On country: Identity, place and digital place

2021 ◽  
Vol 11 (1) ◽  
pp. 111-123
Author(s):  
Kit Devine

Place is central to the identity of Aboriginal and Torres Strait Islander peoples. The Narrabeen Camp Project explores the use of immersive technologies to offer opportunities to engage with Indigenous histories, Storytelling and cultural heritage in ways that privilege place. While nothing can replace being ‘on Country’, the XR technologies of AR and VR support different modalities of engagement with real, and virtual, place. The project documents the Stories, Language and Lore associated with the Gai-mariagal clan and, in particular, with the Aboriginal Camp that existed on the north-western shore of Narrabeen Lakes from the end of the last ice age to 1959 when it was demolished to make way for the Sydney Academy of Sports and Recreation. The project will investigate evolving Aboriginal Storytelling dynamics when using immersive digital media to teach culture and to document a historically important site that existed for thousands of years prior to its demolition in the mid-twentieth century. It expects to generate new knowledge about Aboriginal Storytelling and about the history of urban Aboriginals. Expected outcomes include a schema connecting Aboriginal Storytelling with immersive digital technologies, and truth-telling that advances understanding of modern Australia and urban Aboriginal people. The research should promote better mental, social and emotional health and wellbeing for Indigenous Australians and benefit all Australians culturally, socially and economically.

2001 ◽  
Vol 38 (8) ◽  
pp. 1141-1155 ◽  
Author(s):  
G D Osborn ◽  
B J Robinson ◽  
B H Luckman

The Holocene and late glacial history of fluctuations of Stutfield Glacier are reconstructed using moraine stratigraphy, tephrochronology, and dendroglaciology. Stratigraphic sections in the lateral moraines contain tills from at least three glacier advances separated by volcanic tephras and paleosols. The oldest, pre-Mazama till is correlated with the Crowfoot Advance (dated elsewhere to be Younger Dryas equivalent). A Neoglacial till is found between the Mazama tephra and a paleosol developed on the Bridge River tephra. A log dating 2400 BP from the upper part of this till indicates that this glacier advance, correlated with the Peyto Advance, culminated shortly before deposition of the Bridge River tephra. Radiocarbon and tree-ring dates from overridden trees exposed in moraine sections indicate that the initial Cavell (Little Ice Age (LIA)) Advance overrode this paleosol and trees after A.D. 1271. Three subsequent phases of the Cavell Advance were dated by dendrochronology. The maximum glacier extent occurred in the mid-18th century, predating 1743 on the southern lateral, although ice still occupied and tilted a tree on the north lateral in 1758. Subsequent glacier advances occurred ca. 1800–1816 and in the late 19th century. The relative extent of the LIA advances at Stutfield differs from that of other major eastward flowing outlets of the Columbia Icefield, which have maxima in the mid–late 19th century. This is the first study from the Canadian Rockies to demonstrate that the large, morphologically simple, lateral moraines defining the LIA glacier limits are actually composite features, built up progressively (but discontinuously) over the Holocene and contain evidence of multiple Holocene- and Crowfoot-age glacier advances.


2005 ◽  
Vol 11 (1) ◽  
pp. 17 ◽  
Author(s):  
Charlotte de Crespigny ◽  
Inge Kowanko ◽  
Helen Murray ◽  
Carolyn Emden ◽  
Scott Wilson

This paper provides an overview of a major South Australian research project with implications for the health of all Indigenous Australians. The researchers set out to explore the medication needs of Aboriginal people with mental health problems and found that most Aboriginal people have to deal with profound challenges to social and emotional wellbeing with significant medication implications. No previous research had investigated the problem of medication use by Aboriginal people in metropolitan, rural and remote locations to the depth and extent of this project. The research therefore is of widespread relevance and holds interest for many Indigenous and non-Indigenous individuals and groups, consumers, service providers and policy-makers. As a research team comprising Indigenous and non-Indigenous members, we were committed to implementing strategies in the course of the project with immediate benefit to project participants as well as longer-term impact on improved use of medications. The design of the project enabled these strategic interventions and we are pleased to promote this model to other researchers. Recommendations from the project concern services, coordination of care, carers and family members, workforce education, and community development. Readers are advised where the project report and other published papers can be accessed. The project was funded by the Commonwealth Department of Health and Ageing.


