Royal E. Shanks

ARCTIC ◽  
1963 ◽  
Vol 16 (1) ◽  
pp. 48
Author(s):  
Arctic Institute Of North America

Royal E. Shanks was born in Ada, Ohio on November 11, 1912. He lost his life on August 4, 1962 while swimming and studying a coral reef in a bay of the Caribbean Sea in Porte Limon, Costa Rica. He completed his M. S. in 1937 and received his Ph.D. degree a year later. From 1940 to 1946 Dr. Shanks held the post of Professor of Biology at Austin Peay State College in Tennessee with brief periods of service in both the Army and Navy. In 1947 he joined the University of Tennessee as an Associate Professor of Botany and became a Professor two years later. In 1955 a concern with environmental aspects of ecosystems led him to propose some fundamental studies in the most simple environments, those of the arctic regions. It was this interest that developed a close relationship and association between Dr. Shanks and the Arctic Institute of North America. From 1955 until the time of his death he received six grants from the Institute for the study of composition, structure, and productivity of tundra vegetation in northern Alaska. During his field studies in Alaska Dr. Shanks covered an extensive area on the northern coast of Alaska extending eastward nearly to the Canadian border and southward to the mountains and forests. Numerous publications have resulted from this research. Not only has Dr. Shanks made a considerable contribution to arctic research, but his ability has been recognized by his election to office in a number of scientific societies. A colleague of Dr. Shanks has said, "his manner was gentle, his activity great, his enthusiasm contagious".

ARCTIC ◽  
1965 ◽  
Vol 18 (2) ◽  
pp. 147
Author(s):  
Laurence Irving

Many people who mourn the loss of Ivar Skarland who died 1 January 1965, are grateful for his friendship and influence during the development of science and society in Alaska. Ivar Skarland was born in 1899 and grew up in Norway. After graduating from the School of Forestry at Steinkjer, Norway, he worked in the forests of Canada and reached Alaska in 1928. As an undergraduate at the Alaska Agricultural College and School of Mines (now the University of Alaska) he took part in the Biological Survey investigations into the food habits of large northern herbivores. While at the school, he met Otto Geist who induced him to join in excavations at Kukulik, St. Lawrence Island, which led to important archaeological discoveries and a lifelong friendship and association. After receiving his bachelor's degree from the University of Alaska he studied anthropology at Harvard, spending summers in the field in Alaska. He obtained his M.A. in 1942, and that year became associate professor at the University of Alaska. He was soon, however, diverted to Army service in the Aleutian Islands. In 1945 he returned to the University where he remained, except while studying at Harvard for his Ph.D. which he received in 1949. Before the War, Skarland was a powerful supporter of the able and venturesome expeditionary workers who developed the important sites of ancient cultures on Lawrence Island and at Point Hope. After the War these field studies in archaeology continued to progress during his collaboration with Otto Geist and J. L. Giddings and in the company of a sequence of distinguished visitors; important archaeological explorations along the Kobuk River, in the Brooks Range, and on the Arctic coast resulted. Skarland encouraged and supported scientists in their explorations, and although his name did not appear often on publications, he exerted a guiding influence through his firm friendship and wide acquaintance with the land and people of Alaska. As host to the scientists who were developing knowledge of Alaska he was at the focus of a score of investigations that have brought to light localities that are now famous in archaeology and biology, for example: Cape Denbigh, Anaktuvuk Pass, Onion Portage, and Kachemak Bay. He prompted the search in the Susitna Valley and along the Denali Highway that has shown traces of an unexpected ancient population south of the Alaska Range. Ivar Skarland was a charter associate and fellow of the Arctic Institute of North America. Many of its projects in the western arctic resulted from his stimulation and were sustained by his wise counsel. Because of his personal qualities and ability to interest men in scholarly exploration it is not surprising that Skarland was an inspiring teacher. Students liked and trusted him and a considerable number from his small classes published important anthropological papers as undergraduates. Those who became professional anthropologists continued to appreciate Ivar Skarland's encouragement and sincere and constructive criticism. His knowledge and understanding of people made his advice important in matters of public welfare and particularly in political and social considerations of Indian and Eskimo residents as their lands became settled and their ways changed. Looking upon his active life in Alaska we find that Ivar Skarland steadily exerted a powerful influence among scientists, students and his fellow citizens. Not only was he the firmest of friends but his friendship stimulated scholarship, and the progress of the various races as citizens in a northern society.


