Grade Level: All grade levels
Name of Field Trip Developer: Curtis Coney
Name of Field Trip: Davis Creek Park / Slide Mountain
GOAL(s): Changes to the Earth / Earth's Surface
Life Science &endash; Life Cycles
STANDARDS: 10.8.6, 11.8.2, 12.8.1
6.1.1, 6.1.2, 6.1.3,
Logistics: Open year round
Day use / closes at 9:00 P.M.
Bowers Mansion 1 mile south
Field Gear: Hiking clothes / boots
Backpack / water
Projects not supplied
Contacts: Washoe County Parks and Recreation Dept.
Ranger Office (775) 849-0684
Group Camping Reservations 849-0684
Group Picnic Reservations (775) 785-4319
Facilities: 1st come / 1st served
Camping 100 max.
Water and restrooms
Dress for weather
63 unit campground
Costs: none
References: Ranger Office
United States Geological Society &endash; Reno, NV
nbmg.unr.edu
Field Trip activities / investigations:
Slide Mountain
The area of Slide Mountain is covered in loose granite, and lacks enough mineral soil to support plant life. With fracturing and erosion there has been massive
landslides for thousands of years. The last one was in 1983 that caused extensive damage. You can still see where the landslide crossed Franktown Road. The
following is one itinerary to observe the erosion and deposition of material.
0 mi. Go south on Highway 395 from the crossroad of Highway 431.
6 mi. The landslide scars on Slide Mountain are clearly visible in
front of you to the right (west).
2.9 mi. Turn right on State Route 429.
0.4 mi. Turn right into Davis Creek Regional Park.
Take right fork to obtain pamphlets from Ranger booth, take
left fork to Davis Creek Park, Ophir Creek Trail fault area.
The fault that bounds the west side of Washoe Valley goes
through Davis Creek Park and generally lies along the base of
the hill slope. Take the hiking path to the south along a fault to
a small fault scarp. This is the Sierra Frontal Trace Fault that
runs North and South through Bowers Mansion also.
Retrace route back to 429.
0.6 mi. Turn right (south) on State Route 429.
Note light colored bouldery sediments along roadsides in this
area. This is where a debris flow crossed the road in 1983. An
extremely wet winter and rapid spring thaw caused a landslide
of rock and soil to slide of Slide Mountain and extend all the
way to the lake. Houses destroyed, several injuries, and one
death was caused by this erosion event. Similar debris flows
can be triggered by seismic events.
0.7 mi. Bowers Mansion. The swimming pool is geothermal heated,
and hot springs behind the mansion marks the trace of the
Sierra Nevada frontal fault extending through Davis Creek
Park.
Retrace route back to 395 and turn left back to Reno.
Davis Creek Park
If your group only wants to visit Davis Creek park there is a
0.5 mile Nature Trail, 1.5 mile Discovery trail that circles the
park, and a strenuous 6 mile Ophir Creek trail up the
mountain to Price Lake and Tahoe Meadows.
Post Field Trip activities / investigations: You can investigate other field trip locations (learnthegreatbasin.net) to extend lessons from this one.
Students work / project ideas: Drawings or scale models of Slide Mountain.
ASSESSMENTS: Part of our project goal is to incorporate student data and artwork onto the "learnthegreatbasin.net" web site. Please submit appropriate material to us for inclusion on the site.