2025-08-01_PERMIT FILE - C1981019

• Permit No: C1981019
• IBM Index Class Name: Permit File
• Doc Date: 8/1/2025
• Section_Exhibit Name: Rule 2 Permits -ST
• Media Type: D
• Archive: No

RULE 2 PERMITS

South Taylor – Rule 2, Page 25 Revision Date: 7/21/25
Revision No.: MR-267
Good Spring Creek – The Good Spring Creek watershed encompasses an area of about 35 square miles.
The drainage is characterized by steep sloping upland areas and narrow flat valley bottoms. Slopes
approaching or exceeding 50 percent are common, primarily due to the preponderance of exposed
bedrock strata (CDM, 1985b). Incision has created deep gullies in reaches locally within the permit
revision area, and bank sloughing is contributing to channel widening. Other, more stable reaches are
armored along the channel bottom by cobbles or exposed bedrock. Good Spring Creek has a higher
baseflow than other area creeks in part due to flow contributions from perennial springs in the West Fork
of Good Spring Creek.

Wilson Creek – The Wilson Creek watershed encompasses an area of about 20 square miles. Similar to
Good Spring Creek, the Wilson Creek drainage is characterized by narrow upland areas, steeply sloping
hillsides, and flat valley bottoms. The tributary channels are incised into bedrock. The valley bottom
exhibits morphologic evidence of historic landslide debris accumulation, which serves as a transporting
media for bedrock groundwater discharge and side valley runoff to recharge surface water flows (CDM,
1985b). This recharge mechanism is illustrated by seeps along the banks of the stream.

Taylor Creek – The Taylor Creek watershed encompasses an area of about 7.22 square miles. Slopes are
variable, ranging from 20 to 25 percent in the broad upland area in the highest portion of the watershed,
and generally steeper throughout the remainder of the basin leading to the valley bottom. Bedrock
stability in the area inhibits the accumulation of mass-wasting debris (CDM, 1985b). The channel is
relatively steep, typically greater than ten percent, and incision and bank sloughing are limited due to the
bedrock control.

Surface Water Quantity – The South Taylor permit revision area extends from Colowyo’s existing
mining operations in the Good Spring Creek watershed into the Wilson Creek, and Taylor Creek
watersheds. Baseline monitoring was conducted from September 1996 through September 1997 in each
of these drainages. Additional baseline monitoring was conducted in March 1999 through August 2000
in Good Spring Creek. The Colorado Mined Land Reclamation Division’s Guidelines for the Collection
of Baseline Water Quality Data were utilized during the baseline monitoring. Water quality sampling and
laboratory analyses were conducted in accordance with Rule 2.03.3(4) for analytes defined in Rule
2.04.7(2) and for analytes also listed in the Division’sGuidelines for the Collection of Baseline Water
Quality and Overburden Geochemistry. Field measurements for pH, electrical conductivity, temperature,
dissolved oxygen, and flow were monitored monthly. Quarterly monitoring included a full suite of
analyses at each location. Analysis for metals included only total recoverable concentrations.

Baseline surface water monitoring data are presented in Table 2.04.7-34 and Table 2.04.7-35.
Streamflow hydrographs for representative surface water monitoring locations in these drainages are
presented in figures 2.04.7-22 to 2.04.7-28. Surface water quality as measured by specific conductance is
also illustrated to show seasonal variability with respect to stream flows.

Good Spring Creek – Flow measurements obtained from surface water monitoring locations in Good
Spring Creek in 1996/97 ranged from 0.85 cfs at New Upper Good Spring Creek (NUGSC) to 17.0 cfs at
Lower Good Spring Creek (LGSC). Flows increased in the late spring and early summer months,
corresponding to periods of high snowmelt and surface runoff. Flows measured in 1999/2000 ranged
from 0.2 to 13.0 cfs at EFGSC, 0.26 to 7.0 cfs at Lower West Fork Good Springs Creek (LWFGSC), and
0.18 to 6.5 cfs at Upper West Fork Good Springs Creek (UWFGSC), respectively. Flows also increased
in the late spring and early summer months.

Taylor Creek, Wilson Creek, Jubb Creek – Flow measurements obtained from surface water monitoring
locations in Taylor Creek in 1996/97 ranged from 0.01 cfs at Lower Taylor Creek (LTC) to 2.04 cfs at
Upper Taylor Creek (UTC). These flows are typical of intermittent streams in the area. Surface water