he sper ia 75 ( 2006)
Page s 327 – 35 6
Fortificationsof
MountOneion,
Corinthia
ABST RAC T
RecentinvestigationsontheIsthmusofCorinthbytheEasternKorinthia
ArchaeologicalSurvey(EKAS)haverevealedaseriesofrelativelyhumble
fortificationssituatedalongtheridgeofMt.Oneion,whichformsthesouthernboundaryoftheIsthmus.TheseLateClassical–EarlyHellenisticwalls,
alongwithanearbyseriesoflaterVenetianfortifications,weredesignedto
blockaccesstothesouththroughseverallowpasses.Controllingthepassage
of northern armies through the Isthmus to the Peloponnese was clearly a
long-termstrategicconcernfordiverseregionalpowers.
TheIsthmusofCorinthisoneofthemoststrategicallyimportantregionsin
theeasternMediterranean.1Itliesatthejunctionofthemainnorth–south
roadsbetweencentralGreeceandthePeloponneseandthesearoutesbetweentheeasternandthewesternMediterranean.TheCorinthians,with
theirimposingcitadelofAcrocorinth,traditionallycontrolledtheIsthmus,
whichrunsfromthecity’swesternportofLechaiontoitseasternportat
Kenchreai (Fig. 1). At numerous times, however, a foreign power such
asRomeorVenicehassoughttodominatethisstrategicallysignificant
corridor.
TheIsthmusisbotharelativelyfertile,flatagriculturalareaandthe
naturalpointofdefenseforthePeloponneseagainstanyattackfromthe
north.2Only7kmwideatitsnarrowestpoint,theIsthmusiscuttodayby
theCorinthCanalandwascrossedinantiquitybytheDiolkosroad.Itis
1.Wewouldespeciallyliketothank
DanielPullen,codirector,andThomas
Tartaron,fielddirector,oftheEastern
KorinthiaArchaeologicalSurvey
(EKAS).The37thEphoreiaof
ClassicalandPrehistoricAntiquities
andthe4thEphoreiaofByzantineand
Post-ByzantineAntiquitiesprovided
cooperationandencouragementat
everystepofthisproject.Wewould
alsoliketothankRonaldStroud,
JamesWiseman,andMerleLangdon
foradviceandforreadingearlier
draftsofthearticle.Thanksarealso
duetotheanonymousHesperiareferees,
whohelpedusavoidmanyerrorsand
infelicities.HollyCookpreparedthe
potterydrawings,andKarenSoteriou
preparedtheplansoftheMaritsaVenetianfortifications.Finally,special
©T h e A m e r i c a n S c h o o l o f C l a s s i c a l S t u d i e s a t A t h e n s
thanksareduetothemanymembers
ofEKASwhotrudgedupanddown
thesteeppathsofOneioninhotand
sometimesdangeroussituations,often
carryingheavyequipment.Thisarticle
isprimarilythefruitoftheirlabor.
2.Wiseman1978,pp.17–21,52–
56,81–82;IsthmiaV,pp.7–10;Fowden
1995.
328
w i l l i a m r . c a r a h e r a n d t i m o t h y e . g r e g o r y
oneofahandfulofnaturalplacescriticaltothedefenseofGreece,along
withtheeasternpassofThermopylaiandthewesternpassesofKithaironParnesbetweenBoiotiaandtheAttic-Megaridregion.3Althoughthese
threeareashavenaturalfeaturesthathavemadethemeasilydefensible,all
ofthemrequiredcomplexsystemsoffortificationtopreventthepassageof
anenemy.HereweseektoshednewlightonthesouthernmostfortificationsoftheIsthmuscorridor.
AtthesouthernboundaryoftheIsthmianplain,theabruptheightsof
Mt.OneionprovideanaturaldefensivelinefromKenchreaitoAcrocorinth
(Figs.1,2).ForanenemyapproachingMt.Oneionfromthenorth,the
sheercliffsandsteepslopespresentaformidablebarrier.Togainaccessto
landssouthofthemountain,itispossibletopasstheOneionbarrierina
numberofways(Fig.3).Theeasiestmethodistogoaroundit,eitherto
theeastorthewest.Theprincipalroutesofbothancientandmoderntimes
skirtMt.Oneiontothewest,followingthecourseoftheXeropotamos
(Leukon)RiverortraversingthevalleysoftheLongopotamos(Rachiani)
andNemea(Koutsomadiotikos)riversfarthertothewest.4Thedifficulty
withtheseroutesinthepastwasthattheyrandirectlywithintheviewof
thepowerfulfortificationsofAcrocorinth,oftenpromptinganinvading
armytoseekanalternativecourse.
TotheeastarouteranalongthecoastoftheSaronicGulfnearthe
portofKenchreai,justwestofthemoderncoastalhighwaytoEpidauros.5
Thedisadvantageofthisroutewasthatitpassedclosetothefortifications
ofKenchreai,andbeyondthesetheroadnarrowsbetweentheseatothe
eastandthemassofMt.Oneiontothewest.6Hereasmallforcecould
easilyblockaninvader’sprogresstothesouth.Aninvaderwithcontrolof
Figure1.TheIsthmusofCorinth,
withsitesmentionedinthetext.
W.R.Caraher
3.Fowden1995,p.550.
4.FortheXeropotamos,seeWise-
man1978,pp.81,88–90;Salmon1983,
p.36.FortheNemeaandLongopotamosrivers,seePritchett1969,pp.77–
79;Wiseman1978,pp.81,108–110;
Salmon1983,pp.36–37;Bynum1995,
pp.40–45;Pikoulas1995,pp.31–35;
Lolos1998,pp.129–132;Marchand
2002,pp.40–72.
5.Stroud1971a,p.127.Forthe
identificationofwheelrutspresumably
belongingtothisroadalongastretch
ofexposedbedrockonthebeachnorth
ofLoutroElenis,seeKenchreaiI,p.2;
Salmon1983,p.37.
6.Pseudo-Skylax54;KenchreaiI,
pp.6–12.
f o r t i f i c at i o n s o f m o u n t o n e i o n , c o r i n t h i a
329
Figure2.Mt.Oneion,lookingsouth
fromtheIsthmus.TheMaritsapass
isjustrightofcenter.PhotoT.E.
Gregory
7.E.g.,Diodoros(19.54.3)recorded
thatin316Kassanderavoidedacon-
frontationwiththetroopsofPolyperchon,whoheldtheIsthmusatthat
time,bytransportinghismenfrom
MegaratoEpidaurosbysea;seeStroud
1971a,p.142.
8.ForSolygeia,seeThuc.4.42–45;
CorinthI.1,pp.97–99;Stroud1971b;
1994,pp.269–280;Wiseman1978,
pp.56–58.SeeLorandou-Papantou-
niou1999forN.M.Verdelis’sexcavationsin1957–1958;forfindselsewhere,
seeStroud1971b,p.238;Wiseman
1978,p.58.
9.Tartaronetal.,forthcoming.
theseawouldhavefounditeasiertocircumventthedefensesalongthe
SaronicGulf.7
Whenaninvadingarmyfoundthenaturalroutesaroundtheendsof
Mt.Oneionblocked,itmightattempttocrossthemountaindirectly.It
ispossibletodosothroughoneofseveralnorth–southpasses,including
theStanotopiandMaritsapasses,whicharetheparticularfocusofthis
article.Toattempteitherofthesepasses,locatedintheeasternpartofthe
Oneionrange,anattackingarmymusthavehadseriousreasonstobypass
theeasierroutesskirtingitseasternandwesternends.Notonlyarethe
mountainroutesarduous,buttheywouldplacetheattackersinaposition
welleastofCorinthandoutsidethemainroutestotheArgolid.Themost
compellingreasonforusingthesepasseswouldhavebeenthatforcesattemptingtoblocktheIsthmiacorridortypicallyarrayedthemselvesatthe
easternandwesternendsofthemountain,defendingtheeasypassagesand
maintainingclosecontactwiththeresourcesandfortificationsofCorinth
andKenchreai.Anattempttopassthroughthecenterofthemountain
ridge, therefore, may have seemed preferable to meeting concentrated
defensesontheSaroniccoastorintheXeropotamosvalley.
There were other reasons for an invader to seek access to the area
immediatelysouthofMt.Oneionandeastofthetraditionalroutestothe
Argolid.TextualandarchaeologicalevidencefromtheClassicalperiodatteststotheexistenceofanunfortifiedcommunityatSolygeiaintherolling
hillsimmediatelysouthofOneion(Fig.1).8Archaeologicalfindshavebeen
reportednearthetownofAlmyriandonthehillsofBrielthiandVigla.
Moreover,inthecourseofgeologicalworkconductedbyEKAS,scatters
ofancientmaterialinthefieldstothewestofthemodernvillageofRhyto
wereobserved,indicatingthatthehillssouthofSolygeia,reachedtodayby
aroadheadingsouthfromGalataki,mayhavehadsignificantsettlementin
antiquityaswell.9Thepresenceoftheseapparentlyunfortifiedsettlements
withineasyreachofthecoastmayhavetemptedanenemyeithertoforage
330
w i l l i a m r . c a r a h e r a n d t i m o t h y e . g r e g o r y
intheirvicinityortocarryoutdestructiveraidsonvulnerablecentersof
ruralagriculturalproduction.
