地質図幅説明書
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- としみ あわたけ
- 5 years ago
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6 Ⅺ Ⅺ Ⅺ Ⅺ Ⅺ Ⅺ Ⅺ Ⅺ Ⅺ Résumé
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10 km m
11 ,m
12
13 flatlava
14 ,m
15 NWSWNW NE NWNE
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17 m
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19 NE
20 ,m cm.mmmm
21 flatlavaplatylava flat-lava
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24 cm m cm
25 m m
26 ,m
27 km m m,.m
28 mm km
29 m m
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31 mm km mmm m m
32 m m m m,m
33 m,m,m,,m flatlava
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35 ,m,m,m Schneekoppe,m Sonnblick Zngspitze,m
36 ,m.,m..,m m m
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38 m
39 cm m,m m m
40 ,m,m
41 ,m,m m m cm m cm cm
42 cm
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44 cm cmcm m 塡
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46 cm
47 Ⅺ Ⅺ Ⅺ N WNE cm..cm m NW
48 WE NWNESWm mangtaggtcu Pb.Zn.Cu cmmm Ⅺ km m Ⅺ Ⅺ m C
49 Ⅺ,mm C,m C Ⅺ
50 m m No.No m No.No
51 No.No.No Ⅺ m
52 km
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54 Vol No Vol VolNo No No No
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56 EXPLANATORYTEXT OFTHE GEOLOGICALMAPOFJAPAN Scale ASAHIDAKE Abashiri By MoriakiKōnoyaTakehiroKobayashi CheoulWooKimandShinpeiKawachi GeologicalSurveyofHokkaidō Résumé TheareaofAsahidakesheetmapissituatedinlatitude NandlongitudeE.,andislocatedin thedaisetsunationalparkandbelongstokamikawatownhiga shikawatownbieitownandshintokutowninhokkaidōthe Daisetsuvolcanicgroupisincludedinthissheetmapandthe neighbouringdaisetzusheetmap Topography TopographicallytheareaisdividedintotheDaisetsuvolcanic groupandtheirbasementswhicharedistributedintheeastern andwesternpartsthebasementintheeasternpartismainly composedoftheslateandbasemanyraggedmountainranges peralleltothestructureoftheslatethewesternbasement composedmainlyofthepropyliteshowssteepmountainthe Daisetsuvolcanoesarecomprisetopographicallythebroadrelati velyflatplainscomposedofbasallavaflowsdomeshapedmounta inssuchashakuundakeandtomuraushimadeofveryviscous
57 lavasandtypicalstratifiedvolcanoessuchasasahidake InadditionlowflatplaneisdevelopedalongtheIshikaririver inthenortheasternpart Geology ThegeologyofthisareaiscomposedlargelyofPreTertiary HidakaGroupMiocenevolcanicrocksandsedimentsandmany lavaflowsofthedaisetsuvolcanicgroupwhichcovertheabove mentionedformationsinadditionquaternarysedimentsare alsopresent PreTertiaryformationisrepresentedbytheslateofthelo werhidakaformationbelongingtothehidakagroup TheMioceneformationscomprisetheKaunnaipropyliteand YanbetappuFormationTheKaunnaipropylitewhichisexten sivelydistributedinthewesternpartoftheareaisakindof compositeigneousbodybeingcomposedofrhyoliticandbasaltic propylitesinsomeplacesbothholocrystallinefaciesandgreen tuffareassociatedwiththem TheYanbetappuFormationislargelycomposedoflatered palegreenweldedtuffsandiscoveredbynormaldepositscompo sedofthesandstonsintheupperhorizon ThePlioceneFormationsincludetheTomuraushiweldedtuff andtheuniishikarilavasthetomutaushiweldedtuffcompo sedofrhyoliticweldedtuffcoveredbytuffaceoussandstoneis welldevelopedinthisareaaswellasintheadjoiningareaofthe sheetmapoftheupperstreamofthetokachirivertheuni Ishikarilavacomposedofthehyperstheneaugiteandesiteisde velopedintheeasternpartofthearea Theothervolcanicrockscomprisethelavaflowsrelatedto theformationofthedaisetsuvolcanicgroupandcanbegrouped intothefollowingstages ThestageoftheformationofthebasementoftheDai setsuvolcanicgroup
58 ThestageoftheformationoftheOlderDaisetsuVolcano ThestageoftheformationoftheYoungerDaisetsuVo lcano ThestageoftheformationoftheAsahidakevolcano OfthesethestagebelongstothePleoPleistoceneandthest agebelongstotheholocenethelavasofthe stageinclude thebieilowerlavakoganegaharalowerlavanumanoharalava MidoridakelowerlavaKaundakelavaPonchūbetsulavaKogane gaharalavachūbetsudakelavaandtakanegaharalavaallof whicharetwopyroxeneandesitessomtimeswishwelldeveloped platyjointtheyarecharacterizedbytheirextensivedistri butionformingflatlavaplatformsandareofthesocalledflat lavatype The stageincludestheolderdaisetsulavausiroasahidake lavahakuundakelavatomuraushi stlaveandndlavaall ofwhichbelongtothehornblendehyperstheneaugiteandesites withcoarsegrainedphenocrysts ThestagevolcanicsisrepresentedbytheSounkyowelded tuffhyperstheneaugiteandesiticincompositionitsgeologicage isthelatepleistocene InadditionthefirstterracedepositstheHakuyōdairaforma tionandthethirdterracedepositsallofwhicharepleistocene orholoceneinagearedevelopedinthelowlandalongtheishi kaririver GlacialandPeriglacialTopography CirquesduetotheglacialerossionaredevelopedintheKo ganegaharakaundakechūbetsudakeandtakanegaharaandthe iraltitudeishigherthan,mabovethesealevel Periglacialtopographyincludespolygonalsoilsstriationsoils andstonepavementsallofwhicharealsodistributedintheal tiude Economicgeology
59 Anepithermaldepositofcopperleadandzincisfoundinthe midstreamofthekaunnairiveranexplitationwastried oncebutthedepositwasabandonedowingtoitspoorquality Theminingofsulfurwhichwastheimportantnonmetalicdepo sitsinthecraterofasahidakebeendiscontinued Hotspringsareabondantinthisdistrictandmanyof themareusedforbathingsuchastenninkyōyūkomanbetsu andkogenspashotspringswhichissuefromtheupstreams ofyambetappuandtomuraushirivershavenotbeenutilized EspeciallyalongtheupstreamofTomuraushiriverhotsprings higher aredistributedforthedistanceofaboutkmand muchsteamiscomingout
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平成9年度水道事業年報 1概況 2施設
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