1.0 INTRODUCTION
1.1
Purpose
This report presents the results of a comprehensive
study of landslides in Seattle, Washington, using data that
dates back to 1890. The first study of landsliding in
Seattle was performed by Dr. Donald Tubbs in his doctoral
studies at the University of Washington between 1972 and 1973.
The result, Landslides in Seattle, was published in
a circular by the Washington Department of Natural Resources
in 1974 (Tubbs, 1974).
Tubbs based his study on the wet 1971/72 winter that resulted
in the largest number of reported landslides since the winter
of 1933/34. Since then, three major winter storm regimes
have heavily impacted Seattle in terms of landslide damage:
1985/86, 1995/96, and 1996/97.
Seattle is unique among cities in the United
States in that it instituted a full-time position to gather
information on landslides, categorize it in files, and coordinate
landslide information among City of Seattle (City) departments.
Since the pioneer efforts in the 1960s, this landslide file
has been updated periodically and the files have been open
to the public. Despite some spatial and temporal gaps
in the information contained in these files, it is probably
one of the most comprehensive records of landslides in
this country. It is this remarkable record that allows
this study to be completed.
When the city experienced the impact of two
succeeding rainy seasons (1995/96 and 1996/97) of abnormally
high rainfall, the City, with input from the public, decided
to consider new approaches to deal with landsliding in the
City. In order to adopt new City of Seattle policies
for landsliding proaction and response, two approaches were
solicited: (1) public outreach and opinion, and (2)
a scientific approach to understanding the landsliding and
formulating remedial measures to combat it. The first
approach was met by holding a series of five public meetings
during which citizen comments were taken. The second
approach is addressed with this report on the landslides in
Seattle.
The purpose of this study is four-fold:
-
To inventory and catalog landslides
in the City and Shannon & Wilson, Inc. (Shannon
& Wilson) files.
-
To better define landslide hazard zones
within the City.
-
To aid in the landslide policy decisions
by City officials.
-
To increase public knowledge of landslides
and landsliding in the City.
The scope of services for this study was developed
in an iterative manner with officials from Seattle Public
Utilities (SPU). They also received comments from representatives
from Seattle Transportation Department (SEATRAN), Seattle
Department of Design Construction and Land Use (DCLU), and
Seattle Law Department. The following are the topics
of the scope of work:
- Files dating from 1890 were searched in the landslide
file at SEATRAN. Electronic files were received
from DCLU, with landslide data starting in 1986.
Shannon & Wilson files were researched internally.
The landslides covered by the report are those reported
through June 1999.
- The data was categorized and plotted using a Geographic
Information Systems (GIS) base for manipulation and
presentation.
- Landslides in three selected areas (West Seattle,
Magnolia/Queen Anne, and Madrona) were field checked.
Subsequently, the locations of all landslides in the
city were field checked.
- Shannon & Wilson personnel attended public and
policy meetings to discuss technical issues regarding
landsliding and to relate the results of this study.
- The interrelationship between city streets, underground
utilities, and landslides were evaluated citywide.
- Shannon & Wilson formulated typical geotechnical
engineering solutions and unit costs related to landslide
problems typical to Seattle, and developed Stability
Improvement Areas to provide information for prioritizing
remedial efforts and developing approximate cost estimates.
- The citywide locations of potential slide areas were
updated based on our evaluations and field checking.
- The results of this study were summarized in this
report.
This report is presented in two volumes.
Volume 1 contains the report and figures. Volume 2 contains
the Map Folio and the Landslide Database. Volume 1 is
organized into five Parts:
This Part describes the data
sources and methods used to develop, field check, and analyze
landslides in Seattle. It includes descriptions of
the conditions that lead to landsliding in Seattle, including
the topography, geology, groundwater, surface water, climate
and cultural features. This Part also describes the
types of landslides that occur in Seattle, when they occurred,
and how their locations relate to currently mapped hazard
areas.
Part 2 presents a geotechnical
engineering evaluation of the landslides described in Part 1.
It describes typical stability improvements that can be
made for each of the landslide types and typical details
for the stability improvements. We present unit cost
estimates for the typical improvements that could be used
for preliminary budgeting purposes. Finally, this
Part evaluates how City utilities and streets can affect
stability.
Part 3 presents the results
of geological and geotechnical studies we made in the original
three study areas of the City. These areas are:
West Seattle, Magnolia/Queen Anne, and Madrona. The
emphasis in this part of the report is on evaluating factors
that contribute to slope instability and the remedial measures
that could be implemented to improve stability in these
areas.
Part 4 presents the results
of geologic and geotechnical studies we made in four additional
study areas in Seattle: Northwest Seattle, Northeast
Seattle, Capitol Hill, and South Seattle. Similar
to Part 3, this section presents measures for improving
stability in these areas.
The original scope of work
resulted in the preparation of Parts 1, 2, and 3.
In Part 3, three study areas were originally selected
for detailed evaluations including field verification of
landslide locations. This resulted in the identification
of 26 Stability Improvement Areas where landsliding was
prevalent in West Seattle, Magnolia/Queen Anne, and Madrona.
Subsequently, Part 4 was authorized to extend the field
verification process to include landslides throughout the
City, and to identify additional Stability Improvement Areas.
The result was the delineation of 17 additional Stability
Improvement Areas in Northwest Seattle, Northeast Seattle,
Capitol Hill, and South Seattle. Thus, Parts 3 and
4 provide similar results regarding stability improvements
in the respective areas; however, Part 3 includes more description
and GIS analyses of the landslide inventory data than are
presented in Part 4.