In addition, once an army crossed the mountain’s eastern end and
movedsouth,ithadbypassedthedefensesofAcrocorinthandgainedaccesstoacomplexnetworkofroadsleadingtowardthepopulationcenters
ofthesouthwestCorinthia,suchasTenea,Kleonai,andPhlius,aswellas
theSanctuaryofZeusatNemea.Thereafter,anarmycouldlinkupwith
routesintotheArgolidormovetowardthewestthroughtheuplandsof
the northeastern Peloponnese to descend into Sikyonia, Arkadia, and
Achaia.10Italsowouldhavebeenpossibleforaninvadingarmywithout
substantial naval power to proceed south into the Epidauria, although
thereislittleevidenceforthisactuallyoccurring.11Furthermore,east–west
routespassingimmediatelytothesouthofMt.Oneionwouldhavegiven
anarmyrelativelyeasyaccesstothecitywallsofCorinthinthevicinityof
thesoutheastgate,allowingtheinvaderstoattackCorinthfromanunex-
pecteddirection.12
Inthisarticle,wediscussthearchaeologicalevidencefromtheStanotopiandMaritsapassesofMt.Oneionandtheattemptsmadetofortify
theminatleasttwodistinctperiods.TheStanotopipassrunsjusttothe
10.Polyb.4.13.1–6.Theroadsof
thesouthwestCorinthiaandthepasses
intotheArgolidhavebeenwellstudied:
Stroud1971a,p.128;Bynum1995,
pp.14–27;Pikoulas1995,pp.285–288;
Lolos1998,pp.182–190.Walbank
(1957,p.461)proposedthattheAito-
liansmayhavefollowedaroutefrom
SikyontotheeasternpartoftheIsth-
mus,avoidingAcrocorinthafterthe
BattleofKaphyaiin220b.c.
11.Diod.Sic.15.69.1;Dixon2000,
p.94.
12.Thisistheroutetakenby
Dodwell(1819,pp.196–197).Forthe
gate,seeCorinthIII.2,pp.47–54.
Figure3.Routessouththroughthe
Isthmus:(A)thecoastalroute
blockedduringtheClassicalperiod
bythelongwallslinkingCorinthto
itsportofLechaion;(B)thetraditionalroutesouthfollowingthe
XeropotamosRiver;(C)theeastern
coastalroadpassingtotheeastof
Stanotopi;(D)theStanotopipass;
(E)theMaritsapass.W.R.Caraher
f o r t i f i c at i o n s o f m o u n t o n e i o n , c o r i n t h i a
331
westoftheportofKenchreai,andbytraversingit,anenemycouldskirt
theeasterndefensesoftheIsthmusanddescendintotheplaintothesouth.
Stroudhasalreadydiscussedthispassageinsomedetail.13TheMaritsa
passissome2kmfartherwest,betweenKenchreaiandthemodernvillageofXylokeriza,inanarealocallycalledMaritsaorTrypeioLithari.
Scholarsgenerallyhavenotrecognizedthismoredifficultandremotepass;
nevertheless,theremainsofsubstantialfortificationsdesignedtodefend
itsuggestthatitwasperceivedasaviableroutesouthduringtheancient
andearlymodernperiods.14
MAJ O R LINES O F D EFENSE INT H E E A ST ERN
CORINT H IA
13.Stroud1971a.
14.Thispassisnottobeconfused
withthewesternpassnotedbyStroud
(1971a,pp.129,137).
15.Stroud1971a,p.127.
16.IsthmiaV,pp.4–6.
17.Broneer1966;seealsoKardara
1971;Wiseman1978,p.60.
18.Hdt.8.71,9.7.1;Wiseman1978,
p.60;seealsoIsthmiaV,p.5.
19.Wiseman1963;1978,pp.59–
63.SeealsloLawrence1979,p.169;
IsthmiaV,p.5,n.35.
20.Wiseman1963,pp.255–256.
21.IsthmiaV.
22.IsthmiaV,pp.150–151;Malte-
zou1978.TherewaseventalkofrefortifyingtheHexamilionatthetimeof
theGreekWarofIndependenceinthe
early19thcentury.
23.Stroud1971a.Wiseman(1978,
p.59,p.77,n.91)listseightinstances
inwhichOneionwasfortifiedbetween
369and146b.c.
Stroudobservedthattherehavealwaysbeentwolinesofdefenserunning
throughtheCorinthia:afreestandingtrans-Isthmianwallandtheseries
offortificationsalongMt.Oneion.15Theideaofatrans-Isthmianwall
haslongcommandedthelargershareofscholarlyattention.Researchers
haveidentifiedandseriouslydiscussednolessthanfourtrans-Isthmian
fortifications,allofwhichweredesignedtotakeadvantageoftheseries
ofupturnedmarineterracesextendingnorthwest–southeastthroughthe
Isthmianplain.16BroneersoughttoidentifyandtraceaMycenaeanwall
thatranfromthebeachsouthofthecanalnearthemodernsettlementof
IsthmiatotheneighborhoodoftheSanctuaryofPoseidonandpresumably
beyond.17WisemanreportedfortificationsalongtheAyiosDimitriosridge
(Fig.3),arguingthatpottery,loomweights,andthemasonryitselfmight
identifythiswallwiththefortificationsconstructedduringthePersianWars
andmentionedinbooks8and9ofHerodotos.18Healsodocumentedmore
thoroughlyawallofHellenisticdatethatfollowedasimilarlineonthe
AyiosDimitriosridge.19Excavationsonthisridgeuncoveredsubstantial
remainsoftowersandwhatappeartohavebeenbarracks.20Whilethere
wasnoevidenceoftheClassicalwallbeyondthetopoftheridge,WisemanwasabletotracetheHellenisticwallasitturnedtothenorthwestand
ultimatelytothenorthtowardthemoderncityofCorinth.
Thefinaltrans-Isthmianfortification,andcertainlythemostimpressivetoday,istheHexamilion,constructedintheearlyyearsofthe5thcen-
turya.d.andrebuiltonmanyoccasionsafterward.Itsremainsarestillwell
preservedinmanyplaces,andtheycanbetracedfromtheSaronicGulf
totheCorinthianGulf.21Thisformidablefortification,despiteperiodsof
disrepair,servedtoblockaccesstothePeloponneseforover1,000years.In
fact,thelastattempttofortifythelowerlineoftheHexamilionwasduring
thesecondperiod(1686–1715)ofVenetianoccupationofthePeloponnese,
althoughtheVenetiansenatewasevidentlyunabletoprovidethefunds
necessaryforitsproperrepairanddefense.22
ThesecondlineofdefenseservingtofortifytheIsthmiacorridorwas
farthersouthandtookadvantageoftheOneionrangeasanaturalbarrier
againstnorth–southmovement.23Thefortificationsalongthislineleftthe
plainoftheIsthmusundefendedandcouldnotprotectagainstanarmy
thatmovedwesttoenterthePeloponnesethroughanyofthenorth–south
332
w i l l i a m r . c a r a h e r a n d t i m o t h y e . g r e g o r y
rivervalleys.TheOneionfortificationswerealsolessspectacularthanthe
freestandingwallsofthelowerplain,andtheywereapparentlyerectedand
mannedunderlessdramaticcircumstances.Theyareassociatedwiththe
StanotopiandMaritsapasses(Fig.4).
TheStanotopipassrunsbetweentheprincipalmassofMt.Oneion
anditseasternmostprominence,ahillcalledStanotopi.Thispasscrosses
themountainatacomparativelylowelevation,ca.200m.Themainroutes
ascendthemountainfromtheflatlandnearKenchreaianddescendcloseto
themoderntownofLoutroElenis.Thebestpathsfollowtwoconverging
ravinesthatcutintothenorthfaceofthemountain.Theseravinesbegin
ca.150mtotheeastoftheentrancetoamodernquarry(whichatpresent
consumestheeasternextentofthemountain)and40mtothesouthof
thesouthernfenceofamodernGreekarmybase.Onerouteascendsthe
westernsideoftheeasternravineandtheother,probablyeasier,passage
runsjusttotheeast.ThesepathsprovideaccesstothetopoftheOneion
ridge,whichisunder250minelevationatthispoint,andfromtherean
armycoulddescendbynumerousroutestothesouth.
TheMaritsapassrunsacrossthecenterofthemountainridge,ascend-
ingca.2.4kmwestofKenchreaiand2kmeastofthevillageofXylokeriza.
Thebestmodernpathapproachesadeepravinefromtheeast,crossing
abroadalluvialfan.Ascentfromthewestwouldhaveinvolvedamuch
steeperclimb.Thepathfromtheeastascendssharplytowardtheeastside
oftheravinebeforecrossingtothewestsideofabroadsaddlethatpasses
acrossthemountainatanelevationofslightlyover320m.Onthesouthern
sideofthesaddlethepathbreakstotheeast,crossingthesaddleagain,
anddescendssouthalongthespinesofanynumberofalluvialfanstoward
GalatakiandancientSolygeia.
Figure4.Theeasternpartofthe
Oneionridge,withpassesandforti-
fications.Contourinterval20m.
