{"id":392,"date":"2017-12-29T12:45:30","date_gmt":"2017-12-29T11:45:30","guid":{"rendered":"http:\/\/igcas.antstudio.eu\/?page_id=392"},"modified":"2025-02-10T14:50:40","modified_gmt":"2025-02-10T13:50:40","slug":"observatories","status":"publish","type":"page","link":"https:\/\/www.ig.cas.cz\/en\/observatories\/","title":{"rendered":"Observatories"},"content":{"rendered":"<p>[et_pb_section fb_built=&#8221;1&#8243; admin_label=&#8221;section&#8221; _builder_version=&#8221;3.22&#8243; custom_padding=&#8221;20px|0px|0px|0px&#8221;][et_pb_row admin_label=&#8221;row&#8221; _builder_version=&#8221;3.25&#8243; background_size=&#8221;initial&#8221; background_position=&#8221;top_left&#8221; background_repeat=&#8221;repeat&#8221; custom_padding=&#8221;0px|0px|28.95px|0px&#8221;][et_pb_column type=&#8221;4_4&#8243; _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;|||&#8221; custom_padding__hover=&#8221;|||&#8221;][et_pb_text _builder_version=&#8221;3.27.4&#8243; background_size=&#8221;initial&#8221; background_position=&#8221;top_left&#8221; background_repeat=&#8221;repeat&#8221;]Long-term observations of geophysical fields form one of the pillars of\u00a0activities\u00a0of the Institute of Geophysics.\u00a0We record earthquakes and other seismic events in the territory of the Czech Republic and abroad,\u00a0we measure temperatures at the surface and in wells, gravity and electromagnetic fields. Observed data is used to study the structure of our planet and the processes in the Earth. Data is available\u00a0on the portal of the\u00a0infrastructure <a href=\"http:\/\/www.czechgeo.cz\/en\/\"><strong>project CzechGeo\/EPOS<\/strong><\/a>\u00a0which is supported by the Ministry of Education of the Czech Republic.<br \/>\n[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=&#8221;1_3,2_3&#8243; _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;18.6199951171875px|0px|0px|0px&#8221; min_height=&#8221;198.6px&#8221;][et_pb_column type=&#8221;1_3&#8243; _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;|||&#8221; custom_padding__hover=&#8221;|||&#8221;][et_pb_image src=&#8221;https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2018\/02\/vrac_600.jpg&#8221; url=&#8221;https:\/\/www.ig.cas.cz\/en\/observatories\/czech-regional-seismological-network\/&#8221; align=&#8221;center&#8221; align_tablet=&#8221;center&#8221; align_phone=&#8221;&#8221; align_last_edited=&#8221;on|desktop&#8221; _builder_version=&#8221;3.23&#8243; max_width=&#8221;60%&#8221;]<br \/>\n[\/et_pb_image][\/et_pb_column][et_pb_column type=&#8221;2_3&#8243; _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;|||&#8221; custom_padding__hover=&#8221;|||&#8221;][et_pb_text _builder_version=&#8221;3.27.4&#8243;]<\/p>\n<p><strong><a href=\"czech-regional-seismic-network\/\">Czech regional seismic network\u00a0<\/a><\/strong>monitors\u00a0earthquakes, rockbursts and explosions in mines\u00a0in the Czech Republic, in central Europe and globally. It consists of twenty broadband stations\u00a0situated in the territory of the Czech Republic. Data is transferred in real time\u00a0to the data center at the Institute.\u00a0 Seismic service performs daily analysis of earthquakes, creates bulletins of readings of seismic stations and\u00a0catalogues regional events. Digital data is provided to international data centers and serve\u00a0e.g. to expedite the location process of prominent\u00a0earthquakes in the world.