ARCTIC ◽  
1965 ◽  
Vol 18 (1) ◽  
pp. 66
Author(s):  
Henry B. Collins

In the tragic death of Dr. J. L. Giddings on December 9, 1964 from a heart attack following an automobile accident, Arctic archaeology has lost one of its ablest, most brilliant and most productive workers. Born in Caldwell, Texas, April 10, 1909, Louis Giddings studied at Rice University, received his B.S. degree at the University of Alaska in 1932, M.A. at the University of Arizona, 1941, and Ph.D. at the University of Pennsylvania in 1951. From 1932 to 1937 he worked as an engineer for the U.S. Smelting and Refining Company. From 1938 to 1950 he was on the staff of the University of Alaska, progressing from Research Associate to Associate Professor of Anthropology. Between 1943 and 1946, however, he was on active duty as a Navy Lieutenant in the Pacific Area. In 1950 he became Assistant Professor of Anthropology and Assistant Curator of the University Museum, University of Pennsylvania. In 1956 he was appointed Associate Professor of Anthropology and Director of the Haffenreffer Museum, Brown University, becoming Professor in 1959. Louis Giddings was one of the first Associates of the Arctic Institute elected to Fellowship, and he received one of the Institute's first research grants. The Arctic Institute may well take pride in the fact that it was able to support Giddings' 1948 and 1949 excavations at Cape Denbigh, Alaska, which opened entirely new vistas in Arctic archaeology, and that it contributed to the support of his later and equally important work on the Arctic coast. An expert in dendrochronology, Giddings was the first to apply this technique in the Arctic. Working with samples from living trees and driftwood from old Eskimo village sites on the Kobuk, he established a tree-ring chronology for the last 1,000 years of Eskimo culture. Giddings' work at Cape Denbigh was in the opposite direction - it uncovered the roots of Eskimo culture. His 4,500 to 5,000 year old Denbigh Flint Complex was unlike anything previously known in the Arctic. It was a microlithic assemblage with close affinities with the Old World Mesolithic, and it represented a stage of culture that developed into Eskimo. Giddings' later work around Kotzebue Sound and at Onion Portage in the interior produced equally spectacular results. At Cape Krusenstern a long succession of old beach ridges revealed a remarkable record of human occupation extending from the present back to at least 4,000 B.C. The 114 beaches contained materials of the Denbigh Flint complex and of 11 other culture stages. Three of these were new, the Old Whaling culture, 1,000 years later than Denbigh, and Palisades I and II, 1,000 or more years older. The deep, stratified Onion Portage site on the middle Kobuk, discovered by Giddings in 1961, is without doubt the most important archaeological site within the Arctic. Covering some 20 acres and reaching a depth of 18 feet, it has over 30 distinct occupation levels containing in vertical sequence the hearths and artifacts of most of the cultures represented on the Krusenstern beaches, as well as others known heretofore only from undated, unstratified surface sites in the interior. Giddings has described his work at these and many other Arctic sites in more than 50 papers and monographs, the last of which, his monumental work, The Archeology of Cape Denbigh, was published by Brown University only a few months before his death. Louis Giddings is survived by his wife, the former Ruth Elizabeth Warner, and their three children, Louis Jr., Ann, and Russell. To those who cherished the friendship of this remarkably intelligent, vital and warm-hearted man, his untimely death still seems unreal. He will be sorely missed, but he has left his mark large and clear in that field of Arctic research in which he was the dominant figure.


Author(s):  
John E. Hobbie ◽  
Neil Bettez

The Arctic LTER site is located at 68º38'N and 149º43'W, at an elevation of 760 m in the northern foothills of the Brooks Range, Alaska. The location, 208 km south of Prudhoe Bay, was chosen for accessibility to the Dalton Highway, which extends along the Trans-Alaska Oil Pipeline from north of Fairbanks to Prudhoe Bay on the Arctic Ocean (figure 5.1). The rolling foothills at the site are covered with low tundra vegetation (Shaver et al. 1986a), which varies from heaths and lichens in dry sites to sedge tussocks on moist hillslopes to sedge wetlands in valley bottoms and along lakes. Riparian zones often have willow thickets up to 2 m in height. Small lakes are frequent; the best studied such lake is the 25-m-deep Toolik Lake (O’Brien 1992), the center of the LTER research site. Some 14 km from Toolik Lake, the Dalton Highway crosses the fourth-order Kuparuk River, the location of much of the LTER stream research (Peterson et al. 1993). Climate records at Toolik Lake have been kept since the early 1970s when a pipeline construction camp was established. On completion of the road in 1975, climate stations were set up by the U.S. Army Cold Regions Research Laboratory (CRREL, climate reported in Haugan 1982 and Haugen and Brown 1980). Since 1987, the LTER project has maintained climate stations at Toolik Lake (http:// ecosystems.mbl.edu/arc/) whereas the Water Resources Center of the University of Alaska has continuous records beginning in 1985 from nearby Imnavait Creek. An automatic station at Imnavait now reports every few hours to the Natural Resources Conservation Service–Alaska of the U.S. Dept. of Agriculture. The characteristics of the climate in northern Alaska are summarized by Zhang et al. (1996), who pointed out the strong influence of the ocean during both summer and winter months. They reported that the mean annual air temperature is coldest at the coast (–12.4ºC), where there are strong temperature inversions in the winter, and warmest in the foothills (–8.0ºC). At Toolik Lake, snow covers the ground for about eight months, and some 40% of the total precipitation of 250–350 mm falls as snow.