W.R.Caraher
f o r t i f i c at i o n s o f m o u n t o n e i o n , c o r i n t h i a
333
Figure5.Classical–HellenisticfortificationsatStanotopi.Contourinterval
20m.W.R.Caraher
CLASSICAL– H ELLENIST IC FO RT IFICAT IO NS
AT STANO TO P I
TheClassical–HellenisticfortificationsatStanotopihavebeenclearlyand
accurately described by Stroud, who dated the architecture to the 4th–
3rdcenturiesb.c.,withalatestdateof224b.c.,basedonthepotteryfound
inthevicinity,aswellashistoricalprobability.24Themostimpressiveelementofthefortificationsisthefreestanding,nearlysquaretowerlocated
on the summit of the relatively low easternmost spur of Mt. Oneion,
overlooking Loutro Elenis (ancient Chersonesos). Made of rectangular
ashlarblockslaidinroughcourses,itmeasures8.80x9.10mandispreservedtoamaximumheightof1.20m(Fig.5).Tothewestofthetower
istheso-calledupperenclosure,coveringanareaofabout75x125mand
seeminglysurroundedbywallsmadeofcutrectangularblockswhosepreciseextentcannotbedetermined.25Stroudinferredfromthethickscatter
ofpotteryandthepresenceofacisternthatintensiveactivityhadtaken
placewithintheenclosureduringantiquity.26Thecisternandtheashlar
tower may have supported a garrison in the upper enclosure and demonstrateasignificantinterestandinvestmentinthefortificationofthis
strategicheight.
Belowandtothenorthofthetowerandtheupperenclosure,awallran
approximatelyeast–westalongthetopofasteepslopeforca.600m.27In
24.Stroud1971a;seepp.139–145
fordiscussionofthedate.
25.Stroud1971a,pp.129–135,
figs.2,3.
26.Stroud1971a,p.133.Recent
clandestineexcavationshaverevealed
anotherpossiblecisterncutintothe
conglomeratenearthenortheastcorner
ofthetower.Unfortunately,themouth
andshapeofthiscisternweredestroyed
bythelooters,makingitimpossibleto
determinethedimensionswithany
precision.Thelootingalsorevealed
whatmaybetentativelyinterpretedas
threegravesintheupperenclosure;
eachappearstohavebeenca.1.80min
lengthandca.0.70minwidth.Around
onepossiblegravewasalargescatter
ofClassical–Hellenisticcoarse-and
fine-warepotterythatincludedtwo
substantialamphorafragments(11,12;
Fig.13)apparentlydisturbedinthe
courseofthedigging.
27.Stroud1971a,pp.135–137,fig.3.
334
w i l l i a m r . c a r a h e r a n d t i m o t h y e . g r e g o r y
contrasttotheotherstructuresmentionedabove,thiswallwasbuiltwith
twofacesofunworkedstonesfilledwithrubbleandmeasuredca.2.50min
thickness.Althoughtherewerefewtracesofawallalongthesouth,Stroud
reasonablyproposedthatthisnorthwallcontinuedaroundthewholeof
thesummitofStanotopi,withthetowerapproximatelyatitscenterand
apossiblegatealongthewall’ssouthside.Stroudthoughtitlikelythat
thislargerenclosurewasanexpansionoftheupperenclosure,althoughhe
admittedthatthechronologycouldhavebeenreversed.28
Westofthissubstantialcomplex,Stroudnotedtwolongwallsdesigned
toguardthetwolowestroutesacrosstheOneionridge,locatedwestof
Stanotopiandeastofthehilldesignated427inhisfigure1.29Thesewalls
liealongthecrestoftheridgebetweenthetwoheightsandrunroughly
east–west.Theeasternwallwaspreservedforca.245m,thewesternfor
ca.255m.Builtofrubble,inastylesimilartothatofthelargerenclosure,
thewallswere2.40–2.50mthick.Althoughthisareaisovergrownwith
densevegetationandhasbeendisturbedbythebulldozingofaforestroad,
onecanneverthelesstraceshortfragmentsofthewalls(Figs.4,5).
CLASSICAL–H ELLENIST IC FO RT IFICAT IO NS
AT MARI T SA
ThesecondfortressonOneion,abovetheMaritsapass,isalsodatableto
theLateClassical–EarlyHellenisticperiod.Ithasthreeparts:afortress,
orenceinte,andtwoindependentshieldwalls,allapparentlyconstructed
atthesametime(Fig.6).Thefortressenclosesthehighestpointonthe
easternpartofthemountainandconsistsofalargeenclosurewithtwo
majorspurwalls.Theshieldwalls,onetothenortheastandtheothertothe
west,servedasadditionaldefensesforthemainenclosure.TheMaritsaand
Stanotopifortificationsaresimilarinorganization,suggestingcomparable
functionsanddatesofconstruction.
TheMaritsafortresshasacommandingviewofthecentralIsthmia
corridortothenorthandtheravine-dissectedhillcountrytothesouth
aroundmodernGalatakiandancientSolygeia.TheGulfofCorinthand
theSaronicGulfareclearlyvisibletothenorth,althoughpartoftheancient
harborofKenchreaiisobscuredbytheeasternheightsofthemountain.
TheSaronicGulfmaybeseentothesouthandeast,alongwiththecoast
fromLoutroElenistothevillageofAlmyriandthesiteonthesuggestively
namedhillofVigla(meaninglookoutpostorwatch),whichhasevidence
foroccupationfromprehistorytotheByzantineperiod.30Immediatelyto
theeast,thehillofStanotopiwithitstowerisvisibleaswell.Themodern
villagesofExamiliaandXylokeriza,alongwithmuchofAcrocorinth,fall
withinthefortification’sviewtothewest.
Whileitseemslikelyfromthearrangementofshieldwallsthatthe
fortress served to secure the heights of Oneion against an enemy from
the north, it also would have controlled the southern approach to the
pass.Infact,anyonebeginninganascentofMt.Oneionfromthesouth
inthegeneralvicinityoftheMaritsapasswouldquicklyfalloutofthe
viewfromStanotopi,butneverfromtheviewofthefortifiedheightsof
28.Stroud1971a,p.137.
29.Stroud1971a,p.128.
30.Wiseman1978,p.58.
f o r t i f i c at i o n s o f m o u n t o n e i o n , c o r i n t h i a
335
Figure6.Classical–Hellenisticforti-
ficationsabovetheMaritsapass.
Contourinterval20m.W.R.Caraher
Maritsa.ItispossiblethatMaritsa’sfavorablepositionobviatedtheneed
forawatchtowersuchastheonefoundonStanotopiandelsewhereinthe
Corinthia.31
TheOneionridgedominatestheIsthmia/Examiliabasin,andifthe
fortificationwallsstoodhigherinantiquity,whichtheyalmostassuredly
did,theywouldhavebeenvisiblefromtheIsthmus.Fromthesouththe
fortressalsowouldhavebeenvisuallyimpressive.
Ma i n E n c l os u re
31.Watchtowersarenotuncommon
onelevatedlocationsintheCorinthia;
thereareexamplesatKefalari(Wiseman1978,pp.118–119,figs.166–168)
andalongtheEpidaurianborder
(Dixon2000,pp.51–93).
32.Pritchett(1974,pp.133–146)
hasproposedthatsomelowstonewalls
mayhaveservedasanchorsforwooden
palisades.Thepreponderanceoftiles,
however,suggeststhattheselowwalls
weresoclesforupperwallsmadeof
mudbrick.
Thewallsofthemainenclosurearelargelypreserved.Theysurrounda
rocky,mostlytreelesspeakcoveringanareaofover5,000m2.Thepeak
risesgentlytotheeasttowardStroud’shill427;todayaHellenicArmy
GeographicalServicegeodeticmarkerwithanelevationof423.99mstands
justinsidetheenclosurewallatitseasternmostpoint(Fig.6).Theenclosure
hasamaximumlengtheast–westof110mandamaximumwidth,roughly
north–south,of72m.
Thecourseoftheenclosurewallisvisibleforalmosttheentirecircuit.
Thewallsareconstructedofroughlycutstoneslaidintwofaceswitha
rubblefill(Fig.7),thesameconstructionthatStroudnotedatStanotopi.
Thereisnoevidencefortheuseofmortarorrectangularblocks.Inanumberofplacesbothfacesofthewallarevisible;itmeasures1.80–2.00min
thickness.Atitsgreatestheightthewallispreservedtojustover1m,andit
ispossiblethatthestonewallsdidnotstandmuchhigher.Alongthecourse
ofthewallarenumerouslargefragmentsofLakonianandCorinthiantiles
(discussedbelow),andthesemayindicatethattheupperpartofthewall
wasconstructedofmudbrickwithacoveringoftilestoprotectit.32
Themainenclosureisanirregularpolygon,withitswallstakingadvantageofthelocaltopographyasmuchaspossible.Thenorthandeast
336
w i l l i a m r . c a r a h e r a n d t i m o t h y e . g r e g o r y
Figure7.Typicalsectionofthemain
enclosurewalloftheMaritsafortifications.PhotoT.E.Gregory
sidesaretheleastaccessible,astheylieatthetopofsteepcliffs.Thewest
wallisbuiltalongaslightridgeofbedrock.Theeasiestwaytotravelfrom
thepasstothemainenclosureistoascendthegradualwesternslope,but
noevidenceforagateexistsalongthewestwall.Theonlyotherapproach
wouldbefromthesouth,albeitovermuchsteeperterrain.Inthemiddleof
itscourse,thesouthwallprotrudesslightlytothesouthtotakeadvantageof
alocalincreaseinslope.33Ingeneral,however,thegentlerslopeofthesouth
faceofthemountainsuggeststhataccesstothemainenclosurewasgained
fromthatdirection,whichagreeswithourunderstandingthatdefensive
forceswouldhavesoughtprimarilytoholdtheIsthmusagainstinvaders
fromthenorth.Itseemsreasonabletoimaginethatthefortificationsat
bothMaritsaandStanotopi,standingguardoverthenorthernapproach
tothePeloponneseandthesouthernreachesofCorinthianterritory,were
designedtoberesuppliedfromthesouth.
