Collection 01 is online · Six natural-history studies

Kudzu Country Club
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California

Carrizo Plain

The largest single piece of undeveloped grassland left in California sits two hours from the coast, dead flat, and once a decade it turns the hills solid yellow.

Carrizo Plain

Most people drive past the turnoff their whole lives. The Carrizo is a long, dry valley penned between two ranges in the middle of the state - no town, no gas, a hard-pan lakebed called Soda Lake that goes white with alkali when the water dries. It looks like nothing. It is, in fact, the closest thing California has left to the grassland that covered the whole Central Valley before the plows came: pronghorn, kit foxes, giant kangaroo rats, the works.

It runs right over the San Andreas Fault. The fault line is so plainly visible here that geology classes come to stand on it - you can see streambeds that the moving ground has bent sideways over the centuries, a slow-motion record of the continent grinding against itself. On an ordinary day that's the main event: a huge silence, a straight gravel road, and the fault running up the base of the hills like a seam.

Carrizo Plain - supporting photo

Then, in a wet year, the whole place detonates into color. Hillsides go solid yellow and orange with wildflowers, the superbloom you've maybe seen photographed from space. It doesn't happen on schedule and it doesn't last - a few weeks, and then back to brown. That's the deal with the Carrizo. It rewards people who show up to nothing in particular and look anyway.

Carrizo Plain - supporting photo 2
Carrizo Plain - supporting photo 3

Photos - Superbloom: Bob Wick / Bureau of Land Management, Public Domain. Soda Lake aerial: Alfred Twu / Wikimedia Commons, CC0. San Andreas Fault: Nelson Saarni / Wikimedia Commons, CC BY-SA 4.0. Carrizo Plain valley: Ikluft / Wikimedia Commons, CC BY-SA 4.0. All via Wikimedia Commons.

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