Ukuhamba ngezintaba ze-Eruption 30 Years Later
1 - iNtaba yaseSt. Helens evela eJohnston Ridge
INtaba yaseSt. Helens eWashington State yaqhuma ukuqhuma kwentabamlilo ngoMeyi 18, 1980. Ukuqhuma komhlaba, ukuqhuma kwe-lateral, ukugeleza kwe-pyroclastic kanye nomlotha kushabalalisa indawo eyayizungezile, kwabulala abantu abangu-57. I-USGS Geologist uDavid Johnston washona lapha, emgodini obizwa ngegama lakhe namuhla. Manje, eminyakeni engaba ngu-30 kamuva, sasihamba nge-Eruption Trail futhi sagibela umzila we-Boundary Trail kuya e-Spirit Lake kusukela eJohnston Ridge Observatory.
Ngemuva kweminyaka engama-30, impilo ibuyele kancane kancane emfuleni osemahlathini. Umzila owawuba idwala, izimpande kanye ne-fir inaliti egqoke isihlabathi manje isihlabathi esihle nesigcawu sokuqhuma nokuqhuma komlotha kusukela ngo-1980. Leli dome elisha lakhiwe kabusha izikhathi eziningana kule minyaka engamashumi amathathu edlule, kuphela amamitha amahlanu nje bheka enqabeni ye-volcano evela kuJohnston Ridge.
IChibi Lomoya lihlaselwa yizigqoko zemigodi emhlophe elaliqeda lolo suku olujabulisayo, lugudle ogwini lwayo, nomoya kaHarry Truman, umnikazi wezindwendwe ongazange aphume futhi manje wangcwatshwa ngezansi.
Umbono weNtaba iSt. Helens evela eJohnston Ridge ibonakala ingashintshi kakhulu kusukela ngokushesha ngemva kokuqhuma kwe-volcanic ka-1980.
Kusukela kuJohnston Ridge Observatory eNyakatho yeMonument yaseMount St. Helens, izivakashi ziqhele ngamamitha angu-5,5 ukusuka ku-lava dome e-volcano. Phakathi kwe-ridge ne-intaba kuyisigodi esigcwele umlotha futhi sinezintaba ezinamamitha amakhulu. Amanzi aseMfuleni i-Toutle aqoshe ama-canyons amasha emlilweni naselwandle.
Ngomhla ka-18 Meyi 1980 lo mgwaqo wawusehlathini. I-USGS geologist uDavid Johnston wabamba iqhaza lakhe lapha, ehlala ebuka inqwaba ebusweni bentaba enyakatho. Amazwi akhe okugcina axwayisa wonke umuntu, "Vancouver, Vancouver, yilokho!" Ukuvuthwa kwemvelo kunqobe intaba futhi inqwaba yehlelwa phansi emazweni amaningi amakhulu ayeke wabona eNyakatho Melika. Kwakulandelwa ukuqhuma kwesikhala somoya oshisayo wama-600F owabulala ama-mph angu-700 mph owachitha ama-square angaphezu kwama-250 ehlathi ngasenyakatho ye-volcano. Khona-ke ukuqhuma komlotha kwaqhubekela phambili amahora ayisishiyagalolunye, kuphenduka ubusuku ubheke empumalanga ye-Washington ne-Idaho.
INtaba iSt. Helens yaziqhayisa ukusuka ekuphakameni kwayo ngamamitha angu-9677 kuya ekuphakameni okusha kwamamitha angu-8365. Lapho kuqhuma ama-ash ash, i-snowcone eyayivele iphelele yezintaba yayisigobolondo esingenalutho ene-cratter semicircular ngasenyakatho. Intaba ihambe kuphi? Manje usakazeka endaweni engakuzungezile. Iziqondiso zithi rock eyanele yalahlekelwa ukuhamba umgwaqo 3 kuya phezulu ukusuka eNtabeni iStens kuya eNew York City.
Emashumini amathathu eminyaka alandelayo, i-lava enamathele kancane kancane yaqala ukudala i-lava dome entsha emgodini. INtaba iSt. Helens yenze lokhu ngaphambili. Sibona isiqephu sayo samuva nje emlandweni omude wokwakha, ukuqhuma nokuvuselela futhi. I-glacier entsha ihamba ngaphansi kwe-lava dome, nakuba ibukeka ibe mnyama ngasekupheleni kwehlobo, igcwele umlotha. Umlilo, iqhwa namanzi zizoqhubeka zimelela iNtaba iSt. Helens.