<\/p>\n<p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=&#8221;1_3,2_3&#8243; _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;22px|0px|19.6199951171875px|0px&#8221;][et_pb_column type=&#8221;1_3&#8243; _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;|||&#8221; custom_padding__hover=&#8221;|||&#8221;][et_pb_image src=&#8221;https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2018\/02\/vac_600.jpg&#8221; url=&#8221;https:\/\/www.ig.cas.cz\/en\/observatories\/lokalni-seismicka-sit-webnet\/&#8221; align=&#8221;center&#8221; align_tablet=&#8221;center&#8221; align_phone=&#8221;&#8221; align_last_edited=&#8221;on|desktop&#8221; _builder_version=&#8221;3.23&#8243; max_width=&#8221;60%&#8221;]<br \/>\n[\/et_pb_image][\/et_pb_column][et_pb_column type=&#8221;2_3&#8243; _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;|||&#8221; custom_padding__hover=&#8221;|||&#8221;][et_pb_text _builder_version=&#8221;3.27.4&#8243;]<a href=\"\/en\/observatories\/lokalni-seismicka-sit-webnet\/\"><strong>Local seismic network WEBNET<\/strong><\/a> monitors seismic activity in West Bohemia which is known for the occurance of earthquake swarms. Hot and cold mineral springs, and increased CO2 flux (Soos or Hartou\u0161ov moffetes) are other signs of the ceasing volcanic activity in the region. The dense network of seismic stations is operated by the Institute of Geophysics jointly with the Institute of Rock Structure and Mechanics.<br \/>\n[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=&#8221;1_3,2_3&#8243; _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;19px|0px|19px|0px&#8221;][et_pb_column type=&#8221;1_3&#8243; _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;|||&#8221; custom_padding__hover=&#8221;|||&#8221;][et_pb_image src=&#8221;https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2018\/02\/ash-1_600.jpg&#8221; align=&#8221;center&#8221; align_tablet=&#8221;center&#8221; align_phone=&#8221;&#8221; align_last_edited=&#8221;on|desktop&#8221; _builder_version=&#8221;3.23&#8243; max_width=&#8221;60%&#8221;]<br \/>\n[\/et_pb_image][\/et_pb_column][et_pb_column type=&#8221;2_3&#8243; _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;|||&#8221; custom_padding__hover=&#8221;|||&#8221;][et_pb_text _builder_version=&#8221;3.27.4&#8243; custom_padding=&#8221;3px|||||&#8221;]<\/p>\n<p><a href=\"https:\/\/www.ig.cas.cz\/en\/observatories\/local-seismic-network-reykjanet\/\"><strong>Local seismic network REYKJANET<\/strong><\/a> is deployed in Reykjanes penninsula in the southeastern tip of Iceland Mainshock-aftershock sequences as well as earthquake swarms occur in this region close to the North Atlantic ridge. Stations in the REYKJANET network operate in off-line regime. Data is copied several times a&nbsp;year during the service visit of the stations and sent to the Institute of Geophysics in Prague for processing. The network of seismic stations is operated by the Institute of Geophysics jointly with the Institute of Rock Structure and Mechanics.<\/p>\n<p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=&#8221;1_3,2_3&#8243; _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;19.9100341796875px|0px|19.5699462890625px|0px&#8221;][et_pb_column type=&#8221;1_3&#8243; _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;|||&#8221; custom_padding__hover=&#8221;|||&#8221;][et_pb_image src=&#8221;https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2018\/02\/bubd_600.jpg&#8221; align=&#8221;center&#8221; align_tablet=&#8221;center&#8221; align_phone=&#8221;&#8221; align_last_edited=&#8221;on|desktop&#8221; _builder_version=&#8221;3.23&#8243; max_width=&#8221;60%&#8221;]<br \/>\n[\/et_pb_image][\/et_pb_column][et_pb_column type=&#8221;2_3&#8243; _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;|||&#8221; custom_padding__hover=&#8221;|||&#8221;][et_pb_text _builder_version=&#8221;4.6.0&#8243;]<\/p>\n<p><a href=\"\/en\/observatories\/mobnet-pool\/\"><strong>MOBNET<\/strong> <\/a>is a&nbsp;pool of seismic stations installed temporarily in tectonically different regions in\u00a0the frame of\u00a0collaborative seismic experiments. The pool consists of 65 portable units. About half of the seismometers of the pool are short period Lennartz Le-3D sensors, the rest are\u00a0tree-component broad-band seismometers &#8211; Streckeisen (STS-2) and Guralp (CMG-3T, CMG-3ESP, CMG-40T). GAIA data acquisition systems work mostly in offline regime. MOBNET stations have been deployed\u00a0in international passive\u00a0seismic projects\u00a0RETREAT, LAPNET, PASSEQ, MOSAIC, BOHEMA and\u00a0AlpArray.