Author(s):  
Heidi Norman ◽  
Therese Apolonio ◽  
Maeve Parker

With reference to four case study localities in New South Wales, this paper offers new insights into calls from Indigenous Australians for recognition within the national political discourse. Examining the literature on the history of the Aboriginal sector that emerged following the 1970s self-determination policy era, this paper argues earlier conceptions of the ‘Aboriginal sector’ are insufficient and do not grasp the wider shift that Aboriginal people seek within the political life of the nation. Instead, the four case studies reveal Aboriginal initiative and interest in creating a sense of association and being, drawing on pre-colonial patterns of identification and shaped by new imaginings of ‘nations’ and ‘political communities’.


Author(s):  
Andrew T. Chamberlain

The aim of this chapter is to situate the unique discoveries of cave art at the Creswell Crags caves in the context of what is known of the cave archaeology and palaeontology of the caves of the southern Magnesian Limestone outcrop. The long history of archaeological research at Creswell Crags and the spectacular discoveries that continue to be made in the Creswell caves have tended to overshadow the widespread though less prominent distribution of cave archaeological sites along the limestone outcrop to the north and south of Creswell, a region known as the Creswell Crags Limestone Heritage Area (Mills 2001). Recent audits of the archaeology of the region have drawn attention to the large number of cave sites within the Limestone Heritage Area as well as the considerable potential that these sites have for further research into the history of Ice Age people and their environments (Mills 2001; Davies et al. 2004).While the focus of this chapter is on the Pleistocene deposits and Palaeolithic artefacts that have been preserved in the region’s caves, fissures, and rock shelters, these sites were used throughout prehistory by humans and animals and they contain much important cultural and environmental evidence for these later time periods after the end of the last Ice Age. Creswell Crags is located in the southern part of the Magnesian Limestone, a geological term for deposits of Upper Permian age that includes a series of formations of well-bedded oolitic to dolomitic limestones. The Magnesian Limestone forms a narrow north–south oriented outcrop that runs from near Nottingham in the south to the North Sea coast near Tynemouth in the north (Fig. 6.1). About 30 km to the west of the southern part of the Magnesian Limestone is the older Carboniferous Limestone outcrop of the White Peak, which, like the Magnesian Limestone, contains many archaeological caves. The southern part of the Magnesian Limestone outcrop, between Doncaster and Mansfield, is cut through by a series of vales and gorges which expose caves, fissures, and rockshelters along the cliff lines.


1936 ◽  
Vol 2 (1-2) ◽  
pp. 169-177 ◽  
Author(s):  
Philip Ullyott

Sometime after the last retreat of the ice in the Quaternary ice age, the Scandinavian peninsula was separated on the south from the north German plain and Denmark. Later, England was cut off by the Channel from the continental land mass. An estimation of the times at which these two events happened is interesting to archaeologists, botanists and zoologists alike, because the communities with which they are concerned are affected by the barrier of an intervening arm of the sea.So far most of the evidence about the times of separation comes from botanical and archaeological sources, from pollen analysis and the investigation of cultural sites. In this paper the distribution and physiology of certain freshwater animals are used to provide argument that the separation of Scandinavia and of England could only have taken place at times of particular climatic conditions. The climatic definition of the times of separation makes it possible to fit them in to the absolute geochronological scale which has been established by Scandinavian workers.


1969 ◽  
Vol 31 ◽  
pp. 43-46
Author(s):  
Ole Bennike ◽  
Jørgen O. Jørgen O. Leth ◽  
Jørn Bo Jensen ◽  
Niels Nørgaard-Pedersen ◽  
Steen Lomholt

The North Sea is a large, shallow epicontinental sea dominated by a sandy bottom that reflects a high-energy environment. Little is known about the environmental history of the Danish part of this large area during the Weichselian, the last ice age. Parts of it were glaciated during the last glacial maximum and probably also during older glaciations. Shallow parts were dry land, and deeper parts were covered by the sea during ice-free intervals. Large, partly ice-dammed lakes also existed.


