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: TOBE ~ 


REPAIR, EVALUATION, MAINTENANCE, AND 
REHABILITATION RESEARCH PROGRAM 


US Army Corps 
of Engineers TECHNICAL REPORT REMR-CO-1 


STABILITY OF RUBBLE-MOUND 
BREAKWATER AND JETTY TOES; 
SURVEY OF FIELD EXPERIENCE 


by 
Dennis G. Markle 


Coastal Engineering Research Center 


DEPARTMENT OF THE ARMY 
Waterways Experiment Station, Corps of Engineers 
PO Box 631, Vicksburg, Mississippi 39180-0631 


December 1986 
Final Report 


Approved For Public Release; Distribution Unlimited 


Prepared for DEPARTMENT OF THE ARMY 
US Army Corps of Engineers 
Washington, DC 20314-1000 


Under Civil Works Research Work Unit 32278 


The following two letters used as part of the number designating technical reports of research published under the Repair, 
Evaluation, Maintenance, and Rehabilitation (REMR) Research Program identify the problem area under which the report was 
prepared: 


pe Problem=Afeqeaees ——_—Problem Area 
CS _ Concrete and Steel Structures EM Electrical and Mechanical 
GT Geotechnical El Environmental Impacts 
HY Hydraulics OM Operations Management 
CO Coastal 


For example, Technical Report REMR-CS-1 is the first report published under the Concrete and Steel Structures problem area. 


Destroy this report when no longer needed. Do not return 
it to the originator. 


The findings in this report are not to be construed as an official 
Department of the Army position unless so designated 
by other authorized documents. 


The contents of this report are not to be used for 

advertising, publication, or promotional purposes. 

Citation of trade names does not constitute an 

official endorsement or approval of the use of 
such commercial products. 


COVER PHOTOS: 
TOP—Field Research Facility, Duck, North Carolina. 


BOTTOM—One layer of 7.5-ton tribars used on 8- to 12-ton toe 
buttressing stone. Tribar and concrete ribcap 
rehabilitation of a portion of the Hilo Breakwater, Hilo 
Harbor, Hawaii. 


REPORT DOCUMENTATION PAGE 


Ta, REPORT SECURITY CLASSIFICATION 1b. RESTRICTIVE MARKINGS 
Unclassified 


2a. SECURITY CLASSIFICATION AUTHORITY 3. DISTRIBUTION / AVAILABILITY OF REPORT 
Approved for public release; distribution 


2b. DECLASSIFICATION / DOWNGRADING SCHEDULE unlimited 


4. PERFORMING ORGANIZATION REPORT NUMBER(S) 5. MONITORING ORGANIZATION REPORT NUMBER(S) 


Technical Report REMR-CO-1 


6a. NAME OF PERFORMING ORGANIZATION 6b. OFFICE SYMBOL 7a. NAME OF MONITORING ORGANIZATION 
USAEWES, Coastal (if applicable) 
Engineering Research Center WESCV 

6c. ADDRESS (City, State, and ZIP Code) 7b. ADDRESS (City, State, and ZIP Code) 


PO Box 631 
Vicksburg, MS 39180-0631 


8a. NAME OF FUNDING / SPONSORING &b. OFFICE SYMBOL 9. PROCUREMENT INSTRUMENT IDENTIFICATION NUMBER 
ORGANIZATION (if applicable) 
US Army Corps of Engineers 
&c. ADDRESS (City, State, and ZIP Code) 10. SOURCE OF FUNDING NUMBERS 


a ce 
ELEMENT NO. } NO. NO. ACCESSION NO. 
Washington, DC 20314-1000 32278 


11. TITLE (include Security Classification) 


Stability of Rubble-Mound Breakwater and Jetty Toes; Survey of Field Experience 


12. PERSONAL AUTHOR(S) 
Markle, Dennis G. 


13a. TYPE OF REPORT 13b. TIME COVERED 14. DATE OF REPORT (Year, Month, Day) 5. PAGE COUNT 
Final report FROM Feb 84 TOOct 85 December 1986 82 
16. SUPPLEMENTARY NOTATION 


Available from National Technical Information Service, 5285 Port Royal Road, Springfield, 
VA 22161. 


17. COSATI CODES 18. SUBJECT TERMS (Continue on reverse if necessary and identify by block number) 
SUB-GROUP Armor units Rubble mound Wave stability 


(a a a a os yes Toe scour 


Jetties Water waves 
19. ABSTRACT (Continue on reverse if necessary and identify by block number) 


The purpose of this survey of field experience is to present an overview of the 
coastal rubble-mound breakwaters and jetties built and/or maintained by the US Army Corps 
of Engineers that have or have had stability problems related to structure toes. Exten- 
sive discussions with US Army Corps of Engineers division and district personnel, along 
with review of district office files, revealed that rubble-mound toe stability is a major 
repair and rehabilitation problem that can be divided into two major design categories: 
(a) design of buttressing stone placed at the toe of an armor slope to prevent downslope 
slippage of primary armor, and (b) design of toe berm armor size and geometry that will be 
stable for incident wave and flow conditions and will prevent, or at least slow down, 
scour and undermining of a structure's toe. No firm guidance presently exists to aid 
Corps personnel with these two design problems, and most design work is carried out using 


(Continued) 


20. DISTRIBUTION / AVAILABILITY OF ABSTRACT 21. ABSTRACT SECURITY CLASSIFICATION 
GJ UNCLASSIFIEDUNLIMITED (J) same as RPT. Cloric users | Unclassified 


22a. NAME OF RESPONSIBLE INDIVIOUAL 22b. TELEPHONE (Include Area Code) | 22c. OFFICE SYMBOL 


DD FORM 1473, 84 MAR 83 APR edition may be used until exhausted. SECURITY CLASSIFICATION OF THIS PAGE 
All other editions are obsolete. incarcerated 


Unclassified 
SECURITY CLASSIFICATION OF THIS PAGE 


19. ABSTRACT (Continued). 


limited local field experience on past successes and failures. Design guidance in this 


area is urgently needed and will be addressed through the use of coastal hydraulic model 
tests authorized and funded under the Repair, Evaluation, Maintenance, and Rehabilitation 
Research Program Work Unit titled "Rehabilitation of Rubble-Mound Structure Toes." 
field survey was conducted under authority of this same work unit. 


This 


n¢l ifi 
SECURITY CLASSIFICATION OF THIS PAGE 


PREFACE 


Authority to carry out this survey was granted the US Army Engineer 
Waterways Experiment Station (WES) Coastal Engineering Research Center (CERC) 
by the Office, Chief of Engineers (OCE), US Army Corps of Engineers, under the 
Repair, Evaluation, Maintenance, and Rehabilitation (REMR) Research Program 
Civil Works Research Work Unit 32278, “Rehabilitation of Rubble-Mound Struc- 
ture Toes." 

The survey of field experience, which fulfills one milestone of this 
work unit, was conducted under the general direction of Messrs. John R. Mikel 
and Bruce L. McCartney and Dr. Tony C. Liu, REMR Overview Committee, OCE; 

Mr. Jesse A. Pfeiffer, Jr., Directorate of Research and Development, OCE; 
members of the REMR Field Review Group; Mr. John H. Lockhart, REMR Problem 
Area Monitor, OCE; and Mr. William F. McCleese, REMR Program Manager, WES. 

The survey was carried out by personnel of CERC, WES, under general super- 
vision of Dr. James R. Houston, Chief, CERC, and Mr. Charles C. Calhoun, Jr., 
Assistant Chief, CERC; and under direct supervision of Messrs. C. E. Chatham, 
Chief, Wave Dynamics Division, and D. D. Davidson, Chief, Wave Research Branch 
and REMR Coastal Problem Area Leader. Visitations to the US Army Corps of 
Engineers division and district offices to acquire survey data were made by 
Messrs. Dennis G. Markle and Robert D. Carver, Research Hydraulic Engineers; 
Mr. John P. Ahrens, Research Oceanographer; Messrs. Peter J. Grace, R. Clay 
Baumgartner, and Frank E. Sargent, Hydraulic Engineers; Messrs. Willie G. 
Dubose and Maury S. Taylor, Engineering Technicians; Mr. John M. Heggins, 
Computer Assistant; and Mrs. Lynette W. O'Neal, Engineering Aide, during the 
period February 1984 through October 1985. Review of the field experience 
data and preparation of this report were carried out by Mr. Markle. This 
report was edited by Ms. Shirley A. J. Hanshaw, Information Products Division, 
Information Technology Laboratory. 

CERC would like to thank the personnel of the US Army Corps of Engineers 
division and district offices contacted and visited during this survey. The 
timely and thorough completion of this study would not have been possible 
without the outstanding assistance and information provided by these 
individuals. 

Commander and Director of WES during publication of this report was 


COL Dwayne G. Lee, CE. Technical Director was Dr. Robert W. Whalin. 


CONTENTS 


NIBWNCIISG Gooodo00GDDD0DU0D000000E FOOD ODOUDDOD GOD DDODODDODDOODDODDDDDONDDN 1 


CONVERSION FACTORS, NON-SI TO SI (METRIC) 
UNDELS) (OF) MEASUREMENT yoe ojeleielse/eie soo0av0D0DDDDDDDDDNNDN eNehelMekeNonTekclenencisionone 


PART I: DPN TROD U ClenkONrerleteieNeknelekckonekoiclonele do6000000000600006000 SOCIO 


Beaveliewcowinels o 6G0 00 00D DD0DDD ODD 00DD D0 DDD OD GDOO00D000000 00000000000 
Authority, Purpose, and Approach........ 9000000000000000000000000 


PART II: FIELD EXPERIENCE. . 0... ccc cece cc ccc cer c cer er ccc crensssscsees 


ReEvestizal@ Oeaeim IDINALATOING 5666000000 b ODDO 0ODDODODOD DODD DOD000GAD00000 
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Someiwastearan Daiwalsatoinoooq0000000000000000000000000 GHUOO OH OCO000000 D5) 
Lower Mississippi Valley Division........ccccccsccccccccccecs 900 29 
Some ‘Nelleyneste rbyalsaleins 66060066000000000000000000000000000000000 29 
NomehwAGlant:cMDA VA SHO Metereneteneenolederclelekekehotonelevelohelali Reichel hellelelsteiehellenenetet one 40 
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PART TITLE: DISCUSSION. 2.2.2. ecw cece merece vce crceceresessrsecs 5000000 76 
PART IV: CONCLUSION oie). <2 esis) ele «cls oele « 66000000G00000000 o9g00d0000000 78 


3 
4 
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Summary of Contacts and VisitationsS......cscccccccccccccccrcccoss 6 
8 
13 
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CONVERSION FACTORS, NON-SI TO SI (METRIC) 
UNITS OF MEASUREMENT 


Non-SI units of measurement used in this report can be converted to SI 


(metric) units as follows: 


Multiply By To Obtain 
feet 0.3048 metres 
miles (US statute) 1.609347 kilometres 
pounds (force) 4.44822 newtons 
tons (force) 8896.444 newtons 


STABILITY OF RUBBLE-MOUND BREAKWATER AND JETTY TOES; 
SURVEY OF FIELD EXPERIENCE 


PART I: INTRODUCTION 


Background 


1. Failure of rubble-mound breakwater and jetty toes is a problem whose 
solution has plagued the majority of the US Army Corps of Engineers (Corps) 
divisions and districts responsible for designing, constructing, and main- 
taining these structures. Instability of a rubble-mound structure's toe 
directly impacts on the primary armor stability and overall performance of a 
structure. In most instances, instability (failure) of a structure's toe does 
not become evident until it has resulted in damage to the primary armor which 
has progressed up to or above the still-water level (swl). This observable 
damage can range from a minor slumping or reorientation of a few armor units 
around the swl to the total disappearance of large numbers of armor units. 
Left unattended, this type of damage could propagate upslope at a rate depen- 
dent upon incident wave conditions and severity of the toe and lower slope 
armor damage. In many cases, it will result in either localized or widespread 
failure of the structure. 

