fol. f+---'--l,--- - usgs · thlj work was performed as a part of a cooperative program of the...
TRANSCRIPT
commonwealth of Massachusetts oepart!:lm t of Public ·., orks
"I•. F . callahan, C omnissioner
U. S. l.Je?artment of the Interior Geoloe;ical Sur··ey
~ •• E. urather, Director
1 -
Cooperative Geologic Project
Geologic Interpret~tion of Seismic ~ta
Route 128 ( H0rthern Circumferential Highway)
Cut, and Hopkins Stre~t Grade Separation
Stations l-18
in 'h akefield. 11ass.
by
James E· ?Ua yna.rd, Geologist, u. s. Geolo t;ical Survey
and
Rev • .I)aniel Lin ehan, s. J., Seismologist, \',aston College
..J S G eOLOGICAL SURVEY
4 pages of text 3 plates .J
MASS . D E P T O F Pu::: :.. 1C V..'JR KS COOPERATIVE GEOLOGIC Po~OGRAM
OPEN FILE REPORT · ••i th is rPpor t have OC('fl placPJ in op ·n fi h·s for publ i•· in: p:·• ·l •• •:• ut
'.if l '\1 ;TO:\ , D. C., (;E :\ E IL\L SEH\' ICE-, B' LD'C , Fa t 18t h t\: l!•t h . ' \ . \r . C. S. Gl-OLO(; )(':\L SU in· J:Y: LI Bil:\ HY , und offi l'c uf the I · .I ,f \' 1:1-: HI:\G GEO LOG Y BH A:'\ C H.
' 1
' •\ · :\1.-\S:5:\C H {j;;LTT1'i , 100 :\ AS II L \ ST. Offic('.> of t h(' PH O.JECT 1 · . , .J-; U: ,~. :\1.-\SS. DE PT . of PU BLIC \\' O HK S, :.nd of the t ' :\ I TE D
Seis~ic Series # -----. : ·~~~~- ~OLOG IC:\ L SU _ _ _fol._f+---'--l,- --
GeoloGic Interpretation of Sei~~io Data
"Route 128 (~lorthern Circumferential Hi~hway)
Cut, and Hopkins Street Grade ~eparatio~
Stations 1-lS
in i'1akefield, Mass.
oy
James E. l.iaynard, Geologist, TJ. s. Geological Survey
and
Rev. Daniel · Linehan, s. J., Seismologist, ;,aston College
General Statoment
The co~~letior. of a sesment of the ~orthern Circumferential Highway,
Route 128, in ~·.akefield, Mass., requires an underpass bridge at ii o?kins Street,
stctior. 5+50. T!le r,lan of the proj ect shows approxirr.l!tely 1800 feet of
approach cuts :>etween stations 1 and 1a. In October 1945 a preliminary
seismic stuuy was rrede of a segment of this cut ':)et-ueen stations 6+50 and
l3+.JO. Four profiles ;·;ere made at th~ time and a report was submitted by ,,; ~ ' .
. <o· . ..-ton E. Ch ute and Rev. Daniel Linehan (file report of Je.nuo.ry 15). This
-•. ork s ho-••ed e. relA.tivel y shallow (in general, 6 to 12 feot in depth) somewhat
irregular bedroc:c surface bet ,;een statio!l.s 6+50 and l3+5J. Tha-t data
i nd icated the. t much of this segment of the cut will be in ':Jedrocl:. In order
to obtain more c or:1plete data for the preparation of detailed estimates on
the amount of bed,ock to be excavated for this segment of the cut, and also
to obtain sufficient data for the unexplored segment of the cut, 21 additional
sr:: i!;mic traverses were In'3.de in September 1949. The present report contains -o-:1ly the results obtai!"led from t his later work.
- 1 -
Thlj work was performed as a part of a cooperative program of the
:~assachusetts Depart:nent of Public \'. ork: c; and the United States Geoloe;ical
survey.
