VALLE DEL AZUFRE
BAJA CALIFORNIA SUR
ABSTRACT
From:
Shackley, M. Steven, Justin R. Hyland, and María de la Luz Gutiérrez M. (1996). Mass production and procurement at Valle del Azufre: a unique archaeological obsidian source in Baja California Sur. American Antiquity 61(4):718-731.
Valle del Azufre is a newly discovered source of high quality obsidian in central Baja California which exhibits the most intensive exploitation of any known source in the greater US Southwest/Northwest Mexico. Over 15 subsurface trenches and at least one adit occur at the source. Evidence for the prehistoric distribution of Valle del Azufre obsidian is presented based on EDXRF characterization of the source material and artifacts from the Baja California peninsula. Despite the intensity of exploitation at the source, the distribution of Valle del Azufre glass appears to be largely restricted to the central part of the peninsula.
Valle del Azufre es un recién descubierto yacimiento de obsidiana de alta calidad. Este yacimiento exhibe una explotación intensiva, mayor de cualquier otro yacimiento en el suroeste de los Estados Unidos/noroeste de México. Hay más de 15 minas en el yacimiento. Se presenta evidencia acerca de la distribución prehistórica de obsidiana de Valle del Azufre basado en la caracterización química de la materia prima y artefactos que proceden de diversas partes de la península de Baja California. A pesar de la intensidad de la explotación en el yacimiento, aparentemente la distribución del vidrio volcánico de Valle del Azufre se restringe principalmente en el área central de la península.
Location of Valle del Azufre and important archaeological and geological features of the region. Click on the Laguna San Ignacio region or this thumbnail
to view a NASA satellite image of the region.
Prehistorically excavated tailings at Valle del Azufre, Baja California Sur (Sea of Cortez in background).
Total station map of the two domes and relevant geological and archaeological features. Datum in SE (lower right) corner.
One of the trenches found at Valle del Azufre, Baja California Sur. Over 95% of the obsidian in the foreground is culturally altered.
Bidirectionally excavated tunnel at Valle del Azufre, Baja California Sur. Note large lenticular nodules embedded in the tuff, undoubtedly the goal of prehistoric procurement.
Table 1. Elemental concentrations for Valle del Azufre source standards. All measurements in parts per million (ppm). Sample #s correspond to collection localities (D1=Dome 1; D2=Dome 2; TV=Tres Virgenes).
SAMPLE | Ti | Mn | Fe | Rb | Sr | Y | Zr | Nb | Ba | La | Ce |
D1-1 | 870 | 287 | 11084 | 105 | 83 | 22 | 139 | 5 | 996 | 30 | 58 |
D1-10 | 862 | 306 | 11469 | 107 | 84 | 26 | 142 | 8 | 1067 | 33 | 61 |
D1-2 | 968 | 323 | 12624 | 114 | 86 | 25 | 145 | 5 | 927 | 32 | 57 |
D1-3 | 711 | 278 | 10320 | 98 | 78 | 24 | 128 | 8 | 1087 | 31 | 65 |
D1-4 | 874 | 291 | 10981 | 103 | 83 | 26 | 140 | 8 | 936 | 30 | 49 |
D1-5 | 701 | 273 | 10353 | 98 | 76 | 20 | 128 | 6 | 1033 | 28 | 63 |
D1-6 | 905 | 311 | 11772 | 110 | 91 | 28 | 141 | 8 | 957 | 25 | 58 |
D1-7 | 883 | 319 | 11531 | 106 | 85 | 26 | 142 | 7 | 1092 | 32 | 71 |
D1-8 | 625 | 231 | 9149 | 94 | 73 | 20 | 128 | 3 | 920 | 26 | 56 |
D1-9 | 933 | 298 | 11814 | 113 | 91 | 22 | 146 | 3 | 931 | 27 | 55 |
D2-1 | 885 | 286 | 11451 | 110 | 88 | 23 | 142 | 7 | 917 | 22 | 60 |