2 - UJohnston Ridge Observatory - Isikhumbuzo seNtaba yaseMount St. Helens
I-Johnston Ridge Observatory ihlola ngokucophelela ukuqhuma kwentaba yase-Mount St Helens, eWashington.
I-Johnston Ridge Observatory ivuliwe ngoMeyi ngo-Okthoba, ngo-10 ekuseni kuya ku-6 ntambama. Itholakala ekupheleni komgwaqo, State Highway 504. Kungaba ukuhamba kwehora elilodwa ukusuka empumalanga ukusuka ku-I-5 Ukuphuma 49, kanye nokuhamba kwehora eli-2 ukusuka ePortland, e-Oregon. Kukhona imali kumuntu omdala ngokuvakashela uJohnston Ridge noma iColdwater Lake eSikhumbuzweni seNtaba yaseMount St. Helens. I-Interagency Passes (i-Golden Age / Ukufinyeleleka Kokufinyelela) kanye Nonyaka We-Northwest Forest Passes nazo zamukelwa eziteshini ze-Monument Pass.
Izilwane ezifuywayo azivunyelwe ngombono noma ezindleleni.
I-Observatory itholakala ngamamitha angu-4314 ukuphakama, enombono ocacile 5.5 miles ukuya enqumeni yeSt. St Helens. Umbono oqondile phakathi kwe-crater ne-lava dome ziphefumula.
Ngaphakathi kwe-observation kubonisa ukuqhuma kanye nezindaba zalabo abasinda ekuqhumeni. Ifilimu engamaminithi angu-16 iphela ngokuvula isikrini esivinini lesithombe kuya ku-crater.
Kusukela ekuqapheliseni, abahambahambayo bangakwazi ukujabulela umzila we-Ection Eruption and abagibeli abahamba phambili abangakwazi ukuqhubekela phambili emgwaqeni we-Boundary neHarry's Ridge Trail ukuze babone i-Spirit Lake.
Ngikhumbula izingxoxo zomsakazo ne-TV ezivame ukunikezwa ngo-1980 nguDavid Johnston, isazi sezwe se-USGS esibhekwa kuso. Ngaphezu kwabaningi ngesikhathi ngaleso sikhathi, wesaba umcimbi onzima. Lapho kufika ukuthi ngeSonto ekuseni, wadlulisa i-USGS eVancouver, eWashington, kusukela kulolu gwaqo. "Vancouver, Vancouver, yilokho." Umzimba wakhe awutholakalanga, kodwa indawo yokuhlola iyisikhumbuzo esifanele.
Umzila we-3 - Ephuthayo eSikhumbuzweni seNtaba yaseSt
I-Eruption Trail iyindlela engamamitha ayi-1 eqoshiwe eJohnston Ridge Observatory, iSikhumbuzo seNtaba yaseMount St. Helens.
I-trailhead ye-Trail Eruption e-plaza ye-Johnston Ridge Observatory, ekupheleni komgwaqo we-Spirit Lake Highway SR 504. Kuyindlela efinyelelekayo yokudweba ekhuphuka ngamamitha angu-100 futhi ejikeleza emuva uye endaweni yokupaka futhi ibuyele emuva i-observation.
Ngalesi sakhiwo, ubona izihlahla zomuthi eziphunywe kusukela ekuqhumeni kwe-lateral ngesikhathi sokuqhuma. I-compass plaza phezulu kwegquma ibonisa izindawo ezizungezile nxazonke.
I-trail kanye ne-observatory zivele nje ngamakhilomitha angaphezu kwamakhulu amahlanu ukusuka enqumeni yeSt. St Helens kanye ne-lava dome esebenzayo. Lona yindawo yokubukwa okungcono ku-crater ungathola emgwaqweni osemthethweni.
Umzila we-Eruption ungahamba nganoma yiziphi izicathulo zezemidlalo noma zenduduzo . Ngincoma ngokumelene ne- flip flops ngenxa yokwehlisa, kokubili phezulu naphansi. Izihlalo zabakhubazekile zingadinga usizo ngokunyathela. Ukuphakama kwamamitha angu-4200 kuya ku-4300, ngakho-ke abaphansi bezwe bangadinga ukuyihamba kancane futhi bakhumbule ukuthatha umoya ojulile. Noma yisiphi isizathu sokumisa okwesikhashana futhi ucabange ukuthi i-volcano isetshenziswa kahle.
Izilwane ezifuywayo azivunyelwe endleleni. Izimpawu zokuqapha ukuhlala emigwaqweni noma ukubhekana nokuhle okungenani $ 100. Lona izwe elincane elinamanje lisahluleka ukululama.
