A History of Réunion

• Introduction
• Chapter 1 Before Human Footprints: The Volcanic Origins and Unique Ecology of a Future Island
• Chapter 2 Early Encounters: Arab Traders, Portuguese Navigators, and the Uninhabited Island
• Chapter 3 The Dawn of Colonization: The French East India Company and the First Settlers on Île Bourbon
• Chapter 4 The Coffee Boom: Establishing a Plantation Economy and Society in the 18th Century
• Chapter 5 A Society Built on Chains: The Brutal Realities of Slavery on Île Bourbon
• Chapter 6 Voices in the Hills: Maroonage and Resistance to Slavery
• Chapter 7 From Île Bourbon to Île de la Réunion: The Tumultuous Years of the French Revolution
• Chapter 8 Under British Rule: A Brief Interlude and the Rise of Sugar
• Chapter 9 The Sugar Revolution: Transforming the Landscape and Economy
• Chapter 10 The 1848 Abolition of Slavery: A New Era of Freedom and its Challenges
• Chapter 11 Indentured Labor: The Arrival of Indian, Chinese, and African Workers
• Chapter 12 A Creole Society in the Making: Cultural Fusion and Social Stratification in the 19th Century
• Chapter 13 The Late Colonial Period: Economic Struggles and Social Tensions
• Chapter 14 Réunion in the First World War: A Distant Conflict's Local Impact
• Chapter 15 Between the Wars: Economic Stagnation and Social Change
• Chapter 16 The Second World War: Allegiance to Vichy and the Liberation of the Island
• Chapter 17 The End of an Era: Becoming a French Overseas Department in 1946
• Chapter 18 Post-War Reconstruction and the Challenges of Departmentalization
• Chapter 19 The Debré Era and the "Children of Creuse": A Controversial Chapter
• Chapter 20 Economic Modernization and Social Unrest in the Late 20th Century
• Chapter 21 The Rise of a Plural Identity: Language, Music, and Cultural Revival
• Chapter 22 Entering the 21st Century: Political and Economic Landscapes
• Chapter 23 Contemporary Society: Challenges of Unemployment, Inequality, and Globalization
• Chapter 24 A Land of Contrasts: Tourism, Natural Heritage, and Environmental Concerns
• Chapter 25 Réunion Today and Tomorrow: Identity, Autonomy, and the Future within the French Republic

Lost in the vast expanse of the Indian Ocean, some 680 kilometers east of Madagascar, lies a fragment of France, a piece of the European Union where the currency is the euro and the official language is French, yet the air hums with a rhythm that is uniquely its own. This is Réunion, an island born of fire and shaped by waves of human migration, a place whose history is as dramatic and complex as its volcanic, mountainous terrain. It is a story that begins not with people, but with the violent geological forces that thrust a mountain from the seabed, creating a rugged sanctuary of unparalleled natural beauty that would remain untouched by human hands for millions of years.

This book, ‘A History of Réunion,’ embarks on a chronological journey to tell the island's story. It is a narrative that moves from the primal world of its volcanic creation to the twenty-first-century challenges of a globalized society. We will traverse the centuries, from the first tentative sightings by Arab sailors and Portuguese explorers of an uninhabited land they called Dina Morgabin or Santa Apollonia, to the deliberate and transformative colonization by the French. The tale that unfolds is one of profound transformation, of an empty island becoming a home, a colony, and ultimately, a French department.

The story of Réunion is fundamentally a story of encounters. It is the story of how a small, isolated island became a crucible of cultures, a meeting point for people from three continents. The first French settlers did not arrive on an empty stage, but on an island whose unique ecology had evolved in isolation. Their arrival marked the beginning of a new chapter, one that would irrevocably alter the island’s destiny. They brought with them ambitions of fortune, first through coffee and later through the all-consuming cultivation of sugar cane, endeavors that demanded a vast and continuous supply of labor.

Thus began the darkest chapter in Réunion’s history: the era of slavery. For nearly two centuries, men, women, and children were forcibly brought from East Africa and Madagascar to toil on the plantations. Their lives, struggles, and resistance form a critical and painful thread in the fabric of Réunionese society. The hills and inaccessible volcanic craters, the cirques, became sanctuaries for escaped slaves, known as maroons, who forged new communities and a culture of defiance that echoes to this day. This book will delve into the brutal realities of this system and the enduring spirit of those who fought against it.

The island’s identity has been as fluid as its name, which has shifted with the political tides of France. Known for most of its early colonial period as Île Bourbon, in honor of the French royal dynasty, it was renamed Réunion in 1794, a nod to the revolutionary union of forces in Paris. It would briefly become Île Bonaparte under Napoleon before reverting to Bourbon, and then, finally and permanently, back to Réunion in 1848, the very year that slavery was abolished. Each name change signifies a pivotal moment, a realignment of power and identity both in mainland France and on the island itself.

