<p>Advancements in stone bead technology, particularly in drilling techniques, emerged during the Indus Valley (Harappan) civilization. Long-constricted cylindrical drill bits, made from a unique stone called Ernestite, were a distinctive feature of this culture. The origin of Ernestite remains uncertain, as it has no known natural analog and its synthesis process is poorly understood. This study presents a mineralogical and geochemical investigation of Ernestite stones and drill bits from multiple Harappan and contemporaneous sites in Gujarat, India, to uncover their origin. The <sup>87</sup>Sr/<sup>86</sup>Sr and ε<sub>Nd</sub>(0) of the drill bits overlap with those of the Ernestite stones, confirming their genetic relationship. The texture and presence of pseudo-mullite (SiO<sub>2</sub> &gt; 40 wt%) with high Al-Ti-bearing hematite suggest that Ernestites are synthetic, created through a sintering process at ~1100 °C. An abundance of sand to silt-sized detrital quartz, along with Fe-Ti-Zr-rich minerals, indicates the use of unevenly powdered sandstones and laterites as raw materials, with geochemical ties to regional sources.</p>

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Origin of the Harappan Ernestites: Geochemical Insights into Provenance and Fabrication

  • M. K. Mahala,
  • Jyotiranjan S. Ray,
  • A. K. Kanungo,
  • G. N. S. Sree Bhuvan,
  • A. Chatterjee,
  • B. G. George,
  • N. Sorcar,
  • Y. S. Rawat,
  • J. S. Kharakwal,
  • S. V. Rajesh

摘要

Advancements in stone bead technology, particularly in drilling techniques, emerged during the Indus Valley (Harappan) civilization. Long-constricted cylindrical drill bits, made from a unique stone called Ernestite, were a distinctive feature of this culture. The origin of Ernestite remains uncertain, as it has no known natural analog and its synthesis process is poorly understood. This study presents a mineralogical and geochemical investigation of Ernestite stones and drill bits from multiple Harappan and contemporaneous sites in Gujarat, India, to uncover their origin. The 87Sr/86Sr and εNd(0) of the drill bits overlap with those of the Ernestite stones, confirming their genetic relationship. The texture and presence of pseudo-mullite (SiO2 > 40 wt%) with high Al-Ti-bearing hematite suggest that Ernestites are synthetic, created through a sintering process at ~1100 °C. An abundance of sand to silt-sized detrital quartz, along with Fe-Ti-Zr-rich minerals, indicates the use of unevenly powdered sandstones and laterites as raw materials, with geochemical ties to regional sources.