<\/p>\n<p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=&#8221;1_3,2_3&#8243; _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;19px|0px|19.5699462890625px|0px&#8221;][et_pb_column type=&#8221;1_3&#8243; _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;|||&#8221; custom_padding__hover=&#8221;|||&#8221;][et_pb_image src=&#8221;https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2018\/02\/malence_slovinsko_600.jpg&#8221; align=&#8221;center&#8221; align_tablet=&#8221;center&#8221; align_phone=&#8221;&#8221; align_last_edited=&#8221;on|desktop&#8221; _builder_version=&#8221;3.23&#8243; max_width=&#8221;60%&#8221;]<br \/>\n[\/et_pb_image][\/et_pb_column][et_pb_column type=&#8221;2_3&#8243; _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;|||&#8221; custom_padding__hover=&#8221;|||&#8221;][et_pb_text _builder_version=&#8221;3.27.4&#8243;]<strong>Geothermal network GeoCLIMANET<\/strong> consists of three stations in the Czech Republic (Praha, Kocelovice, Svoj\u0161ice), one station in Portugal (Evora-Caravelinha) and one station in Slovenia (Malence). All the stations monitor air and soil temperatures at different depth levels between the surface and a&nbsp;depth of 1&nbsp;m. Except Svoj\u0161ice, all stations measure also bedrock temperatures at depths between 40&nbsp;m to 190&nbsp;m. The observed data is used for the analysis of the air &#8211; ground surface temperature coupling and the heat transfer in different climatic, pedological and environmental conditions.<br \/>\n[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=&#8221;1_3,2_3&#8243; _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;19.570068359375px|0px|19.5699462890625px|0px&#8221;][et_pb_column type=&#8221;1_3&#8243; _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;|||&#8221; custom_padding__hover=&#8221;|||&#8221;][et_pb_image src=&#8221;https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2018\/02\/00138_600.jpg&#8221; url=&#8221;https:\/\/www.ig.cas.cz\/en\/observatories\/geomagnetic-observatory-budkov\/&#8221; align=&#8221;center&#8221; align_tablet=&#8221;center&#8221; align_phone=&#8221;&#8221; align_last_edited=&#8221;on|desktop&#8221; _builder_version=&#8221;3.23&#8243; max_width=&#8221;60%&#8221;]<br \/>\n[\/et_pb_image][\/et_pb_column][et_pb_column type=&#8221;2_3&#8243; _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;|||&#8221; custom_padding__hover=&#8221;|||&#8221;][et_pb_text _builder_version=&#8221;3.27.4&#8243;]<a href=\"https:\/\/www.ig.cas.cz\/en\/observatories\/geomagnetic-observatory-budkov\"><strong>National geomagnetic observatory Budkov<\/strong><\/a> is\u00a0situated in the southern Bohemia, in the district of Prachatice. Since 1996 the observatory meets high international standards and is a&nbsp;certified observatory of the international network INTERMAGNET. The observatory is equipped with two digital magnetometers with 3-axis ferromagnetic fluxgate sensors and with Bobrov type variometers. Data is uploaded to the Geomagnetic Information Node in Edinburgh. Variation measurements are completed weekly by absolute measurements of the geomagnetic field, carried out by a&nbsp;non-magnetic theodolite CARL \u2013 ZEISS equipped with a&nbsp;single-axis Bartington fluxgate sensor.