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http://ppg.sagepub.com/content/37/2/227The online version of this article can be found at:
DOI: 10.1177/0309133312457108
2013 37: 227 originally published online 16 August 2012Progress in Physical GeographyDeborah P. Dixon, Harriet Hawkins and Elizabeth R. Straughan
Wonder-full geomorphology: Sublime aesthetics and the place of art
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Article
Wonder-full geomorphology:Sublime aesthetics and theplace of art
Deborah P. DixonAberystwyth University, UK
Harriet HawkinsRoyal Holloway, University of London, UK
Elizabeth R. StraughanAberystwyth University, UK
AbstractThough not yet readily apparent in articles and book chapters, there is a burgeoning series of ‘in the field’collaborations between geomorphologists and artists focused around the mutual exploration of ‘inspirationallandscapes’, and the harnessing of the emotive dimensions of such body/world encounters in the productionand communication of geomorphological knowledge. Seemingly at odds with the discipline’s emphasis uponthe production of fieldwork data (as opposed to sensed phenomena), as well as its disavowal of the subjective,this work nevertheless resonates with a complex and fascinating aesthetic tradition within geomorphology.Here, we ‘place’ these contemporary collaborations via: reference to Humboldtian science, and the cruciallink between sensibility and precision; a reading of the Kantian sublime in the work of G.K. Gilbert; asketching out of the evisceration of both the aesthetic and art in the second half of the 20th century; and,finally, a review of the current scope of art/geomorphology collaborations, and possible futures.
Keywordsaesthetic, art, G.K. Gilbert, geomorphology, sublime, wonder
I Introduction
Over the past two decades we have been witness
to a variety of efforts to ‘re-enchant’ geomor-
phology. These involve a more ‘direct’ (by which
is meant ‘in the field’) engagement with land-
forms, which becomes a means of prompting
‘out of the box’ thinking in the mode of W.M.
Davis’ (1926) outrageous hypotheses. They have
also generated discussion as to how geomorphol-
ogists should, and could, engage with landforms
as objects of analysis, and communicate their
knowledge (Baker, 1993, 1996, 2008; Baker and
Twidale, 1991; Huggett, 2002; Stoddart, 1981;
Twidale, 1996). In subsequent and related
debates on the past, present and future of geo-
morphology, portentous gaps have been posited
between subjectivity and objectivity, idealism
and realism, empiricism and reductionism and
Corresponding author:Deborah Dixon, Institute of Geography and EarthSciences, Aberystwyth University, Aberystwyth, SY233DB, UK.Email: [email protected]
Progress in Physical Geography37(2) 227–247
ª The Author(s) 2012Reprints and permission:
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so on, each laid one on top of another to form a
disciplinary palimpsest, marked by a deep, see-
mingly impassable fissure. Far from being a ‘phi-
losophically sedate discipline’ (Sherman, 1996:
87), geomorphology continues to grapple with
a variety of conceptual issues, including its place
within and without geography (for example,
Harrison, 1998, 2001; Rhoads, 1993, 1994,
1999, 2006; Rhoads and Thorn, 1994, 1996a;
Slaymaker, 2009).
In this paper we want to engage with these
debates on the character and scope of the
discipline, and explore the potential of a
‘wonder-full geomorphology’. We do so not
to resolve them via an all-encompassing
explanatory framework (as has been attempted
via general systems theory, critical realism and,
more recently, actor-network theory), or shared
concepts (such as relational space). Nor do we
want to create a ‘bridging’ moment based on
mutual concerns (such as global warming, envi-
ronment degradation and loss of biodiversity).
Rather, we want to reconsider key moments in
the study of landforms in order, first, to help
contextualize the emergence of these dichoto-
mies – objective over and against subjective and
so on – within geomorphology, and, second, to
‘place’ current, practice-based, collaborative
projects undertaken by artists and geomorphol-
ogists that do not ‘bridge’ divides so much as
juxtapose and learn from differing approaches
to landforms. Key, here, is a shared interest in
the sensuous encounters via which landscapes
are made sense of, perceptually and cognitively,
and a harnessing of the emotive dimensions of
such encounters in the production and commu-
nication of geomorphological knowledge. This
is an aesthetic mode of inquiry, we argue, which
finds resonance not only in art’s long tradition
of thought and practice, but in aspects of a his-
tory of geomorphology that have tended to be
overlooked or disavowed by its 20th-century
biographers. This is despite continued interest
by some geomorphologists in art and aesthetics
more broadly as manifest in, for example,
Shephard’s (1957) compelling argument on the
way in which emerging geological knowledge
in 1840s New England inspired the region’s art-
ists, and Alexander’s (1982, 1986) observations
on the ‘form of the land’ and the shaping of
Leonardo da Vinci’s and Dante’s artistic output.
The sundering of aesthetic sensibilities from
scientific inquiry is usually traced back to what
is considered to be a momentous, Enlighten-
ment shift in the making of the modern-day geo-
graphic discipline, wherein, as Hartshorne
(1939), for example, observed, geography shed
its ‘pre-critical’ collection phase – based on the
compendium of images as well as texts – and
became a synthesizing effort. Critical analysis
was associated with the sorting and categorizing
of observations, with the ultimate goal of pull-
ing out from this wealth of material a generaliz-
able set of processes. For Stoddart, the year
1769 is pivotal: Captain Cook’s entry into the
South Pacific formally marked the end of a ‘bar-
ren didacticism of capes and bays’ and the inau-
guration of a discipline that produces and seeks
to answer questions concerning ‘man and envi-
ronment within regions’ (Stoddart, 1987: 331).
In both these accounts of disciplinary history,
art, as well as a discussion of the aesthetic, is
barely present. It is unsurprising, then, that
Alexander von Humboldt’s 19th-century ana-
lyses of landforms are so often understood as
on a cusp; and that his Cosmos (1845–1862) is
denoted as tension-laden, and even fatally
flawed, by virtue of his insistence that poetry
and etchings were to be valued alongside sys-
tematic observations of physical processes
(Stoddart, 1975).
Our own discussion of the place of art and
aesthetics in geomorphology returns to and
takes inspiration from Humboldt’s work. Cru-
cial to our argument is the recognition of an
‘expanded field’ of artistic inquiry that predated
the rarification of ‘artworks’ (principally in the
form of oil paintings, watercolours and sculp-
ture), which was firmly institutionalized by, for
example, the founding of the Royal Academy of
228 Progress in Physical Geography 37(2)
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Arts in London in 1769.1 Prior to this strict win-
nowing, however (and continuing to circulate
outside of it, not least in diverse scientific,
mechanic and technological institutions), was
an expanded field that encompassed: the instru-
mentalized graphic arts of maps and charts; a
visual tradition of geological cross-sections
based on explanation and exposition; the visual
economies of a Linnaean Botany; and the ideals
of landscape and view paintings. What we want
to draw out from this is how art was indeed much
more than a mode of representation that allowed
for an ‘accurate’ rendering of the form, feature,
colour and texture of landforms – a mimetic, if
you will – but had, as Humboldt acknowledged,
a range of roles in Enlightenment geographies,
all of which relied upon, albeit in different
modes, the working through of an aesthetic sen-
sibility in the production of geographic knowl-
edges (Hawkins, 2010, 2011).2
Aesthetics refer here not to some personally
held sense of beauty, but to a broad-based inquiry
into multi-sensuous encounters between body
and world, and the manner in which these were
to be made sense of. Indeed, it is in the 18th cen-
tury that such inquiry is formalized in the work of
Alexander Baumgarten and Immanuel Kant. As
such, the aesthetic was by no means to be ‘con-
tained’ in the production and form of paintings
and sketches, but undergirded fieldwork practices
more broadly (Stafford, 1993), as manifest in
Humboldt’s ‘artistic’ philosophy.
Acknowledging the broad sweep of the
aesthetic, we are interested here in its varied
influence within a history of modern-day geo-
morphology. We draw out, for example, how
a Kantian aesthetic has been used to ground
a divide between the intelligible and the
unknown, the latter viscerally experienced as
the sublime and prompting a sense of awe and
wonder that, importantly, prompts thought. And
so in the work of G.K. Gilbert (1843–1918),
often heralded as the ‘father’ of a modern-day,
scientific, process-orientated geomorphology,
we can trace how a felt engagement with the
order of nature prompts a series of analytically
framed questions concerning landform develop-
ment. This is a very particular rendering of
‘wonder’ that persists across the field today,
perhaps most strongly in contemporary plane-
tary geomorphology: here, an (almost) unlim-
ited frontier is afforded for the exploration of
extra-terrestrial landforms and landscapes
(Baker, 2008).