We st er n Shi el dWa l l
Thewesternshieldwallrunsnorth–southalongaridgeca.200mwest
ofthemainenclosure.Itextends220mfromabedrockoutcroppingat
itsnorthernterminustoanabruptdropatthesouth.Itissimilarinconstructiontothewallsofthemainenclosure,witharubblefillandarough
facing without mortar.The western shield wall was thicker, however,
reachingnearly3minsomeplaces.Aswiththewallsofthemainenclosure
andthoseatStanotopi,LakonianandCorinthiantileswereoccasionally
33.Justtotheeastofthissouthward
diversionistheonly,verymeager,evi-
denceforagate.Atthispointthewall
seemstostopabruptly,andseveral
uncutstonespossiblylaidincourses
mayrepresenttheeasternsideofagate.
Thereisnoevidenceforawesternside
ofagate,however,andtheroutetothis
partofthesouthernwallwouldbe
quitesteep.Thepresenceofamajor
spurwallprojectingfromthesouthwest
corneroftheenclosure’scircuitsuggests
thattheprotectionofthissouthern
flankwasapriority,andthismightalso
implythepresenceofagateinthe
southwall.Stroud(1971a,pp.134,
137)notedthatthefortificationsat
Stanotopiaremosteasilyapproached
fromthesouthsideaswell,andthe
onlyevidenceforapossiblegatewason
thesouthernflankofthenorthwall.
f o r t i f i c at i o n s o f m o u n t o n e i o n , c o r i n t h i a
337
foundalongitscourse.Inplacesthewesternshieldwallstandstoaheight
of1.20m.
To the west of the wall, the ground falls away steeply toward the
north–southravinethatformstheMaritsapassthroughthemountain.The
areaimmediatelytotheeastofthewallismoreorlesslevel,andscattered
concentrationsofbrokenpotteryarevisiblethere.Farthertotheeast,the
rockyground,nowheavilywooded,risestothewestwallofthemainenclosure.Thewesternshieldwalldoesnotconnectdirectlywiththemain
enclosure.Thesteepnorthernandsouthernfacesofthemountainwould
havemadeitdifficult,ifnotimpossible,foranarmytoascendtothearea
betweenthewesternshieldwallandthemainenclosure.
Itisimportanttonotethatthisshieldwalldoesnotblockthepass
itself.ItissituatedtooverlooktheMaritsapass,andcanbeseentoday
fromthesouthernendofthepassbelow.Moreover,itstandsataplace
thatisalreadydifficulttoaccessfromthepass;althoughthe1:5,000maps
indicateamodernpathrunningfromthepasstothewall,thiswouldbe
usefulonlyforshepherdsorresincollectors.Thewesternshieldwallwas
therefore probably intended to discourage a direct assault on the main
enclosurefromthepassandtoprotectastretchoflevelhighgroundfrom
whichthepassitselfcouldbecontrolled.Itwouldhaveprovidedabarrier
behindwhichguardscouldhide.Dependingontheprecisecourseofthe
ancientroutethroughthepass,thewallwasbetween200and300mdistant,
placingitatthemarginoftheeffectiverangeofancientprojectiles.34The
potteryonthelevelgroundimmediatelytotheeastofthewallmayreflect
theuseofthislevelareafortroopquarters.
Nort h er n Sh i el dWa l l
34.Mcleod(1965)notesthatthe
rangeofarchersrarelyexceeded200m,
andEchols(1949–1950)suggestsa
similarrangefortheancientsling;
seealsoBaitinger2001,pp.31–32.
Thenorthernshieldwallrunsforadistanceof300malongthetopofthe
northernslopeofthemountain.Itisofthesameconstructionasthewestern
shieldwall,butitisonaverageonly2.50mthick.Theeasternpartofthe
wallrunsfor80malmostnorth–southalongarockyspurprojectingfrom
thefaceofMt.Oneion.Itthenturnssharplytothesouthwestfor80m
beforeturningwest,followingthecontours,fornearly130m.Itswestern
endseemstobeintherockyandwoodednorthernfaceofOneion,40m
tothenorthofthenortheasternwallofthemainenclosure.
Themostdistinctivefeatureofthiswallisanabrupt,right-angleturn
some100mfromitseasternend.Tothesouthofthissharpturn,there
is a natural depression in the exposed bedrock that may have provided
alevelplaceforatower.Thereare,however,noexceptionalconcentrationsofpotteryoradditionaltumblethatmightindicatemoreintensive
activity here than elsewhere along the wall. Nevertheless, there is no
topographical reason for the well-defined right-angle turn in the wall,
anditispossiblethatthenaturaldepressioninthebedrockwasusedasa
foundationforatowerofsomesort,perhapsconstructedofmudbrickor
evenwood.
Potterywasvisibleonthesurfacebetweenthenorthernshieldwalland
theeastwallofthemainenclosure.Althoughtilesofvariouskindswere
338
w i l l i a m r . c a r a h e r a n d t i m o t h y e . g r e g o r y
predominant,therewerealsopithosandamphorafragments,suggesting
thatthedefendersusedthisareaforstorageorhabitation.
Asinthecaseofthewesternshieldwall,theexacttacticalpurposeof
thiswallisdifficulttodiscern.Lessthan200mtothenorthofthewallare
steepcliffs,makingadirectascentfromtheplainbelowperilous.Perhaps
thewallservedtoguardthemainenclosurefromanarmyascendingthe
northfaceofMt.Oneionfromtheeast—adifficult,ifnotimpossible,route.
ItmayalsohaveprotectedtherelativelyflatareaontopoftheOneion
ridgewheretroopspresumablycamped.
FORT IFICAT IONS BE T W EEN STANO TO P I AND
MARI T SA
EastoftheMaritsapeakandthemainenclosure,thegrounddropsdown
toahigh,relativelyflatsaddleandthenrisestoanotherverysmallpeak
at an elevation of 393.80 m, according to the topographic maps of the
HellenicArmyGeographicalService.Aseriesofwallsguardtheascent
tothispeak.Thesearenotwellpreserved;manyoftheirstoneshavebeen
incorporatedintoalargemandra(goatfold)immediatelysoutheastofthe
highestpoint(Fig.8).Intheircurrentconditiontheyappearprimarilyto
haveblockedascentfromtheeastandsouth.Itisdifficulttoevaluatethe
possibilityofaneasternascent,sincealargemodernquarryhasdestroyed
muchofthetopographyofthispartofthemountain.Tojudgefromthe
1:5,000maps,producedalmost40yearsagowhenthequarrywasmuch
smaller,however,itseemsprobablethattheeasiestrouteofascenttothis
partofthemountainwasfromthesouth;theeasternslopesofthemountain
arequitesteepandinterruptedbysheercliffs.
ThehighestpeakbetweenStanotopiandMaritsamayhavereceived
moresubstantialfortifications.Ashortcourseofroughlytrimmedstones
isarrangedinaneast–westlinealongthesteepnorthernslopeimmedi-
Figure8.Wallsontheeasternface
ofMt.Oneion.Contourinterval4m.
W.R.Caraher
f o r t i f i c at i o n s o f m o u n t o n e i o n , c o r i n t h i a
339
Figure9.Trimmedstonesonthe
northernfaceofMt.Oneion.
PhotoT.E.Gregory
Figure10.Nichescutinthesouthernfaceofthemountaineastofthe
Maritsapass.PhotoT.E.Gregory
atelybelowthehighpointoftheridge(Fig.9).Thiswallisflankedtothe
northbyanothereast–westlineofstone,producingwhatcouldwellbe
anentrancetoanupperenclosuresimilartowhatStroudarguedforthe
Stanotopifortifications.Thestonesinthesewallswerequarriedfromthe
mountainitself,andseveralquarrycutsareevidentintheexposedbedrock
oftheridge.
Althoughthesetwoshort,isolatedwallsdonotprovideevidencefor
afull-fledgedashlarfortificationontheOneionridge,theymightsuggest an attempt to fortify the mountain in a more permanent way. On
thesouthernsideofthispeak(seethe“QuarriedArea”inFig.8),several
nicheshavebeencutintherock(Fig.10).Thesearesemicircularinshape
340
w i l l i a m r . c a r a h e r a n d t i m o t h y e . g r e g o r y
andareraisedabovethemoderngroundlevel.Theymayhavebeencut
fortheplacementofvotivesinafashionnotuncommoninantiquity(see,
e.g.,theSanctuaryofAphroditeonthe‘Ιερὰ ‘ΟδόςatDaphni).Thearea
hasbeenextensivelyusedbyshepherdsoverthecenturies,andnoother
tracesofantiquitysurvive,butitisnotimpossiblethatasmallsanctuary
existedatthisspot.
Justtotheeastofthispeakisanother,somewhatlower,outcropping
(shownas355.00montheGreekarmymap)justabovethewesternedge
ofthemodernquarry.Nofortificationwallswerediscoveredonthispeak,
butthereisathickscatteroftileandpithosfragments.Therearenoother
remainsofarchitectureinthisareanoranyevidenceforfoundationcuttings.
