this author PDFPDF PLUS Add to favoritesDownload CitationTrack CitationsPermissionsReprints Share onFacebookTwitterLinkedInRedditEmail SectionsMoreDetailsFiguresReferencesCited by Volume 7, Number 3Fall 1983 Published for the American Society for Environmental History and the Forest History Society Article DOIhttps://doi.org/10.2307/3984486 Journal History This article was published in the Environmental Review (1976-1989), which was continued by the Environmental History Review (1990-1995). © 1983 American Society for Environmental History. All rights reserved.PDF download Crossref reports no articles citing this article.

Sulfur dioxide oxidation and plume formation at cement kilns

Results of source sampling at the Glens Falls cement kiln in Glens Falls, N.Y., are reported for sulfur oxides, ammonia, hydrochloric acid, oxygen, and moisture content. The origin of a detached, high-opacity, persistent plume originating from the cement kiln stack is investigated. It is proposed that this plume is due to ammonium salts of SOx and sulfuric acid that have been formed in condensed water droplets in the plume by the pseudocatalytic action of ammonia. (1 diagram, 1 graph, 22 references, 7 tables)

Eastern Snow Conference issues call for papers

The thirty‐third Eastern Snow Conference will be held at the Queensbury Hotel, Glens Falls, New York, February 5 and 6, 1976.The Eastern Snow Conference is an international organization in eastern Canada and northeastern United States concerned with the origin, precipitation, accumulation, character, melt, and runoff of snow from the viewpoint of meteorology, power generation, conservation, engineering, forestry, hydrology and relatered fields.

Programs, Materials and Techniques

MASTER is a series of workbooks designed to help teach learning disability children basic arithmetic skills but it assumes at least a beginning second grade knowledge of math. Following this is a set of manuals on remedial activities from the Educational Services Center, Glens Falls, N. Y. In a field allied to the MASTER program (there is evidence that spatial ability underlies mathematical skills) is the book of Tangrams which contains 330 spatial problems. They are both valuable for training children as well as for motivating them. The Reading Readiness Program and Animal Stories are filmstrips (and in the latter instance, cassettes) which hold a lot of potential for future development. The readiness program can serve as a very good visual discrimination training series. Carrascolendas is a TV series designed with the special difficulties of Spanishspeaking children in mind. Please continue to send me novel programs and matcrials you'd like to share with other learning disability teachers. Mail them to Dr. Alex Bannatyne, Bannatyne Children's Learning Center, 6950 N. Kendall Drive, Miami, Fla. 33156.

Late Pleistocene Erg in the Upper Hudson Valley, New York

Research Article| May 01, 1972 Late Pleistocene Erg in the Upper Hudson Valley, New York G. G CONNALLY; G. G CONNALLY Department of Geological Sciences, State University of New York at Buffalo, Buffalo, New York 14207 Search for other works by this author on: GSW Google Scholar D. H KRINSLEY; D. H KRINSLEY Queens College, City University of New York, Flushing, New York, 11367 Search for other works by this author on: GSW Google Scholar L. A SIRKIN L. A SIRKIN Department of Earth Sciences, Adelphi University, Garden City, New York 11530 Search for other works by this author on: GSW Google Scholar Author and Article Information G. G CONNALLY Department of Geological Sciences, State University of New York at Buffalo, Buffalo, New York 14207 D. H KRINSLEY Queens College, City University of New York, Flushing, New York, 11367 L. A SIRKIN Department of Earth Sciences, Adelphi University, Garden City, New York 11530 Publisher: Geological Society of America Received: 24 Nov 1971 First Online: 02 Mar 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 Copyright © 1972, 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 (1972) 83 (5): 1537–1542. https://doi.org/10.1130/0016-7606(1972)83[1537:LPEITU]2.0.CO;2 Article history Received: 24 Nov 1971 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 G. G CONNALLY, D. H KRINSLEY, L. A SIRKIN; Late Pleistocene Erg in the Upper Hudson Valley, New York. GSA Bulletin 1972;; 83 (5): 1537–1542. doi: https://doi.org/10.1130/0016-7606(1972)83[1537:LPEITU]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 An area covered by 2250 sq km of active sand dunes existed between Albany and Glens Falls, New York, after retreat of the last Wisconsinan glacier. A scanning electron microscope study of sand grains confirmed the sand dune history and other events inferred from surficial mapping. The dunes were probably active for a brief period between 12,500 and 12,000 yrs B.P. while the upper Hudson Valley was in a local rain shadow caused by southerly winds passing over the Hudson Highlands. 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.