I-4 - I-Blast Area Tree Stumps Isithombe
Ukuqhuma okusabalalisa komkhuhlane waseMeyi 18, 1980 kwawela phansi amamayela angu-250 square, kubandakanya lezi zihlahla kuJohnston Ridge.
Ukukhuphuka kwentaba yaseMount St. Helens ngo-May 18, 1980 kwaqala ngokuzamazama komhlaba okungu-5.2 okwakubangelwa umhlaba omkhulu owake wabhalwa. Njengoba ubuso obusenyakatho bezintaba beqhamuka esigodini esiseduze, kwafunyanwa amagesi aqhutshwa yizintaba-mlilo ezazingakhiwa izinyanga. Ukukhishwa kwe-lateral kwe-300F igesi yahamba ngesivinini esiphezulu, ngamamayela angaphezu kwamakhilomitha angu-700 ngehora, iqonde ngqo enyakatho ngaphesheya kwesigodi namagquma. Ukuqhuma akuzange kukhuphuke, kwavela ngqo ukusuka enyakatho ye-mountain of the mountain.
Ukuqhuma kwaqhuma phansi izingodo ngaphezu kwendawo engamakhilomitha-skwele angu-250. Izihlahla zalala njengemidwebo, zonke zihlanganisiwe ezikude nokuqhuma.
Kukhona khona ukuqhuma kwamabhomu okuqhuma komlilo ngaphambi kokuba lokhu kuqhuma. Iziqhumane ziqhuma njalo, ngqo? UDavid Johnston, geologist olahlekelwe yile ndawo, wayebikezele ukuthi iNtaba iSt. Helens yayizoqhuma ngokuqhuma. Wenzani lapha, ke? Wacelwa ukuba athathe elinye i-geologist elalikhuluma ngeposi le-Coldwater II, ngolunye usuku. Kwakuyilanga eliyingozi.
5 - Ikhampasi Ngethrafikhi Yokuphutha
Ikhampasi lensimbi lisiza izivakashi ukuba zithole futhi ziqambe igama elivela emgwaqweni ophuthumayo eSikhumbuzweni seNtaba yaseSt. Helens National Volcanic.
Ngemuva kokukhuphuka ngamamitha angu-100 ku-Trail Eruption eqoshiwe evela eJohnston Ridge Observatory, izivakashi zingasebenzisa ikhampasi yebhesi ukuthola futhi ziqambe ngamakhilomitha angu-360 ukusuka kwombono.
Ngaphandle kweSt. St. Helens uqobo, cishe amakhilomitha amahlanu kuya eningizimu, izivakashi zingabona iNtaba i-Adams bese zihlola iSt Lake Spirit empumalanga.
Kusuka lapha, umzila we-Eruption uhlela ukuhlukaniswa ne-Boundary Trail futhi uyaqhubeka nokuqhubeka nokupaka izimoto.
6 - I-Blast Zone iNorth of Eruption Trail
Amathafa nezigodi enyakatho yeNtaba iSt. Helens zazihlathini kuze kufike usuku lokuqhuma ngo-1980. Eminyakeni engamashumi amathathu kamuva, basenesikhukhula esincane kuphela.
Izithombe ezivela eJohnston Ridge ngaphambi kukaMeyi 18, 1980 zikhombisa amahlathi aphuma kusukela phansi kwentaba nasenyakatho. Lo mbono wawuyovela ehlathini lapho i-Weyerhaeuser ivunwa izihlahla ezivuthiwe zokhuni.
Umbono lapha, eminyakeni engama-30 kamuva, ubonisa umhlaba ongeyinyumba yezihlahla. I-vista ongayilindela ehlane lasempumalanga ye-Washington, hhayi ehlathini lemvula lamaCascades. Amagquma amhlophe ehlathini abhekene nokuqhuma kwe-lateral asabonakala, kodwa iningi liye lafika emfuleni ogubuzele amagquma, futhi yahlaselwa yaba izakhi ezihlahleni ze-huckleberry kanye nezimbali zasendle ezibuya.
Esikhathini sokuhamba nge-SR 504, izivakashi zibona amahlathi amasha ekhula, kodwa kuphela ezindaweni ezihlwanyelwe umuntu. Ukutshala izihlahla zemvelo akuzange kwenzeke kabanzi.
7 - iNtaba yaseSt. Helens esuka e-Eruption Trail
Imifula kancane idwebe iziteshi ezintsha endaweni yokuqhuma enyakatho yeNtaba St Helens.
