Death Valley National Park, California

Death Valley

  • Location
    Death Valley National Park, California
  • Formation
    ≈1.8 billion years of exposed rock — Precambrian to Recent
  • Season
    Field study (multiple visits)

Death Valley sits at the intersection of geology, mineralogy, and deep time — one of the most compelling field-research landscapes in North America. At 282 feet below sea level it is the lowest, hottest, and driest place in the United States, yet its exposed formations span nearly 1.8 billion years of Earth history — the rock record laid bare by tilting, faulting, and relentless erosion.

Artist’s Palette is the showpiece of the southern valley: a hillside painted by ancient volcanic hydrothermal activity — iron oxides in reds, yellows, and oranges; chlorite in greens; manganese oxides in purples and blacks. The colors are a direct record of volcanism and oxidation locked into the rock.

Racetrack Playa is one of geology’s enduring puzzles — rocks that move across a dry lakebed, leaving long trails in the cracked mud. The mechanism (rare thin sheets of ice and a gentle push of wind) is a reminder that geological processes can be subtle, slow, and stranger than they look.

The expedition also documented Native American petroglyphs carved into canyon walls, the salt flats of Badwater Basin, remnant telegraph infrastructure from the mining era, and a remarkable desert wildflower bloom in the gravel washes. Documentation spans both digital and film, across multiple visits to the valley floor and the surrounding mountains — geological formations, flora, archaeological features, and the logistics of working one of the harshest field environments in the country.

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Specimens and field photography from this archive are available for research, publication, and museum use. Get in touch to discuss licensing or collaboration.

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