Translated literally from its Greek roots of topos (place) and graphein (to write), topography means “the writing of place.” In modern usage, however, the term has taken on more complex significance. As J. Hillis Miller notes (1995, p. 3), the term has come to refer to both the practice of accurate, scientific representation of particular places on the earth’s surface and the actual configuration of those places. In social science, topographies (both representational and actual) are of interest to researchers investigating relationships between societies and local environments. Such studies are common within the disciplines of geography, anthropology, archaeology, and sociology, and are sometimes found within economics and political science. As the diversity of disciplines with topographical interests reveals, the term topography addresses a fundamental aspect of human experience (place) and thus serves as a foundational category around which social inquiry can be organized.
The dominant modern usage of the term has been in reference to the material configuration of places on the earth’s surface, typically with an emphasis on physical geography rather than the built environment. As Robert Christopherson makes clear (2002, p. 338), topographical studies based upon this emphasis are marked by the observation and recording of landscape features such as hill and mountain relief (dramatic or modest), slope angles (shallow or steep), drainage patterns (wetlands and rivers), and terrain characteristics (rugged or smooth, vegetated or barren) for specific locales. The goal of such studies is to define regional topographies (in the material sense) and provide the environmental knowledge (through representation) needed to facilitate land use decisions appropriate to specific social and economic goals. For instance, as Scott Kirsch (2002) outlines in an essay on John Wesley Powell’s (1834–1902) survey of the Colorado Plateau and surrounding area in the 1870s, in the late nineteenth century the U.S. government was keen to gain knowledge of the arid region of the American West so that land and resource use decisions could be made for an expanding nation. In particular, Powell was charged with ascertaining the irrigation potential of the region for agrarian settlement. Due to the undulating and arid topography, he argued, the grid system of land allotment typical of the Midwestern United States was not suited to the area. Instead, he recommended that all lots should abut water sources, even if that resulted in the alienation of land in irregular shapes. By observing and recording the characteristics of the physical geography of the region and combining the information for presentation in cartographic form, Powell’s work provided distant decision makers with knowledge of local environmental conditions, thereby enabling the setting of social policies regarding land allocation and resource rights. Of course, this relationship between topographical information and land and resource use marks a variety of enterprises and activities. From hikers’ use of maps to navigate mountain ranges to military officers’ use of electronic geographical information to locate specific place-based threats and targets, understanding the material arrangement of the physical environment of certain locales is central to decision making and interaction with places.
While modern topographical studies have tended to focus on the material configuration of places on the earth’s surface in order to facilitate land and resource use, this has not been an exclusive orientation. The term topography has been seized upon by a variety of researchers in the social sciences and humanities who are interested in place-based human experience. The humanistic geographer Yi-Fu Tuan (1974) has written about the centrality of place to human experience, the appreciation of which he terms topophilia. Eugene V. Walter, in an attempt to formulate a more general understanding of humans’ physiological attachment to place, has proposed the study of topisitics as a “framework to grasp the whole experience of space and place” (1988, p. 18). Asserting that “topostic inquiry seeks theories that represent and explain forces that make or break the integrity of located experience” (p. 18), Walter seeks to emphasize that places are more than the sum of their material components and that people’s interactions with places form a central front in inquiries into both environments and the human mind. And, in his work on the relationship between literature, philosophy, and place, Miller (1995, p. 4) deploys the term topography to question how particular ways of knowing places have been inserted into modern Western epistemologies through language. Noting that in modern usage topography shifts between signifying representations of places and signifying actual characteristics of places, he highlights the connections between the production of knowledge about places and the experience of them. In different ways, then, these authors and others have moved understandings of topographies beyond concern for merely the material configuration of places and instead highlighted the multiplicity of ways in which humans become attached to and interact with places.
In an essay that brings together the human and physical aspects of place through a historical materialist approach, Cindi Katz argues for a conceptualization of topography as the sociomaterial terrain produced by an ever-globalizing capitalism. She insists that topographical studies “encompass the processes that produce landscapes as much as they do the landscapes themselves, making clear the social nature of nature and the material grounds of social life” (2001, p. 720). Further, Katz argues, the production of topographies “simultaneously turns on, reveals, and specifies the intricate relations among discrete places.” As such, topographical studies “can provide literal and figurative grounds for developing a critique of the social and political-economic relations sedimented into space and for examining the range of social practices through which place is produced” (pp. 720–721). Ultimately, Katz points out that this framework enables the development of a series of countertopographies. She envisions these as “linking different places analytically in order to both develop the contours of common struggles and imagine a different kind of practical response to problems confronting them” (p. 722). In combination, Katz’s conceptualization of topographies and countertopographies provides a resource for critical analyses of place that takes seriously the impacts of political and economic history in shaping local terrain.
As is evident from this survey, topography is a malleable and widely used term. With its focus on place and human understanding of it, the term and the studies organized around it are central to a comprehensive pursuit of social science. Whether material, social, or both, topographies (both representation and actual) mediate the lives people lead and help to define the places in which they are lived.
SEE ALSO Anthropology; Archaeology; Architecture; Geography; Human Ecology; Irrigation; Natural Resources, Nonrenewable; Water Resources
Christopherson, Robert W. 2002. Geosystems: An Introduction to Physical Geography. 4th ed. Upper Saddle River, NJ: Prentice-Hall.
Katz, Cindi. 2001. Vagabond Capitalism and the Necessity of Social Reproduction. Antipode 33 (4): 709–728.
