Fromthemountainswehadaverystrikingviewofthiswhiteandbrilliantaerial-field,whichsentarmsupthevalleys,leavingislandsandpromontoriesinthesamemanner,astheseadoesintheChonosarchipelagoandinTierradelFuego。
WestayedtwodaysatFreyrina。InthevalleyofGuascotherearefoursmalltowns。Atthemouththereistheport,aspotentirelydesert,andwithoutanywaterintheimmediateneighbourhood。FiveleagueshigherupstandsFreyrina,alongstragglingvillage,withdecentwhitewashedhouses。
Again,tenleaguesfurtherupBallenarissituated,andabovethisGuascoAlto,ahorticulturalvillage,famousforitsdriedfruit。Onacleardaytheviewupthevalleyisveryfine;thestraightopeningterminatesinthefar-distantsnowyCordillera;oneachsideaninfinityofcrossing-linesareblendedtogetherinabeautifulhaze。Theforegroundissingularfromthenumberofparallelandstep-formedterraces;andtheincludedstripofgreenvalley,withitswillow-bushes,iscontrastedonbothhandswiththenakedhills。Thatthesurroundingcountrywasmostbarrenwillbereadilybelieved,whenitisknownthatashowerofrainhadnotfallenduringthelastthirteenmonths。TheinhabitantsheardwiththegreatestenvyoftherainatCoquimbo;fromtheappearanceoftheskytheyhadhopesofequallygoodfortune,which,afortnightafterwards,wererealized。
IwasatCopiapoatthetime;andtherethepeople,withequalenvy,talkedoftheabundantrainatGuasco。Aftertwoorthreeverydryyears,perhapswithnotmorethanoneshowerduringthewholetime,arainyyeargenerallyfollows;andthisdoesmoreharmthaneventhedrought。Theriversswell,andcoverwithgravelandsandthenarrowstripsofground,whichalonearefitforcultivation。Thefloodsalsoinjuretheirrigatingditches。
Greatdevastationhadthusbeencausedthreeyearsago。
June8th——WerodeontoBallenar,whichtakesitsnamefromBallenaghinIreland,thebirthplaceofthefamilyofO’Higgins,who,undertheSpanishgovernment,werepresidentsandgeneralsinChile。Astherockymountainsoneachhandwereconcealedbyclouds,theterrace-likeplainsgavetothevalleyanappearancelikethatofSantaCruzinPatagonia。AfterspendingonedayatBallenarIsetout,onthe10th,fortheupperpartofthevalleyofCopiapo。Werodealldayoveranuninterestingcountry。Iamtiredofrepeatingtheepithetsbarrenandsterile。Thesewords,however,ascommonlyused,arecomparative;IhavealwaysappliedthemtotheplainsofPatagonia,whichcanboastofspinybushesandsometuftsofgrass;andthisisabsolutefertility,ascomparedwithnorthernChile。Hereagain,therearenotmanyspacesoftwohundredyardssquare,wheresomelittlebush,cactusorlichen,maynotbediscoveredbycarefulexamination;andinthesoilseedsliedormantreadytospringupduringthefirstrainywinter。InPerurealdesertsoccuroverwidetractsofcountry。Intheeveningwearrivedatavalley,inwhichthebedofthestreamletwasdamp:followingitup,wecametotolerablygoodwater。Duringthenight,thestream,fromnotbeingevaporatedandabsorbedsoquickly,flowsaleaguelowerdownthanduringtheday。Stickswereplentifulforfirewood,sothatitwasagoodplacetobivouacforus;butforthepooranimalstherewasnotamouthfultoeat。
June11th——Werodewithoutstoppingfortwelvehourstillwereachedanoldsmelting-furnace,wheretherewaswaterandfirewood;butourhorsesagainhadnothingtoeat,beingshutupinanoldcourtyard。Thelineofroadwashilly,andthedistantviewsinteresting,fromthevariedcoloursofthebaremountains。Itwasalmostapitytoseethesunshiningconstantlyoversouselessacountry;suchsplendidweatheroughttohavebrightenedfieldsandprettygardens。ThenextdaywereachedthevalleyofCopiapo。
Iwasheartilygladofit;forthewholejourneywasacontinuedsourceofanxiety;itwasmostdisagreeabletohear,whilsteatingourownsuppers,ourhorsesgnawingthepoststowhichtheyweretied,andtohavenomeansofrelievingtheirhunger。Toallappearance,however,theanimalswerequitefresh;andnoonecouldhavetoldthattheyhadeatennothingforthelastfifty-fivehours。
IhadaletterofintroductiontoMr。Bingley,whoreceivedmeverykindlyattheHaciendaofPotreroSeco。Thisestateisbetweentwentyandthirtymileslong,butverynarrow,beinggenerallyonlytwofieldswide,oneoneachsidetheriver。Insomepartstheestateisofnowidth,thatistosay,thelandcannotbeirrigated,andthereforeisvalueless,likethesurroundingrockydesert。Thesmallquantityofcultivatedlandinthewholelineofvalley,doesnotsomuchdependoninequalitiesoflevel,andconsequentunfitnessforirrigation,asonthesmallsupplyofwater。
