‘Partially provided’: geography at the University of Toronto, 1844–1935

In universities, as in everyday life, there is a fundamental need for geographical knowledge, even when no formal departments exist to provide instruction. This need was true in the University of Toronto during the decades before Griffith Taylor was appointed in 1935 to the first university Chair in geography in English‐speaking Canada. Using matriculation and annual university course examinations, university calendars and the papers of President Falconer and Professors James Mavor and Harold Innis, I trace the development of geography at the University of Toronto from the mid‐nineteenth century to the arrival of Taylor. Courses taught in selected aspects of physical and human geography in the Departments of Geology, Political Economy and History are particularly significant. Underlying this instruction, and also the desire to establish a geography department, was an acute awareness of the fundamental importance of geography to help understand a large regionally complex homeland, and a wider world.     

Reviews of books

EUROPE

Walks Around Peebles. By A. E. Maylard. Peebles: J. Kerr and Co., 1935. Price 1s.

Géographie Universelle. Vol. VII. Part II.: Italie, Pays Balkaniques. By J. Sion and Y. Chataigneau. Librairie Armand Colin.

ASIA

A Geographical Analysis of the Khairpur State: A Post‐Barrage Investigation. By M. B. Pithawalla. Karachi, 1935.

Nanga Parbat Adventure. By Fritz Bechtold. Translated by H. E. G. Tyndale. London: John Murray, 1935. Price 10s. 6d.

Extreme‐Orient et Pacifique. By Roger Lévy. Paris: Librairie Armand Colin, 1935. Price 10 fr. 50.

Sumatra. By E. Loeb and R. Heine‐Geldern. Vienna: Verlag die Instituts für Volkerkunde der Universität Wien, 1935.

AFRICA

The Folklore of Morocco. By F. Legey. Translated by L. Hotz. London: George Allen and Unwin Ltd., 1935. Price 12s. 6d.

Abessinien. Raum ab Schicksal. By G. Hermann. Leipzig: B. G. Teubner, 1935. Price Rm. 0.80.

AMERICA

Geografia Universale Illustrata. Vol. VI. America Settentrionale e Centrale. By C. Errera and R. Riccardi. Turin: Unione Tipografico‐Editrice Torinese, 1934.

The Human Geography of the South. By R. B. Vance. University of North Carolina Press, 1932.

GENERAL

Man and the Sea. By J. Holland Rose. Cambridge: W. Heffer and Sons Ltd., 1935. Price 10s. 6d.

Vergleichende Länderkunde. By A. Hettner. Vol. I., 1933; Vol. II., 1934. Leipzig and Berlin: B. G. Teubner.     

British Diplomacy,Propaganda, and War Strategy and the Hungarian-Romanian Dispute over Transylvania in 1939–40

Abstract

Between 1914 and 1935, the cities of Vienna and Pressburg/Bratislava were linked by an electric railway known as the Pressburgerbahn. More than just a line of transportation, the railway became intertwined with the complex politics of identity in Pressburg. The Pressburgerbahn presented nationalists in the Habsburg Empire with a dilemma: it had the potential to contribute to the unification of the nation, but at the same time was transnational by definition. This paradox generated a heated controversy about the Pressburgerbahn between Magyar nationalists and the predominantly German-speaking Pressburg bourgeoisie. Using biologized rhetoric, Hungarian politicians and journalists portrayed their nation as a body politic that was disfigured by having a railway ‘vein’ cross the border into Austria, in particular from such a peripheral location as Pressburg. By contrast, the discourse of the German-speaking bourgeoisie was firmly anchored in an imperial, supra-ethnic landscape. This controversy was replayed following the incorporation of the renamed city of Bratislava into Czechoslovakia in 1919: the Prague-based Ministry of Railways employed the rhetoric of the railway as an integrating structure within the body politic, while the eventual closure of the Pressburgerbahn in 1935 was closely connected to the belated nationalization of Bratislava. The railway to Vienna thus became a symbol of the liminal status of the town as a whole, in terms of nation, geography, politics and culture.     

Visualisierungen in der deutschen Geographie des 19. Jahrhunderts. Die Beispiele Robert Schlagintweit und Hans Meyer

Visualization in 19^th‐century German geography: Robert Schlagintweit and Hans Meyer as examples. – Visual representations of nature formed an essential part of 19^th‐century earth sciences. In particular, colonial photography – as a visual source, and as an instrument of the construction of national identities – serves essential research interests of current history and social sciences. The present paper is a case study on the role and function of photography in German geography of the 19^th and early 20^th centuries. It focuses on the work of the Munich geographer Robert Schlagintweit (1833–1885) and the Leipzig colonial geographer Hans Meyer (1858–1929); the early history of photography in India and the function of images in the geographical exploration of overseas territories are discussed. Although there is nearly half a century between the work of R. Schlagintweit and H. Meyer, their photography shows remarkable parallels. The ideas of both on the practice of visualization are rooted in pedagogic and didactic concepts as well as in popular science. For both geographers photography was essentially a technical help, which often needed graphic revisions. And they both preferred photography to depict people and buildings (compared, for instance, to landscapes). Concerning the more comprehensive question of how far their photography transmitted a specific German ‘image of abroad’, it is indicated that such a specific image should have its essential roots in a peculiar visual culture of German earth sciences in the first half of the 19^th century. Thus the paper offers a starting point for further studies discussing the change from a ‘Biedermeier image’ of foreign cultures to a more ‘colonial’ one in 19^th‐century German geography.     

