The Spanish conquest of Petén was the last stage of the conquest of Guatemala, a prolonged conflict during the Spanish colonisation of the Americas. A wide lowland plain covered with dense rainforest, Petén contains a central drainage basin with a series of lakes and areas of savannah. It is crossed by several ranges of low karstic hills and rises to the south as it nears the Guatemalan Highlands. The conquest of Petén, a region now incorporated into the modern republic of Guatemala, climaxed in 1697 with the capture of Nojpetén, the island capital of the Itza kingdom, by Martín de Ursúa y Arizmendi. With the defeat of the Itza, the last independent and unconquered native kingdom in the Americas fell to European colonisers.
Sizeable Maya populations existed in Petén before the conquest, particularly around the central lakes and along the rivers. Petén was divided into different Maya polities engaged in a complex web of alliances and enmities. The most important groups around the central lakes were the Itza, the Yalain and the Kowoj. Other groups with territories in Petén included the Kejache, the Acala, the Lakandon Chʼol, the Xocmo, the Chinamita, the Icaiche and the Manche Chʼol.
Petén was first penetrated by Hernán Cortés with a sizeable expedition that crossed the territory from north to south in 1525. In the first half of the 16th century, Spain established neighbouring colonies in Yucatán to the north and Guatemala to the south. Spanish missionaries laid the groundwork for the extension of colonial administration in the extreme south of Petén from 1596 onwards, but no further Spanish entry of central Petén took place until 1618 and 1619 when missionaries arrived at the Itza capital, having travelled from the Spanish town of Mérida in Yucatán.
In 1622 a military expedition set out from Yucatán led by Captain Francisco de Mirones and accompanied by Franciscan friar Diego Delgado; this expedition was a disaster, and the Spanish were massacred by the Itza. In 1628 the Manche Chʼol of the south were placed under the administration of the colonial governor of Verapaz within the Captaincy General of Guatemala. The Manche Chʼol unsuccessfully rebelled against Spanish control in 1633. In 1695 a military expedition tried to reach Lake Petén Itzá from Guatemala; this was followed in 1696 by missionaries from Mérida and in 1697 by Martín de Ursúa's expedition from Yucatán that resulted in the final defeat of the independent kingdoms of central Petén and their incorporation into the Spanish Empire.
Geography
The modern department of Petén is located in northern Guatemala. It is bordered on the west by the Mexican state of Chiapas; this border largely follows the course of the Usumacinta River. On the north side Petén is bordered by the Mexican state of Campeche and on the northwest by the Mexican state of Tabasco; Petén is bordered on the east by Belize and on the south side by the Guatemalan departments of Alta Verapaz and Izabal.
The Petén lowlands are formed by a densely forested low-lying limestone plain featuring karstic topography. The area is crossed by low east–west oriented ridges of Cenozoic limestone and is characterised by a variety of forest and soil types; water sources include generally small rivers and low-lying seasonal swamps known as bajos. A chain of fourteen lakes runs across the central drainage basin of Petén; during the rainy season some of these lakes become interconnected. This drainage area measures approximately east–west by north–south. The largest lake is Lake Petén Itzá, near the centre of the drainage basin; it measures . A broad savannah extends south of the central lakes; it has an average altitude of above mean sea level with karstic ridges reaching an average altitude of . The savannah features a compact red clay soil that is too poor to support heavy cultivation, which resulted in a relatively low level of pre-Columbian occupation. It is surrounded by hills with unusually steep southern slopes and gentler northern approaches; the hills are covered with dense tropical forest. To the north of the lakes region bajos become more frequent, interspersed with forest. In the far north of Petén the Mirador Basin forms another interior drainage region. To the south Petén reaches an altitude of approximately as it rises towards the Guatemalan Highlands and meets Paleozoic metamorphic rocks.
Climate The climate of Petén is divided into wet and dry seasons, with the rainy season lasting from June to December, although these seasons are not clearly defined in the south. The climate varies from tropical in the south to semitropical in the north; temperature varies between , although it does not usually drop beneath . Mean temperature varies from in the southeast around Poptún to around Uaxactún in the northeast. Highest temperatures are reached from April to June, and January is the coldest month; all Petén experiences a hot dry period in late August. Annual precipitation is high, varying from a mean of in the northeast to in central Petén around Flores (Nojpetén). The extreme southeast of Petén experiences the largest variations in temperature and rainfall, with precipitation reaching as much as in a year.
Petén before the conquest The first large Maya cities developed in Petén as far back as the Middle Preclassic (c. 600–350 BC), and Petén formed the heartland of the ancient Maya civilization during the Classic period (c. AD 250–900). The great cities that dominated Petén had fallen into ruin by the beginning of the 10th century AD with the onset of the Classic Maya collapse. A significant Maya presence remained into the Postclassic period after the abandonment of the major Classic period cities; the population was particularly concentrated near permanent water sources.
