The Titicaca basin sits at the northern end of the expansive altiplano high plains, straddling the highland border of modern Peru and Bolivia. The grasslands are excellent for herding and are also arable along the lakeshore, being a center of tuber production and the font of the domestic Chenopodium and the potato. The lake is full of edible fish as well as having a range of useful waterweeds and reeds along the lakeshore. Early human evidence suggests foraging, hunting, fishing, and birding were all productive subsistence strategies. When these activities began in the area is not firmly known, but there are solid dates for foragers by 4000 BC.
At around 1500 BC archaeologists can see evidence of the earliest settlements, small ceremonial centers, and the onset of territoriality. The term Formative is used to encompass these changes in lifeways from the preceding foraging era. The Formative Period [Note 1] (1500 BC-AD 475) is defined as the time when humans began marking their landscape, creating more permanent settlements, while they domesticated plants and animals. The Formative Period witnessed the creation of a series of ritually charged and intensively agricultural-herding based polities. Some consider the Formative Period a time of social stratification development, with political spheres centered at the civic-ceremonial settlements (Stanish 2003). Others see these long-lived centers as illustrating a strong sense of autonomy and sustainability (Hastorf 2003; Bandy 2004). The Formative Period in this part of the highlands spans almost 2,000 years, thus extending up to the early expansion of the Tiwanaku polity influence (see Chapter 37 in this volume). The end of the Late Formative is marked by the large-scale hegemonic shift around AD 475, when Tiwanaku’s influence is evident outside of the Titicaca basin. The 2,000-year temporal sequence of the Titicaca basin Formative Period is presented in Table 28.1, which lists dates, local, regional, and northern phase names and changes in the main environmental entity, the levels of Lake Titicaca.
Handbook of South American Archaeology, edited by Helaine Silverman and William H. Isbell.
Springer, New York, 2008
Calendar years |
Lake Levels |
S. Basin Phasing |
Basin Phasing Greater Titicaca |
Rowe Chronology |
1500-1000 BCE |
High |
Early Chiripa |
Early Formative I |
Initial Period |
1000-800 BCE |
Low |
Middle Chiripa |
Early Formative II |
Early Horizon |
800-250 BCE |
High, low |
Late Chiripa |
Middle Formative |
Early Horizon |
250 BCE-CE300 |
High, low |
Tiw. I Qalasasaya |
Late Formative I |
Early Intermediate |
CE 300-475 |
High |
Tiw III Qeya |
Late Formative II |
Early Intermediate |
CE 475-1100 |
High |
Tiwanaku IV-V |
Tiwanaku IV-V |
Middle Horizon |
CE 1100-1450 |
Low, high |
Pacajes |
Senorios |
Later Intermediate |
CE 1450-1540 |
High |
Pacajes-Inka |
Inka |
Late Horizon |
Figure 28.1. Map of the Titicaca Basin with archaeological sites mentioned in text (Drawn by William T. Whitehead)
Research on the Formative Period over the past fifty years, and especially in the past twenty, has been extensive, informed by the work of dozens of outstanding scholars whose publications are too numerous to cite in this brief chapter. Out of this work, we now have a series of ceramic sequences, architectural forms and settlement patterns (Figure 28.1) that give a more accurate sense of the events that occurred during this dynamic time period. In this chapter, I will concentrate on the major cultural events that recent archaeological research is clarifying, with a focus on the Middle and Late Formative phases.