Nevertheless,theremayhavebeenastructurehereroughlycontemporary
withthefortificationsatStanotopiandMaritsa,althoughitisnowimpossibletobecertain.
FIND S FROMT H E ANCIENT FO RT IFICAT IO NS
AT MARI T SA
In2001EKAScarriedoutanintensiveinvestigationoftheareaaround
the Maritsa Classical–Hellenistic fortifications.This involved the de-
taileddescriptionofthearchitecturalremainsandartifacts(mostlypottery)
onthesurfaceoftheground.Thereweretwoimpedimentstoourtask.
First,theveryirregularvisibilityofartifactsduetothedensevegetationon
theOneionridgelimitedourabilitytosamplethesurfacesystematically.
Second, the relatively remote and rugged location of the fortifications
imposedlimitationsonthesizeofoursurveyteamandthetimethatwe
could spend there.These difficulties, combined with our commitment
tolow-impactarchaeologyandthedecisiontoremoveonlyafewartifactsfromthearea,affectedthenatureofourinvestigation.Description,
photography,andillustrationofartifactswerecarriedoutinthefield,and
the vast majority of the objects were left where they were found. Only
smallrepresentativesampleswerebroughtbacktoourstudyareaforfurtheranalysis.Thisapproachwasdeemedappropriatefrombothethical
andscientificperspectives,asthefindsweregenerallysimilarthroughout
thearea.35
Oursurveytechniquewassimilartothatusedinthecourseofthe
EKAShigh-intensity,griddedcollectionsofLocalizedCulturalAnomalies
(LOCAs).36Weestablishedaflexiblegridovertheentiresiteandsampled
sectionsofthegridwherevisibilitypermitted.Thegoalofthismethod
wastodeterminewhethertherewassubstantialfunctionalorchronological
variationpresentonthetopofthehill.Thepoorsurfacevisibilitymade
traditionaldensitycalculationsessentiallyirrelevant.
Overall,757artifactswererecordedusingthechronotypesystem.37
Theartifactswerechronologicallyhomogeneous.Alldatablepremodern
material could be assigned to the Late Classical and Early Hellenistic
periods.Table1providesasummaryofthemostcommonfindsinorder
offrequency.ThesefindsarenowstoredatthefacilitiesoftheOhioState
UniversityExcavationsatIsthmiainKyrasVrysi.
35.Forthisapproach,whichis
consistentwiththemethodsadoptedby
EKASthroughoutthesurveyarea,see
Tartaronetal.,forthcoming;Gregory
2004.
36.Tartaronetal.,forthcoming.
37.Forthechronotypesystem,see
GivenandKnapp2003,pp.14–16;
Gregory2004.
f o r t i f i c at i o n s o f m o u n t o n e i o n , c o r i n t h i a
341
TABLE1.FINDSFROMTH EMARI TSA
FORT IFICAT IONS
Chronotype
Tile,Lakonian,Classical–Hellenistic
Tile,painted,Classical–Hellenistic
Amphora,CorinthianB
Tile,GreekCorinthianpantile,yellowslip
Pithos,orangeandbluecore
Mediumcoarseware,Classical–Hellenistic
Tile,Lakonian,painted,Classical–Hellenistic
Kitchenware,Classical–Hellenistic
Amphora,CorinthianA
Undiagnostic
Quantity
Percent
207
163
124
82
63
31
30
17
13
27
27.3
21.5
16.4
10.8
8.3
4.1
4.0
2.3
1.7
3.6
Theoverwhelmingmajorityofartifactsfound(482,orca.64%ofthe
totalsample)wereLakonianandCorinthiantiles,manyofthemslipped.
Alsocommonwerestorageandtransportvessels,especiallyCorinthianB
amphoras,andfragmentsofpithoi.Classical–Hellenisticcookingpotswere
frequentfindsonthesurfaceofthesite.Fewexampleswerecollectedof
finewareorthesemifine(plainware)potterycommonlyassociatedwith
domesticassemblagesintheCorinthia.
Thefollowingcatalogueprovidesexamplesofcommonfindsfromthe
Maritsamainenclosure.Allmeasurementsaregiveninmeters.
Cata l o g u e
1 StampedAtticblack-glazedbowl
Fig.11
9008-146-1.
P.L.0.025;p.W.0.017;Th.0.003.
Fineredclay(2.5YR5/8)withfewvoids.Fragmentpreservessmallpartof
thebaseandtheattachmentforthemissingringfoot.Shinyblackglazeinterior
andexterior,stamped(rouletted)marksonthebottominterior.
2 Semiglazedbowl
Fig.11
9008-157-101.
P.H.0.030;est.Diam.(foot)0.05.
Fine pink clay (7.5 YR 7/4) with some small voids. Bowl with low ring
foot.
Cf.CorinthVII.3,pp.28–29;probably4thcenturyastheringfootishigher
inthe3rdcentury.
3 Blisterwarejug
Fig.11
9008-157-102.
P.H.0.034;Diam.(neck)0.029.
Relativelyfinepinkclay(5YR7/4)withafewsmallbrowninclusionsandsmall
voids,firedgrayonthesurfaces.Smalljugwithverticalneckandflaringrim.
4 Mediumcoarsejugorpitcher
9008-130-101.
P.H.0.064;est.Diam.(rim)0.10.
Fig.11
342
w i l l i a m r . c a r a h e r a n d t i m o t h y e . g r e g o r y
2
1
3
5
4
Reddish yellow clay (5YR 7/6) with small–medium brown and black and
somesparklinginclusions.Largejugorpitcherwithtaperingneckandflaring,
thickenedrim;lipwithabroadgrooveontheuppersurface.
5 Mediumcoarsejugorpitcher
Fig.11
9008-166-101.
P.H.0.060;est.Diam.(rim)0.12.
Descriptionidenticalto4,exceptthatrimispointed,withashallowgroove
ontheexterior.
6 Coarsemortarium
Fig.12
9008-183-101.
P.H.0.061;est.Diam.(rim)0.29.
Coarse reddish yellow clay (5YR 7/6) with many large white, black, and
brown inclusions and small voids. Mortarium with plain vertical rim; a broad
horizontal ridge, tapering toward the exterior and sharply cut back, probably
servedasahandle.
7 CorinthianBamphoratoe
Fig.12
9008-145-105.
P.H.0.058;max.Diam.(toe)0.051.
Relativelyfinereddishyellowclay(5YR6/6)withsmallblackandredinclusions
andvoids.Bulbousamphoratoewithdistinctroundimpressiononbottom.
8 Pithoswithmoldeddecoration
Fig.12
9008-162-5.
P.W.0.112;p.H.0.096;max.Th.0.022.
Coarseredclay(10R5/8)withmanymedium–largeangularblue-graystone
inclusions and voids, fired gray at core. Body sherd is broken all around; two
raisedhorizontalbands,onerectangular,theotherroundedinsection;thinblack
sliponexterior.
9 SlippedLakoniantile
9008-153-1.
Fig.12
Figure11.Typicalceramicfinds
fromtheMaritsamainenclosure.
Scales1:1(1)and1:2(2–5).H.Cook
f o r t i f i c at i o n s o f m o u n t o n e i o n , c o r i n t h i a
343
6
8
9
7
10
Figure12.Typicalceramicfinds
fromtheMaritsamainenclosure.
Scales1:2(7)and1:4(6,8–10).H.Cook
P.dims.0.140x0.112;Th.0.026.
Medium coarse reddish yellow clay (5YR 6/6) with many medium–large
brown inclusions, small gold sparkling inclusions, and many small–large voids.
Lakoniantilewithchamferededgeanddeepgrooveonconcaveside;orangeslip
alsoonconcaveside.
10 SlippedLakoniantile
Fig.12
9008-150-1.
P.dims.0.198x0.148;Th.0.021.
Mediumcoarselightredclay(2.5YR6/8)withfewmediumwhite,red,and
goldsparkinginclusionsandfewmediumvoids.Tilewithslightlychamferededge;
ratherthin;darkredsliponconcaveside.
Theassemblageisconsistentwithwhatonewouldexpectfromafortifiedareaoccupiedforshortperiodsoftime.Itisunderstandablethatthe
inhabitantsmadeextensiveuseofstoragevessels,asthereisnoevidence
foralocalwatersupply.Cookingvesselsalsowouldhavebeenrequiredby
soldiersencampedonthemountainforanylengthoftime.Theassemblage
lacksanyartifactsrecognizableaspotentiallyreligiousinnature,suchas
miniatures,figurines,orlamps.Chronologically,thefindsgenerallyfitbest
inthesecondhalfofthe4thcenturyb.c.,butitispossiblethatmanyof
themwouldstillhavecirculatedinthe3rdcentury.
344
w i l l i a m r . c a r a h e r a n d t i m o t h y e . g r e g o r y
11
12
Figure13.Twoamphorarimsfrom
theOneionridge.Scale1:4.H.Cook
OT H ER FIND S FROMT H E ONEIO N RID G E
Inadditiontotheintensivecollectionconductedduringthe2001field
season, we also collected nonsystematic, judgmental samples of highly
diagnostic sherds from other areas of the Oneion ridgeline.Two wellpreservedamphorarims,oneCorinthianAandoneCorinthianB,were
recoveredfromaholethatprobablyhadbeendugbylootersonStanotopi
hill.
