Abrigo de Carabali

Folder Type:
Archaeology Site
Primary Title:
Abrigo de Carabali
Alternate Title: Abbreviation
Carabali
Summary Description:
In addition to searching for sites using systematic random transects aligned perpendicularly to the River Santa María, the directors of the Proyecto Santa María followed the practice of selecting specific areas for purposive surveying in the expectation of finding sites that would help resolve major research questions outlined at the outset of the project (Cooke and Ranere 1992). Rock outcrops with perceived potential for housing habitable rock-shelters were one such target since, before 1991, four small shelters in Chiriquí and two in Coclé had provided stratified cultural deposits going back to Preceramic (6000 cal BP): (1) Casita de Piedra, Trapiche, Zarsiadero and Horacio González in the upper drainage of the River Chiriquí (ca 800 masl), (2) Cueva de los Ladrones near the River Grande, Coclé, at 300 masl on the flanks of a large hill (Cerro Guacamayo), and (3) the Aguadulce Shelter in the coastal plains of Coclé not far from the town of Aguadulce. The four River Chiriquí rock-shelters and an open-air site (Hornito-1), located by Ranere and Cooke in the 1970s, contained cultural deposits characterized by a lithic industry of mostly basalt and andesite tools (Talamanca Phase). These were attributed to small family groups of hunter-gatherers. A later industry (Boquete), in which amorphous silicas were now the prevalent raw materials and a wider array of ground stone implements was used, continued to about 2300 cal BP. [More recent research by Ruth Dickau demonstrated that Talamanca Phase peoples were actually farmers, who grew maize (Zea mays), manioc (Manihot esculenta), arrowroot (Maranta arundinacea), coontie starch (Zamia) and yams (Dioscorea)] (Dickau et al. 2007, 2012). During their initial reconnaissance of the Santa María drainage in November, 1991, Ranere and Cooke noticed a prominent elongated hill (Agrigo Carabalí) that lies eastwards of the River Gatú, an affluent of the River Santa María. This hill lies north of the large township of San Francisco, and reaches an elevation of ca 300 masl. It looked to be a promising location for rock-shelters. The base rock belongs to the Cañazas Formation (Upper Miocene) consisting of andesitic and basaltic lavas intermingled with tuffs and volcanic ash. In the dry season of 1983, when an east-west transect (the San Francisco Transect) was surveyed in the vicinity, a search team consisting of Wilson Valerio, Craig Neidig, Francisco Corrales and Doris Weiland located five overhangs in the north-eastern sector of Abrigo Carabalí (SF-5, SF-6, SF-7, SF-8 and SF-9). Small test pits indicated that SF-9 had the greatest potential with a dry floor of ca. 70 m2. The site identifier Abrigo Carabalí was assigned to it. A large boulder divides the shelter into two components akin to chambers. A small test pit (1 x 1 m) excavated that same year on the eastern side of the boulder, and another on the western side (SF-9B) showed that only the uppermost 30 cm contained sherds, and that below this, cultural deposits lacked pottery (Valerio 1985, 1987). Valerio decided to open a trench at SF-9 in 1987, and to use his analysis of lithic materials as the basis for his licenciatura thesis at the Universidad de Costa Rica (Valerio 1987). The shelter talus begins at the drip line. The initial 5o slope increases to ca. 13 o at the end of the 10 m= long stratigraphic trench. Valerio gridded the site out into 1m2 squares assigned letters on the north-south axis and numbers on the east-west axis. The 1983 trench occupied squares 20 G-P. The 1 x 1 m test excavated in the western chamber in 1983 was assigned letter F. Valerio opted to excavate with arbitrary layers of 5 m, exclusively with small hand tools. As in the case of other Panamanian rock-shelters the cultural materials accumulated on the dryish floor were considerably more shallow than those beyond the talus slope whose thickness increased downslope. Two very different stratigraphic members characterize the deposit. The lower one has a reddish tone. Thus it was designated the “red zone”. It does not contain potsherds in the section below the large boulder. The ‘brown zone” above it, however, does contain sherds
Actor: Project Owner
Cooke, Richard
PIDTypeTitleMetadataURL
si_2754952Carabali wall of the shelter for pid si_2754952Carabali wall of the shelterDownload
si_2754954Carabali trench terminated for pid si_2754954Carabali trench terminatedDownload
si_2754955Carabali trench wall for pid si_2754955Carabali trench wallDownload
si_2754956Carabali excavation for pid si_2754956Carabali excavationDownload
si_2754957Carabali long trench for pid si_2754957Carabali long trenchDownload
si_2754958Carabali excavation for pid si_2754958Carabali excavationDownload
si_2754959Carabali lay out for pid si_2754959Carabali lay outDownload
si_2754960Carabali rocks for pid si_2754960Carabali rocksDownload
si_2754961Carabali excavation for pid si_2754961Carabali excavationDownload
si_2754962Carabali excavation for pid si_2754962Carabali excavationDownload
si_2754963Carabali long trench for pid si_2754963Carabali long trenchDownload
si_2754964Carabali test cut for pid si_2754964Carabali test cutDownload
si_2754965Carabali rock-shelter for pid si_2754965Carabali rock-shelterDownload
si_2764659PDF iconStratigraphic and functional analysis of Carabali (SF-9): A rock shelter in the central region of PanamaDownload