This part describes the process
and results of updating the locations of potential slide
areas.
The Figures and Tables for
each Part are presented at the end of the Part to which
they relate. They are numbered sequentially in each
Part, e.g., Figure 1-1, 1-2, etc., for Part 1, and Figure 2-1,
2-2, etc., for Part 2. Volume 2 contains the large
maps in the Map Folio and the Landslide Database.
Maps in Appendix A relate
to Part 1 and maps in Appendix
B relate to Part 3. The maps in Appendix
C relate to Part 4, maps in Appendix
D related to Part 5, and the Landslide Database is in
Appendix E.
This study was performed in general accordance
with the scope of work submitted on November 11, 1997,
to Mr. Robert Chandler of SPU. Mr. Chandler orally authorized
this study on October 9, 1997. Authorization by Mr.
Chandler to proceed with Part 4 and Part 5 was received in
January 1999.
The database information was based on available
records and brief, limited field observations. Differences
between the data and actual conditions may exist. The
database entries draw no conclusions regarding the extent
to which reported contributing factors caused slope instability.
Based on the database and field observations,
geotechnical evaluations were conducted to formulate remedial
measures for improving stability. As a result of this
effort, 43 Stability Improvement Areas were developed.
These are areas where previous instability has been prevalent
(i.e., a concentration of reported landslides). For
each Stability Improvement Area, we evaluated the conditions
that contributed to past instability or that may contribute
to potential future instability, and have presented possible
remedial measures to be considered by the City and private
property owners for improving stability. The remedial
measures presented are intended to be preliminary and are
provided to give the City and others information that can
be used to prioritize remedial efforts and to develop order-of-magnitude
budgets for the work. The proposed remedial measures
are also intended to be illustrative of potential solutions.
Additional evaluation and, in some cases, field reconnaissance,
are necessary to prioritize these proposed remedial projects.
To determine final scopes of work and cost estimates, subsurface
explorations and/or additional engineering studies are required.
The number of recommended stability improvements
are extensive. It is, thus, obvious that a considerable
length of time in years will be needed for conducting further
studies, prioritizing the improvements, allocating funds,
and implementing the work. The recommendations are general
in nature and provide approximate locations where further
analyses could take place for evaluating priorities and scheduling
work. To be effective and to prevent overlapping of
remedial measures, the prioritization process must be coordinated
with the Needs Assessment of the Drainage Policy Study conducted
for SPU by the consulting engineering firm of Black &
Veatch.
Since landslides and potential areas of instability
do not obey property boundaries, the improvements recommended
in Parts 3 and 4 do not consider the location of property
lines and would take place on City property, private properties,
or both. The improvements are those that could be made
by the City to protect utilities, drainage features, streets,
and other City facilities; and also those measures to be coordinated
between the City and private property owners to improve stability
of an unstable slope. Some improvements would be made
by the City, while other improvements or protection would
be the responsibility of private property owners. It
is anticipated that coordination between the City and private
property owners would include expeditious processing of permits;
granting of appropriate easements and variances to code requirements
where needed to improve stability for private and/or public
properties; shared costs, such as by Challenge Grants or Local
Improvement Districts (LIDs); or other cooperative efforts.
On private properties, the City may also facilitate the negotiation
of easements for stabilizing measures.
The recommendations presented in this report
are based on a technical evaluation, and are not intended
to set City policy. The City's landslide responsibilities
are a complicated blend of public policies involving public
and private responsibilities and partnerships; therefore,
the implementation of any or all of the recommendations are
solely at the City's discretion.
Improvement of stability involves actions not
only by the City, but actions by private property owners.
Such actions by private property owners should include accepting
existing conditions and the risks of slope instability, and
accordingly controlling drainage, improving stability, providing
protection for property and structures, and/or obtaining competent
professional advice. Homeowners or potential property
owners should also obtain competent professional advice regarding
site selection, property purchase, site improvements, and/or
new construction. The existing conditions to be accepted
by private property owners include surface and subsurface
drainage conditions, soil conditions and site geology, site
topography, and other factors affecting stability as described
throughout this report. The potential adverse conditions
that may occur during times of very heavy and/or prolonged
precipitation should also be considered. In addition,
private property owners should avoid conducting site work
that would jeopardize stability of adjacent property.
None of our studies have considered nor evaluated
the specific contributing or predominant causes of any previous
landslides. The stability improvements described in
Parts 2, 3, and 4 of this report are general types of action
that could be considered by the City and/or private property
owners to improve stability and reduce landslide risks.
There are always risks of damage to property
and structures involving landslides, for property located
on or adjacent to a slope. Property owners need to accept
those risks. Although the recommended improvements and
homeowner education can lead to immediate or eventual improved
slope stability conditions, the risks of damage cannot be
completely eliminated. In addition to natural factors
(soil, groundwater, heavy rainfall), other factors that may
affect stability are excavations, fills, leaking or broken
utility lines, improper drainage, lack of maintenance of drainage
facilities or vegetative cover, unwise actions by adjacent
property owners, or similar events or unknown conditions that
may cause instability.
Property owners should also be aware of the
advisability of obtaining insurance in addition to standard
homeowner's insurance to specifically cover the risks posed
by geologic hazards including earth and debris movement.
Shannon & Wilson has prepared the following
"Important Information About Your Geotechnical Report"
to assist you and others in understanding the use and limitations
of our reports.
IMPORTANT
INFORMATION ABOUT YOUR GEOTECHNICAL REPORT