WOPE40 EJRC 311614 EARTHQUAKE ALERT MESSAGE NUMBER 001 THIS IS AN AUTOMATIC ALERT FROM THE GLOBAL DISASTER ALERTS AND COORDINATION SYSTEM (WWW.GDACS.ORG). THE DISSEMINATION THROUGH GTS OF THIS PRODUCT IS INTENDED AS GUIDANCE IN SUPPORT OF UN ACTIVITIES: IT IS A PILOT PROJECT BETWEEN WMO AND JRC TO TEST COMMUNICATION AND DISSEMINATION CHANNELS OF VALUE-ADDED PRODUCTS. ************************************************************ * GREEN EARTHQUAKE ALERT IN ISLAMIC REPUBLIC OF IRAN * ************************************************************ SUMMARY ON 31 OCT 2019 15:43:59 UTC (ABOUT 31 OCT 2019 19:22:45 LOCAL TIME) AN EARTHQUAKE OF MAGNITUDE 4.9 OCCURRED IN THE HIGHLY POPULATED REGION OF HORMOZGAN IN ISLAMIC REPUBLIC OF IRAN. BUSTANEH THE NEAREST POPULATED PLACES ARE: BUSTANEH (39.8 KM). THE CLOSEST CIVILIAN AIRPORT IS: SIRRI ISLAND (31.3 KM). EARTHQUAKE EVENT CHARACTERISTICS - SOURCE: NEIC - MAGNITUDE: 4.9 M - DEPTH: 10 KM - LOCATION (LAT/LONG): 26.1558 | 54.6918 - COUNTRY: ISLAMIC REPUBLIC OF IRAN - PROVINCE: - REGION: SOUTHERN IRAN - UTC/GMT (GREENWICH TIME): 31 OCT 2019 15:43:59 UTC - ESTIMATED LOCAL SOLAR TIME: 31 OCT 2019 19:22:45 ============================================================================================================ POTENTIALLY AFFECTED CRITICAL INFRASTRUCTURE: - NUCLEAR PLANTS: N/A - HYDRODAMS: N/A - AIRPORTS: SIRRI ISLAND (31.3 KM), BANDAR LENGEH (43.7 KM), ABU MUSA ISLAND (46.1 KM), KISH ISLAND (82.1 KM) - PORTS: FARRUR ISLAND (23.9 KM), SIRRI ISLAND (31.8 KM), ABU MUSA (47.2 KM), LINGAH (49.1 KM), TUNB ISLAND (60.9 KM), MUBAREK TERMINAL (62 KM), FATEH TERMINAL (69.6 KM), BASIDU (78.8 KM), QEIS ISLAND (79.2 KM), SHARAK (80.2 KM), HAMRIYAH (95.2 KM) BASED ON AN AUTOMATED IMPACT MODEL, THIS EARTHQUAKE, WHICH OCCURRED IN A REGION WITH LOW VULNERABILITY TO NATURAL DISASTERS, HAS POTENTIALLY A UNKNOWN HUMANITARIAN IMPACT. EVENT DATE UNIV. TIME: THU, 31 OCT 2019 15:43:59 UTC EUROPEAN TIME OF THE EVENT: 31 OCT 2019 16:43:59 EAST AMERICA TIME OF THE EVENT: 31 OCT 2019 10:43:59 WEST AMERICA TIME OF THE EVENT: 31 OCT 2019 07:43:59 EAST ASIA TIME OF THE EVENT: 31 OCT 2019 23:43:59 THIS EMAIL REPORT WAS AUTOMATICALLY CREATED BY A COMPUTER AT: 31 OCT 2019 16:14:41 (30 MIN AFTER THE EVENT) SEE THE GDACS WEBSITE FOR LIVE NEWS COVERAGE (INCLUDING OCHA SITUATION REPORTS), THE FULL EARTHQUAKE REPORT IS AT HTTP://WWW.GDACS.ORG/REPORT.ASPX?EVENTTYPE=EQ$AND;EPISODEID=1276594 FOR INFORMATION ON EMERGENCY RESPONSE, PLEASE CONSULT THE GDACS VIRTUAL OSOCC: HTTP://VOSOCC.UNOCHA.ORG ============================================================================================================ POPULATION DENSITY NEAR EPICENTER (PEOPLE/KM2). RADIUS (KM) POPULATION DENSITY (PEOPLE/KM2) 200 5959238 759 175 4330074 551 150 3891879 496 125 2927869 373 100 133812 17 75 83066 11 50 42204 5 20 5 0 10 0 0 5 0 0 2 0 0 THE POPULATION IN THE 50 KM AREA OF THIS EARTHQUAKE IS 5 PEOPLE/KM2. ============================================================================================================ THE EARTHQUAKE OCCURRED AT 31 OCT 2019 19:22:45 LOCAL TIME. 31 OCT 2019 19:22:45 RESILIENCE AND VULNERABILITY ---------------------------- RESILIENCE IS THE CAPACITY OF THE POPULATION TO COPE WITH A HAZARD. SINCE MUCH OF INVESTMENTS IN EARTHQUAKE PREPAREDNESS AND AVAILABLE FUNDS FOR QUICK RESPONSE IS RELATED TO HOUSEHOLD INCOME, THE GDP PER CAPITA CAN BE USED AS A ROUGH INDICATOR OF RESILIENCE. ISLAMIC REPUBLIC OF IRAN HAS A GDP PER CAPITA OF 1587 PPP$ (PARITY PURCHASING POWER DOLLAR, ABOUT 1 EURO) AND IS THEREFORE PART OF THE LOW LEVEL INCOME COUNTRIES. THEREFORE, THE EARTHQUAKE HAPPENED IN AN AREA OF LOW RESILIENCE. BASED ON THE COMBINATION OF 9 INDICATORS, ECHO ATTRIBUTES ISLAMIC REPUBLIC OF IRAN A LOW VULNERABILITY. ============================================================================================================ SECONDARY EFFECTS ----------------- PROBABILITY OF SECONDARY EFFECTS: - LANDSLIDES: THE MAXIMUM SLOPE IN THE AREA OF THE EARTHQUAKE IS N/A% AND THE MAXIMUM ALTITUDE IS N/A M. SINCE THIS IS A LOW SLOPE, THE RISK OF EARTHQUAKE INDUCED LANDSLIDES IS LOW. NOTE, HOWEVER, THAT THE SLOPE DATA IS NOT RELIABLE ON A LOCAL SCALE, WHILE LANDSLIDES DEPEND VERY MUCH ON LOCAL TOPOGRAPHY, SOIL AND METEOROLOGICAL CONDITIONS. - NUCLEAR POWER PLANTS: THERE ARE NO NUCLEAR FACILITIES NEARBY THE EPICENTER. - HYDRODAMS: THERE ARE NO HYDRODAM FACILITIES NEARBY THE EPICENTER. JOINT RESEARCH CENTRE, EUROPEAN COMMISSION (JRC-EC) - OFFICE FOR COORDINATION OF HUMANITARIAN AFFAIRS (UN-OCHA) ________________________________________ DISCLAIMER WHILE WE TRY EVERYTHING TO ENSURE ACCURACY, THIS INFORMATION IS PURELY INDICATIVE AND SHOULD NOT BE USED FOR ANY DECISION MAKING WITHOUT ALTERNATE SOURCES OF INFORMATION. THE JRC IS NOT RESPONSIBLE FOR ANY DAMAGE OR LOSS RESULTING FROM THE USE OF THE INFORMATION PRESENTED ON GDACS WEBSITE. PLEASE REFER TO THE GDACS WEBSITE FOR SUBSCRIBING OR UNSUBSCRIBING FROM THE EARTHQUAKE ALERT EMAIL OR SMS SERVICE. END OF EARTHQUAKE MESSAGE 001