THE EMERGING GEOGRAPHIES OF VIRTUAL WORLDS*

ABSTRACT. The technology of virtual reality is producing new virtual worlds. These worlds are being created and utilized for a number of different purposes. Four main themes and application areas of virtual reality are: the arts and literature, the military, the preservation of aspects of reality, and finance or business. The technology of virtual reality is examined in these themes, and the differences as well as linkages between them are explored. The growing importance of virtual worlds as a topic of geographical analysis is discussed.     

A sedimentological model for the continental Upper Triassic Tadrart Ouadou Sandstone Member: recording an interplay of climate and tectonics (Argana Valley; South‐west Morocco)

The continental Upper Triassic Tadrart Ouadou Sandstone Member was deposited in an extensional setting on the Pangaean continent, strongly influenced by a low‐latitude climatic regime (10° to 20° north). Complex interaction of basin subsidence and climatically driven processes led to high facies variability and a lack of correlatable units across the Argana Valley exposures. A process‐orientated approach integrating detailed facies with architectural element analysis was undertaken, which resulted in a multistage depositional model for the Tadrart Ouadou Sandstone Member. The basin‐scale model shows that basal alluvial fan and braided river systems are confined to the centre of the Argana Valley exposures. Aeolian deposits occur throughout the sequence, but dominate in the north. After a phase of playa deposition, prominent basin‐wide fluvial incision of up to 8 m marks the onset of perennial fluvial flow. These well‐sorted, internally complex and locally highly amalgamated fluvial sandstones are widespread throughout the basin and are focused in a north to south (south‐west) flowing channel system. After a final stage of aeolian sedimentation, sandstone deposition of the Tadrart Ouadou Sandstone Member in the Argana Valley is terminated rapidly by the onlap of lacustrine mudstones of the Sidi Mansour Member. The study revealed that, except for one pronounced period of perennial conditions, sedimentation is controlled largely by ephemeral fluvial flow, alternating ground water tables, deflation processes and periods with limited periodic local run‐off. The study highlights that facies architecture in the basin is the result of complex interaction of local syn‐sedimentary tectonics and the climatic regime within the basin, but also the climate of the catchment area to the east. The data suggest a proximal to mid‐distal basin setting in the rain‐shadow to the west of a mountain range (Massif Ancien), which exerted a strong control on the depositional environments of Triassic deposits exposed in this part of South‐west Morocco.     

Competition and co-operation in the semi-periphery: closer economic partnership and sectoral transformations in Chile and New Zealand

The signing of a strategic economic partnership (the Trans-Pacific SEP or P4) between Chile, New Zealand, Singapore and Brunei Darussalam in 2005 reveals the emergence of a new generation of trade agreements that seek to promote longer-term synergies and cooperation. This is in marked contrast with a purely competitive, market-based model of agreements whereby economies are opened up to oligopsonistic capital. The orientation is clearly more neostructural and strategic in construction, emphasizing the opportunities within the global economy of improved relations with similarly positioned economies within the semi-periphery. This article analyses both the basis for and implications of the P4 for Chile and New Zealand by looking at three sectors in which both countries are competitive in export markets: dairy, wine and fisheries. By assessing similarities and differences, and the ways in which competition or co-operation might be established, the potential impacts of the agreement can be posited. Within a global context of bilateral and multilateral commercial agreements, it is this type of agreement that perhaps best fits the needs of smaller economies in the periphery that seek to establish greater competitive space for their exports in core economies without engaging in a mutually destructive war of competition in similar sectors and products.     

REVISITING THE TOPIA ROAD: WALKING IN THE FOOTSTEPS OF WEST AND PARSONS*

ABSTRACT. In 1940, Berkeley graduate‐student geographers Robert West and James Parsons traveled to Mexico's Sierra Madre Occidental to retrace the Topia Road, colonial Mexico's main trans‐Sierran trail linking isolated mountain mining hamlets with the Pacific Coast and the world beyond, a journey chronicled in a 1941 Geographical Review article. Almost sixty years later, we document an attempt to retrace West and Parsons's route. Based on field observations, interviews with local informants, replication of Parsons's photographs, and his field notes, we evaluate landscape alteration in what West and Parsons referred to as some of the most isolated settlements in Mexico. We assess changes in the still‐remote communities along the route in terms of three influences: mining, migration, and drug trafficking.     

Internal structure of aeolian dunes in Abu Dhabi determined using ground-penetrating radar

A ground-penetrating radar survey of aeolian dunes in the Al Liwa area of Abu Dhabi reveals a variety of dipping reflectors which are interpreted as primary sedimentary structures. The interpretation of the radar profiles has been confirmed by bulldozing trenches through the study area and comparing logged sections in the trenches with the radar profiles. NNW— SSE-orientated radar profiles, approximately parallel to the prevailing wind direction, show two sets of dipping reflectors which are interpreted as sets of cross-stratification and second- and third-order bounding surfaces. Radar profiles orientated WSW—ENE across the prevailing wind direction are dominated by concave-up reflectors which are interpreted as trough-shaped scours and sets of trough cross-stratification produced by oblique progradation of barchanoid dunes. Nested troughs, with small sets of trough cross-stratification within larger troughs, may be due to reactivation following wind reversal, or the superposition of small dunes on larger dunes and the fill of large dune troughs by smaller dunes. Convex-upwards reflectors are interpreted as linear spurs on the convex portions of sinuous dunes or erosional remnants between troughs. Overall there is a tendency for the larger second-order bounding surfaces to dip downwind, which confirms Brookfield's ideas of the relative migration paths of dunes and draa.     

A seasonally ''dry'' interglacial climate in eastern England during the early Middle Pleistocene: palaeopedological and stable isotopic evidence from Pakefield, UK

The pedology and the isotope geochemistry of the early Middle Pleistocene interglacial 'rootlet bed' at Pakefield, eastern England, record the climate when this unit accumulated. Horizons of nodular pedogenic calcrete indicate the existence of a strongly seasonal precipitation regime that produced a pronounced net soil moisture deficit during which secondary carbonate was precipitated. The isotopic composition of these nodules confirms the seasonality of annual precipitation, as this indicates that intense soil moisture evaporation was a major mechanism in secondary carbonate formation. The climatic interpretation is enhanced by the palaeoecology of the unit that indicates average summer temperatures significantly warmer than those of the present. The climate of this period was, therefore, different from that of the present day in terms of both temperature and the seasonality of precipitation. Although it has previously been shown that certain interglacial periods in northwest Europe were warmer than the Holocene, this is the first study to show that the precipitation regime of one such episode may also have been significantly different.