<br \/>\n[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=&#8221;1_3,2_3&#8243; _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;19.570068359375px|0px|19.5699462890625px|0px&#8221;][et_pb_column type=&#8221;1_3&#8243; _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;|||&#8221; custom_padding__hover=&#8221;|||&#8221;][et_pb_image src=&#8221;https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2018\/02\/pribram_naklony_600.jpg&#8221; url=&#8221;https:\/\/www.ig.cas.cz\/en\/observatories\/earth-tides-observatories\/&#8221; align=&#8221;center&#8221; align_tablet=&#8221;center&#8221; align_phone=&#8221;&#8221; align_last_edited=&#8221;on|desktop&#8221; _builder_version=&#8221;3.23&#8243; max_width=&#8221;60%&#8221;]<br \/>\n[\/et_pb_image][\/et_pb_column][et_pb_column type=&#8221;2_3&#8243; _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;|||&#8221; custom_padding__hover=&#8221;|||&#8221;][et_pb_text _builder_version=&#8221;3.29.3&#8243;]<\/p>\n<p>In the geodynamic networks <strong><a href=\"https:\/\/www.ig.cas.cz\/en\/observatories\/earth-tides-observatories\">CZET<\/a>, <\/strong><a href=\"https:\/\/www.ig.cas.cz\/en\/observatories\/webgeodyn\/\"><strong>WEBGEODYN<\/strong><\/a> and <a href=\"https:\/\/www.ig.cas.cz\/en\/observatories\/grevolcan\/\"><strong>GREVOLCAN<\/strong><\/a> we perform measurements of the earth tides at several tiltmeter stations, precise measurements of surface displacements by the GNSS technology, and observations of the earth\u2019s gravity field and its temporal variations. As well, we continuously record changes of groundwater level at wells. Beside these permanent observations we investigate location, composition and activity of volcanic structures in West Bohemia, Bavaria and Greece.<\/p>\n<p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=&#8221;1_3,2_3&#8243; _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;19.570068359375px|0px|19.5699462890625px|0px&#8221;][et_pb_column type=&#8221;1_3&#8243; _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;|||&#8221; custom_padding__hover=&#8221;|||&#8221;][et_pb_image src=&#8221;https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2022\/01\/photo_lab01-scaled.jpg&#8221; title_text=&#8221;Photo of the Tectonic modelling laboratory (TML)&#8221; url=&#8221;https:\/\/www.ig.cas.cz\/en\/observatories\/earth-tides-observatories\/&#8221; align=&#8221;center&#8221; align_tablet=&#8221;center&#8221; align_phone=&#8221;&#8221; align_last_edited=&#8221;on|desktop&#8221; _builder_version=&#8221;4.6.0&#8243; max_width=&#8221;60%&#8221;]<br \/>\n[\/et_pb_image][\/et_pb_column][et_pb_column type=&#8221;2_3&#8243; _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;|||&#8221; custom_padding__hover=&#8221;|||&#8221;][et_pb_text _builder_version=&#8221;4.6.0&#8243; custom_padding=&#8221;||0px|||&#8221; min_height=&#8221;222.2px&#8221;]<\/p>\n<p>In the <strong><a href=\"https:\/\/www.ig.cas.cz\/en\/?page_id=26857&amp;preview=true\">Tectonic modelling laboratory (TML)<\/a><\/strong>, we perform physical analog experiments to investigate large-scale and long-term geological processes, such as orogenic buckling, salt tectonics in rift basins and fold-and-thrust-belts as well as magmatic plumbing systems. Our laboratory infrastructure consists of a&nbsp;number of modelling devices to simulate tectonic shortening and extension, pure and simple shear strain, magmatic intrusions and eruptions as well as sediment deposition systems. To record deformation and strain patterns, our laboratory is equipped with modern strain quantification techniques such as a&nbsp;3D digital image correlation system and anisotropy of magnetic susceptibility generated by magnetic particles aligned in the deformed material.