ARCTIC ◽  
1957 ◽  
Vol 10 (4) ◽  
pp. 230
Author(s):  
Robert F. Black

Deals with permafrost as the controlling influence on certain engineering projects as observed during field studies, 1945-1951. Its direct and indirect effects on transportation, surface and underground exploration, construction and durability of structures, water supply, sewage disposal, drilling for and production of oil and gas are considered, but no attempt is made to present an overall survey. "Overland transportation is hampered most in the spring breakup and fall freeze-up periods; excavation can be made only in summer in the active layer unless special methods are used. Bench marks can be set properly only in adequately drained backfill to 10 m. depth. Foundation excavations must be kept nearly dry; construction material for roads is lacking except locally. Steel landing mats and concrete can be used safely on gravel beaches for landing strips; small airstrips can be built on sand dunes with little grading and little danger of affecting the permafrost. A frozen runway of pycrete or icecrete utilizing turf and surface soil as the foundation and permafrost as a cold reserve in a heat exchanger is recommended for areas lacking suitable materials."--SIPRE.


1951 ◽  
Vol 17 (1Part1) ◽  
pp. 55-57 ◽  
Author(s):  
Ralph S. Solecki

Several significant pre-Eskimo finds related to early aboriginal occupations in North America were made north of the Arctic Circle during the 1950 season in Alaska. These discoveries were made within and just bordering the northern side of the Brooks Range mountain province. Two of the more important finds were made by Milton C. Lachenbruch and Robert J. Hackman of the U.S. Geological Survey. Another important find was made by Irving, a student at the University of Alaska (Giddings, 1950, p. 20). Lachenbruch's and Hackman's specimens were submitted to the writer for study and are described summarily in this paper. It is reported that Irving found lithic cultural remains similar to those found by Hackman not far from the latter's station near Anaktuvuk Pass.


2014 ◽  

Collection of abstracts from the sixth Annual Undergraduate Research Conference at the Interface of Biology and Mathematics. Plenary speakers: Joseph Tien, Associate Professor of Mathematics at The Ohio State University; and Jeremy Smith, Governor's Chair at the University of Tennessee and Director of the University of Tennessee/Oak Ridge National Lab Center for Molecular Biophysics.


ARCTIC ◽  
1957 ◽  
Vol 10 (4) ◽  
pp. 246 ◽  
Author(s):  
J. Keith Fraser

The Geographical Branch of the Department of Mines and Technical Surveys was created in 1947. Under its terms of references, part of its responsibility is the collection and analysis of geographical information on northern Canada, in particular the territories under the jurisdiction of the federal government. In the decade since the Branch's inauguration, geographers have carried out various kinds of field surveys in the Canadian Arctic and subarctic, from the northern coast of Ellesmere Island to the Hudson Bay coastal plain in Ontario, and from the Alaska boundary to Labrador. These surveys have varied from parties formed entirely of geographers to individual shipboard observers or representatives on collaborative teams of scientists. The collection of basic information on the vast unknown expanses of the Arctic is peculiarly suited to the application of geographic methods. Utilizing the trimetrogon and vertical photography carried out since World War II, geographers have applied sampling techniques in interpreting larger areas, making intensive field studies of representative terrain types and expanding them by use of the air photos in delimiting, describing and analysing physiographic regions. Studies in physical geography have been the backbone of the work of the Branch in the Arctic. Air photo interpretation keys have been prepared for 14 areas: Alert, Eureka, Mould Bay, Resolute, Mackenzie Delta, Darnley Bay, Coppermine, Bathurst Inlet, Boothia Isthmus, Wager Bay, Southampton Island, Kaniapiskau-Koksoak Rivers in Ungava, the Hudson Bay Railway, and the Kenogami River. Reports on the human geography of various areas were included in the field reports and are mainly unpublished; several studies in historical geography also resulted from the field surveys. ...


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