Edward D. Melillo
Since the early 1800s, Chileans have imagined their nation’s history and destiny through an ever-changing array of transoceanic connections with the rest of the planet. At a deeper level, Chile’s relationship with the Pacific Ocean is built upon myriad collective memories and aspirational identities. The long arc of Chile’s linkages with the Pacific World—or the peoples and ecosystems in and around the Pacific Ocean—has yet to be fully explored by historians. This article fills this lacuna by analyzing five diverse historical episodes that span more than two centuries: first, Valparaíso’s growth into a Pacific commercial hub during the early 1800s; second, Chile’s role in the Californian and Australian gold rushes of the mid-1800s; third, the Chilean victory in the late-19th-century War of the Pacific; fourth, Chile’s burgeoning commercial relationship with China, which began in the years following the Second World War; and, finally, the emergence of a Chilean-Pacific variant of neoliberal ideology in the final decades of the 20th century. These five developments reveal a litany of ambiguities and antagonisms in Chile’s complicated, ongoing association with its western ocean.
Mikael D. Wolfe
What role did drought play in the outbreak of the Mexican Revolution of 1910? Although historians of the Mexican Revolution acknowledge that the effects of drought helped catalyze it, they have not explored in any depth what connects drought to revolution. Instead, they usually subsume it within a more general discussion of agricultural cycles to explain the conduct and fortunes of popular revolutionary armies. In particular, they reference the onset of drought between 1907 and 1909 as exacerbating an economic downturn induced by severe recession in the United States. By then, Mexico had become economically integrated with its northern neighbor through rapidly growing foreign investment, trade, and cross-border migration facilitated by the railroad transportation revolution. These socioeconomic and ecological factors together led to steep declines in wages and earnings, devastating crop failures, spikes in food prices (principally corn and beans), and even famine in the lower and middle classes.
Although suggestive, such passing references to drought in the historiography of the revolution do not furnish a clear picture of its effects and how they may have contributed to social and political conflict. In the 21st century, new technologies, methods, and sources—from historical meteorological reports and climate-related accounts gleaned from archival sources to modern historical climatological data reconstructions—facilitate doing more rigorous climate history. This article provides a sampling of these methods and sources on the role of drought in late 19th- and early 20th-century Mexico that can supplement, elucidate, and even revise our understanding of the origins of the Mexican Revolution.
Guillermo Castro H.
An environmental crisis is neither the result of a single factor nor of a combination of such. On the contrary, it results from a complex combination of modes of interaction between natural and social systems, operating for periods in time and space. This holds true for the environmental crisis in Latin America, understood within the context of the first global environmental crisis in the history of our species. The combination of facts and processes with respect to the crisis in Latin America is associated with three distinct and interdependent historical periods: (1) The first period, one of long duration, marks the interaction with the natural world of the first humans to occupy the Americas and encompasses a timespan of at least 15,000 years before the European conquest of 1500–1550. (2) The second period, one of medium duration, corresponds to European control of the region between the 16th and 19th centuries, a timespan that witnessed the creation of tributary societies grounded in noncapitalist forms of organization, such as the indigenous commune, feudal primogeniture, and the great ecclesiastical properties, which were characteristics of peripheral economies that existed within the wider framework of the emerging modern global economic system. (3) The third period, one of shorter duration, extended from 1870 to 1970 during which capitalist forms of relationships between social systems and natural systems in the region developed. This period was succeeded, beginning about 1980, by decades of transition and crisis, a process that is still ongoing.
In this transition, old and unresolved conflicts reemerge in a new context, which combines indigenous and peasant resistance to incorporation into a market economy with the fight of urban dwellers for access to the basic environmental conditions for life, such as safe drinking water, waste disposal, energy, and clean air. In this scenario, a culture of nature is taking shape, which combines general democratic demands with values and visions from indigenous and African American cultures and those of a middle-class intellectuality increasingly linked to global environmentalism. This culture faces state policies often associated with the interests of transnational corporations and complex negotiation processes for agreements on global environmental problems. In this process, the actions of the past have led to the emergence of a great diversity of development options, all of which are centered in one basic fact: that, in Latin America as elsewhere around the word, if we want a different environment we need to create different societies.
The Caribbean’s most emblematic weather symbol is the hurricane, a large rotating storm that can bring destructive winds, coastal and inland flooding, and torrential rain. A hurricane begins as a tropical depression, an area of low atmospheric pressure that produces clouds and thunderstorms. Hurricane season in the Caribbean runs from June 1 through November 30, although there have been infrequent storms that formed outside these dates. Hurricanes are classified according to their maximum wind speed, and when a tropical system reaches the wind speed of a tropical storm (35 mph), it is given a name. Lists of names, which are rotated periodically, are specific to certain regions. If a named storm is responsible for causing a significant number of deaths or property damage, the name is retired and replaced with another.