Luzerne Readvance near Glens Falls, New York

The Woodfordian glacier advanced southward to the terminal moraine on Long Island and then retreated northward up the Hudson Valley. By 15,000 yrs B.P. the ice margin had retreated to the Wallkill Moraine and, after a readvance near Rosendale, New York, retreated a minimum of 130 mi farther north into the Champlain Valley, fronting an expanding Lake Albany. The ice margin then readvanced at least 20 mi into Lake Albany, to the Luzerne Mountain gorge of the Hudson River west of Glens Falls, New York. The type section for the Luzerne readvance is designated as that at the Luzerne Mountain gorge where the Luzerne readvance till occurs, over sands of Glacial Lake Warrensburg, over main Woodfordian till, and over contorted, pre-Woodfordian lacustrine clays. The western margin of the readvance is reconstructed from isolated morainal segments and associated outwash, and from the postulated ice dam for Lake Warrensburg. Pine Log Camp bog, developed in Luzerne readvance outwash, yielded an 8.0 m record. The base of the bog was dated at 13,150 ± 200 yrs B.P. in the herb pollen zone, and the base of the spruce pollen zone was dated at 12,400 ± 200 yrs B.P. The herb pollen zone was identified from several herbs, several grains of the genus Shepherdia, and a 35 percent maximum of nonarboreal pollen. The spruce, pine, and oak pollen zones are all well represented. Rapid encroachment of vegetation, illustrated by the time transgressive spruce zone and kettle morphology, are cited as evidence that bog deposition closely postdates glacial recession. The Luzerne readvance is pre-Port Huron in age and is correlated with the Gowanda Moraine of western New York, the Valley Heads Moraine of central New York and the Mohawk Valley, and the Burlington drift of Vermont. The Bridport readvance in the mid-Champlain Valley is inferred to Be Port Huron in age and is correlated with the Hamburg Moraine in western New York, the Waterloo-Auburn Moraine in central New York, and the Valley Heads Moraine in the Mohawk Valley. The relationship of local glaciers in the Adirondack Mountains and Lake Warrensburg, indicates that local glaciers were active during the Luzerne readvance and also are pre-Port Huron.

Continuous Diabetes Screening in a Rural Area

FOR a chronic disease problem to justify the institution of a public health service program, it must conform to essentially the same criteria as other disease problems: (a) there must be available either a means of prevention or an effective treatment, (b) the problem must be of such a nature that it (or a, significant part of it) cannot be solved by the traditional physician-patient relationship, (c) the problem must affect a significant number of people, and (d) it must have community significance. Casefinding in diabetes mellitus conforms to the above criteria. Although no method of primary prevention is known other than control of heredity (which in our present society is not very practicable), early diagnosis and continuous medical supervision can prevent the early complications of diabetes, and some of the late complications can be avoided or postponed (la). Relatively few people have formed the habit of presenting themselves for routine physical checkups, with the result that no opportunity is presented to diagnose an estimated 50 percent of those who have diabetes. The problem is large; it is estimated that there are over 2 million diabetics in the United States (ib), half of whom are unknown. Finally, the disease has an important degree of significance to the community, as it causes a considerable amount of disability, prema,ture death, loss of productivity, and increased demands on health and welfare facilities (2). Diabetes detection programs have been conducted for some years and are an accepted part of the public health scene. There are many types of programs, which vary, in time, from 1-day drives to year-round activities, and in technique, from rapid screening for sugar in the urine to exact, painstaking, and expensive blood determinations. Justification for thel operation of a diabetes detection program is based on the hypotheses that diabetes mellitus is often unrecognized and asymptomatic in the adult; that early diagnosis and treatment of diabetes improves prognosis and reduces complications; and that it is practical to screen postprandial hyperglycemic individuals from the general population by means of a community-operated clinic seirvice (3). One of the best methods of conducting such a screening program is by means of the test developed by Wilkerson and Heftmann (4), using the clinitron. This apparatus provides a rapid, inexpensive, and reasonably accurate method of screening large groups of people. Permanent, year-round diabetes screening programs using the clinitron seem to have been restricted thus far to urban populations. On March 1, 1958, the Glens Falls District Office of the New York State Health Department began a continuous screening program in a rural section of upstate New York, including Saratoga, Warren, and Washington Counties. Data during the first 10 months of operation are presented in the hope that they will contribute toward closing the gap between urban and rural public health practice in diabetes screening. The population of this tricounty area approximates 177,000, 25 percent of whom live in Dr. Meyer was health officer for the Glens Falls District, New York State Department of Health, at the time this paper was written. He is now director of health in Bucks County, Pa.