<\/p>\n<h2><\/h2>\n<p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][\/et_pb_section]<\/p>\n","protected":false},"excerpt":{"rendered":"<p>[et_pb_section fb_built=&#8221;1&#8243; admin_label=&#8221;section&#8221; _builder_version=&#8221;3.22&#8243; custom_padding=&#8221;20px|0px|0px|0px&#8221;][et_pb_row admin_label=&#8221;row&#8221; _builder_version=&#8221;3.25&#8243; background_size=&#8221;initial&#8221; background_position=&#8221;top_left&#8221; background_repeat=&#8221;repeat&#8221; custom_padding=&#8221;0px|0px|28.95px|0px&#8221;][et_pb_column type=&#8221;4_4&#8243; _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;|||&#8221; custom_padding__hover=&#8221;|||&#8221;][et_pb_text _builder_version=&#8221;3.27.4&#8243; background_size=&#8221;initial&#8221; background_position=&#8221;top_left&#8221; background_repeat=&#8221;repeat&#8221;]Long-term observations of geophysical fields form one of the pillars of\u00a0activities\u00a0of the Institute of Geophysics.\u00a0We record earthquakes and other seismic events in the territory of the Czech Republic and abroad,\u00a0we measure temperatures at the surface and in [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":4844,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_et_pb_use_builder":"off","_et_pb_old_content":"Dlouhodob\u00e1 pozorov\u00e1n\u00ed geofyzik\u00e1ln\u00edch pol\u00ed tvo\u0159\u00ed jeden z\u00a0pil\u00ed\u0159\u016f \u010dinnosti Geofyzik\u00e1ln\u00edho \u00fastavu. Registrujeme zem\u011bt\u0159esen\u00ed a dal\u0161\u00ed seismick\u00e9 jevy na \u00fazem\u00ed \u010cesk\u00e9 republiky i ve sv\u011bt\u011b, prov\u00e1d\u00edme m\u011b\u0159en\u00ed teplot, gravita\u010dn\u00edho zrychlen\u00ed,n\u00e1klon\u016f povrchu a elektromagnetick\u00e9ho pole Zem\u011b. Nam\u011b\u0159en\u00e9 \u00fadaje slou\u017e\u00ed k\u00a0v\u00fdzkumu stavby na\u0161\u00ed planety a proces\u016f, kter\u00e9 v\u00a0n\u00ed prob\u00edhaj\u00ed. Data jsou dostupn\u00e1 na port\u00e1lu infrastrukturn\u00edho <strong>projektu CzechGeo\/EPOS<\/strong>, kter\u00fd je podporovan\u00fd Ministerstvem \u0161kolstv\u00ed, ml\u00e1de\u017ee a t\u011blov\u00fdchovy \u010cR.\r\n\r\n\u00a0\r\n<table style=\"width: 892px; height: 1400;\" border=\"0\">\r\n<tbody>\r\n<tr>\r\n<td style=\"width: 150px; text-align: center;\"><img class=\"alignnone wp-image-613 size-thumbnail\" src=\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2018\/01\/kliuchevskoi-volcano-kamchatika-russia-from-space-aerial-nasa-2-150x150.jpg\" alt=\"\" width=\"150\" height=\"150\" \/><\/td>\r\n<td><strong>\u010cesk\u00e1 region\u00e1ln\u00ed seismick\u00e1 s\u00ed\u0165 <\/strong>registruje zem\u011bt\u0159esen\u00ed v\u00a0\u010cesk\u00e9 republice i ve sv\u011bt\u011b. Skl\u00e1d\u00e1 se z\u00a0cca dvaceti \u0161irokop\u00e1smov\u00fdch stanic na \u00fazem\u00ed \u010cR. Data jsou nep\u0159etr\u017eit\u011b p\u0159en\u00e1\u0161ena do datov\u00e9ho centra v\u00a0GF\u00da.\u00a0 Seismick\u00e1 slu\u017eba vytv\u00e1\u0159\u00ed katalogy zem\u011bt\u0159esen\u00ed v\u00a0\u010cR a ve st\u0159edn\u00ed Evrop\u011b a bulletiny \u010dten\u00ed seismick\u00fdch stanic. Digit\u00e1ln\u00ed data jsou poskytov\u00e1na mezin\u00e1rodn\u00edm datov\u00fdm centr\u016fm a slou\u017e\u00ed mj. k\u00a0rychl\u00e9 lokalizaci v\u00fdznamn\u00fdch zem\u011bt\u0159esen\u00ed na cel\u00e9m sv\u011bt\u011b.