The abolition of slavery in 1848 did not end the demand for cheap labor. It merely opened a new chapter of migration, this time in the form of indentured servitude. Workers were brought from South India, and to a lesser extent from China and other parts of Africa, introducing new languages, religions, and cultural practices to the island. This period cemented Réunion’s status as a profoundly mixed, or créole, society. The interplay between these diverse groups—European landowners, the descendants of African slaves, Indian laborers, and Chinese merchants—created a complex social hierarchy and a vibrant, syncretic culture that is the island's most defining characteristic.

Our journey will continue through the tumultuous twentieth century. We will examine the island's experience of the two World Wars, its allegiance to the Vichy regime during the second great conflict, and its subsequent liberation. A pivotal moment came in 1946, when Réunion transitioned from a colony to an overseas department of France, a change in status that promised equality and integration but also brought a new set of challenges. This departmentalization profoundly reshaped the island's economy, politics, and social structure, tying it ever closer to metropolitan France.

The latter half of the twentieth century was a period of modernization and social change, but also of significant social unrest. We will explore the controversial "Debré era," which included the organized relocation of over two thousand Réunionese children to rural France, a deeply divisive episode known as the "Children of Creuse" affair. This period highlights the complex and often fraught relationship between the island and the French mainland, a dynamic of dependence, assimilation, and the persistent search for a distinct Réunionese identity.

Today, Réunion is a land of striking contrasts. It is home to one of the world's most active volcanoes, the Piton de la Fournaise, whose frequent eruptions are a constant reminder of the island’s fiery origins. Its dramatic landscapes, from the volcanic peaks and lush forests to the coastal lagoons, have earned it a UNESCO World Heritage Site designation and made it a prime tourist destination. Yet, behind the postcard image of a tropical paradise lie pressing contemporary issues: high unemployment, significant social inequality, and the environmental pressures that come with a growing population on a small island.

This book aims to provide a comprehensive and accessible account of this intricate history. It is a story that, while centered on a small island, reflects broader global themes of discovery, colonialism, the brutalities of slavery, the complexities of cultural fusion, and the ongoing struggle for identity and self-determination in a post-colonial world. It is the story of how an uninhabited volcanic rock in the middle of the ocean became the vibrant, complex, and fascinating society of Réunion today. Our narrative begins, as the island itself did, in fire and isolation, with the geological saga of its birth.

Long before any sail broke the horizon, before the island had a name or a place in the minds of men, it was a work in violent progress. Réunion did not rise gently from the Indian Ocean; it exploded into existence, a colossal mountain of fire built layer by layer from the seabed, four thousand meters below. For millions of years, this geological infant grew in the profound isolation of the sea, its story written not in words but in flows of basalt and pillars of steam. Its history began in the deep furnace of the Earth’s mantle, a process that continues to shape the island to this day, providing a constant, fiery reminder of its primordial origins.

The island owes its very being to a geological feature known as the Réunion hotspot. This is a stationary plume of exceptionally hot rock rising from deep within the mantle, a kind of permanent blowtorch aimed at the underside of the Earth's crust. Tectonic plates, vast rafts of crust, drift slowly over these hotspots. As the Indian Plate crept northwards for millennia, this particular hotspot punched through it repeatedly, creating a chain of volcanic islands and undersea plateaus like a string of pearls. This grand volcanic lineage begins spectacularly some 66 million years ago with the Deccan Traps, a gargantuan flood of basalt that covered a huge portion of central India and may have played a role in the extinction of the dinosaurs. As the plate continued its journey, the hotspot went on to form the Laccadives, the Maldives, the Chagos Archipelago, and finally the Mascarene Islands, of which Réunion is the youngest and only remaining volcanically active member.

The island as we know it began to break the ocean surface between two and three million years ago, a relative newcomer in geological terms. It is not a single volcanic cone, but a composite of two massive shield volcanoes. The first and larger of the two is the Piton des Neiges, or "Peak of the Snows," which forms the northwestern two-thirds of the island. This elder giant built itself up through countless effusive eruptions, where fluid lava flowed steadily outwards, creating a broad, gently sloping edifice. Reaching an impressive 3,070 meters (10,072 feet), it is the highest point in the entire Indian Ocean basin. The name is a touch optimistic—true snow is a rare dusting seen only in the austral winter—but it speaks to the immense scale of this dormant peak.

Though Piton des Neiges has been quiet for at least 20,000 years, its retirement has been anything but peaceful. The forces of erosion, fueled by tropical deluges, began to relentlessly dismantle the mountain. The volcano's structure, weakened by the collapse of its old magma chamber, became susceptible to massive landslides. Over thousands of years, this process of collapse and erosion carved three enormous, breathtaking amphitheatres into the volcano's flanks. These are the island's famous cirques: Salazie to the east, Mafate to the northwest, and Cilaos to the south. They are not gentle valleys but vast, steep-walled basins, hemmed in by towering cliffs, or remparts, that can exceed a thousand meters in height. These cirques are the very heart of the island's dramatic topography, colossal wounds that reveal the geological bones of the ancient volcano and create a world within a world, isolated and difficult to access.

