The stabilisation of the landslide in the cadastral district. Ratiboř (Q58059): Difference between revisions

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(‎Removed claim: EU contribution (P835): 42,828.0476 euro)
(‎Changed an Item: Fixing rounding issue)
Property / EU contribution
 
42,828.05 Euro
Amount42,828.05 Euro
UnitEuro
Property / EU contribution: 42,828.05 Euro / rank
 
Preferred rank
Property / EU contribution: 42,828.05 Euro / qualifier
 
exchange rate to Euro: 0.04 Euro
Amount0.04 Euro
UnitEuro
Property / EU contribution: 42,828.05 Euro / qualifier
 
point in time: 10 January 2020
Timestamp+2020-01-10T00:00:00Z
Timezone+00:00
CalendarGregorian
Precision1 day
Before0
After0

Revision as of 20:30, 22 September 2020

Project in Czech Republic financed by DG Regio
Language Label Description Also known as
English
The stabilisation of the landslide in the cadastral district. Ratiboř
Project in Czech Republic financed by DG Regio

    Statements

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    1,070,701.19 Czech koruna
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    42,828.05 Euro
    10 January 2020
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    1,259,648.47 Czech koruna
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    50,385.9388 Euro
    10 January 2020
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    85.0 percent
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    3 April 2017
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    29 March 2018
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    31 March 2018
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    Obec Ratiboř
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    49°22'19.38"N, 17°54'10.55"E
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    75621
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    Projekt spočívá v realizaci nejnutnějších opatření pro stabilizaci sesuvu v k.ú. Ratiboř u cyklostezky vedoucí z obce do města Vsetín. Jedná se o sesuv nad nárazovým břehem Ratibořky na pozemku parc. č. 843/22 v katastrálním území Ratiboř u Vsetína. Bezprostřední příčinou porušení stability svahu bylo zvodnění deluviálních hlinitých až hlinito-kamenitých sedimentů vsakujících srážkovou vodu a vodu z tajícího sněhu v prostoru úzké plošiny mezi cyklostezkou a přilehlým pravým údolním svahem. (Czech)
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    The project involves the most necessary measures to stabilise the landslide in the cadastral district. Ratiboř for cycle paths from the municipality to Vsetín. These are sesues above the emergency bank of Ratibodra on plot No 843/22 within the cadastral area of Ratiboř u Vsetín. The immediate cause of non-compliance with the stability of the slope was the aquifer of the fluidal, clay-rocky sediment of the ground water and melting snow in an area of narrow space between the cycle path and the adjacent real valleys of the cycle. (English)
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    Identifiers

    CZ.05.1.24/0.0/0.0/16_034/0002327
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