These themes continue into the 20th century,
wherein we find a ‘sense of place’ as part and
parcel of the ‘scientific study of scenery’ (Marr,
1900). Leveson, for example, notes how, for a
geologist, ‘the pleasing landscape is endowed
with geologic clarity: material, structure,
process, and time are meaningfully articulated’
(Leveson, 1988: 85). An extension of this argu-
ment can be seen in the work of Semken (2009,
2011), who not only emphasizes a sense of place
within Navajo and Blackfeet cultural reper-
toires, but weaves these into a native American
geoscientific knowledge base that parallels, for
example, ‘western’ models of dynamic equili-
brium (see also Semken and Brandt, 2010). This
experiential dimension, however, was written
out as unnecessarily subjective by the propo-
nents of a quantitative revolution, a moment that
was to prove pivotal in the recasting of Hum-
boldt and Gilbert as proto-quantitative scientists
(Chorley, 1978). Yet, while the scientism of this
post-war period may have appeared extreme,
even here we can find the continuing presence
of aesthetics, but in an anaemic form. That is,
sensuous encounters with nature are cast as the
source from which systematic, methodological,
technologically mediated procedures can pro-
duce data, the latter now clearly set apart from
‘mere’ sensed phenomena. Furthermore, this
approach to aesthetics sees value in art works,
but only insofar as they provide an accurate ren-
dering of the world they are understood to
mimic, thus enabling them to function as proxy
data sets.
While we recognize the legacy of such
framings, in the following we want to shed some
Dixon et al. 229
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light on what might be termed a ‘geomorpholo-
gic aesthetic’, wherein knowledge of the emer-
gence and transformation of landforms is
attained via a multi-sensuous engagement with
landscape, and the making sense of that experi-
ence. This creative mining of geomorphology’s
back catalogue allows us to then to place the
emergence, in recent years, of field-based, col-
laborative projects between artists and geomor-
phologists that, among other things, seek to:
prompt the generation of ‘inspirational data’;
ask questions relating to audience and commu-
nication; and offer productive re-visionings not
only of fieldwork and practice, but also the
nature of the objects geomorphologists are
working with.
II Putting art in its place
In this section, we want to begin our exploration
of the place of art by returning to the ‘Age of
Wonder’ wherein ‘Romantic Science’, as
Richard Holmes (2010: xvi) puts it, ‘grew out
of eighteenth-century Enlightenment rational-
ism, but largely transformed it, by bringing a new
imaginative intensity and excitement to scientific
work’. Publics across Europe and the USA fol-
lowed with trepidation the cosmic voyages of
William and Caroline Herschel, the flights of bal-
loonists, as well as the maritime expeditions of
Captain Cook and Charles Darwin, each of
which encountered peoples and places, objects
and practices that provoked new ways of think-
ing about a dynamic world, how it might work,
and our place within it; and which also, as
Holmes makes clear, undercut any notion of an
antithesis between various fields of knowledge,
as well as between adventure and diplomacy,
experiment and spectacle, lay and expert.
Weimar Germany was to provide a similar
locus of Romantic-cum-Enlightenment activity
around such figures as Goethe, Bach, Schiller
and Herder, as well as Alexander von Humboldt
(1769–1859), broadly considered a ‘celebrated
patriarch’, as Buttimer (2001) puts it, of the
modern-day geographical sciences, and the
‘creator’, according to Ackerknecht (1955), of
geomorphology in particular. For historians of
science, Humboldt has become a key figure in
the exploration of ongoing tensions in this era
around the aesthetic sensibilities of the field
scientist, and the empirical rigour of the arts and
humanities (Dettelbach, 2001), tensions that
were to foreshadow the humanist/spatial
science debates of the 20th century. Neverthe-
less, any sense of a profound disjuncture
between the humanities and the sciences would
be misleading: in Weimar Germany an emer-
ging collection of geological maps and atlases,
for example, were to have a profound cultural
impact not only upon German landscape art
(Mitchell, 1993), but literature also, contribut-
ing to what Piper (2010: 27) calls a ‘new sense
of space and self according to the principles of
stratification, discretization, and relationality’.
Humboldt’s object of analysis was the Earth’s
surface, to which he applied a physiognomic3
mode of study. That is, in taking landforms as his
focus, Humboldt sought to interpret form and
feature as the profound, sensible expression of
a holism that not only extended to the insensible,
but undergirded the universe itself. Hence, land-
forms were not signs to be read, as though they
were but the inferior semblance of things more
real, but part and parcel of this mutually depen-
dent assemblage of people, animals, vegetation,
microclimate, elevation and so on, all animated
and kept in harmonious balance by these forces
– forces that, for Humboldt, were not to be con-
fused with a creationism.4 Indeed, the surface of
the Earth, as an object of analysis for Humboldt,
lent itself to being sensed by the cultivated, gen-
tleman explorer, who not only had the intellect5
to discern such a beautiful holism, but the finan-
cial wherewithal to be able to enhance his ‘gaze’
via a series of ‘apparatus’ such as magnetic com-
passes, thermometers, electrometers and so on,
which allowed for the systematic and measured
re-presentation of certain key aspects of the
field.
230 Progress in Physical Geography 37(2)
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It is this commitment to systematic study –
translated into a series of diagrams that tabu-
lated and cross-referenced various forces, thus
enabling comparisons to be made and rudi-
mentary forms of multivariate analysis to be
conducted – that have earned Humboldt the
moniker of the first ‘geovisualizer’ (Jackson and
Romanowski, 2009). His projections of land-
scape are physiognomic silhouettes of rising
plateaus and falling elevations, which expressed
the character of people as well as place. His iso-
thermal lines, curves of constant annual mean
temperature mapped for both surface position
and mountain elevation, expressed a harmonious
balance of all forces. Certainly, such diagrams
worked to a topological imaginary that carved
space into lines, interiors, exteriors and so on.
But, as Dettelbach points out, within Humboldt’s
aesthetic, ‘sensibility and precise measurement
cannot be separated’. This is because the latter
is ‘embedded in a particular account of philoso-
phical authority, the mind, its faculties, and their
legitimate scope’ (Dettelbach, 1999: 477).
Humboldt’s sketches, undertaken in the field,
were later polished by European artists in the
form of dioramas of a landscape’s diverse
organic and inorganic components. These
would in turn inspire landscape painters such
as Frederic Edwin Church, who produced the
large-canvas oil painting ‘Heart of the Andes’
(1859). Exhibited in New York, the painting had
a profound impact: ‘When confronted with its
immensity, the crowd becomes hushed. Women
feel faint’ (Poole, 1998: 107). Such methodolo-
gies were especially important to Humboldt
insofar as they allowed certain sensuous
encounters with the land to be perceived,
digested, made sense of in light of this holistic
reality, and communicated to others.
While admiring of Humboldt’s attempt at sys-
tematic and error-free surveying and measuring
practices, as well as his far-flung substantive
interests, historians of geomorphology have
tended to look upon his holistic philosophy as
an unfortunate imposition of cultural ideas
peculiar to the epoch. Stoddart, for instance,
writes disapprovingly that, ‘These works aimed
to demonstrate the interconnections of phenom-
ena and the continuity and completeness of
knowledge, rather than to adduce principles or
explore problems: hence Mackinder’s little-
remembered remark that the Cosmos ‘‘helped
to delay the advance of science’’’ (Stoddart,
1975: 17–18). The German public’s adoption of
Humboldt’s universal harmony as a spiritual-
cum-political belief no doubt exacerbated Mack-
inder’s sentiments. More recent commentators,
however, writing on the complexities inherent
to a history and philosophy of geomorphology,
have been more forgiving, with Buttimer
(2001: 105), for example, observing that ‘there
are aesthetic and experience-based facets of
[Humboldt’s] overall vision which enable the
work to transcend tensions between objectivity
and subjectivity, macro-scale survey and micro-
scale theatre, scientific explanation and artistic
representation’.
Humboldt’s enrolment of art, as well as his
desire for precise and systematic measurements
of sensible phenomena, becomes, for Buttimer,
folded into his overall aesthetic; that is, a particu-
lar mode of encounter with nature. Bunske (1981)
goes further, and observes that such an encounter
was illustrative of what has been termed the sub-
lime. At first blush, the sublime refers simply to
the overwhelming sense of wonder and awe felt
when regarding the vastness of nature, as evinced,
for example, by the public’s response to Church’s
‘Heart of the Andes’. In this broad sense, it par-
takes of many centuries of philosophical thought
regarding human-environment relations, as well
as the influential treatise of Edmund Burke
(1756) in particular, in which he traces his physio-
logical, as well as emotional, response to such
grand vistas. Yet, and this is what we want to flesh
out below, in acknowledging the importance of
the aesthetic it is also possible to draw out, in
the work of another ‘founding father’ of geomor-
phology, G.K. Gilbert, another rendering of the
sublime, one associated with the work of
Dixon et al. 231
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philosopher and physical geography lecturer
Immanuel Kant (1724–1804).
