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Unaware of Penfield's discovery, University of Arizona graduate student Alan R. Hildebrand and faculty adviser William V. Boynton looked for a crater near the Brazos River in Texas. [10] Their evidence included greenish-brown clay with surplus iridium, containing shocked quartz grains and small weathered glass beads that looked to be tektites. [16]
Quartz monzonite is an intrusive, felsic, igneous rock that has an approximately equal proportion of orthoclase and plagioclase feldspars. It is typically a light colored phaneritic (coarse-grained) to porphyritic granitic rock.
One of many old stone walls found around the southern and eastern San Francisco Bay in California, this one near San Jose. The East Bay Walls, also known as the Berkeley Mystery Walls, are a misnomer, as many such walls can be found throughout the hills surrounding the San Francisco Bay Area, and extend as far as Chico, Red Bluff and Montague.
For these reasons, the researchers believe that the walls were instead a way to help the inhabitants of the region get around, essentially an ancient Mayan “Google Maps,” they said. The walls ...
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Quartzite can have a grainy, glassy, sandpaper-like surface. Quartzite is a hard, non-foliated metamorphic rock which was originally pure quartz sandstone. [1] [2] Sandstone is converted into quartzite through heating and pressure usually related to tectonic compression within orogenic belts.
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