Surface Geology
At this location the proposed road will traverse the southeast side of a
Large bedrook-till hill that is flanked by a sand-eravel kame terrace. The --? oorly defined boundary t Qf the terrace and the till area crosses th.e proposed
center!J.ine in the vicinity of station 5+70. Numerous outcrops of bedrock
occur with in 200 feet of the centert_line; they are c o.m;>osed of somewhat
coarse gra i ned, slightly pink granite, medium-~rained dark-colored melanite,
or a comb i nation of both of these t ypes of roo k . 'l'hese rocks appear to
underlie the ent ire area of ~~e proposed cut. The till as observed in shall~'
t es t pits is loose to moderately loose in texture; in most places it is covered
by a layer of fine sand fran a few inches to 3 feet i n thickness. The s'..lr face
beology of the site and of the adjacent surroundinb area sugsest~ that the till
is a rather thin veneer on an irregular bedrock surface. A ceelogie map with·
t he locations of the center~line and the seis~ ic traverses js shown on sheet 1,
S~ismic Traverses
The layout of t he seismic trt1verses is sh own on the geologic mep., sheet 1.
Tne lengths, in feet, of the seismic traverses are as follows:
A '-I3 1 , 165 K 1-L 1 , 165 D-Q, 220 B •-c I. 165 N-o. 220 F-,., "'• 220 A.'-DI, 110 P-Q, 220 G-H, 220 E '-F I. 150 K'-~, 220 H-I, 220 F'-I', 165 A-.a, 220 I-J, 220 ~ '-H ', 165 B-e, 220 K-L, 165 H'-J', 180 C-D, 220 L-1~. 220
- 2 - ' -
The shot points for i..he seismic traverses were located as follows:
A'' station 5+30 B I, II 3+65
c '. n 2+00 v D '' 108 feet to the left (north) of station 5+08 E ', 50 " n n n n II • 5+38 • F I, 50 n n n n II n a 3+88
I'' 50 n • n n n • " 2+23 G I, 50 .n " " riGht (south) • •• 5+30 HI, 25 " II " n n II II 3+65 J I I 55 " " II n n n n 1+85 K ', station 5+95 11, 15 n II II n (s.s.) n " 8+14 N, 50 n II n " II n II 6+07 0, 55 n " n n II " n 8+20 P, 50 n .. II left (N .Yi.) n n 5+82 Q, 54 n " " n II " " 8+14 A., 32 " II n n " n " 17+20 B, 53 II n " II " n n 15+00 c, 57 '" II " " II " " 12+80 D, 55 II II " " n " " 10+40 F, station 17+00 ,. II 14+80 'JJ
H, 15 feet to the right (s.E.) II II 12+58 I, 18 II II II " " II II 10+20 J, 4 " " " II n n II 8+22 K, 42 II II II II " II n 11+88 L, 63 " II: II II II II n 10+26
Depths to Bedrock
The depths to bedrock at the shot points as calculated from the seismic
datu are as follows:
A' - 7 feet K I - 7 feet D- 10 feet 3' - 15 n (average) 11 - 11 • F - 10 " C' - 10 II N 9 II
G - 14 " Dl - 7 II 0 8 " H - 12 '" E' - 9 " p - 11 II I - 15 .II
F' 13 II '-4 12 " J - 10 II
I ' - 12 .. J.... - 10 " K - 8 "
G' - 9 • B 8 " (averae;e) L- 10 II
HI - 13 • c 8 " II
J I - 7 If
- 3 -
Geol~ic Interpretation of Seis~ic ~ta
The. geoloO" ic sections as interpreted from the seismic ciata,_and-the
geol~y of the site are sh~nn on sheets 1, 2, and 3. Although the bedrock
surfaces are ~hown by smooth curves in the sections, it is probable that the
actual bedrock surface is much more irregular than these curves SU€ges~ as
the detectors were too widely spaced to pick up very small ridr;es and points.
The f'Ositions of the bedrock surfaces in the vicinity of shot points B', F',
c, and b II§ly be closer to the surface and may differ appreciably in ·c onfigu
r~tion from these forms sh~Nn on the sections. ~uch of the difficulty in
interpretation at these places may have been caused by the re&istration of
side refractions instead of vertical refractions when shooting in opposite
directions fro;~ c ornmon shot points. The most logical interpretation from the
avsilable seismic data and the Eeology is shown by the dotted lines. The
act •.Hll deoths to bedrock at shot points A', J', C, A, K, K', O) and N may vary
a foot or :nore from the reported value, for they were calculated from assumed,
though reliable, till velocities deter::nined from nearb~· traverses. The depth
to bedrock at shot point F was similarly calculated because the two detectors
ne~rest the shot point failed to register; this value also should be of
re~ sonable accuracy.