III A sublime nature
For Kant, a key problematic recurring through-
out his work was the question of how we come
to know the world around us, and in doing so
come to know ourselves. It is in this context that
the sublime, and the related concept of the beau-
tiful, becomes a way of framing this encounter.
Both the beautiful and the sublime, Kant pro-
posed in his Critique of Judgement (1790), should
not be understood as the intrinsic qualities of
objects, such as landforms; rather, they emerge
from a person’s perceptual and cognitive ‘making
sense’ of such objects, and a judgement of some-
thing as either beautiful or sublime. Whereas the
former is manifest as a feeling of pleasure in the
fact that one can discern a harmonious order to
an object (and this certainly echoes Humboldt’s
views on the pleasure felt in observing nature),
the sublime emerges from the discernment of a
boundlessness or formlessness (whether by virtue
of scale or scope) to nature. But, and this is cru-
cial, while phenomena such as volcanoes and
earthquakes evoke a wonder and awe that sug-
gests a physical powerlessness, and propose the
apparent limits of imagination, nevertheless it is
the uniquely human recognition of this limit that
in turn evidences the superiority of understanding
(Rolston, 1995). The sublime, then, is much more
than a particular appreciation for a ‘grand’ nature;
it brings into play the intellectual response to such
grandeur. It is an invitation to thought.
Here, we want to think through the role of
such an aesthetic in G.K. Gilbert’s wondering
engagement with the order of nature, manifest
as a series of analytically framed questions con-
cerning its development. Broadly considered
one of the founding fathers of a modern-day
geomorphology (Orme, 2002), or ‘onlie beget-
ter’, as Tinkler (1985) puts it, referencing Sha-
kespeare, of a process-orientated, dynamic
approach, Gilbert’s mode of inquiry is more
usually described in positivist, methodological
terms, as the ‘interplay of observation and
deductive reasoning wherein data were accumu-
lated within a robust and logical theoretical
framework’ (Chorley, 2000: 569).
Importantly for our argument, Gilbert’s artis-
tic practices emerged out of an ‘expanded field’
that included geologic cross-sections, field
sketches and photography, as well as the chromo-
lithographics, woodcuts and so on that formed
such a large part of the output of key
knowledge-forming institutions such as the
Smithsonian in Washington, DC (see Nelson,
1980). Gilbert, trained in geology and mathe-
matics as well as anatomy, was hired to assist
on John Wesley Powell’s geographic and
geologic survey of the Rocky Mountain Region,
1874–1879, producing ‘Geology of the Henry
Mountains’ in 1877. With the establishment of
the US Geological Survey in 1879 he was
appointed Senior Geologist, and went on to
publish his study of the (Pleistocene) Lake Bon-
neville in 1890. Over the course of his career,
Gilbert also speculated as to the manner in which
meteor impacts shaped lunar landscapes, and in
1906 documented with camera and notes earth-
quake damage along the San Andreas fault-line.
We want to look in depth at his artistic prac-
tice in the two years (on and off) Gilbert spent
in the Henry Mountains. Reading his published
monograph, we gain a sense of how the ‘compre-
hensive views from the mountain tops’ (1877:
vii) afforded Gilbert an overall, visual grasp of
landform; this ‘field of surpassing interest’
(p. 2) is rendered as a pared and pinned-back spe-
cimen, opened up for observation not by the
hands of an anatomist, but by physical processes
of weathering and erosion. He wrote:
The deep carving of the land, which renders it so
inhospitable to the traveler and the settler, is to the
geologist a dissection which lays bare the very anat-
omy of the rocks, and the dry climate which makes
the region a naked desert, soilless and almost plant-
less, perfects the preparation for his examination.
(Gilbert, 1877: 2)
232 Progress in Physical Geography 37(2)
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This was no mere record of slash and cut, how-
ever, opening all to the God-like gaze of the
scientist, but the prelude to what B.M. Stafford
(1993) calls a ‘finer touch’, that used the full
complement of senses in an exploration of
objects.6 This was a visual imagining that
acknowledged and then disavowed grand sur-
face impressions as open to myriad interpreta-
tions, and hence duplicities, and sought
instead, via a series of more intimate encoun-
ters, signs telling of the work of primal forces.
In the process, as she goes on to write, ‘a
‘‘hard’’, prestigious method, deemed intellec-
tually superior to the ‘‘soft’’, loose, irregular,
or geometrically shapeless material it was sup-
posed to regularize, was imposed from on high
and from the outside’ (Stafford, 1993: 466).
Gilbert’s attentiveness to how things look
became part and parcel of this imagining. In deli-
neating the Blue Gate and Tununk shales, for
example, it is their perceived colour and banding
that is deemed crucial to their categorization;
thus, ‘They are beautifully laminated and are
remarkably homogeneous. It is only in fresh
escarpments that the lamination is seen, the
weathered surface presenting a structureless
clay’ (1877: 5). Such loose, amorphous, complex
visual scenes prompt a feeling of uncertainty,
and, in Gilbert’s imagining, are hence very much
an invitation to thought. Following a description
of the thickness of the individual strata in the Gray
and Vermilion Cliffs, he observes:
The thickness of individual strata in these great sand-
stones is remarkable, and is one of the elements which
must be taken into account in the discussion of the
problem – which to my mind is yet unresolved – of the
manner in which such immense quantities of homo-
geneous sand were accumulated. (Gilbert, 1877: 7)
More often than not, such visual acuity is sup-
plemented by touch, so that, ‘The rock of the
Flaming Gorge group’, for example:
is of a peculiar character. It is ordinarily so soft that
in its manner of weathering it appears to be a shale.
It is eroded so much more rapidly than the Henry
Fork’s conglomerate above it, that the latter is
undermined, and always appears in the topography
as the cap of a cliff. Nevertheless, it is not strictly
Figure 1. ‘View of the Canon and the Waterpocket Flexure. The Cliff at the left is capped by the Henry’sFork Conglomerate. The arched rocks to the right are the Gray and Vermilion Cliffs Sandstones’, G.K.Gilbert, from ‘Report on the geology of the Henry Mountains’ (1877).
Dixon et al. 233
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speaking a shale. The chief product of its
weathering is sand, and wherever it can be exam-
ined in its unweathered condition it is found to be
a fine-grained sandstone. (Gilbert, 1877: 8)
Gilbert’s field sketch of the Gray and Vermilion
Cliffs (Figure 1), which also takes in the Henry
Fork conglomerate, emerges from this visual
imagining of the encounter between body and
land. That is, it systematically records and
locates in visual terms the key sighted and felt
aspects of these encounters, but is also a crucial
means of ‘thinking through’ how these aspects,
rendered legible to self and others, can become
subject to explanation.
In a following sketch of the Waterpocket Flex-
ure (Figure 2), we see a loose grouping of tiny fig-
ures, some walking across the base of the cliffs,
some seemingly gazing with rapt attention at the
grandeur and sweep of the intersected landscape
before them, which becomes, with distance, more
white space than line. If we compare this to the
previous view of Waterpocket Canon, what we
see are two very different registers of sketch exist-
ing side by side within Gilbert’s text. In the first,
we see the use of field-sketching to render the
landscape structurally intelligible, a form of topo-
graphic art that foregrounded an accuracy of deli-
neation, while in the second sketch we see Gilbert
practising a mode of working akin to view-
painting, wherein the focus is on capturing the
scene but to emphasize a subject-centred, aes-
thetic appreciation of it.
During his time in the Henry Mountains Gil-
bert was to detail his observations and findings
in the form of numerous notes and sketches, all
woven together as he strove to make sense of
how particular landforms had been shaped by
underlying physical processes (see Hunt, 1988,
for reprints of these).
Yet Gilbert’s notebooks have usually been
described as evidencing a move from ‘faithful’
description to idealized hypothesis, the latter
alone being deemed scientific in character
(Egger and Carpi, 2008), or, more figuratively,
as the move from seed to germinating plant
(Pollard and Fletcher, 2005: 458).7 Gilbert’s
drawings of Mt Hillers are proffered here; made
on repeat visits, they take the form of field
Figure 2. ‘Waterpocket Flexure, as seen from the south end of Mount Ellen’, G.K. Gilbert, from ‘Report onthe geology of the Henry Mountains’ (1877).
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sketches of the type noted above, as well as
iterative drawings of the laccolite he surmises
to be the result of magma inserted into the sedi-
mentary layers of the region (see Figure 3).