2. No guidance presently exists for the preparation of adequate repair 
and/or rehabilitation designs for damaged or failed rubble-mound structure 
toes. A concentrated effort to better understand the various types of toe 
stability problems and to develop and document effective repair methods is 
urgently needed. Through the development of sound design guidance, the need 
for frequent repair work will be minimized which will result in substantial 


dollar savings. 


Authority, Purpose, and Approach 


3. Under the Repair, Evaluation, Maintenance, and Rehabilitation (REMR) 
Research Program, the US Army Engineer Waterways Experiment Station's (WES's) 


Coastal Engineering Research Center (CERC) has been authorized and funded to 


carry out a work unit under the Construction, Operation, and Maintenance 
Research Area titled "Rehabilitation of Rubble-Mound Structure Toes." The 
prime objective of this work unit is to develop guidelines for repair and/or 
rehabilitation of rubble-mound structure toes. This will be accomplished 
through conduct of the following four work phases: 


a. Through telephone contacts with design, construction, and opera- 
tions personnel in the Corps' division and district offices it 
will be determined where structures exist that have, are felt to 
have, or have had toe-related stability problems. Once this is 
accomplished, follow-up visits will be made to the division and 
district offices to gain a better understanding of the problems, 
and the steps that were taken (if any) to alleviate the prob- 
lems, and the relative success or failure of the repair or 
rehabilitation work. 


Once an overall understanding is gained of the various toe 
stability problems confronting field designers, they will be 
categorized according to type. Subsequent to this, general 
experimental model testing programs will be developed to address 
the various problem types. The goal of these tests will be to 
experimentally determine and document improved methodologies 
through which successful toe repair and rehabilitation work can 
be designed and carried out. 


|o 


c. The experimental model tests (both two- and three-dimensional) 
will be carried out over a 2-year period. During this time, the 
scope of the tests will be subject to periodic changes based on 
continued information obtained and additional understanding 
gained on the problems confronting field personnel. 


d. A thorough analysis of the data compiled during the model tests 
will be carried out in an effort to produce general rubble-mound 
toe repair, and rehabilitation guidelines and a comprehensive 
report covering the model tests and presenting the experi- 
mentally developed guidance will be prepared and published. 


Item a has been completed and is reported herein. Continued efforts will be 
made to maintain contact with and to obtain additional information from field 
personnel faced with rubble-mound toe stability problems. Item b has been 
completed for the presently available data, and two-dimensional experimental 
model tests (Item c) have been developed and initiated. A three-dimensional 
test series (Item c) is being developed based on findings of the two- 
dimensional tests. As previously stated, Item b and, in turn, Item c are 


subject to change as more field experience information becomes available. 


PART II: FIELD EXPERIENCE 


Summary of Contacts and Visitations 


4. During the period February 1984 to October 1985, 9 division and 
21 district offices (Table 1) of the Corps were contacted by telephone in 
order to determine whether any rubble-mound toe stability problems presently 
exist or have existed on the coastal structures under the jurisdiction of the 
various offices. The points of contact at each district office were those 
recommended by the REMR Field Review Group members from the district's 
division office. Of the 21 districts contacted, 12 responded positively 
regarding existing or past toe stability problems. 

5. Prior to a district office visit, a copy of the district's project 
index maps was obtained in order to become familiar with the authorized 
coastal structures and their current status. During the planning stages for a 
district visit, it was requested through the district point of contact that 
upon arrival at the district office a meeting be held so that a detailed 
explanation of the purposes of the visit could be given and so that an over- 
view of the district's coastal structures and the various problems and repair 
histories related to them could be obtained. Notably, the Wave Research 
Branch (WRB) of CERC is funded for three REMR work units other than the one 
being addressed herein, namely, (a) "Use of Dissimilar Armor for Repair and 
Rehabilitation of Rubble-Mound Structures," (b) "Repair of Localized Damage to 
Rubble-Mound Structures," and (c) "Techniques of Reducing Wave Runup and Over- 
topping on Coastal Structures." In addition to these, the WRB has been autho— 
rized under the Coastal Program's Research and Development Work Unit titled 
"Breakwater Stability" to write case histories on all breakwaters and jetties 
built and/or maintained by the Corps of Engineers. All of these work units 
require the gathering of field data; and for this reason when WRB personnel 
visited a district office, data were gathered, when available, for each of the 
work units. It was requested that, where possible, the meeting be attended by 
district representatives from planning, design, engineering, construction, and 
operations. In this way, it was assumed that the data obtained would reflect 


all areas of concern relative to a district's coastal structures. 


Table 1 


Divisions and Districts Contacted 


Method of Contact 


District/Division Telephone ~=Visitation Problems 
Honolulu/POD* Yes Yes Yes 
Alaska/NPD Yes Yes No 
Seattle/NPD Yes Yes Yes 
Portland/NPD Yes Yes Yes 
San Francisco/SPD Yes Yes Yes 
Los Angeles/SPD Yes Yes No 
Galveston/SWD Yes Yes Yes 
New Orleans/LMVD Yes Yes Yes 
Mobile/SAD Yes Yes Yes 
Jacksonville/SAD Yes Yes No 
Savannah/SAD Yes Yes No 
Charleston/SAD Yes Yes No 
Wilmington/SAD Yes Yes Yes 
Norfolk/NAD Yes Yes No 
Baltimore/NAD Yes Yes Yes 
Philadelphia/NAD Yes Yes Yes 
New York/NAD Yes Yes No 
/NED Yes Yes Yes 
Buf falo/NCD Yes Yes No 
Detroit/NCD Yes Yes Yes 
Chicago/NCD Yes Yes No 


* POD - Pacific Ocean Division; NPD - North Pacific Division; SPD - South 
Pacific Division; SWD - Southwestern Division; LMVD - Lower Mississippi 
Valley Division; SAD - South Atlantic Division; NAD - North Atlantic Divi- 
sion; NED - New England Division; NCD - North Central Division. 


6. Following the entrance meeting, all available information on the 
district's coastal structures (design memorandums, plans and specifications 
texts and drawings, reconnaissance reports, photographs, etc.) were retrieved 
from the district's files and duplicated. The data were then taken back to 
CERC for scrutiny by the principal investigators assigned to the various work 
units. 

7. Where representative structures were near the district offices, 
site visits were made to gain a better understanding of the type of construc- 
tion used on the district's structure. During these site visits, photographs 
were taken to document the above-water conditions of the structures. Because 
of time constraints and remoteness of the structures, site visits were not 
possible at some of the district offices. 

8. Prior to departure from the district office, an exit meeting was 
held for WRB personnel to summarize their findings to ensure that no miscon- 
ceptions were drawn from the data gathered. Where possible, the same 
personnel attended the exit meeting as had attended the entrance meeting. 

9. In some instances, the quantity of data contained in the district's 
files was so massive that time was not sufficient for WRB personnel to dupli- 
cate the data during the time allotted for the visit. When this situation 
occurred, a request was made for the district to provide personnel, when and 
where available, to duplicate data and send it to CERC. In some instances, it 
was determined that an additional visit to a particular district by WRB 


personnel was needed to adequately review the available data. 


Pacific Ocean Division 


10. The Honolulu District of POD has three breakwaters which have 
problems and/or design questions that are related to toe stability. Two of 
the structures, Nawiliwili and Hilo, had a related problem. The head and 
adjacent 500 ft* of breakwater trunk at Nawiliwili Harbor, Kauai, Hawaii 


(Figure 1), were rehabilitated in 1959 using 17.8-ton tribars. Model 


* A table of factors for converting non-SI units of measurement to SI 
(metric) units is presented on page 3. 


VICINITY MAP 


B 
HARBOR 10-TON STONE PACIFIC @HANALE! 


1/2-TON STONE 


1.5 
MLLW EL 0.0° 


1/2-TON STONE: -12.0° 
(QUARRYRUN) ; 
1/2-TON STONE @WAIMEA rere 


NAWILIWILI) 


BREAKWATER 
HARBOR 


TYPICAL SECTION A-A 


“NAWILIWILI 


BULK SUGAR PLANT-»S\\, 


PIER SHEDS - <9 2 


oS 
Fetes ee 


REVETTED FILL AREA. . | 


aa 


BREAKWATER 


B SMALL B 4 
; OAT & 
% ARBOR H 


CONCRETE POST~: a8 
CONCRETE CAP 
HARBOR 
_MELWEL 0.0" 


BREAKWATER 
TYPICAL SECTION B-B 


Figure 1. Nawiliwili Harbor Breakwater, Kauai, Hawaii 


tests*, conducted at WES in 1958, revealed that two layers of randomly placed 
tribars on the head and one layer of uniformly placed tribars on the trunk 
were the best methods of rehabilitating the storm damaged structure. A survey 
in 1975 revealed extensive tribar breakage, and later it was found that the 
toe buttressing stone recommended for placement at the toe of the one layer of 
uniformly placed tribars had not been incorporated into the construction 
specifications. It was surmised that in the absence of these buttressing 
stones the tribar toe slid on the hard bottom which resulted in an en masse 
slippage and breakage of several tribars. This area was rehabilitated with 
two layers of randomly placed 11l-ton dolosse onslope and through the use of 
special placement of the toe dolosse. This latter work was also model-tested 
at WES.** 

11. A repair similar in design to that used on Nawiliwili in 1959 was 
completed on the Hilo Harbor Breakwater, Hawaii, Hawaii (Figure 2), in 1981. 
One layer of uniformly placed 7.5-ton tribars was placed on the sea-side slope 
of the breakwater between sta 11+00 and sta 20+00. Based on knowledge gained 
through the failure of the Nawiliwili tribar section, a row of 8- to 12-ton 
buttressing stone was incorporated into the toe repair. No design guidance is 
presently available to aid in sizing the buttressing stone for an incident 
wave environment, and no model tests were conducted. For this reason, close 
monitoring of the repair work should be carried out after storm events. Thus, 
POD and the Corps as a whole will gain from prototype experience which can be 
used to complement the data acquired during the experimental model tests on 
toe buttressing stone design proposed to be carried out under this work unit. 

12. Haleiwa Harbor, located on the north side of the Island of Oahu, 
Hawaii (Figure 3), was modified in 1975 by the addition of a revetted mole and 
two stub breakwaters. Subsequent to this time, repairs were required on the 
80-ft breakwater due to a slippage failure of the primary armor stone. Close 


inspection of the structure revealed that the bedding and berm had been 


* R. A. Jackson, R. Y. Hudson, and J. G. Housley. 1960 (Feb). "Design 
for Rubble-Mound Breakwater Repairs, Nawiliwili Harbor, Nawiliwili, 
Hawaii," Miscellaneous Paper No. 2-377, US Army Engineer Waterways 
Experiment Station, Vicksburg, Miss. 

** D. D. Davidson. 1978 (Jan). "Stability Tests of Nawiliwili Breakwater 
Repair," Miscellaneous Paper H-78-4, US Army Engineer Waterways Experi- 
ment Station, Vicksburg, Miss. 