Intaba yaseSt. Helens ingamakhilomitha amahlanu ukusuka ku-Eruption Trail eJohnston Ridge Observatory. Uma ubheka phansi, ubona iziteshi eziqoshwe ekuqhumeni komlotha nomlotha owenziwe yi-landslide ne-lateral ukuqhuma ngoMeyi 18, 1980.
Ngaphambi kwalolo suku, ngabe ubheke phansi ehlathini eliya ngasezintabeni, ne-timberline cishe ngezinga lezinyawo ezingu-6000. Singamamitha angu-4200 kuJohnston Ridge.
Kuze kube yiNtaba iSt. Helens iqhuma ngokuqhuma kwayo, ayengazi ukuthi yini eyadala ama-hummocks edwaleni abonayo nxazonke ezinjenge-Mount Shasta eCalifornia. Manje siyazi ukuthi kwakuyizinhlobonhlobo zamadwala ezinwabuzelayo eceleni kwezintaba.
Izivakashi ezingenangqondo zingathola indawo egcwele amafu, inkungu noma imfucuza. Izivakashi ezihlezi zingase zibone ukuqhuma noma ukuqhuma komlotha, njengoba ngenza eminyakeni eminingana ngaphambili.
8 - Intaba yeSt. Helens Kwalabo Ababulewe Ephupheni Ngo-18, 1980
Udonga lwe-granite lubhala amagama alabo ababulewe ekuqhumeni. Abaningi bafa ngaphandle kweLuhlu Olubomvu oluvinjiwe.
Ngemuva kokuhla eThethweni Lokuphutha, i-Trail Boundary idlulisa isikhumbuzo kulabo ababulewe yi-eruption.
Babenjani laba bantu lapho? Amagama afaka inani elicindezelayo labashadile. Kwakungaba yibo bonke abaqhamukayo ababefanele bazi kangcono kunokuba babe khona eduze nendawo yokuqhuma kwentaba?
Ngo-May 18, 1980 ngavula i-Sunday Oregonian yami ukubona isihloko esithi umgwaqo omkhulu ungene endaweni evinjiwe wawuvulwa ngempelasonto kubahlali. Umbusi wayevumela labo abanemikhaya nezinkampani zokuvakasha endaweni ukuba bathathe impahla yabo, njengoba intaba yayithule amasonto amathathu.
Indawo Ebomvu yayincane kakhulu futhi ukuqhuma kukhulu kakhulu. Izazi ze-geologists, kuhlanganise noDavid Johnston, zincoma indawo enkulu ebomvu kakhulu, kepha izithakazelo zokuhlala kanye nezakhamuzi bezibeke kahle ngendawo. Ngaphezu kwalokho, kwakungelula ukuzungeza amabhuloho emigwaqweni, enezincwadi ezingekho emthethweni ezitshela abantu ukuthi bangayisebenzisa kanjani imigwaqo yokungena ukuze bangene ezindaweni ezingavinjelwe.
Umhlahlandlela on the trail wangitshela indaba yendoda yakhe. Wajoyina abangane ukuthola ama-athikili avela ekamelweni lawo lokuvakasha. Kwakudingeka bahambe ekushoneni kwelanga kodwa banquma ukuhlala ubusuku. Wakhumbula ukuthi kwakudingeka athole inja yomakhelwane ekhaya futhi washiya phakathi kwamabili. Abangane bakhe abazange bahambe ngesikhathi esilandelayo ekuseni futhi bafa ekuqhumeni.
Okungaphezulu kwakuyobe sekufa uma intaba ingakaze ivele ekuseni ngeSonto ekuseni. Ngesikhathi abanye abavukuzi befa, bekungeke kube okungenani okungenani abangu-300 endaweni yokuqhuma ngoMsombuluko ekuseni.
Ezinye zezindaba zalabo abasinda ziboniswa kuJohnston Ridge Observatory.
Ukufa kuvele kusukela ekuqhumeni kwe-lateral nokuphuma kwe-pyroclastic. Abantu nabo babulawa yonke emfuleni i-Toutle njengoba kwaphenduka inqwaba yamagodo, idwala nomlotha emkhunjini owonakele owabhubhisa umgwaqo kanye namabhuloho kuze kube ku-I-5, 50 miles ukuya entshonalanga.
I-9 - Umzila Wemikhawulo Yezakhiwo kuya echibini lomoya
Kusuka eMthonjeni Wenqwaba eduze kwaseJohnston Ridge Observatory, i-sliver encane yeLwandle Lomoya ingabonakala empumalanga.