Although there is insufficient data to accurately estimate population sizes at the time of contact with the Spanish, early Spanish reports suggest that sizeable Maya populations existed in Petén, particularly around the central lakes and along the rivers. Before their defeat in 1697 the Itza controlled or influenced much of Petén and parts of Belize. The Itza were warlike, and their martial prowess impressed both neighbouring Maya kingdoms and their Spanish enemies. Their capital was Nojpetén, an island city upon Lake Petén Itzá; it has developed into the modern town of Flores, which is the capital of the Petén department of Guatemala. The Itza spoke a variety of Yucatecan Maya.
The Kowoj were the second in importance, and they were hostile towards their Itza neighbours. The Kowoj were located to the east of the Itza, around the eastern lakes: Lake Salpetén, Lake Macanché, Lake Yaxhá and Lake Sacnab. Other groups are less well known, and their precise territorial extent and political makeup remains obscure; among them were the Chinamita, the Kejache, the Icaiche, the Lakandon Chʼol, the Mopan, the Manche Chʼol and the Yalain.
The Yalain appear to have been one of the three dominant polities in Postclassic central Petén, alongside the Itza and the Kowoj. The Yalain territory had its maximum extension from the east shore of Lake Petén Itzá eastwards to Tipuj in Belize. In the 17th century the Yalain capital was located at the site of that name on the north shore of Lake Macanché. At the time of Spanish contact the Yalain were allied with the Itza, an alliance cemented by intermarriage between the elites of both groups. In the late 17th century Spanish colonial records document hostilities between Maya groups in the lakes region, with the incursion of the Kowoj into former Yalain sites including Zacpeten on Lake Macanché and Ixlu on Lake Salpetén.
The Kejache occupied a territory to the north of the Itza, between the lakes and what is now Campeche. To the west of them was Acalan, inhabited by a Chontal Maya-speaking group with their capital in the south of what is now Campeche state. The Chʼolan Maya-speaking Lakandon (not to be confused with the modern inhabitants of Chiapas by that name) controlled territory along the tributaries of the Usumacinta River spanning southwestern Petén in Guatemala and eastern Chiapas. The Lakandon had a fierce reputation among the Spanish. The Xocmo were another Chʼolan-speaking group; they occupied the remote forest somewhere to the east of the Lakandon. Never conquered, the Xocmo escaped repeated Spanish attempts to locate them and their eventual fate is unknown; they may be ancestors of the modern Lacandon people. The Manche Chʼol held territory in the extreme south of what is now the Petén department. The Mopan and the Chinamita had their polities in the southeastern Petén. The Manche territory was to the southwest of the Mopan.
Background to the conquest
Christopher Columbus discovered the Americas for the Kingdom of Castile and León in 1492. By 1580 this had unified with neighbouring kingdoms to form one Spanish kingdom. Private adventurers thereafter entered into contracts with the Spanish Crown to conquer the newly discovered lands in return for tax revenues and the power to rule. In the first decades after the discovery, the Spanish colonised the Caribbean and established a centre of operations on the island of Cuba. They heard rumours of the rich empire of the Aztecs on the mainland to the west and, in 1519, Hernán Cortés set sail with eleven ships to explore the Mexican coast. By August 1521 the Aztec capital of Tenochtitlan had fallen to the Spanish. Within three years of the fall of Tenochtitlan the Spanish had conquered a large part of Mexico, extending as far south as the Isthmus of Tehuantepec. The newly conquered territory became New Spain, headed by a viceroy who answered to the Spanish Crown via the Council of the Indies. Cortés despatched Pedro de Alvarado with an army to conquer the Mesoamerican kingdoms of the Guatemalan Sierra Madre and neighbouring Pacific plain; the military phase of the establishment of the Spanish colony of Guatemala lasted from 1524 to 1541. The Captaincy General of Guatemala had its capital at Santiago de los Caballeros de Guatemala and covered a wide territory that also included the Mexican state of Chiapas as well as El Salvador, Honduras and Costa Rica. The Spanish imposed colonial rule over Yucatán between 1527 and 1546, and over Verapaz from the 16th to the 17th centuries, leaving the area between – essentially Petén and much of Belize – independent long after surrounding peoples had been subjugated.
Impact of Old World diseases
A single soldier arriving in Mexico in 1520 was carrying smallpox and thus initiated the devastating plagues that swept through the native populations of the Americas. The European diseases that ravaged the indigenous inhabitants of the Americas also severely affected the various Maya groups of Petén. It is estimated that there were approximately 30,000 Chʼol and Chʼoltiʼ Maya in western Petén at the start of the 16th century. Between 1559 and 1721 they were devastated by a combination of disease, war and enforced relocations.
When Nojpetén fell in 1697 there were approximately 60,000 Maya living around Lake Petén Itzá, including a considerable number of refugees from other areas. It is estimated that 88% of the inhabitants died during the first decade of colonial rule because of disease and war. Although disease was responsible for the majority of deaths, internecine warfare between rival Maya groups and Spanish expeditions also took their toll.
Weaponry and armour