WHY WAS HUMBOLDT FORGOTTEN IN THE UNITED STATES?*

ABSTRACT. In the nineteenth century Alexander von Humboldt was acclaimed as “the second Columbus” and “the scientific discoverer of America.” His prestige and fame were such that on 14 September 1869, the hundredth anniversary of his birth, a grand celebration was held with parades, speeches, concerts, and the unveiling of memorials in cities across the country. Humboldt's popularity in the United States endured for the remainder of the nineteenth century, but he dropped from public consciousness in the twentieth century. To account for the eclipse of Humboldt's fame in the United States three hypotheses are discussed: a shift in the character of scientific endeavor; the quality of Humboldt's written work; and the rise of anti‐German sentiment with a concurrent rush to “de‐Germanize” the United States in the early twentieth century.     

Man and Nature: George Perkins Marsh and Alexander Von Humboldt

George Perkins Marsh's book Man and Nature was the first work of natural history to fundamentally influence American politics. This paper establishes the powerful impact that Alexander von Humboldt's writings had on Marsh. Marsh took ideas that Humboldt introduced across his books and synthesized them into a single powerful argument regarding the dangers of deforestation. These warnings eventually led to policies that sought to more carefully manage forestland, plant trees, and spawn the 20^th century conservation movement.     

ALEXANDER VON HUMBOLDT'S IMAGE AND INFLUENCE IN NORTH AMERICAN GEOGRAPHY, 1804–2004

ABSTRACT. Alexander von Humboldt is universally identified as a key figure in laying the foundations for modern geography. His main sites of research and scholarly production were centered on Europe, Latin America, and Russia. He drew on global sources of geographical data and knowledge in constructing and producing his voluminous works. Although he only briefly knew North America firsthand—at the outset of his career, in the late spring of 1804—he maintained a lifelong interest in the realm, especially in the United States. In turn, many North American scholars were admirers and followers of his perspectives, practices, and publications. Although geography did not emerge as an institutionally based discipline in the United States until the late nineteenth century, Humboldt's influence and impact on its antecedents were considerable. Contrary to conventional wisdom, his authority and influence in geography persisted well beyond Humboldt's death in 1859. His vision of demonstrating nature's unity in diversity and his enlightened views on social issues have continued to appeal to select sectors and actors in North American geography, especially Latin Americanists, historians of the discipline, and, more recently, proponents of an engaged, critical geography.     

THE LAPWING IN ANDEAN ETHNOECOLOGY: PROXY FOR LANDSCAPE TRANSFORMATION*

The Andean lapwing (Vanellus resplendens Tschudi) prompts rethinking of ethnoecology in neotropical cloud forests and páramos and challenges notions about conservation in mountain protected areas. Using archaeological, historical, and current evidence, I argue that the role of humans in shaping viable high‐mountain bird populations is an important factor in the conservation priorities of tropandean landscapes, particularly in the mountains. The presence of the Andean lapwing demonstrates the intricate linkages between culture and nature in the Andean region. I highlight a paradox of conservation, using the Andean lapwing as the avian indicator of global environmental change as an example of the contest between landscape change, biodiversity, and ethnoecological insights. Landscape stewardship, conservation easements, and cultural landscapes are options for inclusion in the repertoire of scenarios for the survival of healthy avifaunal assemblages in high‐mountain environments that have evolved in synchrony with humans, such as in páramos, cultural landscapes worth protecting in the tropical Andes.     

HUMBOLDT AND THE HABITABILITY OF CANADA'S GREAT NORTHWEST*

ABSTRACT. Alexander von Humboldt's influence in British North America during the nineteenth century was filtered mainly through British imperial applications of “Humboldtian” sciences, including geomagnetism and biogeography. The best‐known examples include Edward Sabine and John Henry Lefroy, Royal Artillery officers who, during the 1830s and 1840s, transformed British North American outposts and territories, including Rupert's Land, into Humboldtian sites and regions in Great Britain's imperial “magnetic crusade.” Important groundwork had already been laid by John Richardson, who applied data accrued during John Franklin's overland Arctic expeditions during the 1820s to systematize Humboldtian inquiries into the habitability of Canada's Great Northwest. Despite both the relative decline of Humboldtian sciences by midcentury and Humboldt's own reservations about the political ramifications of his science, his “cosmic” outlook circulated in Canada to refine territorial expansionists' scientistic arguments justifying annexation of Rupert's Land after the monopoly of the Hudson's Bay Company expired in 1869.     