Time–geography,gentlemen, please: chronotopes of publand in Patrick Hamilton’s London trilogy

This paper considers the time and the place of drinking in modern British life, as represented in Patrick Hamilton’s trilogy of novels set in the publand of London’s West End in the interwar years, through Mikhail Bakhtin’s concept of the chronotope and with critical nods to Hagerstrand’s time–geography corpus. The chronotopes of pubs and their neighbourhoods, which we term ‘publand’, are discussed initially in their novelistic presentation in Twenty Thousand Streets Under the Sky (1935), and then in relation to the ‘character zones’ of the novels’ principal protagonists. The key themes, defined in the paper, are the asynchronicity of personal and social relations, the dialogic construction of heterochronicity, and the presentation of a prosaic chronotope. Though the paper is a contribution to literary geography, we aim to contribute to the cultural geographic understanding of the time–space rhythms and routines of everyday leisure drinking, making claims for the wider significance of chronotopic analysis.     

Iron mineralization and dolomitization in the Paran Fault zone,Israel: implications for low‐temperature basinal fluid processes near the Dead Sea Transform

Petrography, Eh‐pH calculations and the stable isotope composition of oxygen are used to interpret geochemical processes that occurred during iron oxide mineralization and dolomitization along the Menuha Ridge segment of the Paran Fault, southern Israel, adjacent to the Dead Sea Transform (DST). Iron mineralization is strongly localized in the fault zone as ferruginous lenses, whereas Fe dolomitization spreads laterally into the Cenomanian‐Turonian carbonate host rock as stratabound beds. The average oxygen isotope fractionation between syngenetic quartz and iron oxides in the ferruginous lenses gives a temperature of 50 ± 10°C and δ¹⁸O SMOW water = ?3.5‰; consistent with an origin from metalliferous groundwater flow in the sedimentary basin. Ferroan dolomite initially formed under strongly reducing conditions, but this was followed by oxidation and pseudomorphic replacement of the dolomite by a mesh of fine‐grained iron oxides (simple zoned dolomites). This cycle of ferroan dolomite formation and replacement by iron oxides was repeated in complex zoned dolomites. Dolomite oxygen isotope compositions fall into two groups: a high δ¹⁸O group corresponding to the simple zoned dolomites and non‐ferroan dolomites and a low δ¹⁸O group corresponding to the complex zoned dolomites. Water‐rock calculations suggest that the epignetic dolomites formed under fluid‐buffered conditions: the high δ¹⁸O group are indicated to have formed at temperatures of ca. 25°C for waters with δ¹⁸O = ?4 to 0‰; the low δ¹⁸O complex zoned dolomites at 50–75°C for waters with the same isotopic composition. A kinetic calculation for a complex zoned dolomite‐bearing bed indicates that dolomitization must have occurred at high values of the dolomite saturation index. This requirement for high Mg supersaturation and the indication that epigenetic dolomitization is more protracted in stratigraphically deeper formations located closer to the DST is consistent with models proposing that Mg‐rich solutions originated in the Dead Sea Rift.     

Geography's secret powers to save the world

The purpose of this paper, prepared to present at the 2018 joint Canadian Association of Geographers (CAG) and International Geographical Union (IGU) regional conference, is to suggest three strategies, framed as proposals, that geography and geography education can deploy to “save the world.” The first proposal is to expand explicit instruction in spatial thinking to close gender‐based achievement gaps. The second proposal is to apply research from the learning sciences to develop persuasive geography curricula and instructional materials. The third proposal focuses on ways social media and geospatial technologies can be employed in civic education, an idea termed “spatial citizenship.” The paper suggests a re‐envisioning of geography education with an enhanced focus on teaching for, in, and about a world that fully appreciates difference and acts on that appreciation.     