Cata l o g u e
11 CorinthianAamphora
Fig.13
ST1.
P.H.0.128;Diam.(rim)0.122;Diam.(handle)0.036.
Coarseredclay(2.5YR5/8)withmanysmall–largered,brown,andblack
inclusionsandvoids.TypicalCorinthianAamphorawithheavypointedfolded
rimandovalhandles.
12 CorinthianBamphora
Fig.13
ST2.
P.H.0.128;est.Diam.(rim)0.15.
Hardlightredclay(2.5YR6/8),fairlyfinewithfewsmallvoids.Smallpart
oftheshoulder,halfoftheneck,andaboutaquarteroftherim.Verticalneck
withbroadwheelridgesontheinterior;flaring,pointedrim,horizontalonthe
top.Attachmentforaverticalovalhandlejustbelowtherim.
Ontheoutcropimmediatelytothewestofthemodernquarry,weobservedseveralwell-preservedexamplesofpaintedLakoniantilesidentical
tothosefoundinthevicinityoftheMaritsafortress.Atthesamespot,a
largefragmentofaparticularlyelaborateClassical–Hellenisticpithosbody
sherdwasalsofound.AtnoplacealongtheentirelengthoftheOneion
ridge was there any concentration of pottery from a period other than
theClassical–Hellenisticera.InanareasuchastheCorinthia,whichis
generallycharacterizedbyacarpetofchronologicallyvariableartifacts,the
uniformityofthesefindsistrulyremarkableandmostlikelytestifiestothe
exceptionalcircumstancesunderwhichthisnearlyinaccessiblemountaintop
wasfortifiedandused.
f o r t i f i c at i o n s o f m o u n t o n e i o n , c o r i n t h i a
Figure14.Densityoffindsinthe
vicinityoftheMaritsafortifications.
Contourinterval4m.W.R.Caraher
345
Figure 14 shows the findspots and the gridded density of artifacts
fromtheMaritsafortifications.Althoughthedensegroundcoveraround
manypartsofthefortificationscertainlyaffectedourabilitytorecognize
artifacts,itseemsthatthearchaeologicalmaterialwasconcentratedprimarily in two areas: one along the western wall of the main enclosure,
theotheratitseasternedgeanddowntheslope,especiallytothenorth
andnortheast.Countswerecertainlyfarlowerinthecentralareaofthe
enclosure.Thisdisparitymaybetheresultoftheuseoftilestocapapossiblemudbricksuperstructureonthestonefoundationsofthefortification
walls.Inaddition,itispossiblethattheinhabitantsofthefortifications
spentmoreoftheirtimealongthewallsthantheydidinthecentralpart
ofthedefensivearea.
H ISTO RY,TO PO G RAP HY, AND F UNC T IO N O F
T H E ANC IENT FO RT IFICAT IO NS
38.Wiseman1963;Stroud1971a,
pp.139–145.
Wiseman and Stroud have ably discussed the literary evidence for the
fortificationoftheIsthmusduringantiquity.Theyfocusprimarilyonthe
LateClassicalandHellenisticperiods,whentheIsthmusbecameahigh-
wayfortheforcesofoutsidepowerssuchasAttica,Thebes,andMacedon seeking to intervene among the rival and recalcitrant cities of the
Peloponnese.38Politicalconditionsdictatedthatalmosteveryoccasionfor
thedefenseofMt.Oneionwasconnectedwiththemovementofanorth-
ernarmysouthintothePeloponnese.Thestrategyoffortifyingthemoun-
tain and allowing a large stretch of fertile Corinthian land to remain
346
w i l l i a m r . c a r a h e r a n d t i m o t h y e . g r e g o r y
undefendedreflectstheinterestsofforeign(non-Corinthian)powersin
defendingtheIsthmus.39
Thefunctionofthefortificationsdocumentedinthisarticleishighly
relevanttodebatesonwhetherweshouldunderstandGreekfortifications
asalocal,inthiscaseCorinthian,defensiveresponseorastheworkofnon-
localpowerssuchasAthens,Thebes,Sparta,orMacedon.40AsWiseman
andStroudhaveargued,itisnotnecessarytoassumethatthemountain
wasfortifiedbytheCorinthianssimplybecauseitislocatedinCorinthian
territory.ThepresenceofasecondroughfortificationabovetheMaritsa
passdoesnotsubstantiallychallengeStroud’sconclusionsregardingthe
defenseoftheIsthmusalongtheOneionline.Itdoes,however,allowus
toofferseveralmodestcontributionstopreviousdiscussionsofthehistory
andtopographyofthisregion.
TounderstandthefortificationsonMt.Oneion,itisnecessarytoreview
brieflytheancientunderstandingofthetopographyandcommunication
networkinthearea.Whilenumerousscholarshavestudiedtheroadsin
the southwestern Corinthia and the passes to the Argolid, the eastern
Corinthia, particularly the area immediately south of the Isthmus, has
notreceivedasmuchsystematicattention.41Nevertheless,Stroud,Wiseman,andDixonprovidegeneraltreatmentsofthehistoricaltopography
ofthelargerregion,establishingtheimportanceofMt.Oneionwithin
thiscontext.
TherearenoexplicitreferencestomilitaryactivityonMt.Oneionin
thecenturybefore366b.c.Theunsettledconditionsofthesecondhalfof
the4thcentury,coincidingwiththeestablishmentofMacedonianpower,
alongwiththeevidencefromthefindsassociatedwiththewalls,makeit
certainthatthesepasseswereusedanddefendedduringthistime.Stroud
thusestablishedasoundhistoricalterminuspostquemofca.350b.c.forthe
fortificationbasedonarchaeologicalandhistoricaldata.Thebestinsights
intotheintendedfunctionofthefortificationsandtheirrespectivepasses,
however,derivefromanearlierperiod,370–366b.c.,whenThebanarmies
underEpaminondasmovednorthandsouththroughtheIsthmus.42The
accountsoftheThebanwarsinXenophondescribetheeffortsofvarious
forcestoblocktheeasternroutesoverMt.Oneionwithoutpermanent
fortifications.TheseeffortsandtheregularitywithwhichEpaminondas
breachedtheIsthmusatthispointmighthaveledtothefortificationof
themountainsometimeafter350b.c.
ThehumblewallsatStanotopiandMaritsadonotfeatureprominently
intheliterarysourcesfromlaterperiods.Onepassage,alreadynotedby
Stroudandothers,maymakeanobliquereferencetothepresenceoffortificationsintheproximityofKenchreaiandtheOneionridge.In315b.c.,
during theWars of the Successors, Alexander, the son of Polyperchon,
soughttoholdtheCorinthiaagainstKassander.Diodoros(19.63.4)tells
usthatKassander
καὶ τὸ µὲν πρῶτον Κεγχρεὰς ἐπολιορκήσας ἐδῄωσε τὴν χώραν
τῶν Κορινθίων, µετὰ δὲ ταῦτα δύο φρούρια κατὰ κράτος ἑλὼν
τοὺς ὑπ’ Ἀλεξάνδρου καθεσταµένους φρουροὺς ὑποσπόνδους
ἀφῆκεν.
39.Stroud(1971a,pp.139–145)
providesacarefulsummaryofthevariouspartieswhogarrisonedtheIsthmus,
andtheOneionlineinparticular.
40.E.g.,Lauter-Bufe1988;
McCredie1966.
41.AnexceptionisDixon2000.
42.Stroud1971a,pp.139–142,with
sources.
f o r t i f i c at i o n s o f m o u n t o n e i o n , c o r i n t h i a
347
firsttookKenchreaiandplunderedthefieldsoftheCorinthians.
Then,aftertakingtwofortressesbystorm,hedismissedunder
trucethegarrisonsthathadbeenplacedinthembyAlexander.43
Justoneyearearlier,thesetroopshadforcedKassandertotakehis
troopsfromMegaratoEpidaurosbysea(Diod.Sic.19.54.3).Althoughthe
passagelacksanydetailconcerningthetwofortifications,Stroudthought
thatthefortificationsonStanotopi,nearKenchreai,werereasonablecandidatesastheywere“inthevicinityoftheheaviestfighting.”44Following
this logic, and considering that Diodoros puts the conquest of the two
fortificationsdirectlyafterthesiegeofKenchreai,webelieveitisplausible
tosuggestthatthetwofortressesarethoseofStanotopiandMaritsa.
Whiletheexactdateandspecificfunctionofthesedefensesremain
unclear,itseemsmostlikelythattheenclosuresonStanotopiandMaritsa
werefortifiedcampsdesignedtoprovideprotectionandabaseofoperationsforforcesassignedtoholdtheseimportantpasses.45Theirsimple
architecturalstyle,limitedevidenceforlong-termoccupation,andstrategic
placementfindparallelsinotherstrategicsettings,suchasthefortifications
attheDemaGapnearThermopylaiandthebetter-built,moresubstantial
DemaWallbetweenMt.AigaleosandMt.Parnes.46Moreover,therecurrent instances of foreign detachments being stationed in the Corinthia
during the Late Classical and Hellenistic periods help to explain the
presenceofmodestfortificationssuitableforshort-termdefensivedeployments.Itisworthnotingthat,incontrasttotheDemaWallinAttica,
thesefortificationsdidnotservetoblockthepassitself.Itseemslikelythat
theyweredesignedtoallowaforceresponsibleforblockingthepassto
occupyafortifiedpositiononhighgroundintheimmediatevicinity.FollowingStroud’sinterpretationofthewallsonStanotopi,weconcludethat
thefortificationsonMt.OneionattheMaritsapassbelongtoagrowing
corpusofhumblefortificationsthatservedtocomplementandreinforce
themoresophisticatedandsubstantialexamplesofmilitaryarchitecture
foundthroughouttheGreekworld.