HUMBOLDT'S MEXICAN TEXTS AND LANDSCAPES*

ABSTRACT. While in New Spain from 1803 to 1804, Alexander von Humboldt interacted with some of its landscapes and the texts that represented them. Analysis of those interactions regarding the Basin of Mexico and the Gulf lowlands demonstrates what purely text‐based studies of the production of places cannot: The contrasting landscape elements and patterns that had emerged over millennia during precolonial times in those two places, their relative degrees of depopulation during the colonial era, and the relative degrees of rigor Humboldt applied to interacting with the resulting landscapes and the texts that represented them greatly affected his representations of those places in his 1811 Essai politique sur le royaume de la Nouvelle‐Espagne. His representations of the precolonial Basin of Mexico as productively developed and of the precolonial Gulf lowlands as pristine have influenced the transformations of those places in the two centuries after New Spain became the Mexican republic through its wars of independence (1810–1821).     

The Legacy of Jedidiah Morse in Early American Geography Education: Forgotten and/or Forgettable Geographer?

Despite numerous and significant writings by historians of geography and biographers from other disciplines, and his authorship of the first geography textbooks written in and for the new American republic, most geographers are largely unaware of the contributions of Jedidiah Morse in academic geography. Writings about Morse suggest that he had alienated himself from many of his contemporaries early in his career through his authoritarian brand of Calvinistic republicanism, a perceived contradiction of that style with his entrepreneurial ambitions, his role in the controversial Bavarian Illuminati, and a dispute with a noted New England historian. But subsequent, broader intellectual movements sealed Morse's fate as a forgotten geographer (to most), including the end of the Second Great Awakening, Transcendentalism, Darwinism, and the “new,” process‐based geographical thinking inspired by Carl Ritter, Alexander von Humboldt, and Arnold Guyot. Regardless of the reasons for Morse's lost legacy, his contributions to geographical education are important and should be remembered.     

Why is there no Coastal Cordillera at the Arica Bend (Western Central Andes)?

The architecture of the Western Andes is remarkably constant between southern Peru and northern Chile. An exception, however, is present near Arica at 18°S, where the Andes change their strike direction by ca. 50° and the Coastal Cordillera is absent over an along‐strike width of 50 km. Although this feature has been mentioned in several previous studies, no effort has been made yet to describe and explain this peculiar morphology of the Western Central Andean forearc. Here, we propose a large‐scale model to explain the Myr‐long low uplift rate of the Arica Bend concerning seismic coupling and continental wedge‐top basin evolution. New geomorphic and sedimentologic data are integrated with seismicity and structural data from the literature to interpret the post‐Oligocene pattern of uplift, erosion and sediment transport to the trench. Results show that the Arica Bend has been marked by exceptionally low coastal uplift rates over post‐Oligocene timescales. In addition, this uplift anomaly at the Arica Bend correlates with relatively high sediment discharge to the corresponding trench segment since late Oligocene time. We interpret that before 25 Ma, the forming seaward concavity of the subduction zone induced trench‐parallel extension at the curvature apex of the overriding forearc. The subsequent low uplift rate would have then triggered a feedback mechanism, where the interplay between relatively low interplate friction, low coastal uplift and relatively high sediment discharge favoured Myr‐long relative subsidence at the Arica Bend, in contrast to Myr‐long uplift of the Coastal Cordillera north and south of it.     

Unroofing the core of the central Andean fold‐thrust belt during focused late Miocene exhumation: evidence from the Tipuani‐Mapiri wedge‐top basin,Bolivia

