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INTERNATIONAL MOUNTAIN LOGGING AND |
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11TH PACIFIC NORTHWEST SKYLINE
SYMPOSIUM |
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Jeffrey R. Laird, C.E.G. |
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Shannon & Wilson, Inc. |
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Seattle, Washington |
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CALIFORNIA |
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OREGON |
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WASHINGTON |
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Z’berg-Nejedly Forest Practice Act adopted in
1973. |
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Act requires a THP to be prepared by a RPF for
approval by California Dept. of Forestry and Fire Protection. |
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The THP must include measures to avoid
accelerated erosion near streams and/or special provisions to protect
unique areas. |
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An engineering geologic report may be required
as part of the THP. |
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This report can only be prepared by a geologist
or engineer who is registered in California. |
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Nation’s first Forest Practice Act adopted in
1972. |
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Standards were set for reforestation, road
construction and streamside buffers. Enforced by Oregon Dept. of Forestry. |
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Comprehensive revision of rules for harvest and
roads was completed in 1983 following severe winter landsliding. Concept of
‘high risk sites’ and ‘written harvest plans’ for streams and wildlife was
introduced in these revisions. |
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A rule was adopted in July 1999 to provide for
public safety below steep, unstable, forested slopes. Engineering geology report may be
required for these high risk sites. |
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Practice of geology and engineering requires
state registration. |
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Forest Practices Act enacted in 1974. |
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Timber Fish Wildlife (TFW) established in 1987. |
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Forest Practice Application is required for most
forest operations and is reviewed by Dept. of Natural Resources. |
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Watershed analysis program adopted in 1992 to
improve FPA process and address ‘cumulative effects’. |
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Forest and Fish permanent rules adopted July
2001 |
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Units with “potentially unstable slopes or
landforms” can be designated as Class IV-Special. FPA must include information prepared by a ‘qualified expert’
regarding the unstable slopes and proposed mitigating measures. |
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Qualified expert approved by DNR. Practice of
geology and engineering requires state registration. |
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Field reconnaissance-level, engineering
geologic evaluation of existing natural and human-influenced conditions,
with consideration of impacts from past and potential future forest
practices. |
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Topography- steep, convergent and/or unusual
topography, drainages |
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Geology- rock type, strength, structure,
stratigraphy |
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Soils- engineering properties, depths |
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Forest Slope Hydrology-climate, bedrock,
topography, drainage network, slope seepage, ET, interception |
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Past and Current Forest Harvest Practices - most
state/commercial forests have been previously logged with much less
sensitive methods |
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Past Slope Instabilities- where and why |
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Deliverable Hazards - public resources impacted,
risk to humans Required Leave Areas - streams, wildlife and green-up trees,
HCPs |
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Generally use limit equilibrium methods (ratio
of driving to resisting forces) to calculate Factor of Safety (FS). |
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May be deterministic (one FS value) or probabilistic
(range of FS values). |
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Assume groundwater is steady-state and
controlled by topography. |
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Most models utilize infinite slope stability
model. |
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May be site-specific or distributed (GIS-based). |
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Most
important element of evaluation - aerial photographs and maps are too large
scale, not current |
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Field
visit should include: |
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- identified areas of past instability |
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- high to moderate risk areas identified in
slope stability studies |
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- steep, converging slopes; inner gorges |
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- stream channels |
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- proposed road alignments and landings |
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- slopes underlain by weak bedrock, faults and
contacts |
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- recently harvested areas in vicinity with
similar topography |
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Include
forester or designate unstable sites in field |
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Soil and
rock characteristics |
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Seepage,
phreatophyte vegetation |
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Swooped,
jack-strawed and pistol-butted trees |
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Rapid
creep: loose soil, deep soil deposits on uphill side of trees |
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Deep-seated movement - cracks, bulges, hummocks, benches, sag ponds, deranged drainage,
back-tilted benches, scarps |
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Incised
channels, eroding stream banks |
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Measure
range of slope gradients |
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Characterize both stable and unstable ground |
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Unlike
mitigative alternatives for civil structures, there are not a lot of
options for harvest units - |
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the trees are either cut or they are not. |
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How much
impact will harvesting have on slope? |
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Required
stream channel buffers of varying widths commonly include marginally-stable
ground. |
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Designate leave areas on and adjacent to marginally-stable
ground. |
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Partial
or selective harvests. |
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Reduce
yarding impacts - full suspension, seasonal restrictions. |
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Frequency of harvest-related landslides has been
significantly reduced. |
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Regulations |
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- New
forest practices |
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Engineering geologic reviews |
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Landslides
are a natural phenomena. |
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- Always
a risk of slope instability. |
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Determining the cause - natural or result of harvest - is problematic. |
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- Timber
removal will likely be blamed. |
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Limited
mitigation measures |
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Beneficial effects of current measures need further study. |
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GIS-slope
stability models |
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- A
useful tool, but simplifies complex conditions. |
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- Too
time-consuming for harvest unit scale, use at watershed scale. |
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- Must
compare/calibrate model with actual landslide occurrence. |
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- Models
only consider shallow landsliding. |
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- Should
not be considered a substitute for engineering geologic field evaluation. |
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Required leave areas should not be designated solely on model output. |
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Historic
aerial photographs are very useful and irreplaceable - treat them better
than gold! |
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Most
(70-80%) forest-practice-related landslides are due to roads - comparatively
more effort should be invested in proper location, construction and
maintenance. |
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Role of
root strength - under current forest practices, may be overestimated. |
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Role of
forest slope hydrology - may be underestimated. |
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Practical (read dollars) limitation to extent of harvest unit
evaluation. |
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Engineering geologist provides an opinion based on training,
experience, personality and company policy. |
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Landowner/manager and regulatory agency must decide on level
of acceptable risk. |
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