Umzila we-Boundary uqala njengesivinini esivela ku-Trail Eruption eduze neJohnston Ridge Observatory. Iyaqhubeka empumalanga ngasemgwaqeni bese ihamba eduze no-Elbow sikaDeveli ukubuka iLimo Lomoya.
I-Boundary Trail ingumlotha ongaguquki kanye negravel. Kuyindawo enhle kakhulu yokuhamba ngezinyawo ezifanele izicathulo zezemidlalo noma izicathulo zomzila . Umzila unama-ups and downs kodwa ukuhamba okulula kakhulu kuze kube yi-Elbow ka-Devil. Njengoba ihamba eduze no-Elbow kaDeveli, incane kakhulu ngokudonsa izinyawo ezingu-1000 kanye nezinye izindawo lapho umzila ungasebenzi khona. Labo abangenaso ukwesaba bangase bafise ukuphenduka ngalesosikhathi, kodwa ngokwenza kanjalo uzobe udlula imibono emihle yeLwandle Lomoya.
INtaba ye-Hiker.com Incazelo kanye nemephu
10 - Umzila Wemingcele kuJohnston Ridge
Umzila omhlophe womzila womngcele ungabonakala kuJohnston Ridge.
Ekhoneni elingezansi elingakwesokunxele, ungabona isikhumbuzo semisindvo kulabo ababulewe ekukhuphukeni komhlaka-18 Meyi 1980. Umzila uqhubekela phambili emgwaqeni. It has a few ups and downs kodwa ikakhulukazi indawo enhle igravel, kahle drained. Udlula izimbali zasendle. Kusukela emakhilomitha amabili eceleni komgwaqo unemibukiso emangalisa yecala elingasenyakatho yeNtaba iSt. Helens kanye ne-pumice plain ngezansi.
Kusuka lapha, ungabona uMt. I-Adams igxila phezu komgwaqo kude, ne-sliver encane yeLwandle Lomoya ekhoneni eliphezulu lesokudla.
11 - Mount St Helens Boundary Trail Travers View
Abahambahamba banombono oncomekayo kaMt. USt. Helens sonke eduze kweBoundary Trail Traverse.
Le ngxenye ye-Boundary Trail # 1 evela eJohnston Ridge Observatory ilandela umugqa wezintambo ngezinye izintaba ezincane nezintaba ezisezingeni elibanzi. Ubuso luwumlotha kanye negravel elifakwe ukuqhuma okuphambene nangoMeyi 18, 1980. Kuyindawo enhle yokuhamba, ikakhulukazi ngaphandle kwamadwala amakhulu noma izimpande.
Ungathola isifo se-volcanic emehlweni akho lapha, ngakho labo abagqoka ama-lens angathinta izinyathelo zokuphepha.
Letha ikhamera ukuthi ithathe isikhonkwane seNtaba yeSt. Helen esenyakatho, engamakhilomitha angaba ngu-5 ukusuka kude. I-North Fork yoMfula i-Toutle ihamba kancane kancane imidwebo engamamitha angama-1000 ngezansi ngamakhulu ezinyawo zezintaba ezihlanjululwayo ezifakwe emhlabathini kanye nokuqhuma kwe-1980.
Intaba iyabonakala emgwaqeni omkhulu wamamitha amabili ukuya lapho umzila ulula khona futhi uhamba eduze no-Elbow sika-Elbow.
12 - Hlalani ku-Sign Trail
Abahamba ngezinyawo baxwayiswa ukuba bangathinteli ukutakula okunokonakala kwezitshalo nezilwane endleleni.
Ukuvakashela uJohnston Ridge eminyakeni engu-30 ngemva kokuqhuma, ngashaywa yizimboni ezincane ezazitholile. Ngiyaphambene nalokhu nemvelo nje ngamakhilomitha ambalwa ukusuka eColdwater Lake. Ukuhamba kwami okokugcina kwakudinga ukuthi kube nomcibisholo ku-bushwack ngokusebenzisa izihlahla ezikhulayo eziphakeme kakhulu kunami.
Kodwa lapha kulesi sigqoko esingenalutho, azikho izihlahla. Izihlahla ziyingcosana, kungaphezulu kwemvelo engaphansi kwesibhakabhaka.
Azikho izindawo zokungcebeleka noma imithombo yamanzi eceleni kwe-Trail Boundary lapha.
Hlala endleleni ukuze uvumele imvelo ukubuyisela impilo lapha.
13 - Blast Zone Trees
Umbono oya enyakatho yeJohnston Ridge ungena emagodini amhlophe ezihlahla ezibhujiswe ekuqhunyeleni kwe-lateral, ngo-1980.