D2-10 | 903 | 297 | 10311 | 100 | 83 | 25 | 134 | 4 | 795 | 25 | 48 |
D2-11 | 1066 | 287 | 11308 | 107 | 85 | 25 | 142 | 2 | 812 | 30 | 48 |
D2-13 | 1119 | 328 | 11758 | 112 | 89 | 26 | 151 | 5 | 786 | 29 | 52 |
D2-14 | 961 | 318 | 11976 | 113 | 85 | 22 | 141 | 4 | 931 | 26 | 64 |
D2-2 | 947 | 312 | 11673 | 108 | 91 | 23 | 143 | 4 | 943 | 32 | 58 |
D2-3 | 996 | 357 | 13002 | 112 | 91 | 25 | 149 | 6 | 937 | 28 | 58 |
D2-4 | 857 | 279 | 11256 | 105 | 83 | 21 | 142 | 7 | 911 | 31 | 53 |
D2-5 | 985 | 304 | 11845 | 112 | 88 | 25 | 144 | 10 | 989 | 31 | 64 |
D2-6 | 783 | 320 | 10997 | 102 | 79 | 25 | 136 | 5 | 990 | 37 | 58 |
D2-7 | 922 | 334 | 12432 | 116 | 90 | 22 | 146 | 9 | 967 | 30 | 63 |
D2-8 | 808 | 288 | 11062 | 102 | 82 | 25 | 134 | 6 | 880 | 25 | 57 |
D2-9 | 807 | 312 | 10791 | 97 | 79 | 25 | 135 | 8 | 1014 | 29 | 62 |
TV1 | 840 | 250 | 11180 | 95 | 83 | 23 | 144 | 9 | |||
TV2 | 855 | 220 | 11140 | 97 | 85 | 22 | 143 | 6 | |||
TV3 | 828 | 216 | 10980 | 95 | 81 | 20 | 143 | 5 | |||
TV4 | 889 | 176 | 10390 | 92 | 72 | 20 | 125 | 6 | |||
TV5 | 810 | 177 | 10277 | 85 | 72 | 21 | 135 | 3 | |||
TV6 | 788 | 167 | 9972 | 86 | 75 | 20 | 129 | 7 | |||
TV7 | 730 | 168 | 10581 | 91 | 83 | 21 | 132 | 11 | |||
TVMD1 | 830 | 249 | 10270 | 100 | 82 | 25 | 132 | 5 | 832 | 22 | 54 |
TVMD2 | 986 | 294 | 11317 | 108 | 89 | 25 | 143 | 9 | 828 | 19 | 56 |
TVR1 | 922 | 293 | 11384 | 105 | 84 | 26 | 139 | 9 | 864 | 24 | 45 |
TVR2 | 823 | 247 | 10552 | 96 | 79 | 22 | 133 | 7 | 998 | 28 | 64 |
TVR3 | 905 | 244 | 10558 | 102 | 82 | 23 | 131 | 9 | 856 | 22 | 56 |
TVR4 | 917 | 232 | 9297 | 88 | 75 | 24 | 126 | 6 | 838 | 20 | 53 |
TVR5 | 788 | 217 | 9400 | 93 | 73 | 21 | 125 | 10 | 1057 | 27 | 67 |
TVR6 | 1068 | 377 | 12833 | 118 | 90 | 30 | 143 | 6 | 798 | 21 | 54 |
Mean and central tendency for the data in above table. All measurements in ppm
For more information about the geology and chemistry of the sources of archaeological obsidian in the Baja California region, contact:
M. Steven Shackley ([email protected])
and the recent references below:
Laylander, D. 2006, Obsidian studies and Baja California's Prehistory. Memorias Balances y Perspectivas 2005: IV Encuentro Binacional-La Antropología e Historia de Baja California (CD ROM). Centro INAH Baja California, Mexicali.
Panich, L.M., A. Porcayo M., M.S. Shackley, 2012, Obsidian sources of Northern Baja California. California Archaeology 4:183-200.
Panich, L.M., É. Morachel M., and A. Porcayo M., 2015, Exploring patterns of obsidian conveyance in Baja California, Mexico. Journal of California and Great Basin Anthropology 35:257-274.
Panich, L. M., M.S. Shackley, and A. Porcayo M., 2017, A reassessment of archaeological obsidian from southern Alta California, and northern Baja California. California Archaeology 9:53-77.
Shackley, M.S., J.R. Hyland, and María de la Luz Gutiérrez M., 1996, Mass production and procurement at Valle del Azufre: a unique archaeological obsidian source in Baja California Sur. American Antiquity 61:718-731.
Sosa, A.D., 2014, Obsidian exchange in prehistoric Baja California: an initial look at regional exchange networks in the peninsula. Master's thesis, Department of Anthropology, California State University, Northridge.
This page maintained by Steve Shackley
Copyright © 2018 M. Steven Shackley. All rights reserved.
Revised: