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Analysis of preparatory factors of landslides, Vsetínské vrchy Highland
Klimeš, Jan ; Vilímek, Vít (advisor) ; Kirchner, Karel (referee) ; Krejčí, Oldřich (referee)
iEiiiffgi gi íiiígiiĚ giiii é giggEgiá- iágiiiiiga,ť*lařii;Éiígí;aiiÉglgg*íi EÉiffEli{!Ě ,lzžíu:;: ,il1:žT:l:z1: !;! iglÉ ;11Ě,;E; EáÉž11#1i ť*1E ?:EEi íÉĚ:iá iíiieiei;=íii*{iiáEgi ialgi *Ě:;Ě:Ě í:; ;iiiiiilai;; 9iÉiiÉíE 1* EÉ*ílÉ:;EÉ *aili-řěEEř€ aÉ-ite-5š;iiÉiá3 ;Ěi zl1tE ag;EE5E Ě -= u;Ěii ltgigEgi;iílEi:i€* iiti*g;iE; iiŤáEEĚ, *šiE;á=E íiiíšiř{;iEi{!i?iáĚi iii{i*g: iiigEEigE:íii;giis glggšitÍgí ĚĚ : Ě5 É!* u ; E ; ?Ei ; ei; l Éiii* ii i ĚÉíÉ1ž=ž? z,EE íEt * ggái i* gi šiiiigi i i iE ; *ÉiEi i; i iii € u i €g:É€ 5 3 6 Hiř:"? = ?.:i ř:č j'* i g5E =;řfrE: l = ) i ;E;* g !=;= ě € ==.gE ;;:EE E HŤ*E !,.Žr'Ý-ž ;ri-*€ = =:€i E Íá 3= sěÉcÉi;É3ET Ú a,=._ 53J } o .aš'iÉá EEĚ.ř= ;Ť{E= sšgéí,,ž,z-ý.j2é k:= cL'2 TEÉE= ai =É;€ :iÉÉ=řÉ€iEiř € 8 Ť: q ÍE a š. Í :ál*gŘ3ŤcE;; ;F=Ee*EĚĚ.=_?É igBiE;.!3s=, se*č..:;Eg Ee g; E3: €ŤEŤ g,.eě P (n L a {) {ts {) 0.) q I (J q O () ag a 9 Ó] a a an gÉE.;É!€ťEŤ€É=E ť; :':=veu.?!7 Éi'*Ť 3 .=':.9Ú'=t.*; ;:aEi ;€E=iE;:éL c7..-9 -a TiečryE,.€: ;ě€:g = =*=uši*=.'! cÍsĚr + *E; :9*t;€* E;šTšž ;.0'Ěgřl;!ř ucc;ř 1 +Ú ó.9'-5Ť.=- a frĚ5c 3 * 1.ž=E6=:{3; č€*..Eg ,š i-E0]sĚ';5=É.a:ř*E 5 Íš;tĚ3É='*,7E':ĚE :Ě gEát;g;+-iE T':,ťqE € iš;:=E.3třř #tzĚÍ'. .2 :ť'i.ť:*E!šsaťíÉEě EĚE59;;EE! :řEi'i Č ĚE-eaiÉÉ;;sě::ÉřEa-.Lu q.'|..:-€= .t>.;oEi = ;É€"",,šÉÉ5:!E:ezzi íi2žeÉ':"' ěE b x 5 .''E :=...