VENE T IAN D EFENSES O N MO UNT O NEIO N
TheStanotopiandMaritsapasseswerealsofortifiedduringtheSecond
Venetian period. Both sets of fortifications were designed to cut the
north–southroutesbetweentheIsthmusandtheareasouthofMt.Oneion.
Theywereconstructedofidenticalmasonry,withexteriorwallsofirregular
blocks filled with rubble and mortar.The exterior blocks were roughly
hewnontheiroutersurfacetomakearelativelysmoothface.Theouter
43.Trans.R.M.Geer,Cambridge,
Mass.,1947.
44.Stroud1971a,p.143;seen.7,
above.Cf.Perlman2000,pp.148–149.
45.Fornumerousexamplesfrom
throughouttheGreekworld,see
McCredie1966;Pritchett1974,
pp.133–146;Lawrence1979,pp.160–
167.Forsomerecentdissentingopin-
ions,particularlyregardingthefortificationsatKorone,seeLauter-Bufe
1988.FortheDemaWall,seeMunn
1993.
46.Forthesometimesacrimonious
discussionofthecomplexfortifications
aroundThermopylai,manyofwhich
areverysimilarinconstructiontothe
wallsonMt.Oneion,seePritchett
1958,1994;MacKay1963;Cherf1996,
pp.56–59.
348
w i l l i a m r . c a r a h e r a n d t i m o t h y e . g r e g o r y
surfaceswerecoveredbyacoatofmortarthathasmostlydisappearedbut
waspresumablyappliedovertheentireface.Theexteriorfacesofthewalls
haveasignificantupwardtaperorbattering,acharacteristicofmilitary
constructioninthisperiod.Inthefirstquarterofthe20thcentury,Fowler
observedafinishedtopmadeoftriangular-shapedblocksatseveralpoints
alongtheStanotopiwall.Thewalltopsarenolongerpreservedateither
locationtoday.47
Eachfortificationcomplexisabarrierwallwithafightingplatform
along the interior, terminating in a rectangular tower (hypothesized for
Stanotopi,asthewesternendwasdestroyedbyquarryingduringthepast
30years).Ineachcase,thewallcrossestheroadthroughthepassrelatively
lowonthemountain,aboutathirdofthewaytothetop,atapointwhere
theroaditselfchangedcourseandthenaturallayofthelandmadeevasiondifficult(seeabove,Fig.4).Thepurposeofthetowerwastoblockan
evasiondownhill,whilepermittingenfiladingfirebackupacrosstheroad.
ThefortificationsattheMaritsapasscontinuedupthemountainabovethe
tower,tofurtherpreventanarmyfromascendingthepassorfrompositioningitselfbehindthefortifications,wherethedefenderswouldhavebeen
unprotected.ThedesignoftheStanotopifortificationswasmorecomplex
(Fig.15).Thewallranbetweenaseriesofnaturalheights,eachofwhich
wasdefendedbyabastion.Theeasternandwesternbastionswereopenin
therear,whilethecentralbastionwaspentagonal,evidentlydesignedto
coverthestretchofwallbotheastandwest.
Wehavenoideawhetherthesetwofortificationswereactuallyusedto
defendthePeloponneseatthetimeofthefinalOttomanattack.Probably
theywerenot,becausetheirusefulnessdependedontheVenetiansbeing
abletoholdthemainlinesofattackattheHexamilion,thecoastlinenear
Kenchreai,andtheXeropotamosValley.FinlayreportsthatinlateJulyof
1715,theOttomans,underthecommandofAliKumurgi,descendedinto
theCorinthiawithaforceof70,000men,whiletheVenetianshadonly
8,000soldiers.48TheVenetiansplacedtheirhopesinthelocalGreekpopulationandelectedtodefendonlyfiveofthefortressesinthePeloponnese;
theVenetianSenateorderedthedismantlementoftherest.Accordingly,
theVenetiansofferednoresistanceattheHexamilionand,afterashort
siege,AcrocorinthsurrenderedonAugust3.49ByAugust11,theOttomans
wereintheArgolidandthedefenseofOneionwasmoot.
AsiscommonatVenetianfortificationselsewhereinGreece,virtually
nopotteryorotherfindsassociatedwiththeperiodofusewerefoundin
oraroundtheVenetiandefenses.Onlytwopiecesofundiagnosticmedium
coarsepotterywerefoundjustoutsidethetoweratMaritsa,whilenopotteryatallwasseenwithinthefortificationsatStanotopi.Inpartthismay
beattributabletothedensegroundcoveratbothlocations,butitmayalso
indicatethatthedefenseswereneverusedorinhabited.50
47.CorinthI.1,p.104.
48.Finlay1877,pp.217–222.
49.Theaftermathwasthefamous
slaughterofmanyVenetiansand
Greeks,portrayedvividlybyByronin
hisepicpoem“TheSiegeofCorinth.”
50.Alternatively,certaingroups
ofpeopleintheVenetianperiodmay
nothavemadegreatuseofceramic
vessels;seeVroom1998;2003,pp.85–
86.
f o r t i f i c at i o n s o f m o u n t o n e i o n , c o r i n t h i a
349
Figure15.Venetianfortifications
atStanotopi.Contourinterval4m.
W.R.Caraher
The Fort i f i c at i on s at S ta n otop i
FowlerwasthefirsttomentiontheStanotopifortifications,andhisdescription,evenwithoutaplan,haslongbeenconsideredsufficientandaccurate.51
Hisinterpretationremainsfundamentallycorrect,andsoweproceedfromhis
observations.Thefortificationsweredesignedtoblocktworoutesthrough
Mt.OneionintheStanotopiarea,representingthewesternmostofthepassagesalsoguardedbytheClassical–Hellenisticfortifications(Fig.15).These
passesfollowedthecourseoftworavinesthatdescendtotheplaininthe
vicinityofthemodernarmycamp.TheVenetianfortificationswereoriginally
madeupofthreebastions.Thebastionsattheendsweredesignedtoblock
theroads.Thebastionapproximatelyinthecentersitsataheightabovethe
othertwo.Itisnoteworthythatthisfortificationcomplexwasbuiltinthe
ageofgunpowder,whenanenemycouldovercomeanydefensesimplyby
placingartilleryatanearbyhigherelevation.Thefortificationstodayarein
relativelygoodcondition,althoughasectionofthewallabovetheeastern
bastionhasrecentlybeenbulldozedforconstructionofaforestroad,while
thewesternbastionhasbeencompletelydestroyedbythemodernquarry.
East er n Bast ion
51.CorinthI.1,pp.104–105.Cf.
Stroud1971a,pp.137–138,n.9;Peppas1990,pp.51–57andplan36;1993,
pp.142–143.
52.CorinthI.1,pp.104–105.
Theeasternbastionisathree-sidedfortificationwithoutawallprotecting its southwestern, upslope exposure. Its eastern wall runs for some
20mparalleltothecourseoftheravine.Thiswallispiercedbythreedrains,
whichallowwateraccumulatinginsidethebastiontorunouttowardthe
ravine(Fig.16).Atitssouthernend,itturnsalmost90degreesandruns
some15mtothesouthwest.Atitsnorthernend,thiswallalsoturnsat
90degreesandextendsnearly50muphill,alsoinawest/southwestdirection.Thewallofthebastionispreservedtodaytoamaximumheightof
2.62mabovethegroundontheexterior(atthesoutheastcorner).Onthe
interior,thereisafightingplatformca.1.45mwide;accordingtoFowler,
this was once 1.25 m below the top of the wall.52The northeast and
350
w i l l i a m r . c a r a h e r a n d t i m o t h y e . g r e g o r y
Figure16.Venetianfortifications
atStanotopi:eastwalloftheeastern
bastion,fromthenortheast.
PhotoT.E.Gregory
southeastcornersoftheeasternbastionarebettermadethantherestof
thefortifications.Theywereconstructedofheadersandstretcherslaidin
alternatingcourses,acharacteristicofthemasonryinsomecontemporary
VenetiancastlessuchasthePalamidiatNauplion.
Theeasternbastionguardsapathextendingalongthewesternside
ofashallowravine.Itstandsaboveapointwheretheravinesplitsintwo
directions, either of which would have provided access to the summit
ofStanotopiandbeyondtothelandsouthofMt.Oneion.Presumably,
however,anytravelerorattackingarmyintendingtoreachthetopofthe
mountainwouldnothavewalkedatthebottomoftheravine,asatmany
pointsthefloormeetsimpassable,nearlyverticalwallsofbedrock.
