In 1953–55 the Canadian government experimentally relocated Inuit (Eskimo) families from the region of Port Harrison (Inukjuak), on Quebec's Ungava peninsula, to Ellesmere and Cornwallis Islands in the Arctic Archipelago. Today Inuit relocatees allege that they were deceived by the government and suffered greatly as a result of the experiment. The government asserts that the relocation was undertaken for humanitarian reasons. The controversy has recently resulted in hearings before a Canadian parliamentary committee on aboriginal affairs and the Human Rights Commission. A study of the relocation issue prepared for the government, known as the ‘Hickling Report’, rejects Inuit claims of mistreatment. In this paper the Hickling report's findings are assessed. Contrary to the report's conclusions, documentation suggests that one of the government's motives for undertaking the relocation pertained to Canadian sovereignty and exercising ‘effective occupation’ of the islands.

In summer 1990 a Soviet-Norwegian expedition spent three weeks travelling to and around Zemlya Frantsa-Iosifa (Franz Joseph Land). The main purpose of the expedition was to locate the remains of Fridtjof Nansen and Hjalmar Johansen's wintering quarters of 1895–96, and other historical sites at Cape Flora, Eira Harbour, Camp Ziegler, Buchta Tichaja and Teplitz Bay were also visited. The group experienced an amazing openness in this area which has been closed to visitors since 1930. The historical sites and their present condition are described.

Alaska's North Slope Borough, established in 1972, is a unique institution of Native-controlled local government in the north. Providing a case study of Native self-determination under favourable conditions of indigenous, local control of resource wealth and political power, it has been the instrument by which local Inupiat capturedand used oil wealth, with clear economic and political benefits. They have gained high levels of local public services, jobs, and incomes; and effective representation in negotiations with external corporate and government authorities; the borough has also preserved and adapted critical elements of traditional culture. Costs of development and changeunder borough leadership have included waste and inefficiency, crime and corruption. Centralized power in borough headquarters has reduced the independence of borough villages and encouraged borough citizens to act like clients and consumers. Borough economy remains dependent on uncertain tax revenues from oil, with uncertain future employment opportunities for a rapidly growing Native population. North Slope Borough government has provided the Inupiat with means to greater political self-sufficiency, and the borough has responded effectively, under great pressure, to the opportunities and problems that petroleum development has brought to the region.

This paper proposes management responses to problems perceived in an earlier paper on King George Island (Polar Record 27(162): 193–204, 1991). Available management instruments and barriers to solutions are reviewed, and new management approaches and tools postulated. The category of Antarctic Protected Area (APA) is proposed for areas needing special protection, with sub-designations of Natural, Scientific and Historic Reserves. Multiple-use Planning Areas (MPAs) are endorsed for areas of high use needing local and regional planning, including station environs, but with sub-designations Environmentally Sensitive Areas, Scientific Research Sites and Facilities Areas. Both APAs and MPAs will require management plans: APAs will be accessible only by entry permit. Also recommended are a scientific and logistic register, scheduled meetings among station commanders, development of an internationally coordinated regional scientific strategy, and an environmental information system. To manage tourism a commercial tourism licence system and tourist levy are recommended, with the industry controlled under management plans developed for APAs and MPAs, plus general Treaty provisions. Workload arising from these revisions would necessitate the Committee on Environmental Protection in the forthcoming Protocol on Environmental Protection to the Antarctic Treaty, with a permanent Treaty secretariat. This framework, requiring a multinational approach to management more sophisticated than has so far been achieved under the Antarctic Treaty, would improve and coordinate management throughout Antarctica.

Scientific cooperation in the Arctic has gained momentum during the last two years. The changing attitude of the Soviet Union, the most advanced Arctic state in this respect, has played a crucial role in this evolution. This article, which focusses on non-Soviet research efforts in Soviet Arctic waters, concludes that the Soviet Union has lately given a clear signal by allowing foreigners, after many years of repeated refusal, to conduct marine scientific research close to its own coasts. In doing so the Soviets have further clarified the legal status of their northern waters.

Seals were hunted in the Bay of Bothnia during the 16th century in four areas — inshore open water, fast ice, ice edge, and pack ice — with methods appropriate for each area. Inshore open water sealing involved netting and some seining, exclusively for ringed seals. On fast ice the techniques used were stalking, den-hunting, and breathing hole-hunting, again for ringed seals. Grey and ringed seals were hunted on the ice edge. Provincial tax returns have provided information on methods used by sealers from different parishes in the Bay of Bothnia area. Catching techniques, tools, prey species, numbers of crews, hunting seasons, catch figures and annual yields are discussed.

The East Antarctica ice sheet advanced onto the continental shelf during the last glaciation but appears to have been thinner (<300 m) than previously hypothesised and probably did not everywhere extend to the edge of the continental shelf. Where the shelf is wide, the ice probably terminated against shallow banks on its outer edge. There may not have been time for the sheet to develop the maximum profile form and thickness predicted by Hollin (1962) and Hughes and others (1981) of about 1000–500 moverthe shelf. Large outlet glaciers occupied deep troughs that conveyed most of the ice towards the edge of the shelf: intervening areas were less intensely glaciated. Much of Prince Charles Mountains and Amery Oasis were not ice-covered: Vestfold, Bunger and Casey oases were glaciated. Vestfold and Bunger oases became ice-free after 10 ka BP under the influence of the Holocene marine transgression, which was complete by about 6 ka BP. During at least the last 5–6 ka these oases have been approximately their present size. Since then the margins of the Antarctic continental ice sheet have maintained almost steady state conditions against the landward edges of the hill masses.