- 4 -
Sto 2
Y'
I
ISO ·
1\.)Q •
0
Sand 8 910v~l ~ ?.OOO 11 V, 2900 ff./S~CS _. .-- - -
.. ----B~dtoek v, 11000 -18000 fr / ucs B~drock V, IICOO - o<:. ff / UCJ
-,-------------,------------,---100 165 200 300
lndtfll'llff Doundar~ bfhUt l'l _ / ' sand 8 Qrovel and t ill
PLAN OF TRAVERSES
SCALE ' IINC H =IOO FHT
Ltlll"t5 rel l" t IC' 'hot ~0 · n~ s c ~ ! 1'105 o ' I ro we r se 5 Numbers refer to O. P. W. stat ions on center lines .
\ Ind ef inite contoct
150
100 330
•!..:
NOTE: Dotted pott 'oM of nct ions ind•tolt inconc lusivt seismtt dolo .
, I , ,, ,
CO M~' O '.W [ Il L T t1 fH ~ !o !>SAG .; u :, [TT 5
Q[r- t~ R T M [ II. T t: r P L. SL I( W1RY<;
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:._ LJGI(.A_ "~ llv[ <
r;,)O " fF..l. TIVf j( _'(; I (. PI./I Jt , 1
' 2 00
IS O -150
B~dtock v, 10000 -20000 It /s~cs
L.oo IOO-j-----0 100 110
INTERPRETATIVE GEOLOGIC SECTIONS ALON G SE ISMIC TR AVER SES
v.
WAKEFIELD ROUTE NO 128
GRADE SEPARATION-STATION 5+ 50 CUT STAT IONc::S_;I_;-Ic::B _______ -t
SCAL E. I I NCH • 40 FE ET
Apport"' seo s m•t v~t l<~t ily (•e'l on le;:lpt• sttond
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S( tS MtC. QAl A BY OANI[I. LI NE. H All , S J
ENG tNEE.Rl NG 9r WI LLI AM H SH A D
OfiT E SEPTEMBER ,1 94 SHf E' I U 3
Go
r 200 . zoo
Sand 8 gror~ l
__...-:- V,~100 · 2J00 ff / SUS
~--------------r Sond 8 gror~l
• ---~"w.L;a_OO_!.!(l!fL_
150 ' '-150
s~ato~* V, 8000 26000 ff / ucs B~droc* V. 7000-21000 ff / Ucs I
,,
zoo
B~drocJ V. 11000 -15000 f t/ucs B~droO V. 6000
CO '~\' Q f, II [ A,_T-i t' ' '.I:. C:,S AC.;u· f_ T T<.,
D f·llo~f'.:t~ T I " " LBl 'f 'h q ., r,
S '(0 ,, 1:- ' p,• t_ NT · r T ~ f N lt_ lof 'J r.
·t: . ) "': ·' - -,.,.Q., E ~
[ ,
. 200
II 'S~CS
100--------- ----- - ---,---,---- ----1-100 34 >
100---------- -,-------· ---,--- ----- ---· . •00 0 100 lBO 200
c .._,
200-
p '-
200 .