As the highest part of the central Andean fold‐thrust belt, the Eastern Cordillera defines an orographic barrier dividing the Altiplano hinterland from the South American foreland. Although the Eastern Cordillera influences the climatic and geomorphic evolution of the central Andes, the interplay among tectonics, climate and erosion remains unclear. We investigate these relationships through analyses of the depositional systems, sediment provenance and ⁴⁰Ar/³⁹Ar geochronology of the upper Miocene Cangalli Formation exposed in the Tipuani‐Mapiri basin (15–16°S) along the boundary of the Eastern Cordillera and Interandean Zone in Bolivia. Results indicate that coarse‐grained nonmarine sediments accumulated in a wedge‐top basin upon a palaeotopographic surface deeply incised into deformed Palaeozoic rocks. Seven lithofacies and three lithofacies associations reflect deposition by high‐energy braided river systems, with stratigraphic relationships revealing significant (～500 m) palaeorelief. Palaeocurrents and compositional provenance data link sediment accumulation to pronounced late Miocene erosion of the deepest levels of the Eastern Cordillera. ⁴⁰Ar/³⁹Ar ages of interbedded tuffs suggest that sedimentation along the Eastern Cordillera–Interandean Zone boundary was ongoing by 9.2 Ma and continued until at least ～7.4 Ma. Limited deformation of subhorizontal basin fill, in comparison with folded and faulted rocks of the unconformably underlying Palaeozoic section, implies that the thrust front had advanced into the Subandean Zone by the 11–9 Ma onset of basin filling. Documented rapid exhumation of the Eastern Cordillera from ～11 Ma onward was decoupled from upper‐crustal shortening and coeval with sedimentation in the Tipuani‐Mapiri basin, suggesting climate change (enhanced precipitation) or lower crustal and mantle processes (stacking of basement thrust sheets or removal of mantle lithosphere) as possible controls on late Cenozoic erosion and wedge‐top accumulation. Regardless of the precise trigger, we propose that an abruptly increased supply of wedge‐top sediment produced an additional sedimentary load that helped promote late Miocene advance of the central Andean thrust front in the Subandean Zone.     

SQUINTING BACK AT STRABO*

ABSTRACT. Strabo of Amasia (ca. 64 B.c.‐ca. A.D. 23) wrote the first comprehensive geography of the world known to the Greeks and Romans. Interest in Strabo and his Geography, which survives nearly intact in seventeen books, has fluctuated over the centuries among both classicists and historians of geography. After some historical background on Strabo and his reception, this essay considers the contribution of two significant recent English‐language treatments, as well as Strabo's Geography itself, and suggests ways in which the Strabonic model may have renewed relevance to the geographer's task of interpreting the oikoumene in the contemporary world.     

Early Middle Miocene broken foreland development in the southern Central Andes: evidence for extension prior to regional shortening

Most authors suggest that the main contraction phases in the southern Central Andes started in the Late Miocene. Along the flat‐slab segment, deformation has progressively involved basement and a broken foreland has developed. Recent work suggests that construction of the Andes by late Neogene shortening may have been controlled by lithospheric thinning and crustal structure generated during mid‐Tertiary times in the Southern and Central Andes. Exposures at the eastern border of the Famatina Ranges in western Argentina in the flat‐slab segment document basement involved extension of approximately this age. The Del Abra Formation, the lower unit of a major Andean synorogenic cycle (Angulos Group), reveals a distinct and previously unrecognized early Middle Miocene tectonic event. This is suggested by a 505‐m‐thick thinning‐ and fining‐upward megasequence. Dominantly conglomeratic facies record a continuous progression from fault‐scarp‐related high‐gradient colluvium to relatively distal terminal‐fan facies. The fining–thinning upward megasequence characterizes progressive scarp backstepping and decreasing relief after active extension. Interpretation of the stratigraphic fill and the associated structure (high‐angle hinterland‐dipping fault) favours tectonic inversion of an originally normal fault. This allows reappraisal and new understanding of the early‐stage architecture of the Central Andean foreland. Early Middle Miocene extension may have had an important bearing on the later evolution of the broken foreland.     

Tropicality,the unruly Atlantic and social utopias: the French explorer Henri Coudreau (1859 − 1899)

This paper addresses the works of Henri Coudreau, a little‐known French explorer of Guiana and Amazonia who was later forgotten by the ‘heroic’ histories of exploration because of his unruliness and nonconformist attitudes. Drawing on the literature of postcolonialism and tropicality as well as on recent studies of anti‐colonialist geographies, I address for the first time Coudreau's geography from the perspective of anarchist and critical thinking. My main argument is that Coudreau's work is a further example of the complexity and heterogeneity of the European intellectual field during the imperial age. Despite having come of age intellectually among all the European racist and ethnocentric prejudices of his day, Coudreau developed a different outlook thanks to two factors, viz., his personal experience in living for years with the indigenous communities of Amazonia, and his exposure to anarchist anti‐colonialist ideas through his collaboration with Elisée Reclus. Coudreau's tropical utopia of an independent Amazonia, and his endorsement of the stateless nature of local communities, ran counter to French imperial politics, occasioning Coudreau's dismissal from the French administration and his professional exile in Brazil at the time of the Franco‐Brazilian border dispute (1897?1900).     