Leaving to one side this framing of science as
the delineation of cause-effect relations, what
we can draw out of these notebook excerpts is
the Kantian sublime. When faced with the com-
plex landscape of this site, for example, Gilbert
wrote in his notes, ‘I don’t understand Mt
Hillers’ (quoted in Egger and Carpi, 2008:
n.p.). In order to make sense of this formation
Gilbert has recourse to a graphic representation
of a key process – magma intrusion and subse-
quent uplift and erosion – thereby typifying,
regularizing and shaping a Henry Mountain
‘structure’. To be sure, Gilbert’s artistry here
can be described as providing a visualized
mode of description and explanation, but what
is also apparent is that its varied forms – scenic
view, topographic sketch, diagrammatic cross-
section, and so on – all speak to a multi-
sensuous, and hence aesthetic, encounter with
landscape, and a sustained reflection upon how
this encounter is to be made sense of percep-
tually and cognitively.
Nevertheless, it is this sense of ‘progress’
from one mode of thinking and communicating
(ostensibly descriptive) to another (scientific)
that was to become dominant in accounts of the
history of geomorphology. As Sack (1992)
observes, it was Gilbert’s emphasis upon pro-
cess geomorphology, and particularly his atten-
tiveness to a thermodynamically based method
of systems analysis, that was to become lauded
by a new cadre of quantitative analysts, such as
Strahler and Hack, while historiographies by,
for example, Church (2010) have stressed
Gilbert’s figurehead role in regard to general
systems theory. Part and parcel of this
‘installation’, as Sack calls it, of a new paradigm
was, we would add here, the delinking of
aesthetics (that is, sensuous encounters and
sense-making) from the art ‘object’. As we go
on to discuss below, while such aesthetics were
to remain a disciplinary stalwart, albeit unac-
knowledged as such in the form of fieldwork,
the art work was to be pinned down and
accounted for in thoroughly instrumental terms
as a mimetic of real-world processes and events.
IV Enhanced’ field encounters andart as mimetic
As Sack (1992) observes, Gilbert’s installation
came at the expense of W.M. Davis. In presenting
his ‘geographical cycle’ of landform develop-
ment as a matter of ‘structure, process, stage’,
Davis, of course, borrowed directly from
Darwin’s evolutionary framing of organisms and
Figure 3. ‘Ideal Cross-Section of a Laccolite, showing the typical form and arching of overlying strata’, G.K.Gilbert, from ‘Report on the geology of the Henry Mountains’ (1877).
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the transformation of species. Whereas Gilbert
had deployed an anatomical imaginary that prior-
itized the intimate exploration of bodies via a
‘finer touch’, Davis’ biological borrowing was
firmly grounded in the gaze and the surface
appearance of formations. Hence, his field
sketches were initially based on maps of an area
so that Davis could gain a sense of extant form;
these would be redrawn after a field visit, but very
much in accordance with the stage in the cycle of
erosion that Davis wanted to emphasize. In conse-
quence, what we see in Davis’ famous block illus-
trations are very much ‘ideal types’.
A useful articulation of this form-based ima-
ginary, and its manifestation in the field sketch,
is provided by Woolridge who, in vehement
defence of Davis, wrote:
In the first place I regard it as quite fundamental that
Geomorphology is primarily concerned with the
interpretation of forms, not the study of processes.
The latter can be left to Physical Geology. Here an
analogy may be helpful. The fact of organic evolution
was sufficiently demonstrated by comparative anat-
omy long before the details of its mechanism came
to light . . . Similarly Davis proceeded essentially
by recognizing a developmental series of forms.
Sketch, or better still photograph, a large number of
river meanders and you will readily convince yourself
of the reality of downstream shift or ‘sweep’, as well
as the stages leading to cut-off. (Woolridge, 1958: 31)
Even here, however, we can see the emphasis
upon the sketch as an accurate mimetic of real-
world events and objects – such that it can be
‘bettered’ in this role by the photograph8 – as
opposed to a thinking through of a multi-
sensuous encounter with nature. To be sure, these
encounters remain today a crucial part of the
much-vaunted field trip (Ritter, 1986), but are
now rigidly systematized as the technologically
enhanced, error-free measurement and recording
of variables. Such encounters, in effect, allow
for the production of data, which, because it
has been methodologically and technologically
mediated, is not to be confused with mere sensed
phenomena. If we compare such a methodology
with that of Humboldt, precision has by now
become firmly sundered from the aesthetic sensi-
bilities of the European gentleman.
Contemporaneously, the instrumentalization
of art as a now separate, reified sphere of prac-
tice reached its apogee in the emergence of a
body of work that seeks to use paintings, sketches
and other artistic media as data proxies (Gemtou,
2011).9 For Grove, an early pioneer of this
approach, while oral narratives were ‘not to be
taken at face value’, the detail provided on paint-
ings of the Mt Blanc massif ‘is so accurate that
full dependence may be placed on them as a
source of evidence’ (Grove, 1966: 135). Gellatly
(1985) and Schubert (1980, 1984, 1987) have
situated paintings and photographs as part of a
suite of sources to reconstruct past glacier posi-
tions in Mt Cook National Park and the Sierra
Nevada de Merida, respectively. In similar vein,
Parham (2005) looks to Chinese art for evidence
of type of local bedrock, the intensity of rock
weathering, and the status of soil erosion, while
Hejl (2005) notes tafoni weathering in a Greek
prehistoric wall painting.
As Cosgrove’s (1979) analysis of the aes-
thetics of Ruskin draws out, in some contexts the
faithful representation of nature in all its colour
and morphology is a matter of artistic principle.
What is problematic, however, in such geo-
morphic analyses is the disavowal of the context
within which art-making occurs, including but
not limited to: the intentions of the artists and their
existential and metaphysical concerns; the socio-
cultural environments within which they work;
changing stylistic modes, such as the introduction
of the picturesque; and the symbolic deployment
of a colour and brush palette. Analyses that look
to art to accurately represent nature (or not), we
would emphasize, both draw upon and reinforce
a more general, scientific understanding of visual
culture as principally mimetic. Also, as Rhoads
and Thorn (1996b) note, this mimeticism is itself
predicated upon a logical empiricism, wherein a
fundamental gap is posited between an apparently
objective observation that picks out real-world
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truths, and a subjective theorization that must
then work in accord with these truths.
V The return of the aesthetic?
Over the past two decades we can discern an
intermittent call for a return to more ‘direct’
encounters with nature as a source of intellectual
inspiration, but also the productive channelling of
an all-too-human curiosity. In 1981, for example,
Stoddart appealed, in rather more appreciative
vein, to the inspirational nature of landforms, as
evidenced in the work of Humboldt. He writes:
We take pleasure in an aesthetic and even emotional
appreciation of the landscapes we perceive and proj-
ect our imaginations on to them. Often we think this
to be a modern development, though Humboldt
treated it at length in the Cosmos. And it leads to the
sense of wonder which we all must feel, on the coral
reef, in the redwood forests, in high mountains or
the desert, and indeed in Los Angeles or Calcutta,
Istanbul or Peking, in the realization not only of
Earth’s diversity but of man’s [sic] ingenuity in cop-
ing with it in the process of making a living . . . Let
us not allow an arid formalism to replace the true
attraction of geography, either at the elementary
or the research level. (Stoddart, 1981: 296)
Ten years later, Baker and Twidale made a simi-
larly nostalgic call for a return to the ‘Golden
Age’ of geomorphology, wherein Gilbert,
Powell and their contemporaries were inspired
intellectually and emotionally by the grand
landscapes of the American West. They write:
‘Explanatory paradoxes posed by the newly
reported landforms and landscapes stimulated
creative thinking that expanded and improved
explanations for already familiar landscapes’
(Baker and Twidale, 1991: 74). Here, the invita-
tion to thought proffered by complex landscapes
is contrasted with a predictive, systems
approach, which, they argue, relies upon meth-
odological innovation and which, they imply,
is hence lacking in wonder and excitement. For
our own part, we discern here an interest in what
may be termed the ‘affective capacity’ of
landscape, a capacity that takes us back to the
sublime as a viscerally felt invitation to thought.
Such calls are usefully understood, we would
like to suggest, as a return of the aesthetic,
which, as we have argued throughout this paper,
derives its impetus from a consideration of
body/world encounters.
Yet, it must be stressed, given its broad-based
remit, the aesthetic cannot be matched with a
particular theoretical orientation or substantive
domain. Indeed, we can find iterations of the
aesthetic in biology, physics and chemistry, as
well as art and the humanities. In other words,
there is no one ‘hook’ upon which to hang an
aesthetic framing; rather, there is a wealth of
aesthetic modes of inquiry that can be brought
to bear. Underscoring this particular geomor-
phological appeal to more direct encounters is,
we would suggest, a broader reflection upon
visual culture as an embodied (as opposed to
an intellectual or cerebral) practice that brings
the hands, eyes, sensory apparatus, nerve end-
ings, neurons and so on into play. In the language
of mimeticism noted above, ‘re-presentation’ as
a term implies an inferior copy, or sign regarding
something else, and it is precisely this language
that we see being challenged, often via recourse
to a prior Humboldtian or Gilbertian tradition.