To the southeast, nestled on the flank of its older, sleeping sibling, is Réunion's second volcano: the Piton de la Fournaise, the "Peak of the Furnace." The name is entirely appropriate. This is one of the most active volcanoes on the planet, a dynamic and frequently erupting shield volcano that ensures the island’s creation story is an ongoing narrative. Having emerged from the sea more than 500,000 years ago, it is a geological youngster, characterized by a large U-shaped caldera, the Enclos Fouqué, which is open to the sea on its eastern side. Within this caldera rises the main cone, topped by two craters, the older Bory and the currently active Dolomieu.

The eruptions of Piton de la Fournaise are, for the most part, of the Hawaiian type. They are more spectacle than menace, featuring mesmerizing fountains of fire and fluid lava flows that travel down the volcano's slopes. Most of this activity is contained within the uninhabited Enclos caldera. The lava flows steadily towards the ocean through a burnt, alien landscape known as the Grand Brûlé ("Great Burnt Land"), occasionally tumbling over the coastal cliffs and into the sea in a dramatic explosion of steam, adding new territory to the island. With eruptions occurring, on average, more than once a year, the Furnace provides a constant, tangible link to the powerful forces that built Réunion from the ocean floor.

For eons, the island was a sterile landscape of bare volcanic rock. Life, however, is tenacious. The colonization of this isolated landmass was a slow and haphazard affair, governed by the "Three Ws": wind, waves, and wings. Microscopic spores of ferns and mosses, light as dust, would have been among the first arrivals, carried across thousands of kilometers of ocean by high-altitude winds. Seeds, too, could make the journey this way, particularly those with parachute-like structures. The ocean itself acted as a conveyor belt, carrying floating mats of vegetation torn from the coasts of Africa or Madagascar, which could harbor small lizards, insects, or seeds protected within their fruits.

The final vectors were birds. Migratory or storm-blown seabirds, using the new island as a resting place, would have carried seeds with them, either stuck to their feathers or, more commonly, within their digestive tracts, to be deposited with a convenient dose of fertilizer. This biological invasion was a lottery; only a tiny fraction of species from the surrounding continents could survive the arduous journey and then establish themselves in the harsh volcanic soil. Those that did found themselves in a world of opportunity, free from the competitors and predators of their ancestral homes.

This unique combination of isolation and opportunity led to the evolution of a truly distinct flora. The colonizing plants, over countless generations, adapted to the island's varied microclimates, from the humid, windy eastern coast to the drier leeward west, and from the hot coastal plains to the cool, misty highlands. This process of adaptive radiation resulted in a high degree of endemism, with a remarkable number of plant species found nowhere else on Earth. Before the arrival of humans, the island was cloaked in a dense and varied tapestry of forests. The lowlands were thick with palms and hardwood trees. As one ascended, these gave way to misty, primeval forests dominated by unique trees like the highland tamarind (Acacia heterophylla) and groves of giant tree ferns, or fanjans (Cyathea borbonica), creating an almost prehistoric landscape. The island's flora also includes a stunning variety of native orchids, hibiscus, and palms, making it a botanical treasure trove.

The first animal colonists were, by necessity, small and hardy. Insects, spiders, and mollusks likely arrived via the same windborne and seaborne routes as the plants. Reptiles, such as geckos and skinks, probably rafted in on floating debris. Conspicuously absent were any native land mammals. The vast ocean expanse was an impassable barrier for creatures like cats, primates, or large herbivores. The only mammals to make it on their own were bats, arriving, of course, on the wing. This absence of ground-based predators had a profound effect on the evolution of the animals that did successfully colonize the island.

Birdlife, in particular, flourished. With no predators to fear on the ground, some species began to lose their powerful flight, a trait that requires enormous energy to maintain. The most famous of these, though known only from early accounts and subfossil remains, was the Réunion Solitaire. A relative of the dodo from neighboring Mauritius, this was a large, whitish ibis that was described by early visitors as being virtually flightless and was later hunted to extinction. The island was also home to a host of other now-vanished birds, including a native swamphen, a kestrel, a night heron, a pink pigeon, and a parrot. Those that survived into the modern era include endemic species like the Réunion stonechat, the Réunion bulbul, and the Réunion olive white-eye, all perfectly adapted to their unique island home.

The pristine ecosystem of early Réunion was a finely tuned world, developed in serene isolation. Large, slow-moving tortoises grazed on the lowland vegetation, while fruit-eating birds and bats acted as crucial seed dispersers, helping the forests to regenerate and expand. The rivers ran clear from the mountains to the sea, and the coastlines, built from black volcanic sand and rugged lava cliffs, were fringed in places by fledgling coral reefs. It was a complete world, dynamic and self-sustaining, forged by the planet's internal fire and sculpted by wind and rain. It was a land that had never known the tread of a human foot, a unique biological sanctuary entirely unaware that its long, splendid isolation was about to come to an abrupt and irreversible end.