Izindleko zamahlathi amakhulu ahlanganisa uJohnston Ridge kanye namagquma angasenyakatho kwawo kubonakala emithonjeni emhlophe ehlanjululwayo yezihlahla ezachithwa ngoMeyi 18, 1980, ngokuqhuma okwenziwe kamuva kwe-Mount St Helens.
Ngokushesha ngemva kokuqhuma, lezi zintaba zaziqedile izihlahla ezigqamile njengezigcawu, konke okushiwo ngokuphelele ukuqhuma. Eminyakeni engama-30 edlule, baye bajula kakhulu emlilweni nasezimpandeni ezibekwe yi-eruption. Bakha ama-nursery logs kanye nomanyolo wezimbali zasendle kanye nezihlahla. Abaningi baye bahlanza emanzini ukuze babe yizinkuni.
Kunamandla ukubuka lezi zigwaqo futhi ubone ukuthi bambalwa izihlahla ezibuyiselwe zona ngokwemvelo eminyakeni engama-30. Amahlathi amancane esasihamba nawo endleleni eya entabeni atshalwe ngumuntu emva kokuqhuma.
14 - ama-White Rock Deposits avela e-Mount St. Helens Eruption
Izindawo ezimhlophe ezibonwa emagqumeni yiziqu zedwala ezikhishwe phakathi nendawo yentaba ngokuqhuma komhlaka-18 Meyi 1980.
Emakhilomitha amahlanu kuya kwangu-7 ukusuka emgodini weNtaba iSt. Helens, ungabona izindawo zedwala elimhlophe. Lezi zindawo yidwala elalikhishwe ekuqhumeni okukhulu kwe-lateral ngoMeyi 18, 1980. Umbala nokwenziwa kwala mawa kusho izazi zezwe ukuthi zivela entabeni. Akumangalisi ukuthi akukho muntu noma isilwane esasinda kulokhu kuqhuma kulolo suku.
15 - i-Penstemon
I-Penstemons ikhula eduze ne-Boundary Trail eJohnston Ridge, eSikhumbuzweni seNtaba yaseSt. Helens National Volcanic
Abavakashi beJanston Ridge kulo lonke ihlobo bangabona izimbali zasendle ziqhakaza. Lezi zimbali ziye zabuyela ezindaweni ezibhuqiwe.
I-Penstemon isitshalo esibekezela isomiso, esifanelekile kulo mgwaqo owomile.
I-Pearly Everlasting
I-Pearly Everlasting ikhula eduze noJohnston Ridge.
I-pearly ehlala njalo iyinhlangano yasemfuleni yasendle esingawomiswa futhi yengezwe ezinhlobonhlobo ze-bouquets. Kodwa-ke, lesi sibonelo siseSikhumbuzweni seNtaba yaseMount St. Helens futhi kukhona ukukhetha noma ukuhlukumeza amahlamvu. Thatha izinkumbulo kuphela bese ushiya izinyawo nje kuphela.
17 - Paintbrush yamaNdiya
I-Paintbrush yamaNdiya ikhula kuJohnston Ridge.
I-Paintbrush yamaNdiya, i- Castilleja linariifolia iyisibonakaliso sendawo yasendle eNorth West, futhi iyisimbali sezwe sase-Wyoming. Lapha likhula eduze noJohnston Ridge endaweni yokuqhuma yaseMt. USt. Helens.
18 - I-Elbow ka-Diyabeli emgwaqweni wezintaba
Umbono we-Elbow sika-Elbow.
Emakhilomitha angaba ngu-2 empumalanga yeJohnston Ridge Observatory, Umzila we-Boundary # 1 ufinyelela emthonjeni ohamba ngezinyawo futhi uwela eceleni kwe-Elbow sika-Elbow.
Umzila ukhonjiswe ekudoneni okungamamitha angu-1000 kolunye uhlangothi. Ezinye izindawo zihlaziywa futhi zijwayele ukuhamba. Okuningi:
Ngiphakamisa ukuthi abagibeli abahamba ngezinyawo kuphela abagqoke izicathulo zokuhamba ngezinyawo baqhubekela phambili ku-Elbow sika-Elbow.
19 - I-Elbow ka-Diyabeli emgwaqweni wezinyawo
Esikhatsini sikaDeveli
Lo mbono weNgxenye kaDeveli kaDeveli ye-Boundary Trail ayikho kulabo abasaba ukuphakama nokuvezwa. Umzila uncane kakhulu futhi, ngezimpelasonto, kungenzeka ukuthi ufanele wenze indlela yabagibeli abaza ngaphesheya.