10 


8 TON STONE 


SEA SIDE 


MLLW_EL. 0.0 
Se BRE) 


EL. -12.0 


2 TON STONE 


BREAKWATER (COMPLETED) 
TYPICAL SECTION A-A 


LOCATION MAP 
ISLAND OF HAWAIL 


: ea 
TES. 


oo E 


BREAKWATER 
10,080 FT LONG 


KUHIO. BAY | 
Coa o 
WAILUKU RIVER f \ S <) Be \= 


Whe 


' 

| WAIAKEA a HARBOR BASIN 

A 2,300 FT. LONG 1,400 FT. WIDE 
PROJECT DEPTH 35 FT 


CONC RIBS DOWELED 
INTO CREST STONE 


OCEAN SIDE 


ONE TRIBAR THICK 
7.68 TON TRIBARS 


10% 
—~ SCALE \N FEET 


2000 


1 TO 2 TON 
UMNDERLAVER 
OME ROW OF & TO i2 TOM ARMOR STONES ALONG BREAKWATER TOE 


TRIBARS REPAIR SECTION B-B 
STA 11400 TO STA 20+00 


Figure 2. Hilo Harbor Breakwater, Hawaii, Hawaii 


iil 


HALEIWA 
2 LAYER OF 2 TO 4 HARBOR 
TON STONES 


EXIST GROUND REVETTED MOLE 125° BEDDING STONES 
TYPICAL SECTION A-A SPALLS TO S0# 


LOCATION MAP 
ISLANO OF OAHU 
O8466 


SCALE IN MILES 


ENTRANCE CHANNEL 
740 FEET LONG 
12 FEET DEEP 
100/120 FT WIDE 


AVE ABSORBER \: 
140 FEET LONG 


EXISTING 
ENTRANCE CHANNEL 


BOAT SLIPS 


200 


SCALE IN FEET 


QUARRY : 1975 DESIGN 


10, 
RUN 2# SS SE 
TO 50# BUDS 2 LAYERS 


REVO 1T TO 2T STONE 


2 LAYERS 100# TO 
400# STONE 
9 &LO 


EXISTING 
BOTTOM VARIES BOTTOM VARIES 2#TO50#STONE ‘BEDDING 


TYPICAL SECTION TYPICAL SECTION 
110 BREAKWATER —_ 80’ BREAKWATER 


Figure 3. Haleiwa Harbor Breakwaters, Oahu, Hawaii 


12 


omitted from the construction. Localized scour had undermined the armor stone 
toe and resulted in the slippage failure. The structure was repaired by ex- 
cavating around the perimeter of the structure down to firm bottom and over- 
laying the structure head with an additional layer of 1- to 2- ton armor stone 
which extended down to the toe. This repair was feasible due to the shallow 
depth of the sand in the area of the west breakwater. No stability problems 


have been observed since the repair was completed. 


North Pacific Division 


Seattle District 

13. The south jetty at the entrance to Grays Harbor, Washington (Fig- 
ure 4), has sustained severe scour on the channel side toe. The outer 
5,600 ft of the jetty are presently below mean lower low water (mllw). It is 
not known if the toe scour is the cause, or a portion of the cause, of the 
present deteriorated condition of the jetty. Presently, no repair work is 
planned for the Grays Harbor Jetties. 

14. As of August 1985 plans were being developed for the repair of the 
rubble-mound breakwaters at Edmonds Harbor, Washington (Figure 5). It is not 
definitely known that toe stability was a cause of some of the existing 
damage, but it is thought to be a probable cause. The bottom drops off on a 
1V:2H slope to a deep depth just out from the toe of the breakwaters. There 
is some thought that this deep water adjacent to the structure, which allows 
large amounts of wave energy to reach the structure, could be initiating toe 
stability problems. No firm decisions had been made on the repair design when 
this report was being prepared. 

Portland District 

15. The north jetties at the mouth of the Columbia River, Tillamook 
Bay, Yaquina Bay, Siuslaw River, Coos Bay, and Rogue River, the south jetties 
at Nehalem Bay and Umpqua River, both jetties at the Chetco River, and Jetty 
"A" at the mouth of the Columbia River have all shown toe stability problems. 
The problems at these 11 sites (Figures 6-14) are the result of one or a 
combination of the following: (a) ebb and/or flood flows training on the 
channel side of the jetties which undermine the jetty toes, displace the toe 
berm stone or a combination of both, (b) wave- and flow-induced displacement 


of toe berm armor and foundation scouring and undermining at the jetty heads, 


13 


OCEAN 


v 
& 
6 
x 
a 


NORTH JETTY 


SCALE IN FEET 


so 


evETTY 
VARIES 


5) 


' 
ROCK BLANKET 
MIN. THICKNESS 3° 


SOUTH JETTY 
SCALE IN FEET 
5 


20° 0 0" 190) 
TYPICAL_SECTIONS 


(LOOKING WEST) 


SURFACE 


FAN SHORE 


== 
Z oc 


2 

> § 

“ ae - 

S . er a 

S » GRAYS” 
1975 JETTY “HA RBOR 
REHABILITATION. % 

S SUBMERGED JETTY ~ if f 

= \,200) 

w 

~ 

S 

NX 

Q 


‘Potht 
Chehalis 


Westport]. 


/ SUBMERGED JETTY 


ans Rivet 


BAR CHANNEL 


fol 


600° WIDE 966 ETTY BAY CITY CHANNEL 
30’ DEEP REMABIEITATION 100' WIDE, 14’ DEEP 


VICINITY MAP 


SCALE IN FEET 
SCALE IN MILES 5000 


10.000 


Figure 4. Grays Harbor Jetties, Washington 


14 


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MEAD OF 
NAVIGATION 


MORIZ. CL. - 92° 
VERT. CL - 20" 


VICINITY MAP 
° 


Rox 
L LAM OO K 


2 


wicGhway 
ELEVATION IN FEET 


16 i] To 10 0 10 
DISTANCE IN FEET DISTANCE IN FEET 


SECTION A-A SECTION B-B 
NORTH JETTY SECTIONS 


3 


Beach 


10 10. 
DISTANCE IN FEET 


EE a; | @SECTIONLC SCs SECTION D-D 
Federal Project SOUTH JETTY SECTIONS 


(EXISTING CONDITIONS SHOWN) 


Nehalem 


Base Point of mileoge is about 530 feet 
shoreward from the outer end of the 
Jet ties. 


OREGON 


SCALE IN FEET 


2090 1500 o 1600 3000 


Wheeler fo Tillamook 


Figure 7. Nehalem Bay Jetties, Oregon 


17 


Twin Rocks 


Sr) 4 SECTION A-A 


18 Feet Deep, No 

Width Specified | 35° 
Sonica 
‘eet Wide. Turni: 

Basin 500 Feet Wide VICINITY MAP 
pode im Bee 

° 190 

Mooring Basin 

@ Approach i2 Ft Deep. 


* XS g ==“ MORIZ. CL. - 937 
a / VERT. cL. -HI" 
South Jetty ariba 5 4 
8,000 Feel Long 4 =~ =~ tf Miami R. 


a Oi Upstream Limit 
Federal Project 


SECTION B-B 


LL AM OO K 
GS oO WIN mw ve 


123°50" 


Boulder Point 


Rock Point : * 
Dick Point : i MORIZ, CL. - 15" 


1 VERT. cL. - 28° 
Note: ee 
Bose Point of mileoge is in za 


line with shore line north of ir 
Jetty ond is 4500 feet seaward ‘ 
(olong range tine) from U.S. 
Highway No./0/. 


\ fa) 
‘\0ceanside es are. 
\ PREF 68 ow 


TILLAMOO 
é 


{ 


TRUE BORTH 


MORIZ. CL. - OS" 
VERT. Ch. - 14.5" 


COR 

fmol ia een oie oe ae ras =a B moRIE. CL. - 70" 

ee aE ee Ee ae ae 
20 ° Lr) @ 


TYPICAL DIKE SECTION 


SCALE IN FEET 
8000 


as] Dara within boxes pertain to Authorized 
Project 


Figure 8. Tillamook Bay Jetties, Oregon 


18 


° 
OurmPia 


LINCOLN COUNTY 


Channel 30 feet deep, 
300 feet wide from end 
of Entrance Channel to 
McLean Pt, 


VICINITY MAP. 
TN MIL 


Dato within boxes pertain 
to Authorized Project. 


Q 


Base pointofmileoge is one 
8°X 20" Sheeting mile downstream trom U.S. 


Highway 101 Bridge. 
MOORING lighway 101 Bridge. 


BASIN 


TYPICAL BREAKWATER SECTION Naa) EY SET) AB 
SCALE IN FEET TYPICAL SECTIONS 


10 9 i} SCALE IN FEET 


SCALE IN FEET 500 1000 


Figure 9. Yaquina Bay and Harbor Breakwater and Jetties, Oregon 


19 


igs EL. Varies 


¢ Stone prior to 


: a 
Stone prior to 


Mae Waeeaiinn TYPICAL NORTH JETTY SECTION 


rehabilitation 


TYPICAL SOUTH JETTY SECTION 25 ° 25 50 


25 ° 25 50 


NORTH JETTY 


EXISTING ENTRANCE CHANNEL 7790 FEET 


18 FT. DEEP BY SOO FT. WIDE FROM 
DEEP WATER TOA POINT 1,500 FT. 
INSIDE OUTER END OF EXISTING 
NORTH JETTY. 


600' FOOT NORTH 
JETTY EXTENSION 
UNCONSTRUCTED 


SOUTH JETTY 
4200 FEET 


EXISTING CHANNEL 200 FT. 
WIDE BY IGFT. DEEP TO 
FLORENCE 


STONE GROINS (5) 


eG 


CUSHMAN Va 


MORIZ. CL. -110" 
VERT. CL.-NO LiMiT CHANNEL 2 FT. DEEP 
uy BY ISOFT. WIDE 


PILE DIKE c FLORENCE TO Mi. 16.5 
GROINS (6) GCENADE ae 


EXISTING TURNING BASIN I6 FT. 
DEEP BY 400FT. WIDE BY 600 FT. 
LONG 


VICINITY MAP. 


SCALE IN MILES 


Figure 10. Siuslaw River Jetties, Oregon 


20 


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PACIFIC 


VICINITY MAP 
“SCALE IN MILES 
——— 


Bonk Protection 


5 astcec erm of 
3 Federal Project 
i Gronnat t 13f1. deep Vp 
300 ft. Gao y] eee 


Am i 
« Le, preckwater 


_—_—— 
T 
VE JCM OMIE NCL 200 By Locol interests 
df 


OCEAN 


7a 38° 


Turning Basin 
1341. deep, SOOT. 
wide & 65011. long 


: [7 5 
Two Jetties | j GOLD BEACH 


PACIFIC 


| Ge, Here TYPICAL JETTY SECTION 


SCALE IM FEET 


Channel 10 ft. deep 
and (00f!. wide 


Dato within boxes pertain to Authorized 
Project. 


Ej, 


SCALE IN FEET 
° 2p00 


2p00_ poo 


Figure 13. Rogue River Jetties, Oregon 


23) 


PROTECTIVE DIKE 
(781_ FT. LONG, EL./8 


DIKE CONSTRUCTED 
OY LOCAL INTERESTS 


Upstreom Limit of 
Federal Project 
\ 
\N 


SMALL BOAT ACCESS CHANNEL 
NORTH 100 FT. WIDE BY 12 FT. DEEP 
AT MLL. 


XN SMALL BOAT BASIN 
12 FT. DEEP AT M.L.L.W. 
PROVIDED BY 
LOCAL INTERESTS 

f HARBOR 

| _ th] i VICINITY MAP 

I: so ° so ' 

MILES 


BARGE TURNING BASIN 
250 FT. WIDE BY 650 FT. LONG 


eT AND 14 FT. DEEP AT MLLW 
‘ Ea 


BARGE SLIP - PROVIDED 
8yY LOCAL INTERESTS 


BOAT BASIN 
PROVIDED BY 
LOCAL INTERESTS 


woss r 


NORTH JETTY| 8B 
1350' LONG 


SECTION B-B 

& YY 

4 OUTH JETTY). 

Cheteo Rwe- A’ LSSONLONS: j ENTRANCE CHANNEL 
On Entrance Light “0 120 FT. WIDE BY 14 FT. DEEP 
2 7 ee CUP REEL NOTES: 
7 aN 
© E g DATA WITHIN BOXES PERTAIN 
TO AUTHORIZED PROJECT. 