Kirsch, Scott. 2002. John Wesley Powell and the Mapping of the Colorado Plateau, 1869–1879: Survey Science, Geographical Solutions, and the Economy of Environmental Values. Annals of the Association of American Geographers 92 (3): 548–572.
Miller, J. Hillis. 1995. Topographies. Stanford, CA: Stanford University Press.
Tuan, Yi-Fu. 1974. Topophilia: A Study of Environmental Perception, Attitudes, and Values. Englewood Cliffs, NJ: Prentice-Hall.
Walter, Eugene Victor. 1988. Placeways: A Theory of the Human Environment. Chapel Hill: University of North Carolina Press.
David A. Rossiter
Features. Egypt naturally divides into the river valley, the delta, the Faiyum depression, the mountains running parallel to the river, and the deserts both east and west of the river. The valley is a broad floodplain of black clay alluvium that runs from the first cataract near Aswan to the tip of the delta just north of Cairo. The delta consists of land bordered and crossed in ancient times by seven branches of the Nile. The land is moist and becomes marshy as it nears the coast of the Mediterranean Sea. The Faiyum depression was a lake in ancient times that collected excess water from the Nile. It was connected to the river by a channel now called the Bahr Yousef. The mountain ranges on either side of the river are limestone cliffs in the north, sandstone south of Esna and granite in the Aswan area.
Until the founding of Alexandria by Alexander the Great in 331 b.c.e., Herakleion was the largest harbor in ancient Egypt. Hercules supposedly changed the course of the Nile River at this site. Located at the mouth of the Canopus branch of the Nile, the port city steadily declined in importance until about 800 C.F. when a massive earthquake sent Herakleion and the nearby cities of Canopus and Mcnouthis sliding into the sea. Until recently what little information archaeologists had on the three cities was derived from Greek tragedies and legends. However, in 2000 c.e. an underwater search approximately four miles off the coast of Egypt revealed the site of the ancient harbor. Archaeologists have discovered temples, foundations, and ten sunken ships in waters roughly twenty to thirty feet deep. Among the artifacts recovered thus far are statues of Hapi, the god of the Nile flood, and an unidentified pha-raoh and his queen. Hieroglyphic text on a small stela, or stone tablet, gives the city’s name. Other tablets announce the tariff rates on Greek trade items.
River Valley. The river valley is a convex floodplain. This configuration causes the silt carried by the river to be deposited faster in the middle of the river channel than it is on the plains. These deposits formed high natural levees made of silt and sand. The levees reached heights of five to ten feet and provided protection from the flood during most of the year. Basins formed behind the levees allowing the water to collect when the river did overflow its banks. These basins collected water to a depth of about seven feet. They served as collection centers for water. Irrigation canals could then channel the water to the fields.
Shattered Myth. Irrigation was controlled locally in ancient times. There was no need to control the entire valley in order to practice local irrigation. Farmers could breach the levee to fill the irrigation basin and close the levee again without significantly depleting the stock of water downstream. Thus, early theories that civilization came to the Nile Valley stimulated by the need to control irrigation are likely untrue.
The Delta. During Dynasties 4 and 5 (circa 2700–2400 b.c.e.) the government established new farming institutions in the delta. These institutions, called Mansions of the Gods, managed fruit orchards and vineyards and raised cattle. This activity suggests that the delta was less densely populated than the valley in the earliest dynasties. Cattle remained important to the delta throughout Egyptian history, suggesting that pastureland was its major feature.
The Faiyum. This area experienced considerable development during Dynasty 12 (circa 1938–1759 b.c.e.). In this period the channel connecting the Nile with the lake was open and kept the lake full. New settlements, palaces, and temples were built in this area at the height of the higher floods occurring in the Middle Kingdom (circa 1980–1630 b.c.e.).
Karl W. Butzer, Early Hydraulic Civilization (Chicago: University of Chicago Press, 1976).
Barry J. Kemp, Ancient Egypt: Anatomy of a Civilization (London & New York: Routledge, 1991).
William J. Murnane, The Penguin Guide to Ancient Egypt (Harmondsworth, U.K.: Penguin, 1983).
to·pog·ra·phy / təˈpägrəfē/ • n. the arrangement of the natural and artificial physical features of an area: the topography of the island. ∎ a detailed description or representation on a map of such features. ∎ Anat. & Biol. the distribution of parts or features on the surface of or within an organ or organism. DERIVATIVES: to·pog·ra·pher / -fər/ n.
The relief or surface configuration of an area. Topographic studies are valuable because they show how lands are developed and give insight into the history and relative age of mountains or plains. Topographic features are developed by physical and chemical processes. Physical processes include the relatively long-term tectonic actions and continental movement that lead to subduction of lands in some cases or to the development of high elevation mountains. Earth surface forms are usually altered more quickly by the action of water, ice, and wind, leading to the development of deep canyons, leveling of mountains, and filling of valleys. Chemical processes include oxidation, reduction, carbonation, solution, and hydrolysis. These reactions lead to the alteration of organic and mineral materials that also influence the topographic forms of the earth.
topography (təpŏg´rəfē), description or representation of the features and configuration of land surfaces. Topographic maps use symbols and coloring, with particular attention given to the shape and elevations of terrain. Relief is portrayed by means of contour lines, hachures, shading, or coloring to represent elevations, depressions, and depths of water; natural and human-made features, such as rivers, forests, urbanized areas, bridges, roads, and power lines, are indicated by symbols and color overlays. Topography is often used incorrectly as a synonym for relief; the submarine analogue is bathymetry.
—topographical (top-ŏ-graf-ikăl) adj.