New and past geochemical data on fresh to brine waters of the Salar de Atacama and Andean Altiplano,northern Chile

The paper deals with the major chemistry and stable isotopes (hydrogen, oxygen, carbon, sulfur, strontium) of waters and solutes from the Salar de Atacama basin (Rio Pedro, Honar Creek and Laguna Chaxa) and Andean Altiplano (Laguna Miñique and Laguna Miscanti). The water inflows of the Salar are chemically quite different, the Rio San Pedro being of Na‐Cl type and the Honar Creek of Na‐HCO₃ type, in keeping with the sedimentary‐evaporitic and volcanic nature of the catchment rocks respectively. The δ³⁴S and δ¹⁸O values of sulfate and the ⁸⁷Sr/⁸⁶Sr ratio of strontium in the streams match those of drained rocks, whereas the δ¹³C values of dissolved carbonate are largely controlled by vegetation. The lagoons are evaporated meteoric water bodies, and the relative air humidity estimated from the slope of the isotopic evaporation line is in accordance with historical data on air humidity in the area. The Laguna Chaxa is Na‐Cl rich, and its isotopic composition are consistent with a mixed sedimentary‐volcanic provenance of sulfur and strontium solutes. The Laguna Miñique is Na‐SO₄ rich, and its sulfate δ³⁴S is nearly identical to that of Laguna Chaxa. The δ¹³C(HCO₃) values are quite different in the Laguna Chaxa and Laguna Miñique, with the former being notably enriched in ¹³C probably because of preferential uptake of ¹²C by the high biological productivity occurring in the lagoon. The limited set of new data is interpreted in the context of a much larger literature database. In particular, previous chemical data on inflows and brines in the Salar de Atacama were revisited, and compared with evaporation path models and mineral stability diagrams (boron, lithium and Mg‐minerals) computed using updated software and thermodynamic databases. The modeling shows that the removal of boron and lithium from sulfate‐rich brines possibly occurs, respectively, as ulexite and sulfate salts, and carnallite should be the final magnesium phase of the brine evolution.     

Travelling down the road to postdisciplinarity? Reflections of a tourism geographer

Like many other forms of scholarship in geography, tourism geography has evolved as a distinct subfield of inquiry within the discipline, although the contributions of tourism geographers are perhaps more readily acknowledged in the multidisciplinary realm of tourism studies. I trace the evolving relationship of tourism geography to both the discipline of geography and to the field of tourism studies. In doing so, I reflect on such influences as the role of institutions, paradigm shifts, technology, and other factors that affect the creation and management of geographic knowledge in the twenty‐first century. The intent of this article is two‐fold: first, to appeal to geographers for greater recognition of the importance of tourism as a quintessential component of geographic study that in today's world warrants integration into core aspects of geographic enquiry; second, to use current debates within both tourism studies and geography to reflect on issues of disciplinarity, interdisciplinarity, transdisciplinarity, and even postdisciplinarity.     

International geography field courses: practices and challenges

Abstract

This paper introduces a special issue of the Journal of Geography in Higher Education on the practices and challenges associated with taking undergraduate geography students abroad on field courses. I argue that geography is positioned to benefit from both the internationalization of higher education and the demand by students for global experiences. The papers in this special issue focus on three aspects of international field courses: curriculum design and international partnerships, student engagement during short-duration field courses, and how encounters with place can be aided through reflection and play. I conclude with suggestions for future research on international field courses.     

On What's Right and Keeping Left: Or Why Geography Still Needs Marxian Political Economy

Recently the value of Marxian approaches to human geography has again been called into question in the pages of Antipode. In this paper I review the reasons as to why geographers re‐discovered Marx and then, from the late 1960s, began to engage with Marxian approaches. I then consider some of the reasons why Marxian approaches in their turn became the subject of critique in geography and some of the alternatives explored in the wake of this. The conclusion is that a pluri‐theoretical human geography is necessary but that Marxian approaches remain of central significance to radical and critically minded geographers.     

Chemical and isotopic signatures of Na/HCO3/CO2‐rich geofluids,North Portugal

Geochemical and isotopic studies have been undertaken to assess the origin of CO₂‐rich waters issuing in the northern part of Portugal. These solutions are hot (76°C) to cold (17°C) Na–HCO₃ mineral waters. The δ²H and δ¹⁸O signatures of the mineral waters reflect the influence of altitude on meteoric recharge. The lack of an ¹⁸O‐shift indicates there has been no high temperature water–rock interaction at depth, corroborating the results of several chemical geothermometers (reservoir temperature of about 120°C). The low ¹⁴C activity (up to 9.9 pmC) measured in some of the cold CO₂‐rich mineral waters (total dissolved inorganic carbon) is incompatible with the presence of ³H (from 1.7 to 4.1 TU) in those waters, which indicates relatively short subsurface circulation times. The δ¹³C values of CO₂ gas and dissolved inorganic carbon range between ?6‰ and ?1‰ versus Vienna‐Peedee Belemnite, indicating that the total carbon in the recharge waters is being diluted by larger quantities of CO₂ (¹⁴C‐free) introduced from deep‐seated (upper mantle) sources, masking the ¹⁴C‐dating values. The differences in the ⁸⁷Sr/⁸⁶Sr ratios of the studied thermal and mineral waters seem to be caused by water–rock interaction with different granitic rocks. Chlorine isotope signatures (?0.4‰ < δ³⁷Cl < +0.4‰ versus standard mean ocean chloride) indicate that Cl in these waters could be derived from mixing of a small amount of igneous Cl from leaching of granitic rocks.     