Where Baker and Twidale (1991) look to the pro-
ductive, sensuous engagement of body and land,
Tooth looks to the affective capacity of the ‘vir-
tual globe’ (2006) and the satellite image (2009).
Each of these also engage the sublime, which, as
we hope the example of the Heart of the Andes
used earlier indicates, is by no means ‘contained’
in the field. It can very much be discerned in such
spectacles: their status and import in this regard
lies in their singular capacity to affect people.
Part and parcel of this challenge is a
renewed, disciplinary interest in art, a body
of thought and practice that, manifest via its
own modes of expression, has a long and com-
plex aesthetic tradition. In recent years, how-
ever, we are also witness to collaborative
practices in the field, as well as associated
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works produced by artists for diverse publics,
from school children to gallery audiences. A
pivotal point for such collaborations tends to
be particular landscapes (some extreme, others
considered mundane) that are considered com-
plex in the sense that they prompt uncertainty
over and against surety, as well as an acknowl-
edgement of how this uncertainty has been nar-
rativized in diverse ways across the disciplines.
The term ‘inspirational’, as used in the
collaborative work of glacial geomorphologist
Peter Knight and visual artist Miriam Burke, for
example, denotes how their mutual collaboration
has led them to explore how it is that they
‘notice’ and understand landscape differently,
and, further, how this recognition prompts them
to reconsider the nature of what was once overly
familiar. Based in explorations of the local
landscapes of North Staffordshire and its
history during the last Ice Age, the project, devel-
oped over the course of three years, saw methodo-
logical exchange in both the cold lab and the field
(with Burke visiting Iceland), culminating in the
exhibition ‘Know this Place for the First Time’.10
Included in this exhibition was Burke’s ‘Measur-
ing Spoon’, a sculptural reflection on the ad hoc
use Knight makes of a teaspoon for scale in his
photographs (Figure 4).
Beyond these reflections on scientific
method, both Burke and Knight see artistic
practices, and particularly the arts’ traditional
emphasis upon measuring the individual over
and against a sublime Nature11 as a means to
take account of the inherent uncertainty in
science. Indeed, in a comment thoroughly
reminiscent of the Kantian Sublime, and the
tension at its heart between the comprehensi-
ble and incomprehensible, Knight writes:
Despite progress in remote sensing and analytical
techniques, our reconstructions of past glaciations
remain tentative, our understanding of modern glacial
processes incomplete and our modelling of their
future unreliable. In nineteenth century art, glaciers
represented romance, mystery and unassailable
majesty. In twenty-first century science their position
is perhaps similar, but what art calls ‘mystery’,
science calls ‘uncertainty’. (Knight, 2004: 385)
Questions around risk and prediction are, for
Knight, thoroughly emotive ones, insofar as
they excite feelings of wonder and awe.12
Risk and uncertainty have also underscored
the collaborative work of vulcanologist Carina
Fearnley and designer/performer Nelly Ben
Hayoun. Key to their project ‘The Other Vol-
cano’ is a desire to communicate the viscerality
of living with volcanic landscapes, and in partic-
ular how wonder, excitement, fear and trepida-
tion can be usefully harnessed as a means of
prompting more sustained reflection upon how
the risks associated with volcanoes are to be
communicated.13 The project takes the form of
what the artist describes as ‘semi-domesticated
volcanoes’, each capable of ‘randomly’ erupting
dust and gloop (from a combination of gunpow-
ders, potassium nitrate and sugar), and housed in
galleries – including the Welcome Trust, Lon-
don (October–December 2010) and the Central
Booking Gallery, New York (April–June 2011)
– and the living spaces of volunteers (Figure 5).
It is while ‘waiting’ for the eruption, which
sometimes does not happen, that observers are
presented with the complexity of natural disas-
ters, as well as the challenges faced by those who
predict natural hazards. As with Burke and
Knight’s work on glaciers, ‘The Other Volcano’
highlights the potential for art to move beyond the
sense of accurately conveying scientific informa-
tion, to communicate the ambiguities and hesitan-
cies of Earth science, as well as its explanatory
frameworks and ameliorative advances.
These ideas about risk and public com-
munication, especially in relation to uncertain
futures, are drawn together in a number of recent
collaborations with artists and archaeologists
undertaken by fluvial geomorphologist Mark
Macklin. As part of an ongoing research project
to examine the intersections between river
dynamics and the archaeological record on the
Teleorman River, a lower catchment of the
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Danube, Macklin has worked with artist Judy
Macklin to gather data on recent changes in the
landscape – thereby adding to a multi-sourced
‘thick description’ of the site (Macklin et al.,
2011) – as well as to raise public awareness of the
longer-term evolution of the river landscape and
the likely impacts of climate change.
Intersecting this work with the European Union-
funded project ‘Art-Landscape Transformation’,
Macklin and Macklin (2011) developed a pro-
gramme of creative activities with local residents,
including a four-day workshop with 30 pupils
Figure 4. ‘Measuring Spoon’, Miriam Burke (2011), photographer Guy Archard.
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and their teachers at a school in the valley. Here,
using aerial photographs and river walks, and the
making of sketches and large-scale earth-art-style
sculptures using natural and found materials, the
children were encouraged to get to know and to
model the river landscape within the scale of their
lifetime, as well as that of their parents, grandpar-
ents and beyond (Figure 6).
The collaborative ventures outlined here –
and more are appearing each year – very much
resonate with the appeals for context by
Harrison (1998, 2001), Rhoads (1999) and
Spedding (1997, 1999), appeals that query the
ontic character of landforms as well as their
epistemic framing. It is no small matter that
these calls are sometimes wrapped in an appre-
ciation for earlier geomorphic inquiries that
have an avowed commitment to the aesthetic.
Harrison’s (2001) quantum-based arguments
regarding the importance of emergent features
and forms, for example, contains a persuasive
call for an attentiveness to the diverse, sensible
attributes of landforms, wherein:
Earlier writers on the nature of landscape and the sci-
entific study of scenery, perhaps freer of the con-
straints imposed upon them by issues of process or
time, appeared to identify with the emergent struc-
tures of landscape. For instance, Marr (1900: 2) sug-
gested that, ‘in viewing any scene, the attributes
which strike us specially are size, form, character of
surface, colour and movement . . . ’ and reductionists
argue that these are the subjective elements of a
land-scape since the only objective variables are the
elementary ones. The question can then be asked:
what does this attitude say about our ontological and
epistemological treatment of such emergent charac-
teristics, especially since these elements are those
which constitute the necessary (to human geomor-
phologists) parts of landscape? (Harrison, 2001: 334)
In similar vein, Rhoads (2006: 17) makes a
strong argument for the dissolution of a
subjective-objective divide, insofar as ‘human
experience is as real as the existence of elemen-
tary particles and that experiences such as aes-
thetic appreciation, purposiveness, valuation,
feeling, and harmony have equal ontological
status to the entities of physical science’. Such
Figure 5. ‘The Other Volcano’, Nelly Ben Hayoun (2010), photographer Nick Ballon.
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a holistic effort is consistent with ‘the great tra-
ditions of Humboldt and Ritter, both of whom
were interested in the interconnections among
the physical, biotic, and human features on the
face of the earth’ (Rhoads, 1999: 767).
Yet, while we note that the aesthetic very
much resonates with such contextual concerns,
it is also important to emphasize once more that
there are many forms that such inquiry can take.
Whereas Humboldt, as we outlined earlier,
looked to a holistic universe of harmonious
forces, and Gilbert developed his ‘finer touch’
as a means of illuminating the process-based
nature of landforms, the current collaborative
projects we describe are not so easily categor-
ized. In large part this is because they are not
predicated upon ‘bridging’ disciplinary, con-
ceptual or methodological divides, nor is differ-
ence subsumed, such that one becomes a mere
resource for the other. Instead, these collabora-
tions appear, we want to suggest, to work to a
post-Science Wars zeitgeist, wherein various
aesthetic impulses and traditions are brought
together and valued precisely because of their
differential character.14 Geomorphologists do
not become artists, or vice versa; rather, the aes-
thetics generated by each serve to render the
familiar unfamiliar. In the process an awareness
of other narratives, other modes of research,
other concerns and other publics certainly
emerges, and, we would argue, this awareness
is crucial if geomorphologists and physical geo-
graphers more broadly wish to intervene in what
are heavily politicized, multi-sited debates on
issues such as climate change, biodiversity,
environmental degradation and so on. This, for
Graf (1996), would be evidence of a ‘maturing’,
outward-orientated subfield. As recent events in
the USA, and increasingly in the UK, have made
clear, physical geographers can no longer rest
assured that their data is received as objective.