Kodwa ukuze uthole imibono engcono kakhulu e-Spirit Lake, udinga ukuqhubeka. Ukubuyela emuva manje, usube nemibono emihle eNtabeni iHelen Helens kodwa hhayi ngeLomoya Lake.
20 - I-Elbow kaDeveli kanye ne-Mount Helens Crater
Ingxenye kaDeveli kaDeveli ye-Boundary Trail incane kakhulu. Ingxenye yesenyakatho yeNtaba yaseSt. Helens ingamakhilomitha amahlanu kuphela ngaphesheya kwesigodi.
21 - Wendy Uphendukela Emlonyeni KaDeveli
Umndeni udabula ingxenye engcolile ye-Boundary Trail ku-Elbow sika-Elbow. Nginguye umgibeli ku-jacket eluhlaza. Umthwebuli wezithombe wayenesibindi esikhulu kunami. Angizange ngithande ubuso obungaguquki bomdwebo kanye nezinkomba ezimbalwa, ezisezingeni eliphansi nezinhla. Ungabona isibazi esimhlophe esifundeni sezintaba esibonisa ukuguguleka okusha.
Kukhona ama-hikers omdala futhi kukhona ama-hikers angamaqhawe, kodwa ingabe kukhona abagibeli abadala, abanesibindi?
Nganquma ukuthi angisekho okwesibhakabhaka-okwanele nesibindi-okwanele ukubeka engozini ukuhamba ngezinyawo ezingu-1000 phansi kobuso bomgwaqo. Ukuhlengwa kwezindiza kungaba yinto ehlazeka kakhulu.
Kusuka lapha, umthwebuli wezithombe uNona Litch waqhubeka ngesibindi ekubukeni kweLimo Lomoya kanye neHarry's Ridge Trail. Ngabuyela kuJohnston Ridge Observatory ukuze ngijabulele izinkulumo zama-ranger.
22 - I-Elbow i-Droboff emgwaqeni weNtaba
Umbono we-dropsff wezinyawo ezingu-1000 ukusuka kwesigaba sikaDeveli sika-Elbow esincane se-Boundary Trail. Iningi lale nqubo emfushane yendlela ephethe idwala elihle, elisezingeni eliphansi futhi elizinzile elihlangene. Kodwa-ke, endaweni lapho kwakukhona khona umzila wokuhamba nokuhamba komhlabathi ngamanqina amancane nezinsika ezincane, ngishaya i-Retreat. Intengo yokukhokhela ukushiya ingaba ngaphezu kwe- ankle ehlutshiwe .
23 - Ukuqala kokuqala kweLwandle Lomoya ovela eBoundary Trail
Umvuzo walabo abanesibindi ngokwanele ukuqinisa isibindi sikaDeveli sikaDeveli ungumbono oseduze weLwandle Lomoya. Nasi umbono wokuqala wechibi ngemuva kokugoqa ukugoba.
Ukubukwa kwechibi kubonakala kumaphoyinti angu-3-4 ukusuka kuJohnston Ridge Observatory ku-Boundary Trail # 1.
24 - Ichibi leMoya elivela eBoundary Trail
Emakhilomitha amane ukusuka empumalanga yeJohnston Ridge Observatory, abagibeli bafinyelela kulo mbono weLwandle Lomoya. Bangase baphenduke lapha noma baqhubeke neHarry's Ridge Trail ukuze uthole amaphuzu amaningi.
Izindawo ezimhlophe ogwini akuzona idwala noma iqhwa. Ziyizihlahla ezihlanjululwayo zezihlahla ezaqothulwa ekuqhumeni kuka-1980, izimpumputhe zidonsa ogwini lwaseMoya. Bahamba bezungeza echibini. Abahamba ngezinyawo bathi bangakholwanga izinombolo eziningi zalezi zingodo ezikhona lapho, eminyakeni engu-30 kamuva.
Ichibi ngokwayo laphulwa ngaphandle kwesibhakabhaka ngokuqhuma komhlaka-18 Meyi 1980. I-lodge namahhovisi eholide kanye nomhlali onenkani uJarob Truman wanyamalala phakade. Ukuqhuma kwagcwalisa leli chibi ngedwala nomlotha. Amanzi abuyela echibini, manje ahlala ngamamitha angu-200 aphakeme, futhi izinsika eziqothulwe zahlulwa kuwo.
