Interiér kostnice, sektor 62B. Západní řez. Pohled od východu.
Interiér kostnice, sektor 62B. Západní řez. Pohled od východu.
Interior of the ossuary, sector 62B. Western cut. A view from the east.
Interiér kostnice, vstupní část. Pohled na zkoumanou plochu. V popředí zakrytý výkop se sektorem 65. Pohled od jihovýchodu.
Interiér kostnice, vstupní část. Pohled na zkoumanou plochu. V popředí ...zakrytý výkop se sektorem 65. Pohled od jihovýchodu.
Interior of the ossuary, entrance part. A view of the area under study. A covered excavation with sector 65 in the foreground. A view from the southeast.
The shallow medieval Jeroným Mine is located at a distance of about 25 km southeast of the Nový Kostel focal zone where the most intensive seismic activity in West Bohemia (Czech Republic) has been ...documented. Permanent seismological monitoring has been carried out since 2004 in this mine. During the 2011 and 2014 seismic swarms, more than 1000 triggered records comprising almost 1500 earthquakes were recorded at the permanent station in the mine. Three short-term seismological experiments were accomplished during these swarms. Several temporary seismic stations were simultaneously placed in different parts of underground spaces which enabled comparison of vibration effect caused by near earthquakes in different parts of the mine. Although the depth of the lowest parts of mine is only about 60 m, a vibration effect generated by earthquakes from the Nový Kostel focal zone is not the same for the whole underground complex.
Prispevek prikaže glavne glasoslovne poteze krajevnih govorov, in sicer na slovenski strani Babno Polje, Novi Kot, Osilnica, Bosljiva Loka in na hrvaški strani Prezid, Tršće, Ravnice, Gerovo, ...Hrvatsko. Natančneje se prikaže govor Tršća v obliki fonološkega opisa, ki izhaja iz izhodiščnega splošnoslovenskega fonološkega sistema. Namen prispevka je na osnovi narečnega gradiva potrditi, da so omenjeni krajevni govori del istega narečja. Potrdijo se sledeče delovne hipoteze: državna meja ne predstavlja tudi narečne meje; obravnavani govori ne izkazujejo mešanosti; vse govore moremo umestiti v eno narečje, tj. v zahodni del kostelskega narečja dolenjske narečne skupine slovenskega jezikovnega sistema.
The time series of two continuously operating gas monitoring stations at Oldřišská and Nový Kostel located along seismoactive faults in the epicentral area of the NW Bohemian swarm earthquakes (Czech ...Republic) are compared with water level fluctuations in two boreholes positioned along these faults and with gas flux variations of a mofette at the Soos mofette field at 9 km distance. The seasonal trend of the monitored CO2 concentration with a maximum in November and a minimum in March/April is governed by groundwater temperatures, superimposed in spring by soil temperatures. CO2 concentration variations identified at Oldřišská are also reflected in gas flux variations in the Soos mofette and/or water level fluctuations of two boreholes. Variations in the gas monitoring recordings of station at Nový Kostel are also linked with variations at Oldřišská. In all data sets, diurnal variations generated by earth tides occur, reflecting a daily stress – fault permeability cycle. Additional stress interferes with this cycle. Significant, abrupt changes are attributed to geodynamic processes linked with seismic events, as revealed by local seismicity or by the transient of waves of a strong remote earthquake. Simultaneous variations of the gas concentrations in the Nový Kostel area and in the gas flux in the Soos point to an interconnected hydraulic conductive fault systems present in the northern part of the Cheb Basin. Sharp falls in gas concentration, during or subsequent to, earthquake swarms may reflect fault compression associated with impeded gas migration. However, gas variations also occur in periods without seismic activity, indicating changes in fault permeability were caused by local aseismic fault movements, as revealed by events with opposite trends in the gas recordings at Oldřišská, Nový Kostel and the Soos. Therefore, a mathematical approach to establish a correlation between seismicity and gas geochemical variations is not possible.
Time series of a multiyear gas monitoring at three stations along seismoactive faults and at a mofette are presented. It revealed variations in gas concentration and gas flux in an hydraulic conductive fault network in the NW Bohemian swarm earthquake region (Cheb Basin, Czech Republic) caused by geodynamic processes. The seasonal trend of the monitored CO2 concentration is governed by groundwater temperatures, deviations from the trend can be used to identify long‐term changes of stress. Changes in CO2 gas flux and CO2 concentrations at two sites probably caused by fault movements.
Pohled na zkoumanou plochu očima návštěvníka kostnice.
Pohled na zkoumanou plochu očima návštěvníka kostnice.
A view of the area under study through the eyes of a visitor to the ossuary.
SZ segment. Pyramida z lidských kostí během rozebírání. Záchranný archeologický výzkum proběhl v ploše pod pyramidou.
SZ segment. Pyramida z lidských kostí během rozebírání. Záchranný archeologický ...výzkum proběhl v ploše pod pyramidou.
SZ segment. Pyramid from human bones during disassembly. Rescue archaeological research took place in the area below the pyramid.
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