- 96
FOUR TRUNKS OF INDONESIAN PETRIFIED WOOD
Estimate
2,500 - 3,500 USD
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Description
- GENTENG FORMATION, BANTEN, WEST JAVA, INDONESIA
Four trunks of Dipterocarpaceae (20 x 61 x 20 cm; 20 x 90 x 20 cm; 20 x 72 x 16 cm; 15 x 58 x 15 cm), Pliocene (5-3 million years ago).
Condition
To request a condition report for this lot, please email science@sothebys.com
In response to your inquiry, we are pleased to provide you with a general report of the condition of the property described above. Since we are not professional conservators or restorers, we urge you to consult with a restorer or conservator of your choice who will be better able to provide a detailed, professional report. Prospective buyers should inspect each lot to satisfy themselves as to condition and must understand that any statement made by Sotheby's is merely a subjective qualified opinion.
NOTWITHSTANDING THIS REPORT OR ANY DISCUSSIONS CONCERNING CONDITION OF A LOT, ALL LOTS ARE OFFERED AND SOLD "AS IS" IN ACCORDANCE WITH THE CONDITIONS OF SALE PRINTED IN THE CATALOGUE.
In response to your inquiry, we are pleased to provide you with a general report of the condition of the property described above. Since we are not professional conservators or restorers, we urge you to consult with a restorer or conservator of your choice who will be better able to provide a detailed, professional report. Prospective buyers should inspect each lot to satisfy themselves as to condition and must understand that any statement made by Sotheby's is merely a subjective qualified opinion.
NOTWITHSTANDING THIS REPORT OR ANY DISCUSSIONS CONCERNING CONDITION OF A LOT, ALL LOTS ARE OFFERED AND SOLD "AS IS" IN ACCORDANCE WITH THE CONDITIONS OF SALE PRINTED IN THE CATALOGUE.
Catalogue Note
Petrified wood (from the latin Petro, meaning stone, and thus literally meaning "wood turned to stone") is the result of a process in which organic materials transition to stone via mineralization. Petrified wood is distinct from other fossilized plants, which are typically impressions, as they are actually three-dimensional representations of the original material, in which cell walls are replicated by minerals, and in most cases, completely replaced by them. Each chemical transformation is unique, with each specimen having its own distinct coloration; here we see mineralizations reminiscent of quartz, chalcedony, and jasper. A beautiful grouping, with colors of coffee, caramel, ivory and blue.