Ososayensi baye bafunda isimiso esiyinqaba sechibi iminyaka engu-30. Ngokushesha ngemva kokuqhuma, kwakuyisichibi esishisayo, esingafi. Inhlobo yama-bacterium eLegionnaire ahluma futhi agula abanye ososayensi. Ngesinye isikhathi, iningi laleli qhwa lalimbozwe izihlahla eziwile. Baba umanyolo futhi ichibi liye lashintsha ngokuqhubekayo. Manje sezemidlalo impilo eminingi kunokwenza ngaphambi kokuqhuma.
25 - Huckleberry Bush
Ukuthokozisa kwabagibeli kanye nezilwane zasendle, izihlahla ze-huckleberry sezibuyele endaweni yokuqhuma ngaphezu kweLwandle Lomoya.
AmaHuckleberries afana nama-blueberries, kodwa atholakala endle.
26 - I-Harry's Ridge Trail Sign
I-Harry's Ridge Trail ihola i-kilomita elilodwa ukusuka ku-Boundary Trail eya eHarry Viewpoint.
Umzila ubizwa ngokuthi nguHarry Randall Truman, umnikazi oneminyaka engu-83 ubudala kanye nomqhubi we-Mount St. Helens Lodge eMoya Lake. Nakuba le ndawo yayisezindaweni ezivinjiwe, wenqaba ukuphuma lapho intaba isasebenza. I-War World War I yayisixoxwa ngaso sonke isikhathi yizindaba zendawo kusukela ngoMashi kuya kuMeyi ka-1980.
I-lodge, uHarry, namakati akhe angama-16 awazange aphile ekugezeni kwe-pyroclastic eyangcwaba uMoya Womoya ngaphansi komlotha nomlotha ongaphezu kuka-150. Ungumuntu wokuqala owakhumbula kakhulu lapho ekhumbula ukuqhuma kwe-1980.
27 - I-Harry's Ridge Trail Sign
IHarry's Ridge Trail ikhuphuka le nqola ibe yombono ukuze ibheke ngaphezu kweLwandle Lomoya.
I-Harry's Ridge Trail # 208 inikeza imibono engcono kakhulu ye-Spirit Lake nendawo engasenyakatho ye-Mount St. Helens. Kuyinto ekhuphuka kakhulu, efinyelela ngamamitha angaba ngu-500 ngehora elilodwa.
Kulabo abaqale eJohnston Ridge Observatory, bazoba nemikhumbi engu-7.8 ehamba ngezinyawo uma beya phezulu eHarry's Ridge.
28 - Ichibi leMoya elivela eHarry's Ridge Trail
Kusukela kuHarry's Ridge Trail, abagibeli bangabona okuningi kweLwandle Lomoya. I-Mount Adams ikude.
29 - UHarry's Ridge Trail View kuya kuJohnston Ridge Observatory
Kusukela kuHarry's Ridge, abagibeli bezinyawo bangabheka ngasentshonalanga ekuqaleni kwabo eJohnston Ridge Observatory.
Ufikile ngaphezu kwamakhilomitha angu-3.5 ubeka indawo yokuhlola futhi ungabona emuva.
30 - Ichibi leMoya eNtabeni iHelen Helens
Umbono oseduze weLimo Lomoya eMount St. Helens.
Umkhathi omhlophe ogwini oluthile lweMoya Lake yizingodo eziluhlaza ezimhlophe - izinkuni ezixoshwa ngokuqhuma komzimba kanye nokugeleza kwamanzi ngoMeyi 18, 1980. Manje, eminyakeni engama-30 kamuva, basalokhu bahamba kulwandle.
IChibi Lomoya lihlala ngamamitha angu-200 ngaphezulu kunalokho okwenze ngaphambi kokuqhuma, njengoba ibhasi lalo ligcwele idwala nomlotha okhishwa entabeni. Ichibi lalikhishwe ngokweqile emgodini walo, ngokushaywa ngamamitha amakhulu ezinyawo ngaphezu kwezinga langaphambili lesichibi.
Namuhla, i-alpine lake liphila kakhulu kulo kunanini ngaphambili. Izinhlanzi zibuye zibuyele, nakuba kungenzeka ukuthi azibangelwa ukufuduka kwemvelo, kodwa ngabantu babuyiselwa echibini ngokumelene nenqubomgomo esemthethweni.
31 - Isigqoko Sogqoko Sesiliva Esimnandi Sasegolide
Sivame ukubiza lezi zinsizwa ezincane ze-chipmunks, kodwa igama elifanele yi-squirrels engaphansi kwegolide.
Ungabatshela lezi ngaphandle kwe-chipmunks, abavame ukuhlala ezindaweni ezifanayo, ngoba ama-square squirrels ase-golden-mantled ayinayo imivimbo ebusweni babo, kuyilapho ama-chipmunks enza.