
Soda Butte Creek
August 17-21, 1999
Site Description and History
Soda Butte Creek originates by Henderson Mountain near Cooke City, Montana
and flows approximately 8 kilometers into the northeast corner of
Yellowstone National Park (YNP). Soda Butte Creek joins the Lamar River
inside the park (fig. 1).
Soda Butte Creek is the only stream flowing into YNP that has been
significantly impacted by mining activities. The basin upstream of the
park boundary has been the site of numerous mining operations in the past.
To further complicate the issue, differentiating between natural and human-
induced sources of metals is extremely difficult as the geologic units in the
watershed are highly mineralized.
Potential metal sources within the basin include mine tailings at the McLaren
mill site and the associated tailings dam (fig. 2).
Ore from the McLaren Mine, a gold, silver, and copper mine active from 1933
to 1953, was processed at a mill located next to Soda Butte Creek, four miles
upstream from the Park boundary. Gold, silver, and copper were leached out
with cyanide. During the period the mill was operational, approximately
150,000 cubic yards of tailings were deposited on the valley floor of Soda
Butte Creek, which originally meandered through the area currently overlain
by the tailings. Tailings accumulated during the mine's operation were
placed directly instream covering an oxbow of Soda Butte Creek.
In June 1950 heavy rainstorms and flash flooding in the upper Soda Butte
Creek basin caused the McLaren tailings impoundment to break, spilling a
large amount of the tailings into Soda Butte Creek. In 1969 the creek was
rerouted around the north edge of the impoundment. The tailings were
leveled, graded, covered with a 0.5-1.5 meter thickness of alluvial sand and
gravel, and seeded with grass. In 1989 the U.S. Environmental Protection
Agency and Kennecott installed a buttress berm to reinforce the tailings dam
and removed some of the tailings below the dam. Despite these efforts, the
banks and bed of Soda Butte Creek around and downstream from the tailings
are continuously stained by ground and surface water seeps and drains. The
National Park Service (NPS) has expressed concern that the runoff and ground
water at the mill site and tailings pile still appear to be continuing
sources of metals entering Soda Butte Creek.
(text and figures courtesy of Greg Boughton)
Study Design & Sequence of Events
Study Design
The objective of the study was to determine the principal metal sources
in the Soda Butte Creek basin upstream of Yellowstone National Park. Of
particular interest was the relative loading of metals from the McLaren
mill site and tailings dam. Metal loads contributed by tributaries
of Soda Butte Creek were also determined.
Sequence of Events
| August |
| 17-18 |
Stream measurement and reconnaissance |
| 19 |
Tracer injection begins at 1400 hours |
| 20 |
Water quality sampling (Synoptic sampling); Tracer injection ends |
| 21 |
Final sampling of tracer departure; cleanup
|
Photo Gallery
Synoptic Sites
Key
| str | - stream site
|
| rbi | - right bank
inflow |
| lbi | - left bank
inflow |
| con | - confluence
|
| +++ | - downstream
from designated site |
| --- | - upstream
from designated site |
Miscellaneous Photos
| File |
Description |
| | |
| misc |
Soda Butte Creek |
| misc2 |
Soda Butte Country Club |
Results & Acknowledgments
Results
Study findings are reported in:
Boughton, G.K., 2001, Metal loading in Soda Butte Creek upstream of
Yellowstone National Park, Montana and Wyoming: A retrospective analysis
of previous research; and quantification of metal loading, August 1999:
U.S. Geological Survey Water-Resources Investigations Report 01-4170, 68 p.
Acknowledgments
The Soda Butte Creek synoptic was done in cooperation with the
Yellowstone
River Basin NAWQA (USGS) and the National Park Service. Field
assistance was provided by Greg Boughton, Myron Brooks, Melanie Clark,
Ben Kimball, Glenn Laidlaw, Joe Pohl, Katie Randall, and members of
the research team.