Most deaths in a storm came from drowning, from storm surge along the coast or from flooding or mudslides in the interior. Storm-related deaths also occur when structures collapse or when victims are struck by flying debris. One important and underestimated cause of death after the passage of a storm is disease. Even if the destruction is not immediate, the passage of a hurricane can leave significant ecological damage along the coast and in the interior.
Hurricanes can have a devastating effect on a community that takes a direct hit. Repeated hurricane strikes can leave a sense of helplessness and hopelessness, “hurricane fatigue.” Conversely, survivors of a disaster are often left with a feeling of confidence that, since they have endured the effects of at least one deadly hurricane, they can do so again.
Until the last half of the 18th century, meteorology remained primitive, but the Age of Enlightenment brought scientific and ideological advances. Major beneficiaries were royal navies whose navigation manuals and nautical charts became increasingly more accurate. In 1821, William C. Redfield established the circular nature of storms and their counterclockwise rotation, while other scientists showed how wind currents within the storms moved upward. Once the coiled structure of hurricanes were established by mid-century, the term “cyclone” was applied, based upon the Greek word for the coils of a snake.
After the mid-19th century, scientists moved from information gathering to attempts to predict hurricane strikes. Technology, in the form of the telegraph, was a key component in creating a forecasting system aided by organizations such as the Colegio de Belén, in Havana, Cuba. Later in the century, governments worldwide created official observation networks in which weather reports were radiotelegraphed from ships at sea to stations on land. The 20th century experienced advances, such as the use of kites and balloons, and the introduction of weather reconnaissance aircraft during World War II. In April 1960, the first satellite was launched to observe weather patterns, and by the early 1980s, ocean buoys and sophisticated radar systems made forecasts increasingly more accurate.
The History and Visual Culture of Mexico City’s Xochimilco Potable Water System during the Porfiriato
Jeffrey M. Banister and Stacie G. Widdifield
Historians have extensively explored the topic of water control in Mexico City. From the relationship between political power and hydraulics to detailed studies of drainage and other large-scale infrastructure projects, the epic story of water in this megalopolis, constructed over a series of ancient lakes, continues to captivate people’s imaginations. Securing potable water for the fast-growing city is also a constant struggle, yet it has received comparatively less attention than drainage in historical research. Moreover, until quite recently scholars have not been especially concerned with water control as a process of representation—that is, a process shaped by, and shaping, visual culture. Yet, potable water brings together many stories about people and places both within and outside of the Basin of Mexico. As such, the history of potable water is communicated through a diverse array of objects and modern infrastructures not limited to the idea of waterworks in the traditional sense of the term. A more expansive view of “infrastructure” incorporates more than the commonplace objects of hydraulic management such as aqueducts, pumps, wells, and pipes: it also involves architecture, photography, and narrative history, official and unofficial. Built in the first decade of the 20th century as a response to acute water shortages, the impressively modern Xochimilco Potable Water Works exemplifies a system that delivered far more than fresh drinking water through its series of modern electric pumps and aqueduct. The system was a result of a larger modernization initiative launched by the administration of Porfirio Díaz (1876–1911). It wove together an official history of water, which included the annexation of Xochimilco’s springs, through its diverse infrastructures, including the engineering of the potable water system as well as the significance of the structures themselves in terms of locations and architectural elaboration in neo-styles (also known as historical styles) typical of the period. Demonstrably clear from the sheer investment in making the Xochimilco waterworks appealing to the public is that infrastructure can possess a rich visual culture of its own.
Latin American labor has a well-established historiography, in dialogue with trends outside of the region. Environmental history is a newer and more exploratory field. In basic terms, environmental history explores the relationships of humans with the natural world, sometimes referred to as “nonhuman nature.” This can include how humans have affected the natural world, how the natural world has affected human history, and histories of human ideas and belief systems about nature. Labor and environmental history grows from explorations of the connections between these two spheres. Humans interact with the natural world through their labor and from their class perspective. The natural world shapes the work that people do and the institutions and structures humans create to organize and control labor. Changing labor regimes change the ways that humans interact with, and think about, the natural world. Both labor and environmental histories are in some senses investigations of how humans relate to nature. This essay sets Latin American labor and environmental history in global historical context. After offering a chronological summary, it briefly examines connections between U.S. Latino and Latin American labor and environmental histories, and ends with a discussion of contemporary Latin American critical environmentalisms.