ML 


oo 
F-14 Gravel Embontmen! 


SECTION C-C 


BEODING MATERIAL GROUND LINE 


SECTION A-A 


Ex/sting Stone 
MLL, 


SECTION D-—D 


Figure 14. Chetco River Jetties, Oregon 


24 


and (c) wave-induced displacement of toe berm stone and/or scour of foundation 
material which results in undermining of the structure's toe. As a result of 
this displacement, scour, and/or undermining of the structure's toe, the pri- 
mary armor stone layers become unstable and lead to structural failure. The 
Portland District carries out repair in these scour areas by filling the scour 
holes with small stone, core size or smaller, to form a foundation to rebuild 
the toe and upper portions of the structure. During the repairs and rehabil- 
itations of the north jetty at Yaquina Bay and Jetty "A" at the mouth of the 
Columbia River, a sacrificial berm of core-sized material was placed at the 
structure's toe after the primary armor layers had been placed. It was 
thought that this material would help stabilize the jetty toes by slowing down 
the scour rate as well as providing some degree of armoring of the scour hole 
as the berm stone is displaced into the scour hole. In some instances, scour 
at the jetty heads has been so severe that it was not economically feasible to 
try to fill and stabilize the scour holes. The best approach in these cases 
was to abandon the outer 200 to 300 ft of the jetty heads and rehabilitate the 


remainder of the structure. 


South Pacific Division 


16. The San Francisco District sited the jetties at Humboldt Bay (Fig- 
ure 15) as being the only area showing obvious toe stability problems. The 
channel side of the north jetty and exposed side of the south jetty have shown 
obvious signs of scour and undermining which resulted in instability and 
slippage of the dolos toe. Condition surveys of the area have revealed the 
depths of the scour holes appear to have a seasonal fluctuation. An armor 
stone berm, extending from 70 to 100 ft out from the existing dolos toes, was 
included in the jetty repair work conducted in 1985. The multilayered berm 
consists of a 3- to 6-ton primary armor stone overlying two graded filter 


layers (Figures 16 and 17). 


Southwestern Division 


17. Several rubble-mound structures in the Galveston District have 
experienced toe stability problems. Recent attempts to improve stability 


include the construction of toe berms of core sized material at the toe 


25 


Arcota Whorf GZ 
“AAbandoned) 


i ARCATA CHANNEL 
150 FT. WIDE, 18 FT. DEEP 
: (Not Used) 


TURNING BASIN 
1000 FT WIDE, IOO FT LONG 
35 FT DEEP 


SAMOA CHANNEL 
400 FT. WIDE, 35 FT. DEEP’ 
: EUREKA CHANNEL 


. 1 4 f MILE 4.29 TO MILE 5.00 
400 FT. WIDE, 35 FT. DEEP 
. Y MILE 5.00 TO MILE 6.30 
BAR AND ENTRANCE CHANNEL 
1600 FT. TO 500 FT. WIDE, 
40 FT. DEEP 


E CHANNEL AND GUNTHER /SLAND) 
zE = 


See inset mop for details. | 


Of this 0°00 ——y | 


CROSS SECTION 


NORTH AND SOUTH JETTIES 
VIEW 1S SEAWARD 


TYPICAL 


CHANNEL SIDE| OOLOSSE 
(Not to Scale) 


Existing Ground, — 
A’Stone Fill 


: TURNING BASIN CROSS SECTION Too of 42 Ton 
E00 FT. WIDE, 26 FT. DEEP RS. aa a EGE 
| 800 FT. LONG NORTH AND SOUTH JETTY HEADS 
ea te 
jOTE. 


AY BASE POINT OF MILEAGE IS 1800 FT, SHOREWARD 
OF SOUTH JETTY BEACON, 


SCALE IN FEET 
5000 10000 


Figure 15. Humboldt Bay Jetties, California 


26 


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28 


of the structures. Insufficient data were available to make a judgment on the 


success of the berms. 


Lower Mississippi Valley Division 


18. The New Orleans District has a unique design problem in that the 
majority of their jetties are constructed on very soft foundations. It is 
thought that a majority of the repair and rehabilitation work required on the 
jetties results from the structures sinking into the foundation. The jetties 
at Southwest Pass and Mississippi River Gulf Outlet (Figures 18-20), have 
required considerable repair work due to this subsidence, but it is thought 
that some of the damage on small localized areas of these jetties is the 
result of toe slippage. Toe slippage in turn results in downslope slippage of 
the primary armor resulting in loss of jetty design elevations. Efforts have 
been made to use toe berms to reduce toe slippage and help prevent foundation 
slip failures caused by the loading of the jetty construction materials. The 
berms have provided some additional toe stability, but subsidence of the 
jetties and slippage of the jetty toes and foundations continue to plague the 


New Orleans District. 


South Atlantic Division 


Mobile District 

19. The Mobile District has a problem with jetty subsidence but, unlike 
the New Orleans District's problem, theirs is not thought to be related to 
low-density foundations. It is generally thought that toe scour is the 
significant problem after major storms. Bedding layers slough off into the 
scour holes, and this damage migrates back to the toe of the primary armor. 
The resulting instability of the armor stone toe leads to downslope migration 
of the onslope armor and eventual deterioration of the structures. 

20. During the period 1937 to 1938 attempts were made to alleviate toe 
scour problems on the Panama City Harbor Jetties (Figures 21 and 22) by encas- 
ing the jetties with asphaltic concrete. Asphaltic concrete mats (2 in. 
thick) were anchored on the channel side of the jetties and extended over the 
jetties to a point 24 ft seaward of the existing jetty toe. A hot asphaltic 


concrete was poured over the matting in an effort to bond the mats together 


29 


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PARIS ROAD. 
HIGHWAY BRIDGE 


Bid NOSY3453P, 
Yd S3TMvHO Is 


PROJECT 
LOCATION 


GEE Inorovements completes 


= Improvements outnorized 


< 
5 
u 
3 
we 
3 
=9 
Xo 
S 


wotee Sxfoce £100 


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° 
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ctee Swtoce E100 


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ay 


32 


MEXICO 


1siana 


River Gulf Outlet Jetties, Loui 


ississippi 


M 


Figure 20. 


DEPTHS ARE IN FEET AND REFER TO MEAN LOW WATER. 


MILEAGE ON GULF INTRACOASTAL WATERWAY |S FROM 
HARVEY LOCK, NEW ORLEANS, LA 


_\_ 


© MEMPHIS T ENN CnaTranoos 


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wad yy wos {| 
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tpowt Pensa’ 


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MEXICO 


VICINITY MAP 


SCALE 1@MiLES 


AUTHORIZED |\~ 
TURNING BASIN |... 


; 


‘SS 2a 


GUL 
INTRACOASTAL > 


WATERWAY. 
(FOR DETAILS SEE foes 
SHEET 9-2) CE CEHED 


TS AUTHORIZED CHANNEL 
Inside (Bay) 40° x 300° 
Gulf Approach 42x 450° 


GRAND LAGOON CHANNEL 
8° x 100° 


"S 
ST. ANDREWS 
STATE PARK & 


WEST. 
JETTY 


EXISTING CHANNEL, 
Inside (Bay) 32 x 300 


FOR JETTY DETAILS 
SEE SHEET 9-/ 


MEX/1CO 


PLAN 


SCALE IN MILES 


CHAN 
38 x 
Fee 
D> 
Wz 


—— 
NEL 
300 


Gulf Approach 32 x 450 : 


<} PANAMA 


AUTHORIZED ANCHORAGE 
AND LOADING BASIN FOR 
LASH TYPE INTERMODAL 
CARRIERS - DEPTH 40 


A WATSON BAYOU | 
CHANNEL 10'x 100 


ieee 
[ 
| 


BAY HARBOR 


BEACON BEACH 


Figure 21. 


33 


Panama City Harbor Jetties, Florida 


19+65N 
14+89N 


COUNT ¥ 


10+ 25N 


ROCK JETTY EXTENSION 


ST. ANDREWS 


: BAY 
Ki STEEL SHEET 
fj PILING 5 
To: 
ASPHALT 


‘ 


2+ 30S oe ROCK JETTY EXTENSION 
ahaa nN STEEL SHEET 
PILING \ 
Ween i >, WE wy —— 9+99E 


N 


(©) 7T+O4E 


) AY s—— 
ce CA O+00€ 
G24 <3. +005 0+00 
1+ 00N 
40s 


“EAST JETTY Bis 


PLAN 


SCALE IN FEET 
500 1000 1500 


SECTION A-A 


Cap Stone 
Riprap Stone 


i<«—Stee! Sheet Piling 


SECTION C-C 


SECTION B-B 


Figure 22. Details of Panama City Harbor Jetties, Florida 


34 


as well as stabilize them to the existing armor stone structure. This design 
proved to be unsuccessful. Scour initiated at the toes of the mats and, as 
the mats subsided into the scour holes, they pulled the mats and armor stone 
off the upper slope which resulted in general deterioration of the jetties. 
Subsequent repairs were carried out by placing a toe berm of 100- to 200-1b 
stone and, where needed, overlaying the old structure with additional armor 
stone. 

21. Toe scour also has been noted as a problem with the jetties at East 
Pass Channel and St. George Island, Florida, and Perdido Pass Channel, 

Alabama (Figures 23-25, respectively). Scour on the channel side of the east 
jetty at East Pass is so severe that it is thought that portions of the jetty 
may slide into the channel at any time. In the past, this type of slippage 
failure has caused severe damage to the west jetty at Panama City. 

22. Jetties at St. George Island have suffered cover stone loss result- 
ing from the undermining action of toe scour. The west jetty at Perdido Pass 
presently has significant amounts of toe scour on the channel side, and Hurri- 
cane Frederick produced significant amounts of toe scour on the east jetty. 
The overall condition of the Perdido Pass jetties was said to be good; there- 
fore, it is assumed that the toe scour has not caused any obvious damage above 
the waterline. 