<\/td>\r\n<\/tr>\r\n<tr>\r\n<td style=\"width: 150px; text-align: center;\"><img class=\"alignnone wp-image-613 size-thumbnail\" src=\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2018\/01\/kliuchevskoi-volcano-kamchatika-russia-from-space-aerial-nasa-2-150x150.jpg\" alt=\"\" width=\"150\" height=\"150\" \/><\/td>\r\n<td><a href=\"http:\/\/ig.cas.cz\/vyzkum-a-vyuka\/observatore\/webnet\/\"><strong>Lok\u00e1ln\u00ed seismick\u00e1 s\u00ed\u0165 WEBNET<\/strong><\/a> monitoruje seismickou aktivitu v\u00a0aktivn\u00ed oblasti z\u00e1padn\u00edch \u010cech, kde se vyskytuj\u00ed zem\u011bt\u0159esn\u00e9 roje, tepl\u00e9 i studen\u00e9 miner\u00e1ln\u00ed prameny, a \u010detn\u00e9 v\u00fdrony CO2 (nap\u0159. lokalita Soos). To v\u0161e souvis\u00ed v\u00a0dozn\u00edvaj\u00edc\u00ed sope\u010dnou \u010dinnost\u00ed, kterou p\u0159edstavuj\u00ed vyhasl\u00e9 \u010dtvrtohorn\u00ed vulk\u00e1ny Komorn\u00ed h\u016frka a \u017delezn\u00e1 h\u016frka. Hustou s\u00ed\u0165 seismick\u00fdch stanic provozuje Geofyzik\u00e1ln\u00ed \u00fastav ve spolupr\u00e1ci s\u00a0\u00daSMH AV \u010cR.<\/td>\r\n<\/tr>\r\n<tr>\r\n<td style=\"width: 150px; text-align: center;\"><img class=\"alignnone wp-image-613 size-thumbnail\" src=\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2018\/01\/kliuchevskoi-volcano-kamchatika-russia-from-space-aerial-nasa-2-150x150.jpg\" alt=\"\" width=\"150\" height=\"150\" \/><\/td>\r\n<td><strong>Lok\u00e1ln\u00ed seismick\u00e1 s\u00ed\u0165 REYKJANET<\/strong> je rozm\u00edst\u011bna na poloostrov\u011b Reykjanes v\u00a0jihoz\u00e1padn\u00edm c\u00edpu Islandu. V\u00a0t\u00e9to oblasti bl\u00edzko atlantick\u00e9ho st\u0159edooce\u00e1nsk\u00e9ho h\u0159betu se vyskytuj\u00ed jak klasick\u00e1 zem\u011bt\u0159esen\u00ed, tak rojov\u00e1 zem\u011bt\u0159esen\u00ed podobn\u011b jako v\u00a0z\u00e1padn\u00edch \u010cech\u00e1ch. Stanice s\u00edt\u011b REYKJANET registruj\u00ed na pam\u011b\u0165ov\u00e9 karty a data jsou n\u011bkolikr\u00e1t za rok p\u0159i n\u00e1v\u0161t\u011bv\u011b sta\u017eena a odesl\u00e1na do GF\u00da ke zpracov\u00e1n\u00ed. S\u00ed\u0165 patn\u00e1cti seismick\u00fdch stanic provozuje Geofyzik\u00e1ln\u00ed \u00fastav ve spolupr\u00e1ci s\u00a0\u00daSMH AV \u010cR.<\/td>\r\n<\/tr>\r\n<tr>\r\n<td style=\"width: 150px; text-align: center;\"><img class=\"alignnone wp-image-613 size-thumbnail\" src=\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2018\/01\/kliuchevskoi-volcano-kamchatika-russia-from-space-aerial-nasa-2-150x150.jpg\" alt=\"\" width=\"150\" height=\"150\" \/><\/td>\r\n<td><strong>MOBNET <\/strong>je sada\u00a0mobiln\u00edch seismick\u00fdch stanic instalovan\u00fdch\u00a0v tektonicky\u00a0zaj\u00edmav\u00fdch oblastech na omezenou dobu v r\u00e1mci mezin\u00e1rodn\u00edch v\u00fdzkumn\u00fdch projekt\u016f. MOBNET vznikl v r. 1988 a v sou\u010dasn\u00e9 dob\u011b se skl\u00e1d\u00e1 ze 65 mobiln\u00edch stanic.\u00a0Polovina\u00a0seismometr\u016f jsou kr\u00e1tkoperiodick\u00e9\u00a0instrumenty Lennartz,\u00a0ostatn\u00ed jsou \u0161irokop\u00e1smov\u011b sensory\u00a0 Streckeisen a Guralp.\u00a0Datov\u00fd syst\u00e9m GAIA\u00a0pracuje p\u0159ev\u00e1\u017en\u011b v offline re\u017eimu, denn\u011b hl\u00e1s\u00ed stav stanice pomoc\u00ed sms zpr\u00e1v. Online p\u0159enos dat je tak\u00e9 mo\u017en\u00fd.Stanice MOBNET byly pou\u017e\u00edv\u00e1ny\u00a0 v pasivn\u00edch seismick\u00fdch projektech\u00a0RETREAT, LAPNET, PASSEQ, MOSAIC, BOHEMA, AlpArray.<\/td>\r\n<\/tr>\r\n<tr>\r\n<td style=\"width: 150px; text-align: center;\"><img class=\"alignnone wp-image-613 size-thumbnail\" src=\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2018\/01\/kliuchevskoi-volcano-kamchatika-russia-from-space-aerial-nasa-2-150x150.jpg\" alt=\"\" width=\"150\" height=\"150\" \/><\/td>\r\n<td><strong>Geoterm\u00e1ln\u00ed s\u00ed\u0165 GeoCLIMANET<\/strong><\/td>\r\n<\/tr>\r\n<tr>\r\n<td style=\"width: 150px; text-align: center;\"><img class=\"alignnone wp-image-613 