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24-06-2015, 12:11

INTRODUCTION

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.



 

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