Wilmington District 

23. The 3,650-ft-long rubble-mound north jetty located at Masonboro In- 
let, North Carolina (Figure 26), was constructed between August 1965 and June 
1966. The north jetty required extensive repair on the channel-side toe of 
the outer rubble-mound structure in 1969 and to the channel-side toe of the 
inner weir section in 1973. This was prior to construction of the south 
jetty (14- to 22-ton armor stone) in 1980. It was thought that ebb and flood 
flows had caused the channel to move adjacent to the north jetty, creating the 
scour problem. In both repairs, a 2- to 3-layer protection of bedding mate- 
rial and riprap (25 to 2,000 1b) was used. This toe protection butted against 
the existing armor stone toe or sheet-pile weir. The berm width varied from 
30 to 50 ft. It is thought that this work had limited success because the 
jetty has not totally deteriorated, but it is presently in need of repair work 
in several areas. Presently it is unknown whether the deteriorated appearance 


of the north jetty results from a toe scour problem or from the possibility 


35 


DESTIN Ee 
iY 


MORENO POINT 


FIXED BRIDGES 
HOR. CL.78' 
VERT. CL. 38° 


SAND DIKE 
STONE JETTY SECTION 5 


WEIR SECTION / 
DEPOSITION BASIN: 7 


OPEN WATER DISPOSAL SITE 
PLAN 


SCALE IN FEET 
1000 


GULF OF 


DEPTHS ARE IN FEET AND REFER TO MEAN Low water. S/OME JETTY SECTION 


MEMPHIS T ENN CHaTTANOOGA“ 
AS 
Y) 
Le 
7 
' T 
Columbus. * JeiRMINGHAM Ce RATLANTA 
¢ iy PY 
\ 
cla € 
\ | Symmetrico/ obout € 
MONTGOMERY ¢ 
Ry 
= 
S i ~ Existing ground surface 
z (Elev vories) 
~"yRescacout PROJECT © TYPICAL JETTY SECTION 
RIVER, ae 
LA: ) ‘ FLA 
\C Gul!port BRA CACHIC OLA! . 
Cees ge mqoce yom" TALLAHASSEE 


ORLEANS' 


mw? GULF OF MEXICO 


VICINITY MA 


SCALE INMILES 
so 9 50 100 


Florida 


Figure 23. East Pass Channel Jetties, 


36 


E N N CHATTANOOGA 


APALACHICOLA 


‘> 
‘ 
é No 
s Sir 4 
ST. GEORGE f me 
SIP Nec alGereyty 24 
ci] s ey 
CHANNEL 3 WS Ss 
z . 4 3 =) 
10'x 100' TO 200 aS at § 
MISs li WALA 
& 
YAGKSON 3G Meridian AWER 
ls : MONTGOMERY Py 
fle Nl s : 
AGE ya ey 
> news z 
N. fines) AZ S 
\ a | MOBILE = 


~-prascacoury ae 
Dv aver {woae 


“a, 


NITY MAP 


SCALE INMILES 
° 50 100 


VICI 


GULF INTRACOASTAL 
WATERWAY /2°X 125° 


EASTPOINT 
CHANNEL 
6 x/00 


APALACHICOLA 
AIRPORT 


~NSWING BRIDGE 
S BULKHEAD SHOAL 
\ MOR.CL Me, CHANNEL 10'x 100", 
i ——— 1 5 (NOT MAINTAINED) Mee 
ST VINCENT TWO MILE BREA WATERS | \ ra 
TWO MILE CHANNEL CLUECINE \\ i 
SOUND 6x100' CHANNEL fi ee 
AINNER BAR CHANNEL 
10 x 100 


awe” (MAINTAINED TO 12'X 125’ UNDER 
te PROJECT FOR GULF INTRACOASTAL 
WATERWAY.) 


=—eRWAY ; 
a= WATE _-t FIXED BRIDGE «=, 
ee i 388 =cut a HOR.CL 125° 
= 


“s.._ VERT. CL. 50° 


ST. GEORGE ISLAND CHANNEL 
10'x 100' TO 200° 
TWIN RUBBLE MOUND JETTIES _.” 


en" 


os DEPTHS ARE IN FEET AND REFER TO MEAN LOW WATER. 


MILEAGE ON GULF INTRACOASTAL WATERWAY 1S FROM 
HARVEY LOCK, NEW ORLEANS, LA 


PLAN 


SCALE IN MILES 


1 oO U 2 3 
aaa 


TYPICAL JETTY SECTION 


Figure 24. St. George Island Jetties, Florida 


37 


N TERRY COVE 


WALKER ISLAND) 


PERDIDO BAY 


STA. 32+00 ong 
—Q ISLAND 
a 


FIXED BRIDGE CLEARAN 
TO COTTON BAYOU 
ee HORI 

VERT. 29° 
TO PERDIDO BAY 
HOR. 80 
VERT, 35° 


FLORIDA POINT 


€@ UNM 


GULF OF MEXICO PLAN 
SCALE IN FEET 
800 oO 800 1600 
SESE TR 
DEPTHS ARE IN FEET AND REFER TO MEAN LOW WATER. Ca 


MEMPHIS T(E NUN} CHATTANOOGA 


CORESTONE 
CAPSTONE 25 To 2 TONS 


8 TO12 TONS, FOUNDATION BLANKET 


3 Geen 
.) 
\ r 


MONTGOMERY 


TYPICAL SECTION THROUGH JETTY 


« 
x 
é 
5S 
N 
= 
= 
$ 


= psseaaouy t S SCALE IN FEET 
Yama 10 oO 10 20 
Ss )=SE 


APALACHICOLA 
RIVER 


= _ Poromq 
PROJECT *X" 
GULF OF MEXICO 


Figure 25. Perdido Pass Channel Jetties, Alabama 


38 


aN 
NORTH 7T90.< > 
CORE CREEK BRIDGE 
is SIDE CHANNEL Ca 
CAROLINA - & BASIN AT Y 
& JACKSONVILLE SWANSBORO Whe, 
= a 6] ‘ 
CHANNELS TO S. aNGe aS 
JACKSONVILLE & > Z; 2/0 
NEW RIVER INLET Ye \ 
G 
oe SZ Bocue \PELTIER CREEK 
oad Ld INLET N 


= ZA 
S. WA a2 CHANNEL TO p Bi 
% BOGUE INLET € ~ 
hy 0 iG 


CONNECTING CHANNELS 


CG 
MASON BORO INLET a 
are OSI) LG AND CONNECTING iy 
SOUTHPORT f CHANNELS Pang 
f/ CAROLINA BEACH INLET p 


CAROLINA BEACH HARBOR 


—— 
| “342 CAPE FEAR 
END A.1.W.W. SOUTHPORT HARBOR 
WILMINGTON 
DISTRICT 


NEW 
HANOVER 
COUNTY 


SCALE OF FEET 


Figure 26. Masonboro Inlet Jetties, North Carolina 


39 


that the original 7- to 12-ton armor stone may have been an inadequate design 


for the incident wave environment. 


North Atlantic Division 


Baltimore District 

24. The south jetty at Ocean City Inlet, Maryland (Figure 27), is the 
only structure within the Baltimore District that was reported as having 
significant toe stability problems. The original north and south jetties, 
both rubble mound, were constructed in 1934 and 1935, respectively. The crown 
elevation on the shoreward end of the north jetty had to be increased in 1937 
to stop flow of sand into the inlet. The landward end of the south jetty 
required extensions in 1956 and 1963 to repair flanking caused by erosion. 
The south jetty has suffered major deterioration along its outer leg caused by 
ebb flow induced scour and undermining of the structure's inlet side toe. 
During major repair of the south jetty in 1963, the center line of the struc-— 
ture's repair section was offset outward from the inlet (Figure 27). This was 
done to alleviate the need to fill the massive scour hole that existed where 
the inlet side of the structure was originally constructed. The ocean side of 
the existing structure that remained was used as a base against which the in- 
let side toe of the jetty repair section was positioned. By 1982, the 1963 
repair section of the south jetty was once again very deteriorated. Like the 
original, this damage was only on the converging portion of the jetty and was 
caused by ebb flow induced undermining of the structure's inlet side. In 
order to prevent failure of the outer end of the south jetty, which would lead 
to severe inlet shoaling, the scour hole adjacent to the structure was filled 
with dredge material and capped with stone. The lower portion of the inlet 
side of the jetty was overlaid with an intermediate stone size, and the 
remainder of the inlet side slope was covered with primary armor stone. This 
work was completed during 1983 to 1984, and a typical repair cross section is 
shown in Figure 27. The majority of the south jetty's original repair section 
still shows considerable deterioration and is highly overtopped. It is 
unknown how well the scour protection is performing. It appears that scour on 
the north side of the inlet has slowed down, and the north jetty is in good 
condition; however, the overall scour in the throat of the inlet shows no 


signs of stabilizing. 


40 


HOR. CL. 70° 
VERT. CL. 18° 
-DRAWBRIDGE 


S. STNEPUXENT 
MARYLAND . [- 


O.65Mi 
-€ PC RR. 6OR/W. _-N. HARBOR ROAD [7 
= = = —F— = 


10. 


fo} 
ey 


», W. HARBOR 


CESTERj# fF COUNTY 


12° 
ke | +4.N. JETTY, +6 S. JETTY 


SCALE OF FEET 
500 fo} 
1 


OCEAN SIDE 


CAP STONE; 6TON 
MIN. ABOVE -9.0; 
1 500# MIN. BELOW -9 


15 #TO 2 TON 
1 


ORIGINAL 
JETTY 


FILTER, RUN OF 
CRUSHER STONE 


1956 NORTH JETTY REPAIR 


OCEAN SIDE 


CAPSTONE; 
9 TON MIN 


“ELEVATIONS IN FEET 
REFERRED TO MLW 


1’ FILTER; RUN OF CRUSHER 1 TON” 
1963 SOUTH JETTY REPAIR 


150° 
EXISTING 

6.0 TO 10.0 TON STONE 

MIN EL FOR TOP OF ARMOR STONE (-3.0) ~a, 


0.6 TO 1.0 3 OCEAN SIDE 
TON STONE 1 


SAND A Se 


Co 
EXISTING GRADE —™ ~~ - 


ee 


FT 


1983 SOUTH JETTY REPAIR 


Figure 27. Ocean City Inlet Jetties, Maryland 


41 


Philadelphia District 
25. The most common problem occurring on the Philadelphia District's 


coastal structures is subsidence of structures below design elevation. It is 
thought that toe scour contributes to this, but the primary cause is poor 
foundation conditions in the areas where most of the structures have been 
built. This is especially true for those structures located in the Delaware 
Bay area. 

26. The jetties located at Reedy Point, where the Chesapeake and Dela- 
ware Bay Canal intersects the Delaware River, were originally constructed 
prior to 1938 (Figure 28). Both structures were of rubble-mound construction. 
In the 1960's the existing south jetty was removed, and a new south jetty was 
constructed farther south. This was done to increase the entrance size to 
accommodate larger vessels and improve navigation safety. The present jetties 
are both 2,095 ft long, and it was reported that the north jetty has problems 
with toe scour, loss of armor stone, and overall subsidence. 

27. The rubble-mound and sheet-pile composite jetties at Indian River 
Inlet, Delaware, were completed in 1939 (Figure 29). The jetties required 
storm damage repairs in 1956 and 1957. At that time, the north jetty was 
extended inshore a distance of 320 ft. At present both jetties are 1,566 ft 
long. Both jetty heads have deteriorated significantly from a combination of 
toe scour, armor stone slippage and displacement, and overall subsidence. 
Because of the success of the Manasquan River Jetty repairs, dolosse are being 
considered for inclusion in the repair and rehabilitation designs for the 


structure slopes. No details on the proposed toe repair design are available. 


New England Division 


28. Based on review of historical repair data, it appears that three 
project sites within the New England Division that contain rubble-mound jetty 
structures have exhibited stability problems which could be related to in- 
stability of the structure toes. Both jetties at the mouth of the Kennebunk 
River, Maine (Figure 30), have a history of extension and repair. The latest 
jetty rehabilitation work was completed in 1982. Recent inspections show that 
both jetty heads are damaged and that 250 ft of the channel side of the east 
jetty have been undermined. The most recent inspection reports (1973-74), 


indicate that the north and south jetties at Newburyport Harbor, Massachusetts 


42 


Tf Peo Pac 
‘stand 


evancn cnannes > 
envaance 
Delawa 
. > 


\ SURAT BRIDGE 


Ucn Neen 


Oy aie | 
. COUNTY IN | 
= KO Teese ign 

Pr 


, he 5 
Gity = 


Baie! 


Sal 


ce) sy 
x OG - 

CMESAPEAKE CITY> “US Engineer 

ery BR (GH LEVEL) , Resident Office 
rou, Chesepeate City sy 
. Oy Aacheroge @ Meermg Basin 2 
£ (@ece Crees! g 
2 

& 

, 


ST GEORGES 
(HIGH LEVEL) 
AR BR 
(VERTICAL LIFT) 


© H 


5 
oj $s 
SE = fy 
ad s IS 


AEEOY PT OR d 
(HIGH LEVEL) 


MARYL 
O€L aw 


Te Delewere Bey = 


LEGEND 


u S Reservetion Boundery 


, 


SCALE OF FEET 


3.0c0 ) S 10 ic} 2c 2500¢ 
[SS=S5=c —- == 2: 


& 
¢ 


2 


‘Steed 
Bultnecd 45 


HEALTH CENTER 


wary OR. 
(FIXED) 2 LANES ya 


SCALE OF FEET 


Figure 28. Reedy Point Jetties, Delaware 


43 


REHOBOTH 
BAY 


To Rehoboth Beach. 


