Voice of the River

Why and How We Count Pebbles

When the Gallatin dropped to baseflow in mid-August, the Task Force staff, board, and volunteers headed out to the river to count pebbles. Since then, we’ve spent countless hours measuring over 6,000 pebbles. Although laborious and time-intensive, pebble counts (as we affectionately call them) provide a powerful snapshot of fine sediment loads in our rivers and streams.

In case you were wondering how small 4 mm is, check out this nifty visual for standard bead sizes.

In case you were wondering how small 4 mm is, check out this nifty visual for standard bead sizes.

In case you were wondering how small 4 mm is, check out this nifty visual for standard bead sizes.
Sediment is the leading cause of river impairment in Montana. Sediment is a natural part of any river system; however, excess fine sediment (particles smaller than 4 mm) suggests human-induced erosion upstream. In addition, sediment destroys winter refuge for juvenile trout by clogging the spaces between larger pebbles in riffles on the riverbed. By counting pebbles, we can determine how much fine sediment has been deposited since the last high flow event. If the amount of fine sediment in the riffles (shallow, white water sections of the river) exceeds 20%, it is an indicator of poor water quality.

In order to minimize bias in our data, we follow Montana Department of Environmental Quality (Montana DEQ) protocol. Here is a step-by-step guide to counting pebbles paired with stunning images from Rich Addicks, renowned photo journalist and member of the Task Force Board of Directors.

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