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Analysis of preparatory factors of landslides, Vsetínské vrchy Highland
Klimeš, Jan ; Vilímek, Vít (advisor) ; Kirchner, Karel (referee) ; Krejčí, Oldřich (referee)
iEiiiffgi gi íiiígiiĚ giiii é giggEgiá- iágiiiiiga,ť*lařii;Éiígí;aiiÉglgg*íi EÉiffEli{!Ě ,lzžíu:;: ,il1:žT:l:z1: !;! iglÉ ;11Ě,;E; EáÉž11#1i ť*1E ?:EEi íÉĚ:iá iíiieiei;=íii*{iiáEgi ialgi *Ě:;Ě:Ě í:; ;iiiiiilai;; 9iÉiiÉíE 1* EÉ*ílÉ:;EÉ *aili-řěEEř€ aÉ-ite-5š;iiÉiá3 ;Ěi zl1tE ag;EE5E Ě -= u;Ěii ltgigEgi;iílEi:i€* iiti*g;iE; iiŤáEEĚ, *šiE;á=E íiiíšiř{;iEi{!i?iáĚi iii{i*g: iiigEEigE:íii;giis glggšitÍgí ĚĚ : Ě5 É!* u ; E ; ?Ei ; ei; l Éiii* ii i ĚÉíÉ1ž=ž? z,EE íEt * ggái i* gi šiiiigi i i iE ; *ÉiEi i; i iii € u i €g:É€ 5 3 6 Hiř:"? = ?.:i ř:č j'* i g5E =;řfrE: l = ) i ;E;* g !=;= ě € ==.gE ;;:EE E HŤ*E !,.Žr'Ý-ž ;ri-*€ = =:€i E Íá 3= sěÉcÉi;É3ET Ú a,=._ 53J } o .aš'iÉá EEĚ.ř= ;Ť{E= sšgéí,,ž,z-ý.j2é k:= cL'2 TEÉE= ai =É;€ :iÉÉ=řÉ€iEiř € 8 Ť: q ÍE a š. Í :ál*gŘ3ŤcE;; ;F=Ee*EĚĚ.=_?É igBiE;.!3s=, se*č..:;Eg Ee g; E3: €ŤEŤ g,.eě P (n L a {) {ts {) 0.) q I (J q O () ag a 9 Ó] a a an gÉE.;É!€ťEŤ€É=E ť; :':=veu.?!7 Éi'*Ť 3 .=':.9Ú'=t.*; ;:aEi ;€E=iE;:éL c7..-9 -a TiečryE,.€: ;ě€:g = =*=uši*=.'! cÍsĚr + *E; :9*t;€* E;šTšž ;.0'Ěgřl;!ř ucc;ř 1 +Ú ó.9'-5Ť.=- a frĚ5c 3 * 1.ž=E6=:{3; č€*..Eg ,š i-E0]sĚ';5=É.a:ř*E 5 Íš;tĚ3É='*,7E':ĚE :Ě gEát;g;+-iE T':,ťqE € iš;:=E.3třř #tzĚÍ'. .2 :ť'i.ť:*E!šsaťíÉEě EĚE59;;EE! :řEi'i Č ĚE-eaiÉÉ;;sě::ÉřEa-.Lu q.'|..:-€= .t>.;oEi = ;É€"",,šÉÉ5:!E:ezzi íi2žeÉ':"' ěE b x 5 .''E :=...
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The risk assessement of slope deformations for the R35 Highway project in the region of the southern by-pass of Turnov city
Dašková, Barbora ; Kycl, Petr (advisor) ; Krejčí, Oldřich (referee)
The planned R35 expressway has been known in paper form since 1963, but to date only a few sections have been built. These include the planned stretch through Bohemian Paradise. There are several ways to drive the highway, but none of them is perfect. So far, the winning northern variant has a planned southern bypass of Turnov using a tunnel to lead under the villages of Mašov, Hamry and Pelešany. Unfortunately, this area is known as a temporarily soiled landslide area. This thesis deals with the detection of the sliding surface of the sludge by means of geophysical measurement of ERT, mapping of the studied slope in the scale of 1: 5000 and possible impacts of the built tunnel on the municipalities. The mapping took place in March 2016 and together with the documentation points, is a map of the annex to this thesis. Keywords: R35 road, tunnel, ERT, slope stability, landslide mapping
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Geodynamical hazards of the Malé Karpaty Mts. northern part
Briestenský, Miloš ; Stemberk, Josef (advisor) ; Ondrášik, Rudolf (referee) ; Krejčí, Oldřich (referee)
Abstact In the scope of my Ph.D. thesis, the epicentral Dobrá Voda erea was selected for study of geodynamical hazards connected with active faults crossing the area. There was chosen some geomorphological, geological as well as geotechnical methods to discover recent tectonic regime. The obtained results showed close relationship between fault striking and drainage system orientation as well as erosion furrows orientation. Furthermore, wide-ranging slope deformations are located ďong faults with proved activity and the both phenomenons were studied and registered. Moreover, striking faults are reflexing by tufas, sag ponds and swallow holes occurence on the surfaoe. The subsurface active fault display is documented by' sinter damages along the fault in the local Zbojrucka and Slopl Caves. This manifestation influenced these caves to studS' fault microdiplacements and the net was extented by two extensometric TMTI gauges situated on the surface localities too. The monitoring results showed significant tenths and hundredths of mm movement trends per year as well as strain regime ohanges dwing local singnificant earthquakes. On the other hand, sence of the fault displacements showed sinistral block rotation in the wide-rangilg sinistral Mur-Mtirz-Leitha fault zone, which can be changed into dextral block...
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