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.     

Economy,culture and environment: perspectives on the Australian food industry

Intersections between economy, culture and environment pose exciting future challenges for human geography. Part of Griffith Taylor's pioneering role as a geographer was to investigate relationships between these three aspects of human life, although his agenda was that of environmental determinism. This paper considers these intersections as they relate to contemporary geographical studies of restructuring, in particular the emergence of a genuinely global economic system since about 1980. Recent developments in cultural geography argue that geographical analysis of restructuring has been dominated by an economic determinism which has buried other stories which could be told about industrial change. The paper sketches lines of possible dialogue between economic geography and cultural studies, illustrating the argument with examples from restructuring in the Australian food industry. In opening such a dialogue, economic geography would be better placed to return to interactions between economy, culture and environment. In his day, Taylor was not afraid to upset the conventional wisdom about these relationships and this may be one of his most enduring legacies.     

Cretaceous deformation of the southern Central Andes: synorogenic growth strata in the Neuquén Group (35° 30′–37° S)

The Neuquén Group is an Upper Cretaceous continental sedimentary unit exhumed during the latest Miocene contractional phase occurred in the southern Central Andes, allowing a direct field observation and study of the depositional geometries. The identification of growth strata on these units surrounding the structures of the frontal parts of the Andes, sedimentological analyses and U–Pb dating of detrital components, allowed the definition of a synorogenic unit that coexisted with the uplift of the early Andean orogen since ca. 100 Ma, maximum age obtained in this work, compatible with previous assignments and constrained in the top by the deposition of the Malargüe Group, in the Maastrichtian (ca. 72 Ma). The definition of a wedge top area in this foreland basin system, where growth strata were described, permitted to identify a Late Cretaceous orogenic front and foredeep area, whose location and amplitude contrast with previous hypotheses. This wedge top area was mostly fed from the paleo‐Andes with small populations coming from sources in the cratonic area that are interpreted as a recycling in Jurassic and Lower Cretaceous sections, which contrasts with other analyses performed at the foredeep zone that have mixed sources. In particular, Permian sources are interpreted as coming directly from the cores of the basement structures, where Neopaleozoic sections are exposed, next to the synorogenic sedimentation, implying a strong incision in Late Cretaceous times with an exhumation structural level similar to the present. The maximum recognised advance for this Late Cretaceous deformation in the study area is approximately 500 km east of the Pacific trench, which constitutes an anomaly compared with neighbour segments where Late Cretaceous deformations were found considerably retracted. The geodynamic context of the sedimentation of this unit is interpreted as produced under the westward fast moving of South America, colliding with two consecutive mid‐ocean ridges during a period of important plate reorganisation. The subduction of young, anhydrous, buoyant lithosphere would have produced changes in the subduction geometry, reflected first by an arc waning/gap and subsequently by an arc migration that coexisted with synorogenic sedimentation. These magmatic and deformational processes would be the product of a shallow subduction regime, following previous proposals, which occurred in Late Cretaceous times, synchronous to the sedimentation of the Neuquén Group.     

Review symposium: our common future: the world commission on environment and development

In 1983 the General Assembly of the United Nations called for the setting up of a World Commission on Environment and Development. The Commission's ambitious tasks were described by its Chairman, Gro Harlem Brundtland, Prime Minister of Norway, as: (1) to propose long‐term environmental strategies for achieving sustainable developments by the year 2000 and beyond; (2) to recommend ways concern for the environment could be translated into greater cooperation among developing countries and between countries at different stages of economic and social development; (3) to consider ways and means by which the international community could deal more effectively with environmental concerns; and (4) to help define shared perceptions of long‐term environmental issues and the appropriate efforts needed to deal successfully with problems of protecting and enhancing the environment. The Commission's Report, Our common future,was published in 1987.     

THE LEGENDARY “REDISCOVERY” OF GEORGE PERKINS MARSH

The conventional narrative regarding the American reception of George Perkins Marsh, author of Man and Nature (1864), is that his work and ideas were “lost,”“forgotten,” or “neglected” until Lewis Mumford “rediscovered” him and introduced him to geographers at the University of California‐Berkeley through The Brown Decades (Mumford [1931] 1955) and until Carl Sauer made him known to the profession at large beginning in 1938. This article upends the conventional narrative by looking at earlier references to Marsh's later versions of Man and Nature, which were published as The Earth as Modified by Human Action from 1874 to 1907. Analysis reveals that a number of geographers and historians cited these editions between 1875 and the early 1950s. Examining the legend of loss and rediscovery suggests the value of methods utilized in reception studies for research on the history of geography.     