Cross‐Disciplinarity in Australian Geography Presidential Address to the Institute of Australian Geographers’ Conference,Melbourne, July 20071

The disciplinary space that geographers conceive to be theirs has all been previously possessed, or latterly colonised, by other disciplines. Geographers defend their existence on the basis of their oft‐asserted, but never tested, cross‐disciplinarity. The journals in which refereed papers were published by members of the Institute of Australian Geographers (IAG) and the papers in Australian Geographical Studies were analysed for the period 1998–2002 to test the hypothesis of cross‐disciplinarity in both subject and method. IAG members do strongly tend to publish in more than one disciplinary area, and a large proportion of papers in Australian Geographical Studies are integrative across subdisciplines in geography, with many using more than one methodological approach. However, transgression of the physical geography/human geography divide was sufficiently uncommon to create a statistical break between sets of subdisciplines. Based on the data used in the present paper, Australian geographers can make a case for being members of a vital, integrative discipline, likely to make substantial advances in the hybrid spaces.     

Geochemistry and origin of natural gases dissolved in brines from gas fields in southwest Japan

Previous geochemical studies indicated that most natural gases dissolved in brines in Japan are of microbial origin, consisting of methane produced via carbonate reduction. However, some of those from gas fields in southwest Japan contain methane relatively enriched in ¹³C, whose origin remains to be clarified. To address this issue, chemical and isotopic analyses were performed on natural gases and brines from the gas fields in Miyazaki and Shizuoka prefectures, southwest Japan. Methane isotopic signatures (δ¹³C ≈ ?68‰ to ?34‰ VPDB; δ²H ≈ ?183‰ to ?149‰ VSMOW) suggest that these gases are of microbial (formed via carbonate reduction) or of mixed microbial and thermogenic origin. The relatively high δ²H‐CH₄ values and their relationship with the δ²H‐H₂O values argue against the possibility of their formation via acetate fermentation. The δ¹³C‐CO₂ values (≈?5‰), together with the slope of the correlation between δ²H‐CH₄ and δ¹³C‐CH₄ (Δδ²H‐CH₄/Δδ¹³C‐CH₄ ≈ 1), contradict the possibility of their formation via carbonate reduction followed by partial oxidation by methanotrophs. The ³He/⁴He ratios of the gases from Miyazaki (≈0.11–1.3 Ra) and their low correlation with δ¹³C‐CH₄ values do not support an abiogenic origin. It is inferred therefore that the high δ¹³C‐CH₄ values of natural gases dissolved in brines from gas fields in southwest Japan are indications of the contribution of thermogenic hydrocarbons, although whether abiogenic hydrocarbons contribute significantly to the gases from Shizuoka requires further investigation. This study has clarified that, for the future exploration of natural gases in southwest Japan, we should adopt the strategies for conventional thermogenic gas accumulations, such as checking the content, type and maturity of organic matter in the underlying sedimentary rocks.     

Fluid circulation related to post‐Messinian extension,Thassos Island,North Aegean

In the North Aegean Domain, Thassos Island contains a Plio‐Pleistocene basin controlled by a large‐scale flat‐ramp extensional system with a potential décollement located at depth within a marble unit. Numerous mineralizations associated with normal faults of Plio‐Pleistocene age are the sign of fluid circulation during extension. Two main generations of fluid flow are recognized, related to Plio‐Pleistocene extension. A first circulation under high‐temperature conditions (about 100–200°C) resulted in dolomitization of marbles near the base of the Plio‐Pleistocene basin. The dolomites are characterized by low δ¹⁸O values (down to 11‰ versus Standard Mean Ocean Water). Some cataclastic deformation affected the dolomites. Hydrothermal quartz that crystallized in extension veins above a blind ramp also has low δ¹⁸O values (about 13‰). This shows that high‐temperature fluids moved up from the décollement level toward the surface. A second downward circulation of continental waters at near‐surface temperature is documented by calcite veins in fault zones and at the base of the Plio‐Pleistocene basin. These veins have O isotope values relatively constant at about 23–25‰ and C isotope values intermediate between the high δ¹³C value of the carbonate host rock (about 1–3‰ versus Peedee Belemnite) and the low δ¹³C value of soil‐derived carbon (?10‰). The calcites associated with the oxidative remobilization of primary sulphide Zn–Pb mineralization of Thassos carbonates have comparable O and C isotope compositions. Hot fluids, within the 100–200°C temperature range, have likely contributed to the weakening of the lower marble unit of Thassos and, thus, to the process of décollement.