INDIAN RIVER NECK 


\ 


DELAWARE SEASHORE 
STATE PARK 


+; 


CHANNEL SIDE 


Prevent bottom tobe axceraied to 0 depth of -3.0 
Fe permit o min secton of patty 08 shown 

Stee! ance! poling Ihrw 

Mi core @ Cop stone 

u 


TYPICAL SECTION 
“TS. 


() ©, 
rire ANY) : 
a 


OCEAN 


BOTTOM HILLS DRAIN 
US COAST GUARD STATION 


2 ag 
\\se'J INDIAN RIVER 
——= INLET 
FIXED 


BRIOGE 
ELEV 35'MHW 


ATLANTIC 


——ro Bethony Beoch 


TYPICAL SECTION OF REHABILITATED BULKHEADS 


to conus! of 0 graced 


(qwarry run stone, proces Mor stone{3'-0" deep) 10 conniet of preces exighing 
n Win! rrom notions tnon «07 1484 (ham /3 bs @ nol more than 200 D4 
TNS OE Tho/! be placed for Iho tui! wi81h of 1he jally of 


25% ibs 16 200 ioe Jea1t 200' in adrence of placing the Core stone 
35% 200108 ro 2/008 


HALF SECTION-OUTER 300! OF JETTY 
NTS 


MTS 


SCALE OF MILES 


' ° ' 
_——— ———) 


Figure 29. Indian River Inlet Jetties, Delaware 


44 


Behe entSee | 
SWING 8B 

SEEDEAL See heer KENNEBUNK ~ 

RIVER 4 


LOCATION MAP 


SCALE IN MILES 
10 oO 10 zo 30 
[es es | 
6-FT. CHANNEL 
@ 
GUERTIN 


6-FT. ANCHORAGE 
2 ACRES 


100'7| 


oh 
MONASTERY 


6-FT. ANCHORAGE 
4 ACRES 


NONANTUM 
HOTEL \\ 


6-FT. CHANNEL 


KENNEBUNK 
RIVER CLUB 


SEVERANCE r) 
TOWN 
LANDING 


= ‘ = 
OCH BEACH VT: 7 8- FT. CHANNEL 


SAND 
FENCE 


WEST JETTY =~ sep ge 


& EXTENSION 


Figure 30. Kennebunk River Jetties, Maine 


45 


(Figure 31), which have an extensive repair and rehabilitation history, are 
showing considerable damage. This damage appears to result primarily from 
subsidence. Damage on four areas on the channel side of the south jetty most 
likely result from undermining of the rubble toe. The jetties at Hampton 
Harbor, New Hampshire (Figure 32), were originally constructed by the State 
and were turned over to the Corps in 1964. During 1965 to 1966, considerable 
work was done on both jetties. Since that time the south jetty has remained 
in good condition, while the north jetty has required continuous maintenance. 
Most of the repair and rehabilitation work has been needed on the seaward por- 
tions of the north jetty. The last rebuilding of the north jetty was com- 
pleted in 1980, and it is thought that part of this recurring damage can be 


attributed to scour and undermining of the jetty toe. 


North Central Division 


29. There are 38 project sites within the Detroit District which have 
breakwater and/or pier (jetty) structures that have exhibited stability prob- 
lems related to the structure toes. At 14 of these sites problems are associ- 
ated with rubble-mound structures, while at the remaining 24 sites toe prob- 
lems occur on other structure types. Table 2 is a listing of these 24 sites 
and the types of breakwater and/or jetty construction associated with each 
site. The remainder of this section on the Detroit District deals strictly 
with those 14 sites which are having and/or have had toe stability problems 
with rubble-mound structures. At some of these sites, toe stability problems 
have occurred on areas of the structures that are not rubble mound. 

30. Structures at Black River Harbor, Cheboygan Harbor, Hammond Bay 
Harbor, Harrisville Harbor, New Buffalo Harbor, and Point Lookout Harbor, 
Michigan, are purely rubble-mound construction (Figures 33-40). Charlevoix 
Harbor, Michigan; Duluth-Superior Harbor, Minnesota and Wisconsin; and Leland 
Harbor, Muskegon Harbor, Pentwater Harbor, Port Washington Harbor, and 
Traverse City Harbor, Michigan (Figures 41-55), have structures that are com- 
posed of a combination of rubble mound, timber cribs, timber piles, steel 
sheet piles, concrete caissons, steel cells, concrete caps, and concrete 
superstructures. The head of the east jetty on the north end of the Keweenaw 
Waterway, Michigan (Figures 56 and 57), is an old timber crib which is encased 


in rubble. For this reason, its response is very similar to that of a purely 


46 


9.0 FOOT CHANNEL 


(12-FT. DEPTH NOT 
DREDGED-|NACTIVE) 


Figure 31. 


@ANCHESTER 


LOCATION MAP 


SCALE IN MILES 


paease 


NORTH JETTY 
~~ 


SHORE 
REVETMENT 


12 FOOT CHANNE 


(15-FT. DEPTH NOT 
DREDGED- INACTIVE) 


CROSS SECTION OF NORTH JETTY 


TOP OF MOUND EL.12° RIVER SIDE 


7——\_ _M.H.W. EL. 7.8' 
aprii on U.L.w. EL. 0.0 
hl od = 
EXISTING BOTTOM 


CROSS SECTION OF SOUTH JETTY 


SCALE IN FEET 
1000 2000 


Newburyport Harbor Jetties, Massachusetts 


47 


NEW 
HAMPSHIRE 


i @ cCoNcoro é LOCATION MAP 
SCALE Im MILES 


ganting ground surtoce - E110 9-90 (vores) 7 


NORTH JETT Y— SECTION 


SCALE im FEET 
. o > 


STONE JETTIES 


ry 


HAMPTON® 
HARBOR 


8-FT. ENTRANCE CHANNEL 


=) 
Ore 


Inner Sunk Rocks 


SOUTH JETTY SECTION 


SCALE m FEET 
* ° 3 


SEABROOK 


SCALE IM FEET 


Figure 32. Hampton Harbor Jetties, New Hampshire 


48 


Table 2 
Project Sites in Detroit District with Toe Stability Problems 


on Other Than Rubble-Mound Structures 


Types of Structures at 


Location Project Site* 
Algoma Harbor, Wisconsin TP** and TC w/CS 
Areadia Harbor, Michigan SC and TC w/SSP 
Big Bay Harbor, Michigan RM, SC and SSP 
Frankfort Harbor, Michigan G5 WP, SP5 SGy SSR25 CS ema Ger 
Grand Haven Harbor, Michigan Se5 IH, GS eimel EGP 
Harbor Beach, Michigan TC and CS 
Holland Harbor, Michigan SSP, TC, RM, TP, CS and CCP 
Kenosha Harbor, Michigan G5 SSP, SG5 GEP emma CS 
Kewaunee Harbor, Wisconsin TP, CC, RM, SSP, SS, CCP and CS 
Lac La Belle Harbor, Michigan SC and SSP 
Ludington Harbor, Michigan TC Lee SOSP RM, (CGR and ics 
Manistee Harbor, Michigan Soe, ING, IWe5 ame CS 
Manitowoc Harbor, Wisconsin We, G65 Woy SSP5 IM, emal ES 
Menominee Harbor, Michigan and Wisconsin S125 6, GG, Ca? aml CS 
Milwaukee Harbor, Wisconsin TC, SSP, CC, RM, CCP and CS 
Portage Lake Harbor, Wisconsin TC, TP and CS 
Racine Harbor, Wisconsin WG, WP, IMI, SSP, CG, Gee ame GS 
Saugatuck Harbor, Michigan WG, 12, SSP5 amal CS 
Sheboygan Harbor, Wisconsin WG, WP, SSP, smal CS 
South Haven Harbor, Michigan SSP, TC, CCP, and CS 
St. Joseph Harbor, Michigan AG, S25 GIP ehial CS 
Sturgeon Bay, Wisconsin TP, TC, SSP, and CS 
Two Rivers Harbor, Wisconsin TP, TC, SSP and CS 
White Lake Harbor, Michigan WP, IEC, emal CS 


* Not all structure types at each site are experiencing toe problems; how- 
ever, tabulation presents all structure types existing at each site. 

*x TP-timber piles; TC-timber cribs; CS-concrete superstructure; SC-steel 
cells; SSP-steel sheet pile; RM-rubble mound; CC-concrete caisson; SP-steel 
piling; CCP-concrete cap; SS-steel sheeting 


49 


-—\7 
=f 
je 
f 


yi 


Note 

Projec! depths ond soundings are referred to LWD 600.0 feet | 
above MWL at Father Point, Quebec (IGLO 1955) (International VICINITY MAP 
Great Lokes Datum 1955). 


"99 'p 2 30 40 S0 Op 70 eo 
SCALE IN MILES 


GOGEBIC COUNTY (Gl eRseeraree 


ies 2 
MICHIGAN BOAT RAMP=——=P (reel) 


; hoe 
== Suspen 
Foot Bridge 
18 ft. clearance 
B@LAC K RIVER 


CLORURINIE any. Poy O03 Parking Area 


eo 


SCALE IN FEET 


Figure 33. Black River Harbor Breakwaters, Michigan 


50 


Lakeward End to -5 Ft. Contour 


-5 Ft. Contour to +2Ft. Contour 


SCALE 
10 io) 10 20 FT 
= 


+2Ft. Contour to Landward End 


RUBBLE MOUND - BUILT 1957 
EAST AND WEST BREAKWATERS 


Eos! Breokwoter-825 FI. + 


UOTE u es, Breokwoter-555 Ft. + 


Figure 34. Details of Black River Harbor 
Jetties, Michigan 


51 


LAKE HURON 8 / 
=I / 
7, 
16.1.0. EL 576.8' /),’ 
0 G o r 0 ” 2 ty! 
Ue 
: > STRAITS OF “M AC KIN LA C2 
/ 2 3 
/ G2 
/ & 
‘4 s\n S 
” 7) 
Cheboygon Crib Lt Ws \ 
#L/ Nos 
N 
w 40 
° 25 
10 o 
22 hl 
27 
2 0 
D 2s 
Little ee 
SS Sa 10 
SS 10 
PROJECT DEPTH 2/ FT. ¥ 
Qs, 
2 
5 F : 
-= == ’ 
oF 
> As 
A 
= a 
= a 
= A 
-~ = 
- us 
= - 
-_ > _ 
a > 
-_ -_ sie 
eae WM we 
An A 


104 P g 
ae x Atl, 3 TURNING BASIN 


PROJECT DEPTH 2/FT. 