Theriverthisyearwasremarkablyfull:here,highupthevalley,itreachedtothehorse’sbelly,andwasaboutfifteenyardswide,andrapid;lowerdownitbecomessmallerandsmaller,andisgenerallyquitelost,ashappenedduringoneperiodofthirtyyears,sothatnotadropenteredthesea。
TheinhabitantswatchastormovertheCordillerawithgreatinterest;
asonegoodfallofsnowprovidesthemwithwaterfortheensuingyear。
Thisisofinfinitelymoreconsequencethanraininthelowercountry。
Rain,asoftenasitfalls,whichisaboutonceineverytwoorthreeyears,isagreatadvantage,becausethecattleandmulescanforsometimeafterwardsfindalittlepastureinthemountains。ButwithoutsnowontheAndes,desolationextendsthroughoutthevalley。Itisonrecordthatthreetimesnearlyalltheinhabitantshavebeenobligedtoemigratetothesouth。
Thisyeartherewasplentyofwater,andeverymanirrigatedhisgroundasmuchashechose;butithasfrequentlybeennecessarytopostsoldiersatthesluices,toseethateachestatetookonlyitsproperallowanceduringsomanyhoursintheweek。Thevalleyissaidtocontain12,000
souls,butitsproduceissufficientonlyforthreemonthsintheyear;
therestofthesupplybeingdrawnfromValparaisoandthesouth。Beforethediscoveryofthefamoussilver-minesofChanuncillo,Copiapowasinarapidstateofdecay;butnowitisinaverythrivingcondition;andthetown,whichwascompletelyoverthrownbyanearthquake,hasbeenrebuilt。
ThevalleyofCopiapo,formingamereribbonofgreeninadesert,runsinaverysoutherlydirection;sothatitisofconsiderablelengthtoitssourceintheCordillera。ThevalleysofGuascoandCopiapomaybothbeconsideredaslongnarrowislands,separatedfromtherestofChilebydesertsofrockinsteadofbysaltwater。Northwardofthese,thereisoneotherverymiserablevalley,calledPaposo,whichcontainsabouttwohundredsouls;andthenthereextendstherealdesertofAtacama——
abarrierfarworsethanthemostturbulentocean。AfterstayingafewdaysatPotreroSeco,IproceededupthevalleytothehouseofDonBenitoCruz,towhomIhadaletterofintroduction。Ifoundhimmosthospitable;
indeeditisimpossibletobeartoostrongtestimonytothekindnesswithwhichtravellersarereceivedinalmosteverypartofSouthAmerica。ThenextdayIhiredsomemulestotakemebytheravineofJolqueraintothecentralCordillera。Onthesecondnighttheweatherseemedtoforetellastormofsnoworrain,andwhilstlyinginourbedswefeltatriflingshockofanearthquake。
Theconnectionbetweenearthquakesandtheweatherhasbeenoftendisputed:
itappearstometobeapointofgreatinterest,whichislittleunderstood。
HumboldthasremarkedinonepartofthePersonalNarrative,[1]thatitwouldbedifficultforanypersonwhohadlongresidedinNewAndalusia,orinLowerPeru,todenythatthereexistssomeconnectionbetweenthesephenomena:inanotherpart,howeverheseemstothinktheconnectionfanciful。
AtGuayaquilitissaidthataheavyshowerinthedryseasonisinvariablyfollowedbyanearthquake。InNorthernChile,fromtheextremeinfrequencyofrain,orevenofweatherforebodingrain,theprobabilityofaccidentalcoincidencesbecomesverysmall;yettheinhabitantsareheremostfirmlyconvincedofsomeconnectionbetweenthestateoftheatmosphereandofthetremblingoftheground:IwasmuchstruckbythiswhenmentioningtosomepeopleatCopiapothattherehadbeenasharpshockatCoquimbo:
theyimmediatelycriedout,“Howfortunate!therewillbeplentyofpasturetherethisyear。”Totheirmindsanearthquakeforetoldrainassurelyasrainforetoldabundantpasture。Certainlyitdidsohappenthatontheverydayoftheearthquake,thatshowerofrainfell,whichIhavedescribedasintendays’timeproducingathinsprinklingofgrass。Atothertimesrainhasfollowedearthquakesataperiodoftheyearwhenitisafargreaterprodigythantheearthquakeitself:thishappenedaftertheshockofNovember,1822,andagainin1829,atValparaiso;alsoafterthatofSeptember,1833,atTacna。Apersonmustbesomewhathabituatedtotheclimateofthesecountriestoperceivetheextremeimprobabilityofrainfallingatsuchseasons,exceptasaconsequenceofsomelawquiteunconnectedwiththeordinarycourseoftheweather。Inthecasesofgreatvolcaniceruptions,asthatofCoseguina,wheretorrentsofrainfellatatimeoftheyearmostunusualforit,and“almostunprecedentedinCentralAmerica。”
