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PLAN-Boulder County

Comments on OSMP proposed route alternatives
for Trail 13 and Trail 14 in Spring Brook/Doudy Draw Natural Area


 

July 29, 2007

PLAN-Boulder County commends the OSMP staff for careful preparation of alternatives for routing these proposed trails in the short time frame available.

However, proper management of Open Space and Mountain Parks resources requires taking adequate time to ensure:

It is clear from the public field trip on July 17 that the information available to date falls far short of meeting these VMP criteria. To cite one example, thousands of yards of the routes proposed are planned to cut laterally into relatively steep slopes (20-30ˇ) of Pierre Shale. Numerous geotechnical studies [e.g. Squire 2001] have shown this shale unit to be susceptible to rapid erosion and repeated slumping at such angles. Indeed, one geologist on the tour observed many slumps already present along the flagged routes. The reason that the slopes are steep is because the shale erodes rapidly when the edge of the gravel protecting cap is removed.

These elementary soil characteristics have not been taken into account in the initial routing proposal, apparently because of the rush to meet deadlines. This does not reflect badly on the staff who have worked on the detailed preliminary routes, but it does demonstrate that the planning process has been unwisely rushed, and that we need to take the time to do the job right. Rushing to try to begin construction this season will result in badly built, unsustainable, and very expensive trails; serious damage to the resource; an inability to properly monitor the trails' effects; and a much more costly future set of consequences to deal with. There is no major cost associated with taking the time to do the job right. The only problems associated with some delays are that current social trails will continue to be used for a time. The degradation caused by this process, and the difficulty of mitigation, will be trivial compared with that caused by trails built in the wrong places. Once new trails are built, there is likely to be greatly increased visitation in this area, which will enormously compound the problem if this is not done correctly.

Now that a preliminary agreement with the Denver Water Board regarding the canal crossing finally has been reached, it is time to rethink the trail alignments that were largely done without knowing where the crossing would be. Attempts to decide routing in advance of this milestone disrupted monitoring plans for both the Goshawk Ridge Trail and Trails 13 & 14. It is hard to route a trail or to plan monitoring when you don't know where it is going! We congratulate the OSMP staff who have brought these difficult negotiations to a preliminary conclusion. However, it is time for another careful look at the alternatives.

We believe that, in light of the recently negotiated mid-canal crossing location, trail alternatives need to be seriously reconsidered. For example, two possible alternative routes for the Trail 13-Stem Trail have not been considered. These are:

These alternative routes have obvious potential advantages, as staff admitted on the public field trip. These routes warrant serious consideration at the very least.

A third significant problem relates to invasive weeds in the area. Jointed goat grass (Aegilops cylindrica Host) is a major problem on a large number of trails in the OSMP system. This invasive species is difficult to control, and it is easily spread by hikers, animals, and probably mountain bikes. The seeds fit the grooves in Vibram soles, and they will probably fit many bicycle tire treads. A. cylindirca is spread as a seed contaminant in agricultural areas, and thence by grazing livestock like horses, because the seeds survive passing through the guts of ruminants.

Jointed goat grass has become a serious problem and has seriously infested the bottom of the Doudy Draw Trail. The proposed rerouting of the Doudy Draw Trail before this invasive is controlled will only ensure that the infestation moves up the slope and becomes much larger and more difficult to control. Yet the Suitability Analyses do not even mention this invasive except to say that there is a possible problem during construction of Trail 13 Stem if construction is done from the direction of Doudy Draw. There is no mention of it being spread by users, not only to this trail, but to all the others being proposed.

This issue must be seriously considered and preventative measures must be taken before trail construction. Otherwise, it is highly likely to damage the resource and to result in major expenses for weed control.

Recommendations

Our principal recommendations and observations are as follows:

  1. delay construction until next year;
  2. do not build a trail in Spring Brook Meadow; there are a number of alternative routes for the currently mapped Trail 13 alternatives. This meadow provides: exceptional habitat for deer and elk; possible presence of Preble's Jumping mouse; confirmed lion hunting grounds; vulnerability to weed invasion, as demonstrated by presence of high-priority weeds (such as Dalmatian toadflax and Sulfur cinquefoil) along the existing social trail;
  3. funneling visitors into Spring Brook meadow will inevitably promote off-trail travel throughout the area, including the length of the meadow along the desire-line and the current social trail northward;
  4. implement the control of jointed goatgrass in Doudy Draw this fall and winter, and verify that control has been successful before attempting to schedule the construction of the rerouted Doudy Draw Trail or Trails 13 and 14;
  5. as the next step in the public input process, provide maps at a scale useful for trail planning that include critical wildlife habitat areas, critical plant communities; and soils/geology. These are fundamental tools for planning ecologically sustainable trails;
  6. complete a monitoring plan for the natural resources, including evaluation of resource impacts; compliance monitoring; visitor conflict issues; and plans for management actions when expected criteria are not achieved;
  7. as a first step, build a modified route from the Doudy Draw stem trail-possibly up the west side of the stony ridge, staying far enough west to avoid tempting views into the Lindsey Pond area;
  8. this approach should connect with upper Trail 14, which should be followed around its current route, except that it should be re-routed onto the terrace, far enough back to avoid the ecotone, but always less than 100 meters from the edge, avoiding relict grasslands, and fragmenting the forest habitat as little as possible;
  9. monitor the impact of this trail in order to provide adequate impact data for consideration of Trail 13 alternatives;
  10. while the usage of Trail 14 is being monitored, consider the possible routes for 13, including the possibility of routing the upper alternative farther south;
  11. among the criteria for Trail 13 that need to be achieved is the routing of Trail 13-Stem along a less damaging route, which does not repeatedly cross the riparian shrubland, does not remain in the terrace/slope ecotone for long stretches, and does not follow long traverses of unstable, slumping Pierre Shale; there appear to be several possibilities for achieving these goals.
  12. for upper Trail 13, which seems more likely to present a possible route that minimizes resource impacts than lower 13, utilize the time while 14 is being monitored to achieve a well-planned route;
  13. one possibility for routing 13 is to follow the currently proposed alignment for upper 13 approximately 200 yards above the intersection with the currently proposed Trail 13-Stem, and then proceed west and then slightly north to join the current alignment of Trail 13-Springbrook.
We are supportive of OSMP's serious attempts to build environmentally, ecologically, and geotechnically sustainable trails in this incredibly beautiful and sensitive area, and we urge you to agree that some pragmatic rethinking and tuning of this plan will result in a much better outcome for the public.

Reference:

Squire, M., 2001, Stability of Cretaceous Pierre Shale slopes, in Kuehne, M., Einstein, H.H., Krauter, E., Klapperich, H., and Poettler, R., eds. Essen, Verl. Glueckauf.

Thank you for considering this important request.

Sincerely,
Pat Shanks, Chair
PLAN-Boulder County
The People's League for Action Now


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