ROOST SITES AND COMMUNAL BEHAVIOR OF ANDEAN CONDORS IN CHILE*

The Andean condor (Vultur gryphus) is an endangered species. Even southern Patagonia, home to the most stable and abundant populations of Andean condors, is witnessing increasing pressure from development and tourism. Taking the case of Torres del Paine National Park, in the Chilean Patagonia, we examine monitoring of condor populations at roosting sites and communal bird behavior in response to humans as an effective tool for bird conservation within protected areas. Based on field data collected throughout 2007, we identify new roosting places, explore activity patterns and population characteristics of free‐ranging and roosting Andean condors, examine bird behavior in response to humans, and analyze the current and likely future ecological impacts of tourism on the condor population and its habitat. Our results reveal that the impact of tourism is still low and that the Andean condors do not seem to be declining in numbers in the park but that the importance of roosts and animal behavior in response to humans must be considered for future monitoring, bird‐conservation planning, and ecotourism management.     

Geodynamic context for the deposition of coarse‐grained deep‐water axial channel systems in the Patagonian Andes

We present field and seismic evidence for the existence of Coniacian–Campanian syntectonic angular unconformities within basal foreland basin sequences of the Austral or Magallanes Basin, with implications for the understanding of deformation and sedimentation in the southern Patagonian Andes. The studied sequences belong to the mainly turbiditic Upper Cretaceous Cerro Toro Formation that includes a world‐class example of conglomerate‐filled deep‐water channel bodies deposited in an axial foredeep depocentre. We present multiple evidence of syntectonic deposition showing that the present internal domain of the fold‐thrust belt was an active Coniacian–Campanian wedge‐top depozone where deposition of turbidites and conglomerate channels of Cerro Toro took place. Cretaceous synsedimentary deformation was dominated by positive inversion of Jurassic extensional structures that produced elongated axial submarine trenches separated by structural highs controlling the development and distribution of axial channels. The position of Coniacian‐Campanian unconformities indicates a ca. 50–80 km advance of the orogenic front throughout the internal domain, implying that Late Cretaceous deformation was more significant in terms of widening the orogenic wedge than all subsequent Andean deformation stages. This south Patagonian orogenic event can be related to compressional stresses generated by the combination of both the collision of the western margin of Rocas Verdes Basin during its closure, and Atlantic ridge push forces due to its accelerated opening, during a global‐scale plate reorganization event.     

The evolution of the high‐elevated depocenters of the northern Sierras Pampeanas (ca. 28˚ SL), Argentine broken foreland,South‐Central Andes: the Pipanaco Basin

The Pipanaco Basin, in the southern margin of the Andean Puna plateau at ca. 28°SL, is one of the largest and highest intermontane basins within the northernmost Argentine broken foreland. With a surface elevation >1000 m above sea level, this basin represents a strategic location to understand the subsidence and subsequent uplift history of high‐elevation depositional surfaces within the distal Andean foreland. However, the stratigraphic record of the Pipanaco Basin is almost entirely within the subsurface, and no geophysical surveys have been conducted in the region. A high‐resolution gravity study has been designed to understand the subsurface basin geometry. This study, together with stratigraphic correlations and flexural and backstripping analysis, suggests that the region was dominated by a regional subsidence episode of ca. 2 km during the Miocene‐Pliocene, followed by basement thrusting and ca. 1–1.5 km of sediment filling within restricted intermontane basin between the Pliocene‐Pleistocene. Based on the present‐day position of the basement top as well as the Neogene‐Present sediment thicknesses across the Sierras Pampeanas, which show slight variations along strike, sediment aggradation is not the most suitable process to account for the increase in the topographic level of the high‐elevation, close‐drainage basins of Argentina. The close correlation between the depth to basement and the mean surface elevations recorded in different swaths indicates that deep‐seated geodynamic process affected the northern Sierras Pampeanas. Seismic tomography, as well as a preliminary comparison between the isostatic and seismic Moho, suggests a buoyant lithosphere beneath the northern Sierras Pampeanas, which might have driven the long‐wavelength rise of this part of the broken foreland after the major phase of deposition in these Andean basins.