itisnotdifficulttounderstandthatthevolumesofvapourandcloudsofashesmighthavedisturbedtheatmosphericequilibrium。Humboldtextendsthisviewtothecaseofearthquakesunaccompaniedbyeruptions;butI
canhardlyconceiveitpossible,thatthesmallquantityofaeriformfluidswhichthenescapefromthefissuredground,canproducesuchremarkableeffects。ThereappearsmuchprobabilityintheviewfirstproposedbyMr。
P。Scrope,thatwhenthebarometerislow,andwhenrainmightnaturallybeexpectedtofall,thediminishedpressureoftheatmosphereoverawideextentofcountry,mightwelldeterminetheprecisedayonwhichtheearth,alreadystretchedtotheutmostbythesubterraneanforces,shouldyield,crack,andconsequentlytremble。Itis,however,doubtfulhowfarthisideawillexplainthecircumstancesoftorrentsofrainfallinginthedryseasonduringseveraldays,afteranearthquakeunaccompaniedbyaneruption;suchcasesseemtobespeaksomemoreintimateconnectionbetweentheatmosphericandsubterraneanregions。
Findinglittleofinterestinthispartoftheravine,weretracedourstepstothehouseofDonBenito,whereIstayedtwodayscollectingfossilshellsandwood。Greatprostratesilicifiedtrunksoftrees,embeddedinaconglomerate,wereextraordinarilynumerous。Imeasuredone,whichwasfifteenfeetincircumference:howsurprisingitisthateveryatomofthewoodymatterinthisgreatcylindershouldhavebeenremovedandreplacedbysilexsoperfectly,thateachvesselandporeispreserved!Thesetreesflourishedatabouttheperiodofourlowerchalk;theyallbelongedtothefir-tribe。ItwasamusingtoheartheinhabitantsdiscussingthenatureofthefossilshellswhichIcollected,almostinthesametermsaswereusedacenturyagoinEurope,——namely,whetherornottheyhadbeenthus“bornbynature。”MygeologicalexaminationofthecountrygenerallycreatedagooddealofsurpriseamongsttheChilenos:itwaslongbeforetheycouldbeconvincedthatIwasnothuntingformines。Thiswassometimestroublesome:
Ifoundthemostreadywayofexplainingmyemployment,wastoaskthemhowitwasthattheythemselveswerenotcuriousconcerningearthquakesandvolcanos?——whysomespringswerehotandotherscold?——whythereweremountainsinChile,andnotahillinLaPlata?Thesebarequestionsatoncesatisfiedandsilencedthegreaternumber;some,howeverlikeafewinEnglandwhoareacenturybehindhand,thoughtthatallsuchinquirieswereuselessandimpious;andthatitwasquitesufficientthatGodhadthusmadethemountains。
Anorderhadrecentlybeenissuedthatallstraydogsshouldbekilled,andwesawmanylyingdeadontheroad。Agreatnumberhadlatelygonemad,andseveralmenhadbeenbittenandhaddiedinconsequence。Onseveraloccasionshydrophobiahasprevailedinthisvalley。Itisremarkablethustofindsostrangeanddreadfuladisease,appearingtimeaftertimeinthesameisolatedspot。IthasbeenremarkedthatcertainvillagesinEnglandareinlikemannermuchmoresubjecttothisvisitationthanothers。Dr。
UnanuestatesthathydrophobiawasfirstknowninSouthAmericain1803:
thisstatementiscorroboratedbyAzaraandUlloahavingneverheardofitintheirtime。Dr。UnanuesaysthatitbrokeoutinCentralAmerica,andslowlytravelledsouthward。ItreachedArequipain1807;anditissaidthatsomementhere,whohadnotbeenbitten,wereaffected,asweresomenegroes,whohadeatenabullockwhichhaddiedofhydrophobia。AtIcaforty-twopeoplethusmiserablyperished。Thediseasecameonbetweentwelveandninetydaysafterthebite;andinthosecaseswhereitdidcomeon,deathensuedinvariablywithinfivedays。After1808,alongintervalensuedwithoutanycases。Oninquiry,IdidnothearofhydrophobiainVanDiemen’sLand,orinAustralia;andBurchellsays,thatduringthefiveyearshewasattheCapeofGoodHope,heneverheardofaninstanceofit。WebsterassertsthatattheAzoreshydrophobiahasneveroccurred;
andthesameassertionhasbeenmadewithrespecttoMauritiusandSt。
Helena。[2]Insostrangeadiseasesomeinformationmightpossiblybegainedbyconsideringthecircumstancesunderwhichitoriginatesindistantclimates;foritisimprobablethatadogalreadybitten,shouldhavebeenbroughttothesedistantcountries。