But also, perhaps, in their willingness to crea-
tively juxtapose fact and fiction, realism and
idealism and so on, we can gain glimpses of how
Figure 6. ‘Making the River Mosaic’, J. Macklin and M. Macklin (2010), photographer J. Macklin.
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such collaborations can produce novel narra-
tives that no longer ‘fit’ the established spaces
of the journal and the gallery, the field site and
the studio. Such efforts resonate with a
burgeoning art-science movement that eschews
the modern-day, institutional compartmentaliza-
tion that distances the arts, as a subcomponent of
the humanities, from the natural sciences, and
looks instead to how these revolve within a
shared history characterized as much by negotia-
tion, mutual learning, and symbiosis as by the
search for fundamental difference.15
VI A post-human geomorphology?
By way of conclusion, we want to offer some
thoughts – by no means didactic – on how such
collaborative ventures may proceed. To begin,
we would note that the artists so far engaging
with geomorphologists, whatever their medium
of choice or genre, tend to work to a humanist
rendering of the sublime. This is by no means
unusual in the art world, insofar as Kant’s
emphasis upon the play of the imagination and
understanding has generally been taken as an
argument on the human power of reason over
and against a meaningless, agency-less nature.
In human geography also, Kantian aesthetics
have tended to be understood as celebrating a
‘human-mind-social’ nexus over and against a
‘non-human-body-nature’ one; indeed, this
framing has characterized all manner of debates
on the human-environment relationship.
Yet it is possible to articulate a ‘post’-human
aesthetic that incorporates those corporeal bod-
ies – animal, vegetative and bacterial – that are
non-human. Here, aesthetic inquiry picks up on
other sense-made worlds, giving them body and
consequence (Dixon, 2010). This post-human
aesthetic can be extended further, moreover,
into a reconsideration of the ‘agency’ of nature,
not as a bundle of forces, materials and events
awaiting human perception and analysis, but
as existing in and for itself. As Clark writes, this
is a nature that does not lend itself to the human
condition, but to a thoroughly impersonal
cosmos:
[It] bears the trace of an ‘infinity’ that is palpably not
of this world, one that is extra-terrestrial in a material
rather than an ethereal or otherworldly sense: an exor-
bitance that no form of reciprocity, no contract, no
economy on this spherical planet or anywhere else
will ever square up. (Clark, 2010: 8)
This seems at first sight, to be at odds with a
geomorphological tradition that, as Graf
(1996) points out, has emphasized its role
within geography more broadly as an unravel-
ling of ‘human-environment’ relationships; to
paraphrase W.M. Davis, this is an outrageous
concept that, perhaps, disrupts the ‘rooting’ of
more comfortable ones (1926: 465–466). Yet
what is of import here is how the ‘human’ has
itself come under query from a number of quar-
ters, including physics, chemistry and biology
as well as the humanities and arts, and found
in many cases to be wanting. To quote from
Davis’ provocative essay on the role of the out-
rageous in rendering the familiar unfamiliar:
The very foundation of our science is only an infer-
ence; for the whole of it rests on the unprovable
assumption that, all through the inferred lapse of
time which the inferred performance of inferred
geological processes involves, they have been going
on in a manner consistent with the laws of nature as
we know them now. We seldom realize the magni-
tude of that assumption. (Davis, 1926: 465–466)
Acknowledgements
We are very grateful for the engaged and construc-
tive comments of two reviewers, to Stephen Tooth,
Helen Roberts and Mark Macklin for reading prior
drafts, and to Miriam Burke, Nelly Ben Hayoun and
Judy Macklin for letting us reproduce images of their
work.
Funding
Research for this work was funded by an AHRC/NSF
grant [AHRC Grant No. AH/I500022/1; NSF Grant
No. 86908] on ’Art/Science Collaboration: Bodies
and Environments’.
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Notes
1. See Smith (1988) for an account of the intersection of
the aesthetic ideas of the Academy with those of scien-
tists at the time.
2. We share this perspective with both historians of art and
historians of science who refuse to accord a privileged
status to ‘art’ objects, thereby opening up the field of
study such that visual practices and products of science
are set alongside artistic practices and aesthetic
concerns (Alpers, 1983; Cook, 2005; Crary, 1992;
Jones and Galison, 1997).
3. Physiognomy, usually dismissed as a scientific dead-
end, or read as a precursor to biological racism, is most
famously associated with the work of Casper Johann
Lavater who sought to illuminate how the fundamental
character, or ‘mental powers’, of the human being could
be read from a simplified sketch or even profile of the
face. Eschewing the mobility of expression (or pathog-
nomy) as ephemeral and confusing, Lavater looked to
the more truthful signs of the face in repose, often pla-
cing his subjects in a specially adapted chair to draw
their silhouettes. This, he wrote, ‘arrests attention by
fixing it on the exterior contours alone, it simplifies the
observation which becomes by that more easy and
accurate’ (Lavater, 1789: 176–178).
4. As such, Humboldt’s work is in contrast with the ‘artistic
geology’ of his contemporary John Ruskin, who sought in
his landscape paintings to present Christian scripture with
scientific precision via preparatory field sketches and
map reading. Ruskin was also fascinated with landforms,
and looked to the erosional processes that reduced moun-
tains to ruinous architectures, which in turn worked spiri-
tually upon their local populations (see Ruskin, 1856).
5. For Humboldt, a political democrat, intellect was a mat-
ter of learning and refinement, not biology. Hence,
‘T[t]here are nations more susceptible of cultivation,
more highly civilized, more ennobled by mental culti-
vation than others – but none in themselves nobler than
others. All are in like degree designed for freedom’
(Humboldt, 1849: 368). Nevertheless, his emphasis
upon the sensibility and discernment of the gentleman
explorer, as well as the need for large-scale, nature-
based studies, had a profound impact upon what has
been termed ‘empire science’.
6. Gilbert was to use similar rhetoric in describing the depth
of features on the moon’s surface as ‘gigantic furrows’
(1893: 279) and ‘boldest carving’ (p. 278). Here, how-
ever, the finer touch could not yet be brought to bear.
7. Certainly, in other visual histories of science, perhaps
most appropriately those of the geological cross-
section, we find a similar value accorded to the diagram
as an ideal explanatory register (Rudwick, 1976).
8. Thank you to Bruce Rhoads for pointing out that
Woolridge’s comments on the ‘betterment’ of mimetic
representation in photographs resonates with the work
of photographic landscape artist and ‘monkey wrench’
author Edward Abbey, wherein the image captures a
stark reality, but also a transcendent, sublime encounter.
It is worth noting that Abbey is also, of course, famous
for advocating a thoroughly visceral encounter with
landscape, such that you ‘walk, better yet crawl, on
hands and knees, over the sandstone and through the
thornbush and cactus. When traces of blood begin to
mark your trail you’ll see something’ (Abbey, 1968: 97).
9. Art as mimetic is also manifest in analyses of the
intense optical phenomena following volcanic erup-
tions, being used to provide proxy information on aero-
sol optical depth. Zerefos et al. (2007), for example,
reconstruct past aerosol optical depth, before, during
and after major volcanic eruptions, by studying the col-
oration of the atmosphere in 500 paintings that depicted
sunsets between 1500 and 1900. They note that the art-
ists under study ‘appear to have simulated the colors of
nature with a remarkably precise coloration’, and con-
clude that their study provides a ‘basis for more
research that can be done on environmental information
content in art paintings’ (p. 4033).
10. A summary of the exhibition, as presented at the New-
castle Borough Museum and Art Gallery in March
2010, can be found at http://www.newcastle-staffs.
gov.uk/documents/leisure%20and%20culture/arts_
dev/creative%20catch-up%2021.pdf.
11. For Burke, reflection on this lineage is crucial to her
practice: she writes: ‘When Caspar David Friedrich
painted The Polar Sea (1823–24), he inspired a sense
of awe and the sublime in his viewers, yet where does
this wonder reside now that we can pull up images of
the fabled and elusive North West Passage on Google
maps? I start with the premise that uncertainty in sci-
ence could also be described as what we do not know.
As mystery. It is left to our imagination to fill the gaps
where technology holds no answers, it blurs the
boundaries of fiction and reality’ (from http://www.
miriamburke.co.uk/about.php).
12. A similar engagement with the poetics of nature and
scientific knowledge can be seen in the work of artist
Dixon et al. 243
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Joanna Berger and geomorphologist Uwe Dornbusch,
undertaken as part of the European Union’s ‘Beaches
at Risk’ Project (2003–2009). The focus of Berger’s
work, ‘Series 130–141’, was the artificial pebbles used
to assess coastal erosion. Cast in tinted resin, and with
a copper core designed to be easily visible and datable
with a metal detector, Berger wrapped lines of love
poetry around the cores of a batch of 11 and then
placed them on one of the French study beaches. See
http://www.sussex.ac.uk/newsandevents/pressre-
lease/media/media457.html.