The first book to address the vast diversity of Northern circumpolar cinemas from a transnational perspective, Films on Ice: Cinemas of the Arctic presents the region as one of great and previously overlooked cinematic diversity. With chapters on polar explorer films, silent cinema, documentaries, ethnographic and indigenous film, gender and ecology, as well as Hollywood and the USSR’s uses and abuses of the Arctic, this book provides a groundbreaking account of Arctic cinemas from 1898 to the present. Challenging dominant notions of the region in popular and political culture, it demonstrates how moving images (cinema, television, activist and art video, and digital media) have been central to the very definition of the Arctic since the end of the nineteenth century. Bringing together an international array of European, Russian, Nordic, and North American scholars, Films on Ice radically alters stereotypical views of the Arctic region, and therefore of film history itself. Areas covered in the book include: 1) Global Indigeneity; 2) Hollywood hegemony; 3) Ethnography and documentary Dilemmas; and 4) Myths and Modes of Exploration. Key Arctic films from the history of cinema are addressed (from Nanook of the North to Atanarjuat: The Fast Runner), along with little-known works that re-shape our understanding of moving images in the global circumpolar Arctic.


2013 ◽  
Vol 16 ◽  
pp. 165 ◽  
Author(s):  
Mick Morrison

<p>Recent research on shell mounds near Weipa (northeast Australia) has focussed on economic questions, particularly understanding what these sites reveal about the production strategies of Aboriginal people and possible links to broader social and environmental transformations documented in late Holocene northeastern Australia. However, in order to explore such issues it is necessary to acquire a firm understanding of mound development through reference to detailed stratigraphic, chronological and compositional data. This paper presents results of investigations into the developmental history of a range of shell matrix sites including shell scatters, non-mounded middens and mounds that occur at Bweening, to the north of Weipa. It is argued that the early stages of mound formation involved multiple small-scale (1–2m diameter) discard events in ‘clusters’ within close proximity to one another, coalescing through time to form low dome-shaped mounds. However, site development is characterised by a high degree of spatial variability in terms of where discard activities were focussed, and appears to shift in response to quite localised factors.</p>


2009 ◽  
Vol 72 (1) ◽  
pp. 47-56 ◽  
Author(s):  
J. Curt Stager ◽  
Christine Cocquyt ◽  
Raymonde Bonnefille ◽  
Constanze Weyhenmeyer ◽  
Nicole Bowerman

AbstractA nearshore core (LT03-05) from the north basin of Lake Tanganyika provides diatom, pollen, and sedimentary time series covering the last ca. 3800 yr at 15–36 yr resolution. A chronology supported by 21 AMS dates on terrestrial and lacustrine materials allows us to account for ancient carbon effects on 14C ages and to propose refinements of the region's climatic history. Conditions drier than those of today were followed after ca. 3.30 ka by an overall wetting trend. Several century-scale climate variations were superimposed upon that trend, with exceptionally rainy conditions occurring 1.70–1.40 ka, 1.15–0.90 ka, 0.70–0.55 ka, and 0.35–0.20 ka. Around 0.55–0.35 ka, during the Spörer sunspot minimum, drier conditions developed in the northern Tanganyika basin while more humid conditions were registered at Lakes Victoria and Naivasha. This indicates significant variability in the nature and distribution of near-equatorial rainfall anomalies during much of the Little Ice Age.


2008 ◽  
Vol 15 ◽  
Author(s):  
Peter Read

Aborigines and other Australians have not met with amity. Memorials to the Aboriginal people of Australia are not common and some of the more prominent are regularly damaged. Eddies of past tempests slap disturbingly at modern day memorials thousands of kilometres and several generations removed from the eye of furious storms. This article traces a difficult story of what seems at first sight to be blind racism, at a second sight, a rampant colonialism, and at a more reflective third, perhaps, the economy of the pastoralist and the farmer in deadly disharmony to that of the hunter gatherer. Whatever the origins, the consequences of conflict endure for centuries.


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