— = 
R g 
z 
isin & MICHIGAN 
E y oS S oer ho 
oR = ‘ 37 soszen fen 
PROJECT DEPTH (ave INDIANA onIo 
_ \ VICINITY MAP. 
“| SCALE OF MULES 
a s 16 0 
PRI h 4 | 
el a OTE CTs DEPTH 8.5F. 3 
3 la] COVER STONE 
a 5 CHANNEL SIDE WEST 


CHANNEL 
CINE 
I-TOE STONE 


WEST PIER 
‘o| 4 TON MIN 


LAKE si0g 2TONMIN 
RUINS OF OLO Ss 
fae 


two EL 576.8" 


CORE STONE 


MATTRESS STONE 


TLEVELARD 


EXISTING coma 


f>—Lwwc. tock SECTION A-A 
TYPICAL SECTION OF RUBBLE-MOUND BREAKWATER 


SCALE OF FEET 


= 5 4 


Figure 35. Cheboygan Harbor Breakwater, Michigan 


52 


COVER STONE PROJECT DEPTH 
ENTRANCE CHANNEL /2 FT 
HARBOR BASIN IO FT 


_ CHANNEL WIDTH VARIES 


EXISTING BOTTOM 


TYPICAL SECTION 


SCALE OF FEET 


VERTICAL 


HORIZONTAL 


MICHIG 


ENTRANCE CHANNEL 
PROJECT DEPTH 12’ 


MICHIGAN 


MICHIGAN 


INDIANA 


VICINITY MAP 
SCALE OF Bai 


MICHIGAN STATE HIGHWAY PARK AREA 


HIGHWAY les 


PUBLIC ACCESS AREA 
FOR HARBOR 


Project depths, saundings ond elevations are referred to 


Internationa! Great Lakes Datum (1955) for Lake Huron , elevation Scale of Feet 


700 


576 6ft above Mean Water Level (MW.L.) at Father Point, Quebec ""p o tao 200300400800 800 


Figure 36. Hammond Bay Breakwater, Michigan 


53 


NOTE: 
Cover stone 5 ton minimum in types 1 and 1 
3 ton minimum in types II ond I 


oe 
Toe stone 7 ton minimum in types I ond I; 
5 ton minimum in types If ond I t ee 
I] wacxway 
FA ee BB 


HARBOR SIDE LAKE SIDE 


o TYPES Row 


* D> ' 
G.L.0. El 5768" Ro 
——} ae) uy “ 
3 ;) CORE STONE Y_ } 
ia R roe stonk ¢ 


A 


——MaTTRESS STONE a 


AKE BOTTOM 


TYPICAL GROSS TI 


Scole of Fest VICINITY MAP 
SCALE OF WiLeD 


ALCONA COUNTY | 
A 


NOTE 
Project depths, soundings and elevations are referred to 
International Great Lakes Datum (1955) for Lake Huron, elevation 
576.8f1. above Mean Water Level (MW.L.) at Father Point , Quebec. 


SOUTH 
BREAKWATER 
EXPANSION OF 


STATE BERTHING ~ 
FACILITIES 


3. 15.7 
HARGOR BASIN / 
10 FEET OEEP on 
12.0 15.2 ‘ g ’ Bs 
ENTRANCE CHANNEL 
Wo YF te Ob 12 FEET DEEP 
1.G.L.0. El. 576.8" Scale of Feet 


100 0 100 2 3 5 6 7 6 9 1000 
SS 


Figure 37. Harrisville Harbor Breakwaters, Michigan 


54 


(WISCONSIN 


rm 
n 
Vo 
w 
° 


EXPERIMENTAL 
VICINITY | MAP "a" FRAME 


BREAKWATER 
REACH -F 


' 
SCALE OF! MILES REACH-A 480'+ 


300 40 


VILLAGE 


PROJECT DEPTHS AND SOUNDINGS ARE REFERRED 

TO LOW WATER DATUM 576.8 FEET ABOVE MEAN SCALE OF FEET 
WATER LEVEL AT FATHER POINT, QUEBEC. |.G.L.D. =Ss=o=————r 
(1955) (INTERNATIONAL GREAT LAKES DATUM) ° 200 400 


Figure 38. New Buffalo Harbor Breakwaters, Michigan 


55 


12-0" 
AVERAGE |2 TON COVER STONE ¢ 


( RANGE 10 TO 16 TONS) 


EXISTING 
—=LAKE BOTTOM 


CORE STONE (100-LB. TO1 TON 
PLACE LARGER STONE ON OUTSIDE) 


2-0" BEDDING STONE 
(I-LB. TO 50-LB QUARRY 
SPALLS ) 


16 TON TOE STONE 


REACH-A 
BUILT 1975 


¢ 


AVERAGE 6 TON COVER STONE 
(RANGE 5 TO 10 TONS ) 


EXISTING 
ZLAKE BOTTOM 


CORE STONE (I-LB. TO 1,000-LB 
PLACE LARGER STONE ON OUTSIDE) 


2-0" BEDDING STONE 
(1-LB. TO 50-LB. QUARRY 
SPALLS ) 


10 TON TOE STONE 


REACH-B 
BUILT 1975 


AVERAGE 4 TON COVER STONE ¢ Leo! 


(RANGE 3 TO 5 TONS ) 


EXISTING 
LAKE BOTTOM 


ra a aor 


5 TON TOE STONE 
2'-0" BEDDING STONE 
(1-LB. TO 50-LB. QUARRY 
SPALLS ) 


CORE STONE (1|-LB8. TO500-LB 
PLACE LARGER STONE ON OUTSIDE ) 


REACH-C 
BUILT 1975 


fe) (e) 10 20 


CORE STONE (I* TO 500°) 
PLACE LARGER 
STONE OUTSIDE 


AVERAGE 3 TON 
COVER STONE 
(2 TO 4 TON) 


SCALE OF FEET 


EXISTING 
LAKE 


2-0" BEDDING STONE 
(1° TO 5O0°QUARRY STONE) 


REACH-D 
BUILT 1975 


Figure 39. Details of New Buffalo Harbor 
Breakwaters, Michigan 


56 


1/4 TON MIN. VARIES +9° TO+I2 


rors! COVER STONE aac tan 

ey \/4 TON MIN 2/3 TOMMIN 

ccs TONMIN j Zee: STONE 
\ 


Yi 
172 TON MIN 11/2 TON MIN, 


11/2 TONMIN: 1/2 TON MIN- H { 
TOE STONE TOE STONE TOE STONE TOE STONE 


MICHIGAN 


2 MATERIAL TO BE 
EXCAVATED 


LAKE 


vote 


re 


SECTION A-A on Leute 
NO SCALE ‘VICINITY MAP 
SCALE 


10 0 100 Mi 
= 


SAGINAW 


OF CULVERT 
8+00 


18+00 "2 : 
~ : DOWNSTREAM 
: : LIMIT OF FEDERAL 
PROJECT- 


WEST ng j JETTY 
/OFT. PROJECT DEPTH : 12 FT. PROJECT DEPTH: 


NOTES: 


Project depths, soundings & elevations are referred to 
International Great Lakes Datum (1955) for Lake Huron; 


Elev. 576.8 ft, above Mean Water Level at Father Point, Que. 


Figure 40. Point Lookout Harbor Jetties, Michigan 


57 


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Z-27STEEL 
SHEET PILING 


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SHEET PILING pis P 
T- SUBSTRUCTURE 1079-80 Hposr 


STEEL 


SUPERSTRUCTURE 1078-9,1007-9 Bh oag =25.17' PILING 25125) 
REHAB 190! 

35.01' DIA SECTION—-AI 
-38.75" = = =| SS 

| ye ceELL NORTH PIER 

_+7.0' BUILT: SUBSTRUCTURE 1679-80 
i a F SUPERSTRUCTURE 1676,1667-9 

are 7 45.25" REBUILT 1966 
bs 1G.L.0._ 5 Bei 76.80 
_j—$-28 


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STEEL PILING 1 


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SAFETY 
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WALKWAY 


SECTION-B 


NORTH PIER 


BuILT 1897 
REHAB 1981 


SER al : : 276.8" 


| e210 
z-27 
STEEL PILING—\- 


STEEL PILING 


CHANNEL 


-9.5' 


Scale of Feet 


"B % 2 on 30 40 


arpa SECTION-—F 
SOUTH PIER 


ACBUILT 1930 
PEPAIRED i966 


Figure 42. Details of Charlevoix Harbor Jetties, Michigan 


59 


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VICINITY MAP 
SCALE OF MILES 
100 50 100 


D CAUTION 
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© 


MICHIGAN 


1.6.4.0. EL. 576.8’ 


NOTES: 

Project depths, soundings and elevations are referred to 
International Great Lakes Datum (1955) for Lake Michigan, elevation 
576.8 ft. above Mean Water Level (M.W.L.) at Father Point, Quebec. 

Scale of Feet “€bap 
100 ° 100 200 
————————_———S=_—SSSSSSSSS==SS=) 


Figure 44. Leland Harbor Breakwater and Jetty, Michigan 


61 


je DIA 17.5' = 2 


eae 3 oO 
re a ES he ‘ (one fe | Neale YU Sa 
: Re AGGREGATE 
(ARIE re = CELL FILLY 
hal £2. Jo >): 3 
ive | | ee 


—SP-6 STEEL 
SHEET PILE 


=21.5° 


SECTION-B 


BUILT: 1936 
REPAIRED: 1952 
REHABILITATED: 1966 


€ 
250-1000L 8.! 
STONE | 


S-28 STEEL 
SHEET PILING —+ 
ER eee oe = el 
uJ 
oO 
= SECTION-A 
i¢p) CONSTRUCTED: 1968 
8'-0" 
[sa 
BS 
576.8 a ot Hs ; IPRs a bGLO, 


CLOSE PILING 


STONE MATTRESS 


SECTION-C 
BUILT: SUBSTRUCTURE: 1936 
CONSTRUCTED: 1968 


COVER STONE 
5 TON MIN. 


LAKE 


SECTION I -10' 
SECTION I-8' 


1G6.L.D. 


STONE MATTRESS 


SECTION-D 


RUBBLE MOUND 
BUILT: 1941-3 


TOE STONE 
7 TON MIN. 


EXISTING BOTTOM ~ 


TYPICAL CROSS SECTION-RUBBLE MOUND BREAKWATER 


CONSTRUCTED: 1968 


576.8' 


LAL.0. 


STEEL 
SHEET PILING 


SECTION—E 


stv! vn 
SHORE CONNECTION 
QUILT! 1946 


Figure 45. 


62 


Scale of Feet 


ee 


Details of Leland Harbor Breakwater and Jetty, Michigan 


SIDE 


HARBOR 


35 


UPSTREAM LIMIT OF 


TAT! 
SUMS Galas FEDERAL PROJECT 


32 
PROJECT DEPTH USK EGON 
35 
LAKE 
> 44 
NAVAL ” 
- be 
—. @ s 
\ 
% 
2 
%, 
By 
a 
6 
XY 98 CANADA 
30 MUSKEGON . 
3 w) 
ra COUNTY 2 
Ce) 
/GLO ELEV 576.8" 
# 7 2 
v q MANISTEE 
2 
bd 
iS 
= 
S 
= 
ww 
x 
x 
s 
INDIANA 
VICINITY MAP 
r SCALE OF MILES A 
NOTES ; 
Project depths, soundings and elevations are referred to 
NORTH Isternational Great Lakes Datum (1955) for Lake Michigan, elevation 


MUSKEGON 576.8 ft above Mean Water Level (MW.L.)at Father Point, Quebec. 