size-thumbnail\" src=\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2018\/01\/kliuchevskoi-volcano-kamchatika-russia-from-space-aerial-nasa-2-150x150.jpg\" alt=\"\" width=\"150\" height=\"150\" \/><\/td>\r\n<td><strong>N\u00e1rodn\u00ed geomagnetick\u00e1 observato\u0159 Budkov<\/strong> se nach\u00e1z\u00ed na Prachaticku v ji\u017en\u00edch \u010cech\u00e1ch. Od roku 1996 observato\u0159 spl\u0148uje nejvy\u0161\u0161\u00ed mezin\u00e1rodn\u00ed standarty a je certifikovanou observato\u0159\u00ed mezin\u00e1rodn\u00ed s\u00edt\u011b INTERMAGNET. Krom\u011b historick\u00e9 analogov\u00e9 registrace jsou variace geomagnetick\u00e9ho pole zaznamen\u00e1v\u00e1ny modern\u00edm digit\u00e1ln\u00edm t\u0159\u00edos\u00fdm feromagnetick\u00fdm \u010didlem NAROD, jeho\u017e sign\u00e1l je vzorkov\u00e1n s intervalem 1 minuta. Permanentn\u00ed m\u011b\u0159en\u00ed je ka\u017ed\u00fdch 10 dn\u00ed dopl\u0148ov\u00e1no absolutn\u00edm m\u011b\u0159en\u00edm geomagnetick\u00e9ho pole pomoc\u00ed neferomagnetick\u00e9ho theodolitu CARL \u2013 ZEISS, kter\u00fd je roz\u0161\u00ed\u0159en jednoos\u00fdm feromagnetick\u00fdm \u010didlem BARTINGTON.<\/td>\r\n<\/tr>\r\n<tr>\r\n<td style=\"width: 150px; text-align: center;\"><img class=\"alignnone wp-image-613 size-thumbnail\" src=\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2018\/01\/kliuchevskoi-volcano-kamchatika-russia-from-space-aerial-nasa-2-150x150.jpg\" alt=\"\" width=\"150\" height=\"150\" \/><\/td>\r\n<td><strong>Slapov\u00e9 observato\u0159e GF\u00da<\/strong> je s\u00ed\u0165 \u0161esti stanic na registraci slapov\u00fdch dat, kter\u00e1 byla zalo\u017eena v roce 1952. Stanice se nach\u00e1z\u00ed\u00a0v P\u0159\u00edbrami, \u0158\u00edmov\u011b, Ka\u0161persk\u00fdch Hor\u00e1ch, Lazci, Jeze\u0159\u00ed a o ve Skaln\u00e9. Stanice Lazec je sou\u010d\u00e1st sv\u011btov\u00e9 s\u00edt\u011b slapov\u00fdch stanic. Registrovan\u00e1 data z observato\u0159\u00ed poskytuj\u00ed \u00fadaje o \u010dasov\u00fdch zm\u011bn\u00e1ch zemsk\u00e9ho gravita\u010dn\u00edho pole a o deformac\u00edch zemsk\u00e9ho t\u011blesa vlivem silov\u00e9ho p\u016fsoben\u00ed M\u011bs\u00edce, Slunce a planet. Data rovn\u011b\u017e zachycuj\u00ed \u00fa\u010dinky dal\u0161\u00edch geologick\u00fdch proces\u016f, jako jsou zem\u011bt\u0159esen\u00ed, pohyb podzemn\u00ed vody, apod.<\/td>\r\n<\/tr>\r\n<\/tbody>\r\n<\/table>","_et_gb_content_width":"","footnotes":""},"categories":[],"tags":[],"class_list":["post-392","page","type-page","status-publish","has-post-thumbnail","hentry"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v25.9 - https:\/\/yoast.com\/wordpress\/plugins\/seo\/ -->\n<title>Observatories - Geofyzik\u00e1ln\u00ed \u00fastav Akademie v\u011bd \u010cR, v.v.i.<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/www.ig.cas.cz\/en\/observatories\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Observatories - Geofyzik\u00e1ln\u00ed \u00fastav Akademie v\u011bd \u010cR, v.v.i.\" \/>\n<meta property=\"og:description\" content=\"[et_pb_section fb_built=&#8221;1&#8243; admin_label=&#8221;section&#8221; _builder_version=&#8221;3.22&#8243; custom_padding=&#8221;20px|0px|0px|0px&#8221;][et_pb_row admin_label=&#8221;row&#8221; _builder_version=&#8221;3.25&#8243; background_size=&#8221;initial&#8221; background_position=&#8221;top_left&#8221; background_repeat=&#8221;repeat&#8221; custom_padding=&#8221;0px|0px|28.95px|0px&#8221;][et_pb_column type=&#8221;4_4&#8243; _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;|||&#8221; custom_padding__hover=&#8221;|||&#8221;][et_pb_text _builder_version=&#8221;3.27.4&#8243; background_size=&#8221;initial&#8221; background_position=&#8221;top_left&#8221; background_repeat=&#8221;repeat&#8221;]Long-term observations of geophysical fields form one of the pillars of\u00a0activities\u00a0of the Institute of Geophysics.