13. A short summary of the project can be found at http://
www.nellyben.com/projects/the-other-volcano. Their
collaboration has also extended to a series of DIY sci-
ence workshops called ‘Home Chaos’, which explore
‘how to develop thrill . . . Participants were asked to
experiment with their everyday domestic objects, and
try to find them a creative potential. It aims to give
methods on how to juxtapose the epic with banal
details, the extreme with domestic. The result was a
Domestic Super object, which has the property to erupt
dust and gloop at random’ (from http://www.nellyben.
com/workshops/home-chaos-manchester-madlab).
14. As Rhoads (2004) points out, such bridging efforts
may be social as opposed to meta-theoretical.
15. The distinctions drawn between scientific and artistic
endeavours have a long, historical trajectory, punctu-
ated by a series of debates on the relative merits of
each (for example, Arnold, 1882; Huxley, 1880; Lea-
vis, 1962; Snow, 1956). Here, the apparent consensus
regarding the impermeability of their categorical
boundaries has two origins: first, the scientific revolu-
tion of the Renaissance, predicated in large part upon
the rise of Copernican cosmology, empiricism and the
systematic development of modern mathematics, phy-
sics, biology and chemistry; and, second, its gradual
institutionalization in the faculties of the modern uni-
versity, which in the 19th century culminated in the
‘segregation of the European educational system . . .
between classical studies and scientific and technical
training’ (Blair and Grafton, 1992: 535).
References
Abbey E (1968) Desert Solitaire: A Season in the Wild-
erness. New York: McGraw-Hill.
Ackerknecht EH (1955) George Forster, Alexander von
Humboldt, and Ethnology. Isis 46(2): 83–95.
Alexander D (1982) Leonardo da Vinci and fluvial geo-
morphology. American Journal of Science 1: 735–755.
Alexander D (1986) Dante and the form of the land. Annals of
the Association of American Geographers 76(1): 38–49.
Alpers S (1983) The Art of Describing: Dutch Art in the
Seventeenth Century. Chicago, IL: University of Chi-
cago Press.
Arnold M (1882 [1963]) Literature and science. In: Levine
GL and Thomas OP (eds) The Scientist vs. the Huma-
nist. New York: Norton, 29–37.
Baker VR (1993) Extraterrestrial geomorphology: Science
and philosophy of Earthlike planetary landscapes.
Geomorphology 7: 9–35.
Baker VR (1996) Tablets of stone: Ten commandments or a
golden rule? In: McCann SB and Ford D (eds) Geo-
morphology Sans Frontiers. Chichester: Wiley, 60–68.
Baker VR (2008) Planetary landscape systems: A limitless
frontier. Earth Surface Processes and Landforms
33(9): 1341–1353.
Baker VR and Twidale CR (1991) The re-enchantment of
geomorphology. Geomorphology 4: 73–100.
Blair A and Grafton A (1992) Reassessing humanism and
science. Journal of the History of Ideas 53(4): 535–540.
Bunske E (1981) Humboldt and an aesthetic tradition in
geography. Geographical Review 71(2): 379–394.
Burke E (1756 [1987]) A Philosophical Enquiry into the
Origin of Our Ideas of the Sublime and Beautiful, with an
Introductory Discourse Concerning Taste. Oxford:
Blackwell.
Buttimer A (2001) Beyond Humboldtian science and
Goethe’s way of science: Challenges of Alexander
Von Humboldt’s geography. Erdkunde 55(2):
105–120.
Chorley RJ (1978) Bases for theory in geomorphology. In:
Embleton C, Brunsden D, and Jones DKC (eds) Geo-
morphology: Present Problems and Future Prospects.
Oxford: Oxford University Press, 1–13.
Chorley RJ (2000) Classics in geography revisited. Prog-
ress in Physical Geography 24(4): 563–578.
Church M (2010) The trajectory of geomorphology.
Progress in Physical Geography 34: 265–286.
Clark N (2010) Inhuman Nature: Sociable Life on a
Dynamic Planet. Thousand Oaks, CA: SAGE.
Cook S (2005) Late Victorian visual reasoning and Alfred
Marshall’s economic science. British Journal for the
History of Science 38: 179–195.
Cosgrove DE (1979) John Ruskin and the geographical
imagination. Geographical Review 69: 43–62.
244 Progress in Physical Geography 37(2)
at UNIV CALIFORNIA SAN DIEGO on November 18, 2014ppg.sagepub.comDownloaded from
Crary J (1992) Techniques of the Observer: On Vision and
Modernity in the 19th Century. Cambridge, MA: The
MIT Press.
Davis WM (1926) The value of outrageous geologic
hypotheses. Science 63 (1636): 463–468.
Dettelbach M (1999) The face of nature: Precise measure-
ment, mapping, and sensibility in the work of Alexander
von Humboldt. Studies in History and Philosophy of
Biological and Biomedical Sciences 30(4): 473–504.
Dettelbach M (2001) Alexander von Humboldt between
enlightenment and romanticism. Northeastern Nat-
uralist 8(1): 9–20.
Dixon DP (2010) Creating the semi-living: On politics,
aesthetics and the more-than-human. Transactions of
the Institute of British Geographers 34(4): 411–425.
Egger AE and Carpi A (2008) Forming and testing his-
torical hypotheses: G.K. Gilbert and the geology of the
Henry Mountain. Available at: http://www.vision-
learning.com/library/module_viewer.php?mid¼165.
Gellatly AF (1985) Historical records of glacier fluctua-
tions in Mt Cook National Park, New Zealand: A
century of change. Geographical Journal 151: 86–99.
Gemtou E (2011) Depictions of sunsets as information
sources. Leonardo 44(1): 49–53.
Gilbert GK (1877) Report on the geology of the Henry
Mountains. US Geographical and Geological Survey of
the Rocky Mountain Region. Washington, DC: Gov-
ernment Printing Office.
Gilbert GK (1890) Lake Bonneville. Monographs of the
United States Geological Survey I. Washington, DC:
Government Printing Office.
Gilbert GK (1893) The moon’s face: A study of the origin
of its features. Bulletin of the Philosophical Society of
Washington 12: 241–292.
Graf W (1996) Geomorphology and policy for restoration
of impounded American rivers: What is natural? In
Rhoads BL and Thorn CE (eds) The Scientific Nature of
Geomorphology. Chichester: Wiley, 443–473.
Grove JM (1966) The Little Ice Age in the Massif of Mont
Blanc. Transactions of the Institute of British Geo-
graphers 40: 125–143.
Harrison S (1998) Decoherence, quantum theory and their
implications for the philosophy of geomorphology.
Transactions of the Institute of British Geographers
23(4): 501–514.
Harrison S (2001) On reductionism and emergence in
geomorphology. Transactions of the Institute of British
Geographers 26(3): 327–339.
Hartshorne R (1939) The Nature of Geography. Lancaster,
PA: Association of American Geographers.
Hawkins H (2010) Placing art at the Royal Geographical
Society. In: Patel V and Ledda TC (eds) Creative
Compass: New Mappings by International Artists.
London: RGS, 7–16.
Hawkins H (2011) Dialogues and doings: Geography and
art – landscape, critical spatialities and participation.
Geography Compass 5(7): 464–478.
Hejl E (2005) Pictorial study of tafoni development from
the 2nd millennium BC. Geomorphology 64(3): 87–95.
Holmes R (2010) The Age of Wonder. New York: Vintage
Books.
Huggett R (2002) Cranks, conventionalists and geomor-
phology. Area 34(2): 182–189.
Humboldt A (1849 [1997]) Cosmos: A Sketch of the
Physical Description of the Universe, Volume 1. Bal-
timore, MD: Johns Hopkins University Press.
Hunt CB (1988) Geology of the Henry Mountains, Utah, as
Recorded in the Notebooks of G.K. Gilbert, 1875–76.
Boulder, CO: Geological Society of America.
Huxley TH (1880) Science and culture. In: Science and
Culture and Other Essays. New York: D. Appleton and
Company, 7–30.
Jackson ST (ed.) and Romanowski S (translator) (2009)
Essay on the Geography of Plants: Alexander von
Humboldt and Aime Bonpland. Chicago, IL: University
of Chicago Press.
Jones C and Galison P (1997) Picturing Art: Picturing
Science. London: Routledge.
Kant I (1790 [2007]) Critique of Judgement. Oxford:
Oxford World Press.
