Editor’s note: This
article answers the question “What is petrified wood worth?” The
question seems
appropriate since petrified wood is common in
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ntroduction: This report is being conducted at Person X’s request for an assessment and appraisal of a log found just north of Giddings in Lee County, TX in order to determine an estimate of fair market value.
The
log was found in an area occupied by the
mid-Eocene
Yegua Formation (~45 mybp) (Bureau of Economic Geology, 1981). The
Yegua Fm in
central
Description of Log
Characteristics: The log is tan to brown on the outer, weathered surface (Figures 1 and 2), but beige on the inside (Figure 3). The inside is fairly solid, and cellular preservation is good. The fractures and small cavity at the center probably represent desiccation effects before the wood was fossilized. Over most of the exterior, erosion is mild and the log shows fairly good wood texture. Overall, this piece should make a nice display due to the large size and good wood texture over most of the exterior. However, it is recommended that the log undergo a high pressure wash to remove dirt and lichen prior to any exhibition in order to restore the true color of the wood (note lower portion of log in Figure 1 which was under the soil layer prior to excavation).
Weight: The log is approximately eight feet long and is not quite cylindrical because one end is not quite round (a section broken off the trunk) and a bulge in the middle (Figures 1 and 2). Nevertheless, the average diameter is 2.5 feet, 3.5 feet, and 3 feet (from right to left in Figure 1). For approximate calculations, we can round this off to a diameter of approximately three feet. To calculate weight:
V = πr2h = (3.14159)(1.5)2(8) = 56.5487 ft3Since silica is the main fossilizing substance, we can assume the density of the log approximately equals quartz (2.65 g/cc). Therefore:
(97716.098 in3)(16.387 cc/in3)(2.65 g/cc) = 4243375.3 g = 9355 lbs = 4.677 short tons
This is assuming conversions of 453.592 g/lbs and 2000 lbs/short ton.
Because of the approximate nature of the assumptions that went into these calculations, a reasonable estimate of weight would probably be in the range of four to five tons.
Wood Anatomy: A small piece of the log was broken off for microscopic inspection. In cross‑section, the wood has diffuse porosity, vessels either solitary (most common) or in radial multiples of 2 to 4, parenchyma in long, wavy tangential lines typically 1–2 cells wide, and rays 1–3 seriate (Figure 4). This piece was not thin sectioned to observe the radial and tangential surfaces as that was not within the scope of this investigation.
However,
the combination of characteristics listed
above is
typical for only one genus in the Texas Gulf Coast Tertiary—Engelhardioxylon.
Engelhardioxylon
is common in the mid- and late Eocene of the
Estimation of Value:
Retail value of typical
Using the upper limit of value ($0.25 per pound), the value of this log would be about $2,000–$2,500. However this is probably an unrealistically high value because it is a multi-ton lot, and the color of the wood is not remarkable or otherwise extraordinary. A more reasonable estimate of fair market value would probably be closer to about $1,500.
References:
Bureau
of Economic Geology, 1981, Geologic Atlas
of
Manning,
W.E., 1978, The classification within the
Juglandaceae. Annals of the
Figure 1: Front of log |
Figure 2: Back of log |
Figure 3: Cross-section of log. Exposure is relatively fresh. |
![]() Figure 4: Microphotograph of cross-section. Rays are closely spaced vertical lines, parenchyma are horizontal lines. Magnification is approximately 25x. |