Mt. Shasta Springs Project

The Upper McCloud River's Big Springs

The Upper McCloud River's Big Springs

Mt. Shasta’s many springs are critical to California’s water supply

Mount Shasta is a stratovolcano located in the heart of the Klamath-Cascade Region in far northern California (about 50 miles south of the Oregon border).

Its sizable snowpack and glacial meltwater percolate through its porous volcanic geology, eventually emerging as hundreds of springs which feed cold, clear water into the Shasta River, the McCloud River and the Upper Sacramento River.

Mount Shasta’s cold, clean spring waters also feed critical municipal water supplies for the towns of Weed, Mount Shasta, Dunsmuir and McCloud. And provides critical inflow into Shasta Reservoir, which is vital to the state’s agricultural, hydropower, municipal and industrial water supplies.

Despite their obvious importance, no comprehensive study of Mount Shasta’s unique spring resources has ever been created.

In 2007, California Trout convened a group of scientists to design an initial baseline study of Mount Shasta springs — data which is badly needed to help make policy decisions based on the best available data.

Here are the results of that study:

Details Of The Mt. Shasta Springs Study

The scope of the Mount Shasta Springs study included taking water samples from 22 springs on Mt. Shasta. Springs at high, middle, and low elevations, as well as springs located in each of the three watersheds (Shasta, Upper Sacramento and McCloud) were sampled. The water samples were analyzed for a full suite of general water quality and geochemical parameters. A subset of the samples was also analyzed for oxygen and hydrogen isotopes.

Five of the spring samples were age dated based on analysis of the tritium isotope. The purpose of the sampling was to determine the elevation that spring water originates on the mountain, as well as if any of the springs may be related. The flow of nine springs was monitored quarterly to determine if there are seasonal and/or yearly fluctuations. After the first year the study was refined and the 2009 report summarizes and analyzes the first two years of data.

The information collected from the study informed the development of a vulnerability rating for the springs sampled. The rating analysis assumed that Mount Shasta spring waters could be vulnerable to land use (water quality), development (water use), and climate change (variability). The purpose of the vulnerability rating is to assist with water management decisions.



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