LiketheMaritsafortifications,theeasternbastionatStanotopinarrowedtherouteoverthemountainratherthanblockingittotally,leaving
asmall,relativelylevelareatothesoutheastofthebastionwall.Itisalso
notablethatthebastionisnotclosedonitssouthwesternside.Thesouthernwallisnotaslongasthenorthernwall,andthebastionoverallhasthe
shapeofapartiallyopenrectangle.LiketheearlierGreekfortifications,the
Venetianfortificationswereapparentlydesignedtoberesuppliedfromthe
rear,presumablyfromthemainVenetianpowerbasesouthoftheIsthmus,
atNauplion.53
Cent ral Bast ion
Thenorthernwalloftheeasternbastioncontinueswestupthehillinan
approximatelystraightlineandthenturnstothenorthwesttothetopof
theridge,whereawell-builtpentagonalbastionoccupiedthehighpoint
betweentheravines.Inthemiddleofthesouthwestside(thecontinuation
ofthemainwall)isadoorway,ca.1.50mwide,leadingintothebastion.
Thefightingplatformisca.1.50mwideonthenorthernfaceofthemain
wall,andaccordingtoFowler,itwasca.0.50mbelowthetopofthewall.
53.Andrews(1953,pp.237–238)
discussestheVenetians’concernwith
protectingNauplion,attestedby
fortificationsalongthecoastofthe
ArgolidfromNaupliontoDrepanon,
PortoHeli,andPoros.Thehistorically
closerelationshipbetweentheportsof
theSaronicGulfmakesitlikelythat
thefortificationsonMt.Oneionwere
partofthelargerstrategytodefendthis
stretchofcoastline.
f o r t i f i c at i o n s o f m o u n t o n e i o n , c o r i n t h i a
351
Approximately15mwestofthecentralbastionisadoorwaythroughthe
wall,thesamewidthasthatinthebastion.Onthesoutheasternsideof
thedoorwayaseriesofsteps,paralleltothewall,providedaccesstothe
fightingplatformontheinterior.
We st er n Bast ion
Fromthecentralbastion,thefortificationwalldescendsforabout100m
inalinethatcurvesslightlytothenorthandreachesthepointwherethe
westernravineandaroadundoubtedlyonceran.Todaythewallterminates
abruptlyhere,cutbyamodernroadandanenormousquarry.Originally,
however,andeveninFowler’stime,thewallextendeduptheslopeonthe
westernsideoftheravineforabout40m,thenturnednorthandagain
west–northwest until it reached a cliff. It is difficult to understand the
courseofthewallinthisarea,largelybecausethetopographyhasbeen
thoroughlydisruptedbythequarry.Itispossiblethatthewesternendof
thewall,whichwouldhaveturnedsharplytotheeastbeforeendingata
largerock,servedasanotherbastionwithanopenrearexposure.Fowler
describesthearrangementtoallowwatertopassunderthewall,butthese
remainshavesincebeendestroyed.54
The Fort i f i c at i on s at Ma r i ts a
54.CorinthI.1,pp.104–105,fig.73.
TheVenetianfortificationsintheMaritsapassdisplaymanyofthesame
characteristicsasthoseatStanotopi.Theymayhavebeenbuiltatthesame
timeandperhapsbythesameworkcrews.Theyarelocatedastridewhat
musthavebeenthemainroadintothepass,alongtheeasternsideofthe
ravine,andtheyarerelativelylowonthesideofthemountain,beginningat
anelevationofca.236m(Figs.17,18).Themaindefenseisarectangular
tower,ca.8.80x11.20montheexterior(Fig.19),builtonarockoutcrop
thataddstotheelevationofthetoweratapointwheretheoriginalroad
musthavemadeaturnalongthesideoftheravine.Norectangularblocks
wereusedinthefortification,althoughthestoneswereroughlyfinished
tomakearelativelyflatsurface,especiallyontheexterior.Thestonesused
seemtohavebeenca.0.30minlengthand0.20minheight,butmany
largerstoneswerealsoemployed.Boththeexteriorandtheinteriorofthe
wallswereoriginallycoveredwithstucco.Theinteriorfaceofthewallsis
vertical,buttheouterfaceisbattered.
The walls of the tower vary between ca. 0.90 and 1.15 m thick at
theirpreservedheight,althoughtheycertainlywouldhavebeenthinner
higherup.Theyarepreservedasmuchas3mabovethelowestlevelofthe
bedrockinsidethetower,althoughthereareplaceswherethebedrockis
actuallyhigherthanthepreservedtopsofthewalls.Insidethetowerisa
fightingplatform,ca.1.00–1.25mwide,withitsoriginalsurfacepreserved
inseveralplaces.Inkeepingwiththedeclininglevelofthebedrockoutside
the tower, the fighting platform of the north and south walls descends
noticeablyfromeasttowest,creatingaramplikeeffect.Interestingly,there
seemsnottohavebeenanydoorwayintothetower;instead,accessmust
havebeenfromthelevelofthefightingplatformofthecurtainwallbehind
thetower.
352
w i l l i a m r . c a r a h e r a n d t i m o t h y e . g r e g o r y
Figure17.Venetianfortifications
attheMaritsapass,fromthesouth.
PhotoT.E.Gregory
Figure18.Venetianfortificationsat
theMaritsapass,fromthesoutheast;
therectangulartowerisvisibleatthe
center.PhotoT.E.Gregory
Tothesoutheast,themountainousterraindirectlybehindthetower
risesprecipitously.Theoriginalroadwaypresumablywaslocatedjustbehindthetowerandwasblockedbythewallrunninguphillfromthetower.
Thiswallwentfirstinasoutheasterlydirectionforca.10.50m,andthen
moredirectlyeastforabout50mbeforereachingahugeoutcropofrock.
Thiscurtainwallwas,likethewallsofthetower,ca.1.10mwide;itwas
attachedtoafightingplatformca.1.30mwide.Theoriginalsurfaceof
theplatformisrelativelywellpreservedatmanypointsandissometimes
evenhigherthanthecurtainwallitself.Thesurfaceofthegroundinside
thefortificationsisveryirregular,butatonepointthefightingplatformis
ca.1.40mabovethesurface.
Overthetotallengthofthewall,ca.60.50m,theelevationrisesby
ca.21m,creatinganaverageslopeofabout35%.Inordertoallowthe
soldierstogoupanddownthisslopewithrelativeease,aseriesofsteps
Figure19.PlanoftheVenetianfortificationsattheMaritsapass.K.D.Soteriou
354
w i l l i a m r . c a r a h e r a n d t i m o t h y e . g r e g o r y
wereconstructedatpointsofrapidrise,andthesesurviveinthefighting
platformtoday.Thefortificationwallsarenotpreservedtotheiroriginal
height,buttheystandabout2.30mabovethesurfaceontheexteriorat
thehighestpreservedpoint,justbeyondthejoginthewalltotheeast.At
apointmidwayalongtheeastwardstretchofwall,anotherstructureseems
tohavebeenbuiltflushagainstthefightingplatformontheinteriorof
thewall.Thisisnotwellenoughpreservedtoallowustobecertainofits
function,butitmayhavebeenastairwayuptothelevelofthefighting
platformfromthegroundbelow.
Theserelativelymodestfortificationsareafarcryfromtheimposing
castlesbuiltelsewhereinGreecebytheVenetiansatthistimeandknown
fromtheplansexecutedforFrancescoGrimani,thegovernor.55Nonetheless,theymusthavebeendesignedbymilitaryengineerswhounderstood
thelocaltopographyandwhoemployedsophisticatedflourishessuchas
arrangementsforroutingtheflowofwaterthroughthebastionwalls.
CONCLUSION
ThegeographyoftheIsthmusandthegeopoliticsofGreecehavelong
demanded the fortification of this vital north–south corridor into the
Peloponnese.The Hexamilion and its predecessors are well-known examples of such defenses.The presence of a complex, secondary system
offortifications,however,suggeststhatduringsomeperiodsformidable
freestanding barrier walls guarding the Corinthia and the Peloponnese
didnotservethestrategicortacticalpurposesofthosewishingtofortify
theIsthmus.TheLateClassicalandHellenisticperiodsandtheSecond
Venetokratiaweretimeswhenlimitedresourcesandthepaceofevents
encouragedthereinforcementofexistingnaturaldefensestopreventthe
movementofarmiestothesouth.ThesimplefortificationsofMt.Oneion
reflectakeenawarenessoflocaltopographyandsoundtacticalreasoning.
Bothsetsofdefensesweredesignedtopreventtheenemyfromoccupying
localhighground,andbothwerepositionedtotakeadvantageofreinforcementfromthesouth.
Althoughbothfortificationsrequiredlocalknowledgefortheirshrewd
placementandconstruction,theyalsodemonstrateagenuinelyregional
conceptionofdefense.ThesouthernborderoftheIsthmusrepresented
thelastpointatwhichaforcecouldmountaconcerteddefenseofthe
Peloponnese.Farthersouth,thenumerousroutesopentoaninvadingarmy
madethedefenseofanysinglepoint,eventhenarrowDervenakipassrunningsouthtotheArgolid,insufficienttoblockthenorthernorsouthern
passage of a determined foe.The various fortifications of the Isthmus,
rangingfromthefortressatAcrocorinthtothehumblewallsoftheMaritsa
andStanotopipasses,endeavoredtosealofftheentiretyofsouthernGreece
fromanynorthernaggressormovingoverland.Theywouldhaveservedthe
needsofaregionaldefensefarmoreeffectivelythantheinterestsofthe
localCorinthians,whoseterritorywaseffectivelysplitbetweentheexposed
areanorthoftheIsthmusandtheprotectedsouthernvalleys.
55.Andrews1953.
f o r t i f i c at i o n s o f m o u n t o n e i o n , c o r i n t h i a
355
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