Christopher R. Boyer
Human interaction with nature has shaped Latin American ecology and society ever since the first people arrived in the Americas more than fifteen millennia ago. Ancient Native Americans made use of the region’s immense biological diversity and likely contributed to a massive extinction of large animals at the end of the last ice age. Over the ensuing centuries, their descendants took cautious steps to shape the landscape to suit their needs. Colonialism ruptured this process of ecological and social co-evolution, as Europeans conquered the Americas, bringing with them new plants, animals, and diseases as well as a profit motive that gave rise to two economies that further reshaped the environment: the sugar plantation complex and silver mining/hacienda complex. These socio-environmental structures foretold the dynamic of resource extraction and reliance on a single major export destined to more developed countries that characterized most Latin American economies and ecologies after independence. Although most nations sought to break away from this neo-colonial syndrome during the 20th century, they typically did so by increased reliance on agro-industry and the extraction of minerals and petroleum, all of which came at a predictably high ecological cost. At the same time, calls for conservation of resources and biodiversity began to be heard. By the turn of the 21st century, scientists, urbanites, and rural people had become increasingly concerned about the costs of economic “development” and alternative ways of coexisting with nature.
From the time that Columbus arrived in the Caribbean until Spain surrendered power over its mainland American colonies in the early 19th century, Spanish and Portuguese colonial mines poured forth vast amounts of bullion, including some gold and a far greater quantity of silver, both in terms of weight and its overall value relative to gold. Fiscal records indicate that Spanish Americans officially refined gold worth approximately 374,000,000 pesos, each consisting of 272 maravedís, whereas the amount of silver produced reached a value of 3,432,000,000 pesos (to these figures need to be added contraband output, estimated to have been around 17–20 percent). In other words, the colonies refined nine times more silver than gold. While Columbus, Cortés, and other earlier explorers may have fantasized primarily about gold, it was the flood of American silver that touched off the price revolution in Europe and monetarized the emerging world economy, especially because China had a voracious appetite for silver, not gold. At the same time in the American colonies, mining distorted economic life because of the incentives the industry received from a silver-hungry monarchy. Mining also had profound consequences for indigenous society, severely exploited to provide workers for the mines and refining mills.
Colonial refiners used two methods to beneficiate their silver ores, smelting and amalgamation. Smelting was suitable for all types of American silver ores but required large amounts of fuel to heat the ovens. It remained widely used throughout Mexico during the entire colonial period. Amalgamation was a newer technology, adapted to American ores during the mid-16th century. Although it did not require large quantities of charcoal and other fuels, as smelting did, amalgamation depended on the availability of mercury. Nearly all quicksilver used in colonial Spanish American silver mining came from either Huancavelica (Peru) or Almadén (Spain), with occasional supplements from Idria (Slovenia). Whereas both smelting and amalgamation were used widely in Mexico, Andean mines relied on amalgamation.
Alejandro Tortolero Villaseñor
For several years, some of Mexico’s most influential literary figures associated mountains with the presence of certain characteristics: wildlife, botanic variety, and most importantly, backwards and/or mysterious indigenous communities. Order and civilization, it seemed, for writers like Ignacio Altamirano and Manuel Payno, ceased to exist in mountainscapes. For these writes, mountains constituted social afterthoughts—places lacking history and dynamism, places that did not matter. They were, in Braudelian terms, the margins of civilization and factories that supplied human resources to cities.
Such portrayals were not derived from reality, however. Far from solely being dull or dangerous sites where banditry and romantic indigeneity prevailed, Mexico’s mountains were, between the colonial era and the Porfiriato, the places where dramatic transformations took place. Impresarios’ mastery of Mexico’s natural resources fueled the country’s economic growth during the 19th and 20th centuries. Concomitant with this growth came dramatic alterations of the country’s landscape that left much of Mexico’s environment in disrepair.
Mountains, thus, have histories. They are not landscapes where civilization parts ways with society. Such an argument has relevance in parts of the world like Latin America, where nearly half of the people who reside there live at elevations above sea level, and where only 7 percent reside under an elevation of 1,000 meters above sea level.
Before there was Mexico, there was oil. Millennia of organic matter that collapsed and liquefied into fossil fuel rested deep underground and underwater along the half-moon territorial formation that 19th-century geographers named the Mexican Gulf. Hidden by the lush tropical rainforests, marshes, and mangroves that occupied the landscape from the Pánuco River on the border between modern day Tamaulipas and Veracruz and the Bay of Campeche on the South, the oil seeped to the surface in small ponds, sometimes blackening the waters of streams and lagoons from Tabasco to the Huasteca. The human communities who inhabited that part of the globe thousands of years later knew about and utilized nature’s oozing sticky black tar.
The Olmec, who flourished in southern Veracruz from 1200 to 400