Scale of Feet 
500 o 500 1000 1500 2000 
nt 


LOCATION MAP 


MICHIGAN ‘ SCALE OF FEET 
4 ° 3,000 10,000 5,000 ul 


Figure 46. Muskegon Harbor Breakwaters and Jetties, Michigan 


63 


=— 255' TO 195! A -aquarry RUN 
B -1 To 5 Ton 
C- 4 TO 5 TON 
D - 8 To 10 TON 
_ _576.8'_ 


IGLO 


SECTION -—A 
NORTH BREAKWATER 


out 1930-1 


3 
veal SECTION-B 
| NORTH BREAKWATER 


BuILT 1930-1 


SAFETY malenas| 
OUTER 54 LINEAR FEET OF 


SECTION "C" CONSISTS OF 
2 RECTANGULAR CAISSONS 


Wow We WNW 


SECTION — 
SOUTH BREAKWATER 
But SUBSTRUCTURE 1927-30 
SUPERSTRUCTURE 1927-30 


10. 
i i. it ne 
3 3 3 
—+71' - P 


SAFETY RAILING 


[4 
fo} 
a 
a 
< : Lye 
= VS NY 
oH coRECTION TE. 
SECTION — O ovicT  suastmucture 1927-30 
SOUTH BREAKWATER SUPERSTRUCTURE (3877/39 
i 
ounT BUOSTRUCTURE 1927-30 . % ° . SAFETY RAILING 
tT gupERSTRUCTURE 1027-30 liam 1 


SAFETY RAILING 


LAKE SIDE 


ene Toe STONE SEGTION=G 


SOUTH BREAKWATER 


BUILT SUBSTRUCTURE 1926-30 
SUPERSTRUCTURE 1930 
UNDER CONSTRUCTION 1966 


MATTRESS 
STONE 


SECTION-F 

SOUTH BREAKWATER 
BUILT: SUBSTRUCTURE 1926-30 
SUPERSTRUCTURE 1930 
UNDER CONSTRUCTION 1966 


SAFEVY 
RAILING 
Scale of Feet 
10 ° 10 20 yo 40 
576.8' eee —$—— ees: } 


SECTION-H 
SOUTH BREAKWATER 


BuILT SUBSTRUCTURE 1920-30 
SUPERSTRUCTURE 1930 


Figure 47. Details of Muskegon Harbor Breakwaters, Michigan 


64 


HARBOR 


OR 


CHANNEL 


SAFETY RAILINGS (TYP.) 
+ 8.5' 


Z IML, 
i 


PRS 


Scale of Feet 
10 te} 10 20 30 40 


TYPICAL SECTION 


NORTH PIER 


BUILT: SUBSTRUCTURE 1906 
SUPERSTRUCTURE 1933-4 
REHAB. 1980 


S.R 
1904 SECTION - N 
LOS) SOUTH PIER 
BUILT: SUBSTRUCTURE 1875 
SUPERSTRUCTURE 1932-3 
REHAB. 1966 


-45.5 


TYPICAL SECTION - O 
SOUTH PIER 


BUILT: SUBSTRUCTURE 1668,96°99 
SUPERSTRUCTURE (932-3 
REHAB 1966 


Figure 48. Details of Muskegon Harbor Jetties, Michigan 


65 


1GL.D EL. 576.8" 


CHARLES 
MEARS 
STATE 


DUMP GND. 1-1/4 HI, & E 


@ 270° AZ 


MAINTAINED TO 
12FEET 


SUBM. CABLE 


UPSTREAM LIMIT OF 
FEDERAL PROJECT 


LIMITS OF 
APPROVED PROJECT- 


NOTE: Work remaining to be done shown thus: 

Project depths,soundings,and elevations are referred to 
International Great Lakes Datum (1955) for Lake Michigan, 
elevation 576.8 ft. above Mean Water Level (M.W.L.) at 
Father Point, Quebec. 


Scale of Feet 


500 
——— 


INDIANA ' 


VICINITY MAP 


Scole of Miles 
CONCORD ‘90 5 ! 


N T WA 


EOWELIE STREET 


STREET 


FIRST STREET 


il 


SECOND STREET 


THIRD STREET 


Figure 49. Pentwater Harbor Jetties, Michigan 


66 


SIDE 


CHANNEL 


2470 28° 


+7" 


SECTION— A 


NORTH PIER 
BUILT SUBSTRUCTURE 1872,99 
SUPERSTRUCTURE 1938 BUILT 


SECTION—- D 


NORTH PIER 


SASBNAR| 


SECTION— B 


SECTION 


ar 576.8" 
(esmore= = — FH 


SZLERGE 


SECTION — C 


N. 8S PIER NORTH PIER 
NP SP BUILT SUBSTRUCTURE 1870,98899 
SUBSTRUCTURE 1870,98499 869,99 SUPERSTRUCTURE 1938 
SUPERSTRUCTURE 1938 1938 


=JE SECTION -G 


NORTH PIER SOUTH PIER 
BUILT SUBSTRUCTURE 1870,98 6 99 BUILT SUBSTRUCTURE 870,898 BUILT SUBSTRUCTURE 1887,9 
SUPERSTRUCTURE 1938 SUPERSTRUCTURE (938 SUPERSTRUCTURE 1938 


+7 
576.8" 
SOUTH PIER SOUTH PIER 
BUILT SUBSTRUCTURE 1870,99 BUILT SUBSTRUCTURE 1868,99 
SUPERSTRUCTURE 1938 SUPERSTRUCTURE 1938 
10-0" 4 
TOE STONE ‘ 
9 TON MIN a i 2 es LINE 
1 Scale of Feet 
MATTRESS STONE ad 10 0 10 20 30 a0 
/ \ (2820-82828 = ————— —— —— 


TYPICAL RUBBLE MOUND SECTION 


BUILT 1959 


Figure 50. 


Details of Pentwater Harbor Jetties, Michigan 


67 


ST. 


UPSTREAM LIMIT OF 
FEDERAL PROJECT 
6 


WISCONSIN ST. 
FRANKLIN 


GRAND AV 


U.S.141 & ST HWY. 32 
: Y 


RIVER 
STATES 


(o} 


IPSTREAM LIMIT OF 
FEDERAL PROJECT 


MICHIGAN 


27 


27 
PROJECT DEPTHS AND SOUNDINGS 
ARE REFERRED TO LOW WATER DATUM 
576.8 FEET ABOVE MEAN WATER LEVEL 
AT FATHER POINT, QUEBEC. 1.GL.D. (1955) 
(INTERNATIONAL GREAT LAKES DATUM ) 


SCALE OF FEET 
I = 


i = 
200 400 600 600 1000 


VICINITY | MAP 


SCALE OF NILES 
CoAT 1 
MILWAUKEE o = ct 


4 


Figure 51. Port Washington Harbor Jetty and Breakwaters, Wisconsin 


68 


SIDE 


HARBOR 


SUPERSTRUCTURE ON SOUTH 
BREAKWATER 1-6 BELOW 
TOP OF CAISSON. 


NOTE: OUTER 54 LINEAR 
FEET OF SECTION A, NORTH 
BREAKWATER, CONSISTS OF 
TWO RECTANGULAR CAISSONS. 


N 
NORTH & SOUTH BREAKWATER 
NB SB 
BUILT’ SUBSTRUCTURE 1934 1936 


SUPERSTRUCTURE 1934 1936 


CAP STONE 
GROUTED IN 
PLACE 


+7.5' 


PILES ARCH CELL 
TYPE 


cd ro oop 9, 
P0004 aw 2Naa0.60-7--S8sle 


i} -19'To-27' 
SECTION-B SECTION-D 
NORTH BREAKWATER NORTH BREAKWATER 
BUILT: SUBSTRUCTURE 1934 BUILT: 1934 
SUPERSTRUCTURE 1934 
+7.0' 


STEEL SHEET PILES 


BUTTRESS, SINGLE WALL TYPE 
Lw.o 
13:1 SLOPE t1 SLOPE 
i gl 
ig 
LUA = To-17 
FRO PPPOE PPS 
SECTION-E 
NORTH SHORE CONNECTION 
SES VOWS Quit 34 
NORTH BREAKWATER SCALE OF FEET 
BUILT: SUBSTRUCTURE 1934 
SUPERSTRUCTURE 1934 L} ° 0 20 %» 


Figure 52. Details of Port Washington Harbor North and South 


Breakwaters, Wisconsin 


69 


KF 
2 


teres 
wig 


7 7 
SAND & EARTH ty 
FILL 


Beye 
™ en ee) i =| 
(i an H 
Sy a j | 
N Nu 


uJ 
(2) 
7) 
SECTION-F SECTION=-G 

x NORTH STUB PIER NORTH STUB PIER 

BUILT: 1940 BUILT: 1940 
(eo) 
ao 
a ‘ 

6 
< +8.7- lr a 
x= 
—_ —L.W.D. 576.8 
53% 
Sa 
a eS 
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x 
U 


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BUILT: 1936 


SCALE OF FEET 
[=o 50S eS Se ee SS) 
$ [*) Le) 2 30 4 


Figure 53. Details of Port Washington Harbor North Jetty and South 
Breakwater, Wisconsin 


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74 


rubble-mound structure. The remainder of the structures at Keweenaw are tim- 
ber crib with some rubble and steel sheet piles. 

31. In general, the rubble-mound structures in the Detroit District 
that show toe stability problems have shown the results of this problem 
through damage to the upper slope and crown armor. It is not known defi- 
nitely, but it is expected that the toe damage is a combination of toe armor 
instability combined with foundation scour and undermining of the structure 
toes. Repair to a structure is carried out by filling the scour holes with 
stone and then reshaping and repairing the structure's armor stone layer(s). 
Some repairs have been successful thus far, while other areas require frequent 


repair work. 


75 


PART III: DISCUSSION 


32. In general, there appear to be three major problem areas with 
rubble-mound coastal structure toes. One of these pertains to the proper 
sizing and placement of toe buttressing stone. The purpose of the buttressing 
stone is to stabilize the onslope armor by preventing downslope slippage of 
the armor layer. For these stone to function properly, they must be of suf- 
ficient weight and placed in such a way that they are stable in a wave and/or 
flow environment. The second major problem area concerns toe berms. A toe 
berm's primary function is to protect a structure placed on an erodible bottom 
from being undermined by wave- and/or flow-induced scour and to resist down- 
slope slippage of the armor. For a toe berm to function properly it, like the 
toe buttressing stone, must be composed of materials and be constructed in a 
geometry that will be stable in the incident wave and/or flow environment. 
Thirdly, toe buttressing stone and toe berms are susceptible to damage and 
failure when placed on an erodible bottom material. The stone may be sized 
adequately for the level of energy to which they are exposed, but the exposed 
bottom material at the outer perimeter of the structure may readily erode 
and/or an inadequately designed bedding material may allow the foundation 
material to migrate through it and the toe berm armor. Either one or both of 
these factors can result in the undermining and displacement of stone that 
were otherwise able to withstand the wave and flow environment but failed 
because of undermining induced displacement. 

33. In summary, a toe failure may be the result of any one or a combi- 
nation of the above. Guidance exists for proper design of bedding (filter) 
layers based on soil types, but very little guidance is available for the siz- 
ing and geometries needed for the proper design of toe berms and buttressing 
stone for incident wave environments. Most work done by the districts in 
these areas is based on field experience and engineering judgment. A scouring 
bottom is a problem in itself. No matter how well a toe is designed, if the 
local bottom materials (sands, silts, clays, etc.) are exposed to sufficient 
energy levels for scour to occur, the toe of the structure is doomed to fail- 
ure unless the toe berm is extended out to a point where the energy levels are 
below those which will initiate scour. In most cases this is not practical or 
feasible. In these instances, sufficient toe berm material, that in itself is 


stable for the wave and/or flow environment must be placed so that as the 


76 


structure toe undermines, the berm material can slough off into the scour 
hole. This will provide some armoring to reduce the rate of scour and thus 


increase the usable, or functional, life of a structure. 


77 


PART IV: CONCLUSION 


34. Based on extensive discussions with Corps division and district 
personnel and after the review of prototype experience relative to rubble- 
mound toe stability problems, it is concluded that design guidance is 
seriously needed on the proper sizing and placement configurations needed to 
provide adequate buttressing stone and toe berms for rubble-mound coastal 
breakwaters and jetties. Once it is understood how to design toe berms and 
buttressing stone for a range of water levels and wave conditions, these 
designs need to be incorporated into a test series that addresses the way in 
which varying toe geometries influence localized scour. The latter will pro- 
vide some qualitative insight into how a toe berm can be configured or 


positioned to reduce the quantity and/or rate of localized foundation scour. 


78 


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