MINERALOGICAL RESEARCH COMPANY




General physical features of the Fulgurites from

PECOS PLAINS, NEAR MONAHANS, WARD COUNTY, WEST TEXAS


TYPE II  (
Tubular, with pronounced ridges)

GENERAL INFORMATION ABOUT THE LOCALITY:

The fulgurites from West Texas are found in the sand dunes of the Pecos Plains. The dune field is approximately 70 miles long and 20 miles wide, and stretches in a narrow band from 20 miles northeast of Crane, Texas, to the southeast corner of New Mexico. The dune field runs parallel to an area called the Llano Estacado, Spanish for "staked plains" where the early travelers passing through this area had to mark their way with stakes. The sand in these dunes is composed of very uniform near white Quartz sand, with traces of iron-rich clay. The sand was laid down about 16,000 years ago. These dunes are the highest points in the surrounding area, and are natural targets for lightning strikes. The fulgurites are typically found in the dunes with no vegetation -- far removed from power lines, telephone poles, windmills, etc., and other items which would attract the lightning. The dunes shift as much as 70 feet per year due to the seasonal change of prevailing winds. The erosion of the dunes due to the shifting winds exposes the fulgurites. At a typical lightning strike site, one larger diameter fulgurite will often be found sticking up from the sand as much as 6 inches, and several much smaller diameter fulgurites will then be found in an area within 20 to 30 feet of the main strike. It is not uncommon to find as many as 5 of the smaller fulgurites radiating out of the sand as if someone had stuck them in the sand in a random pattern. If there is not much clay in the sand the fulgurites can be excavated. They are very fragile, and most break off in lengths of 3 to 4 inches or less.

OUTSIDE SURFACE:
FORM: The fulgurite specimens in this group are exceptionally attractive, with pronounced ridges running down the length of the fulgurite tubes. In some specimens the ridges are slightly curved around, while at the same time running lengthwise down the tubes.
COLOR: Light gray, to light gray-tan.
TEXTURE: Very rough, with numerous protuberances / ridges.
SAND GRANULES: White to pale tan in color, small to practically nonexistent, i.e., the sand granules were mostly fused during formation.
GLASSY INTERIOR:
COLOR: Colorless, to light smoky gray, translucent to opaque.
TEXTURE: Very smooth, glass-like.
BUBBLES (GAS
POCKETS) PRESENT:
Numerous, microscopic.


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