\u00a0We record earthquakes and other seismic events in the territory of the Czech Republic and abroad,\u00a0we measure temperatures at the surface and in [&hellip;]\" \/>\n<meta property=\"og:url\" content=\"https:\/\/www.ig.cas.cz\/en\/observatories\/\" \/>\n<meta property=\"og:site_name\" content=\"Dom\u016f\" \/>\n<meta property=\"article:publisher\" content=\"https:\/\/www.facebook.com\/GFUAVCR\/\" \/>\n<meta property=\"article:modified_time\" content=\"2025-02-10T13:50:40+00:00\" \/>\n<meta property=\"og:image\" content=\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2018\/01\/Q330.jpg\" \/>\n\t<meta property=\"og:image:width\" content=\"1994\" \/>\n\t<meta property=\"og:image:height\" content=\"261\" \/>\n\t<meta property=\"og:image:type\" content=\"image\/jpeg\" \/>\n<meta name=\"twitter:card\" content=\"summary_large_image\" \/>\n<meta name=\"twitter:label1\" content=\"Est. reading time\" \/>\n\t<meta name=\"twitter:data1\" content=\"6 minutes\" \/>\n<script type=\"application\/ld+json\" class=\"yoast-schema-graph\">{\"@context\":\"https:\/\/schema.org\",\"@graph\":[{\"@type\":\"WebPage\",\"@id\":\"https:\/\/www.ig.cas.cz\/en\/observatories\/\",\"url\":\"https:\/\/www.ig.cas.cz\/en\/observatories\/\",\"name\":\"Observatories - Geofyzik\u00e1ln\u00ed \u00fastav Akademie v\u011bd \u010cR, v.v.i.\",\"isPartOf\":{\"@id\":\"https:\/\/www.ig.cas.cz\/#website\"},\"primaryImageOfPage\":{\"@id\":\"https:\/\/www.ig.cas.cz\/en\/observatories\/#primaryimage\"},\"image\":{\"@id\":\"https:\/\/www.ig.cas.cz\/en\/observatories\/#primaryimage\"},\"thumbnailUrl\":\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2018\/01\/Q330.jpg\",\"datePublished\":\"2017-12-29T11:45:30+00:00\",\"dateModified\":\"2025-02-10T13:50:40+00:00\",\"breadcrumb\":{\"@id\":\"https:\/\/www.ig.cas.cz\/en\/observatories\/#breadcrumb\"},\"inLanguage\":\"en-US\",\"potentialAction\":[{\"@type\":\"ReadAction\",\"target\":[\"https:\/\/www.ig.cas.cz\/en\/observatories\/\"]}]},{\"@type\":\"ImageObject\",\"inLanguage\":\"en-US\",\"@id\":\"https:\/\/www.ig.cas.cz\/en\/observatories\/#primaryimage\",\"url\":\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2018\/01\/Q330.jpg\",\"contentUrl\":\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2018\/01\/Q330.jpg\",\"width\":1994,\"height\":261},{\"@type\":\"BreadcrumbList\",\"@id\":\"https:\/\/www.ig.cas.cz\/en\/observatories\/#breadcrumb\",\"itemListElement\":[{\"@type\":\"ListItem\",\"position\":1,\"name\":\"Dom\u016f\",\"item\":\"https:\/\/www.ig.cas.cz\/en\/\"},{\"@type\":\"ListItem\",\"position\":2,\"name\":\"Observatories\"}]},{\"@type\":\"WebSite\",\"@id\":\"https:\/\/www.ig.cas.cz\/#website\",\"url\":\"https:\/\/www.ig.cas.cz\/\",\"name\":\"Dom\u016f\",\"description\":\"Geofyzik\u00e1ln\u00ed \u00fastav Akademie v\u011bd \u010cR, v.v.i.\",\"potentialAction\":[{\"@type\":\"SearchAction\",\"target\":{\"@type\":\"EntryPoint\",\"urlTemplate\":\"https:\/\/www.ig.cas.cz\/?s={search_term_string}\"},\"query-input\":{\"@type\":\"PropertyValueSpecification\",\"valueRequired\":true,\"valueName\":\"search_term_string\"}}],\"inLanguage\":\"en-US\"}]}<\/script>\n<!-- \/ Yoast SEO plugin. -->","yoast_head_json":{"title":"Observatories - Geofyzik\u00e1ln\u00ed \u00fastav Akademie v\u011bd \u010cR, v.v.i.","robots":{"index":"index","follow":"follow","max-snippet":"max-snippet:-1","max-image-preview":"max-image-preview:large","max-video-preview":"max-video-preview:-1"},"canonical":"https:\/\/www.ig.cas.cz\/en\/observatories\/","og_locale":"en_US","og_type":"article","og_title":"Observatories - Geofyzik\u00e1ln\u00ed \u00fastav Akademie v\u011bd \u010cR, v.v.i.","og_description":"[et_pb_section fb_built=&#8221;1&#8243; 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