Knight P (2004) Glaciers: Art and history, science and
uncertainty. Interdisciplinary Science Reviews 29(4):
385–393.
Lavater CJ (1789) Essays on Physiognomy, Volume I.
London: John Murray.
Leavis FR (1962) Two Cultures? The Significance of C.P.
Snow. London: Chatto and Windus.
Leveson D (1988) Geologic clarity: A geologist’s per-
spective on landscape aesthetics. Landscape Journal
(Fall) 7(2): 85–94.
Macklin JE and Macklin MG (2011) Rivers – lines of time.
In: Mills S (ed.) Interventions: Magura Past and
Present. Bucharest: Renaissance, 59–72.
Macklin MG, Bailey DW, Howard AJ, Mills S, and
Robinson RAJ (2011) River dynamics and the Neo-
lithic of the lower Danube catchment. In: Mills S and
Dixon et al. 245
at UNIV CALIFORNIA SAN DIEGO on November 18, 2014ppg.sagepub.comDownloaded from
Mirea P (eds) The Lower Danube in Prehistory:
Landscape Changes and Human-Environment Interac-
tions. Proceedings of the International Conference,
Alexandria, 3–5 November 2010. Bucharest:
Renaissance, 9–14.
Marr JE (1900 [2008]) The Scientific Study of Scenery.
Whitefish, MT: Kessinger Publishing.
Mitchell TF (1993) Art and Science in German landscape
painting, 1770–1840. Oxford: Clarendon Press.
Nelson CM (1980) William Henry Holmes: Beginning a
career in art and science. Records of the Columbia
Historical Society 50: 252–278.
Orme AR (2002) Shifting paradigms in geomorphology:
The fate of research ideas in an educational context.
Geomorphology 47(2–4): 325–342.
Parham (2005) Art and the Pearl River Delta Region. Paper
presented at the International Symposium on Environ-
ment and Society, Chinese History Center for Chinese
Social History Nankai University, Tianjin, PRC, 17–19
August. Available at: http://www.fas.org/china_lands/
art.pdf.
Piper A (2010) Mapping vision: Goethe, cartography, and
the novel. In: Fisher J and Mennel B (eds) Spatial
Turns: Space, Place, and Mobility in German Literary
and Visual Culture. Amsterdam: Rodopi, 27–51.
Pollard DD and Fletcher RC (2005) Fundamentals of
Structural Geology. Cambridge: Cambridge University
Press.
Poole D (1998) Landscape and the imperial subject: US
images of the Andes, 1859–1930. In: Gilbert MJ,
LeGrand C, and Donato Salvatore R (eds) Close
Encounters of Empire: Writing the Cultural History of
US-Latin American Relations. Durham, NC: Duke
University Press, 107–138.
Rhoads BL (1993) Geomorphology as science: The role of
theory. Geomorphology 6(4): 287–307.
Rhoads BL (1994) On being a ‘real’ geomorphologist.
Earth Surface Processes and Landforms 19(3):
269–272.
Rhoads BL (1999) Beyond pragmatism: The value of phi-
losophical discourse for physical geography. Annals of
the Association of American Geographers 89: 760–771.
Rhoads BL (2004) Whither physical geography? Annals of
the Association of American Geographers 94(4):
748–755.
Rhoads BL (2006) The dynamic basis of geomorphology
re-envisioned. Annals of the Association of American
Geographers 96(1): 14–30.
Rhoads BL and Thorn CE (1994) Contemporary philoso-
phical perspectives on physical geography with
emphasis on geomorphology. Geographical Review
84(1): 90–101.
Rhoads BL and Thorn CR (1996a) Toward a philosophy of
geomorphology. In: Rhoads BL and Thorn CE (eds)
The Scientific Nature of Geomorphology. Chichester:
Wiley, 115–143.
Rhoads BL and Thorn CR (1996b) Observation in geo-
morphology. In: Rhoads BL and Thorn CE (eds) The
Scientific Nature of Geomorphology. Chichester:
Wiley, 21–56.
Ritter DF (1986) Process Geomorphology. Dubuque, IA:
WMC Brown Publishers.
Rolston H (1995) Does aesthetic appreciation of land-
scapes need to be science-based? British Journal of
Aesthetics 35(4): 374–386.
Rudwick M (1976) The emergence of a visual language for
geological science 1760–1840. History of Science 14:
149–195.
Ruskin J (1856 [1904]) Modern painters IV. In: Cook ET
and Wedderburn A (eds) The Works of John Ruskin,
Vol. 6. London: George Allen, 1–485.
Sack D (1992) New wine in old bottles: The historiography
of a paradigm change. Geomorphology 5: 251–263.
Schubert C (1980) Contribucion de Venezuela al inven-
tario mundial de glaciares [Venezuelan contribution to
the World Glacier Inventory], Caracas. Boletın de la
Sociedad Venezolana de Ciencias Naturales 34(137):
267–279.
Schubert C (1984) The Pleistocene and recent extent of the
glaciers of the Sierra Nevada de Merida, Venezuela:
Stuttgart. Erdwissenschaftliche Forschung 18:
269–278.
Schubert C (1987) La extension de los glaciares pleisto-
cenos en la Sierra Nevada de Merida [The extent of
Pleistocene glaciers in the Sierra Nevada de Merida],
Caracas. Boletın de la Sociedad Venezolana de Cien-
cias Naturales 41(144): 299–308.
Semken S (2009) Putting Earth science back in its place.
Arizona Geology. Available at: http://www.azgs.az.gov/
arizona_geology/april09/article_earthscience%20.html.
Semken S (2011) A sense of the American Southwest:
Place-based Earth system science for diverse students.
In the Trenches 1: 1–4.
Semken S and Brandt E (2010) Implications of sense of
place and place-based education for ecological integ-
rity and cultural sustainability in contested places. In:
246 Progress in Physical Geography 37(2)
at UNIV CALIFORNIA SAN DIEGO on November 18, 2014ppg.sagepub.comDownloaded from
Tippins D, Mueller M, van Eijck M, and Adams J (eds)
Cultural Studies and Environmentalism: The Conflu-
ence of Ecojustice, Place-Based (Science) Education,
and Indigenous Knowledge Systems. New York:
Springer, 287–302.
Shephard P (1957) Paintings of the New England
landscape: A scientist looks at their geomorphology.
College Art Journal (Autumn) 17(1): 30–43.
Sherman DI (1996) Fashion in geomorphology. In: Rhoads
BL and Thorn CE (eds) The Scientific Nature of
Geomorphology. Chichester: Wiley, 87–114.
Slaymaker O (2009) The future of geomorphology.
Geography Compass 3(1): 329–349.
Smith B (1988) European Vision and the South Pacific
1768–1850: A Study in the History of Art and Ideas.
New Haven, CT: Yale University Press.
Snow CP (1956) The two cultures. New Statesman and
Nation 6 October: 413–414.
Spedding N (1997) On growth and form in geomorphol-
ogy. Earth Surface Processes and Landforms 22(3):
261–265.
Spedding N (1999) Schrodinger’s cat among the pigeons?
Transactions of the Institute of British Geographers
24(2): 231–235.
Stafford BM (1993) Body Criticism: Imaging the Unseen
in Enlightenment Art and Medicine. Cambridge, MA:
The MIT Press.
Stoddart DR (1975) ‘That Victorian science’: Huxley’s
physiography and its impact on geography. Transac-
tions of the Institute of British Geographers 66: 17–40.
Stoddart DR (1981) Geography, Education and Research.
The Geographical Journal 147(3): 287–297.
Stoddart DR (1987) To claim the high ground: Geography
for the end of the century. Transactions of the Institute
of British Geographers 12(3): 327–336.
Tinkler KJ (1985) A Short History of Geomorphology.
Totowa, NJ: Barnes and Noble.
Tooth S (2006) Virtual globes: A catalyst for the
re-enchantment of geomorphology? Earth Surface
Processes and Landforms 31(9): 1192–1194.
Tooth S (2009) Arid geomorphology: Emerging research
themes and new frontiers. Progress in Physical Geo-
graphy 33(2): 251–287.
Twidale CR (1996) Exceptio probat regulam: Do excep-
tional forms test general theories? In: McCann SB and
Ford D (eds) Geomorphology Sans Frontieres. Chi-
chester: Wiley, 40–52.
Woolridge SW (1958) The trend of geomorphology. Trans-
actions of the Institute of British Geographers 25: 29–35.
Zerefos CS, Gerogiannis VT, Balis D, et al. (2007)
Atmospheric effects of volcanic eruptions as seen by
famous artists and depicted in their paintings.
Atmospheric Chemistry and Physics 7(15):
4027–4042.
Dixon et al. 247
at UNIV CALIFORNIA SAN DIEGO on November 18, 2014ppg.sagepub.comDownloaded from