100 -0
8rd,OCk V, 6500 -30000 If / SUS
--, 100
~-- Loou !Ill V. 2200·2800 lt;s~cs
-.- --200 220
300
150- ·.,, . . ---- . _ -~------
---- ....----..... =~7::-:-:.~ .. ::: ... -.. -.. -.. -.. -.. -.. -.. -.. -._------
0 100 165 200 300 ~ 15
LOOSf' f ill V I_!J2,0.:,!_GC!!!_f~~ --------'~-------=::::~Lo~:..~":.:;:"':.:'~ ,. ' 150
Btdrock V. 9500·16000 ff /s t cs
30C - ,
400
A 'V I - 200
' 4 40 ---,-- - ------
>OO -,
GOO . •00
660
-. -L2f!!.t!.:.!. l~ 200~2r:!!- '!_!!~ --1 ____
1 _
1 ___!!_~druck Y: 7500-~ '.!L!f9- - ---- + IOO
880 900 1000 1100
IOO·---- Bt drock 'I 6500-C><:::. ff /_!~CI __
660 700 800 INTERPRETATIVE GEOLOGIC SECTIO NS ALONG SEISMIC TRAVER SES
PLAN OF TRAVERSES
SCALE I I N C~• -
ltll~ · ~ 't't' 1 ~ \ 1'1 0 1 pc .,. s c• t n'.ls o ' ••o
NOTE Oolttd porr ions of st ct •ons 1nchcott lfiCOfiC hJS I~t Sf iS miC dolo.
WAKEFIELD ROUTE NO 128
GRADE SEPARATION STATION 5+ 50 CUT STATI ONS 1- 18
SCALE l i'o C >1 • 40'-l£'
:. op a ·e r-• \t •\ m•t H~ ' "' ', ~ tsl .~ 'e et Pt • nt'ln~
· -
----------------------------------------------------------------------------------------~----------------~
Stol 4 "+80
t 200
150
J
'r 200
ISO
CO M'-' 0~:W£..t. ~T~ \' I M A<;.SAC>i lJ ...-, £. TT ~
DEPIIJH ME NT ') r- P\J ~ ll( w· ~ · S
U '; D(P.\FH M[ NT ~ r TH ( IN T[ R ) ~
:.. . • JG •~" :. _ ~. ~Vf 1
--~~-=--~::-==~-~L:o~os='='~':_~v~/~90~0=·=2~00:0=:/l=~=·~cs=:~--::~-~==~'f~~~~~:::=~~~~~~~~IJ,~,---------'~ll ____ ~~~==~~~~~~~----_j;-•• --.. ~U / til V, 1900:_!,_200 (I / UCS .'Loost /Ill V, 2100·2200 II/SUS
150 -- / - -1'50 ---~-- 1
B~dro~k a: 11500·15000 fi / StcS B~t!rock v, 9000· C>C 11/srcs &dtocl v. 11000·25000 lf/s~cs
IOO+-------------,--- --------- -- --- ----r------------,----,--------,-- ·-- ----J100 0 100 200 220 }\)(' 400 440 500 600 60 !)
I
'r
I 150
Loosr 1111 --~f!!t.2100 ff/StCS
----__ - _ _!!!!_V:_!!_O~~~- ---
------ I --..... --''" V, 2500 lt./stcs;----_ _.
Brdrod V, 6000 - c::><: ff./st cs Btdrocl V, 90V0· C.C If /St CS Btdrqclt V, 9500·26000 11 / st cs --- ___ - _
IOO,~----------.---------.--.--------.-----------,----,------,------- ----.------~~oo
0 ~ ~= - ~ - - ~ -lnltrsrctio,.
S lo 17 Kt·LI F N
r~ t--=-==~~~==~=-----~L~oo=u~li~II-:V,-2~0~0~0~-20.2~0~0~1"/~~,c~<~ -.......; _______ _
200
ISO ISO
BMrock V, 7500-21000 ff /S~cs ~--------~~~~~---- -'~ v.:...!!o.2.:!o:!E. ''-/S~ 100+----------,--- -------,-+100 100
...!!!t. 'rock V, 4000 -e><:::. fl./sus
660 700 800 880 0 100 200 220
PLAN 0 F TRAVE'RSES
SCALE I I~CH • FEET
INTERPRETATI VE GEOLOGIC SECTIO NS ALO NG SEISMIC TRAVE RSE S
V -
--
WAKEFIELD I ROUTE NO 128
GRADE SEPARATION STATION 5 t 50 CUT STATI ONS 1-18
SCALE I 1 ~1C H ' 40 I[ [T C. E'X.'>Gl' 8 • tl E ( HUH. · J £ MAYN ;.)R O
St~ot -. ~· "'
APDOff , ' ~t · \m l t wr "t I) l• e\) '"teet pe• ~fc~nd
Q:, r SEP T t9>!09 I ) '1 f • • 3 "" r ~