Benjamin Tallmadge: Revolutionary Soldier and American Businessman

Benjamin Tallmadge: Revolutionary Soldier and American Businessman. By Charles Swain Hall. (New York: Columbia University Press, 1943. x + 284 pp. Illustrations, bibliography, and index. $3.50.) Get access Harold M. Long Harold M. Long Glens Falls (New York) High School Search for other works by this author on: Oxford Academic Google Scholar Journal of American History, Volume 30, Issue 4, March 1944, Page 597, https://doi.org/10.2307/1916734 Published: 01 March 1944

Hudson Gorge in the Highlands

INTRODUCTION The Hudson River flows through five physiographic regions. Above Glens Falls, it courses through the ancient crystalline rocks of the Adirondacks; from Glens Falls to Newburgh, it follows the Great Valley of limestone and shale; south of Newburgh, it leaves the broad Appalachian Valley to cross the Highlands, through a relatively narrow, crooked, and steep-sided gorge; from a point just southwest of Peekskill to the city of New York, it follows a contact between the metamorphic rocks on the east and the overlying Triassic on the west; below New York Bay, its channel is cut in the submerged Coastal Plain. The Hudson Highlands are a block of northeastward-pitching pre-Cambrian crystalline rocks, separated from the Great Valley, on the northwest, by a thrust fault, and from the Piedmont, on the southeast, by a normal fault. For the purposes of this paper, these crystalline rocks may be divided into Grenville gneiss . . .

Authigenic Feldspar in Limestone at Glens Falls, New York

Introduction Small quarries on both sides of the Hudson at Glens Falls, New York, are producing stone for lime-burning from beds of Trenton limestone that are 15 feet thick and that dip gently to the south. The lime enjoys an almost exclusive market for use in drawing steel wire because of its freedom from constituents that scratch the wire. A microscopic examination of the insoluble residue of a sample of the limestone showed that it contains many completely developed crystals of albitic feldspar of authigenic origin. Character of the Limestone The limestone is a dark gray to nearly black crystalline-looking rock, which in thin-section is seen to consist of clouded aggregates of very finely crystalline calcite in a matrix of more coarsely crystalline calcite. The clouded aggregates are more or less spherical and have a microcrystalline and cryptocrystalline texture. Their dark color is due to an abundance of minute inclusions . . .

Ice Evacuation Stages at Glens Falls, New York

Research Article| December 30, 1928 Ice Evacuation Stages at Glens Falls, New York GEORGE HALCOTT CHADWICK GEORGE HALCOTT CHADWICK Search for other works by this author on: GSW Google Scholar GSA Bulletin (1928) 39 (4): 901–922. https://doi.org/10.1130/GSAB-39-901 Article history received: 14 May 1928 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 GEORGE HALCOTT CHADWICK; Ice Evacuation Stages at Glens Falls, New York. GSA Bulletin 1928;; 39 (4): 901–922. doi: https://doi.org/10.1130/GSAB-39-901 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 IntroductionThe manner of the ice-withdrawal from the Hudson Valley, and especially its aqueous accompaniment, have long been matters of speculation and even acrimony (see subjoined bibliography). Highly divergent views persist, particularly as to the segment here discussed, yet no one has critically tested his theory by reconstructing the ancient geography step by step, as undertaken in our figures 1 to 8. The only merit claimed for these maps is that they resolve without violence a large number of facts that can not be explained satisfactorily under any other hypothesis. Their implications are considered in the sequel.The original colored maps, exhibited by courtesy of Professor Hyde at the Cleveland meeting, were sketched in crayon on the Government topographic sheets, the ice-buried areas being first overlaid with plain paper to conceal topography and culture before the green conventions representing ice were put on—a method commended to those who desire . . . 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.