The Democratic Republic of the Congo

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The Democratic Republic of the Congo 29°10'E 29°11'E 29°12'E 29°13'E 29°14'E 29°15'E 29°16'E 29°17'E 29°18'E THE DEMOCRATIC REPUBLIC OF THE CONGO 1°30'S 1°30'S GOMA CITY, NYIRAGONGO DISTRICT, NORD-KIVU PROVINCE IMAGERY ANALYSIS: 24 MAY 2021 PUBLISHED 25 MAY 2021 V1 VOLCANO POTENTIALLY STRUCTURES VO20210523COD DAMAGED WITHIN THE LAVA FLOW 1°31'S 1,600 1°31'S Mount Nyiragongo 1°32'S 1°32'S 700 m to the airport facilities DR CONGO 1.3 km to Earthstar Geographics, Maxar 1°33'S the runway 1°33'S Lava flow and affected structures caused by 5 k m Nyiragongo volcanic rad Goma ius eruption, Nord-Kivu zone Airport Province, DR Congo 1°34'S This map illustrates potentially Kibati 1°34'S affected structures and buildings in Nyiragongo district, Nord-Kivu province, DR Congo as detected by satellite image acquired after the eruption of Mount Nyiragongo ≈ 40,000 volcano on 22 May 2021. UNITAR- UNOSAT analysis used a TerraSAR- 1°35'S X image acquired on 24 May 2021, 1°35'S ≈ 4,000 at 16:13 UTC, to observe the lava Kanyanza flow. Within the analysis extent, about 1,600 structures are potentially affected by the lava flow. This is a preliminary analysis and 10 has not yet been validated in the k m field. Please send ground feedback 1°36'S r ad 1°36'S ius to UNITAR-UNOSAT. zone Important Note: Lava flow analysis from radar images may overestimate the presence of the lava tract due to the backscattering properties of the ≈ 521,000 radar signal. 1°37'S 1°37'S ≈ 80,000 Legend City Village ĝÆ Hospital Airport 1°38'S 1°38'S International Boundary 15 km City Boundary ra dius zone Primary Road ĝÆ Buzove Radius Zone see inset for close-up view Maximum lava extent 1°39'S as of 24 May 21 1°39'S ĝÆ Goma 1°40'S 1°40'S Æ ≈ 715,000 ĝ ĝÆ ĝÆ ≈ 200,000 RWANDA 20 1°41'S km 1°41'S r adi Kabinzi us z one Rugerero Gisenyi 1°42'S Nyamyumba1°42'S Spatial Reference Satellite Data (Post): TerraSAR-X Boundary data : OCHA Congo Analysis : UNITAR-UNOSAT Map Scale for A3: 1:60,000 Name: WGS 1984 UTM Zone 35S Imagery Dates: 24 May 2021 City Boundary: Wikimapia Production : UNITAR-UNOSAT PCS: WGS 1984 UTM Zone 35S Resolution: 3 m Population data : WorldPop and HRSL 0 0.5 1 2 KM GCS: GCS WGS 1984 Copyright: TerraSAR-X © DLR e.V. (2021), Buildings : OpenStreetMap Datum: WGS 1984 Pfunda Distribution Airbus DS Geo GmgH Other analysis: USGS ¯ Projection: Transverse Mercator Source: DLR Background ESRI World Imagery 29°10'E 29°11'E 29°12'E 29°13'E 29°14'E 29°15'E 29°16'E 29°17'E 29°18'E 29°19'E UNITAR - UNOSAT -7 bis Avenue de la Paix, CH-1202 Geneva 2, Switzerland - T: +41 22 917 4720 (UNOSAT Operations) - Hotline 24/7 : +41 75 411 4998 - [email protected] - www.unitar.org/unosat.
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  • Human Health and Vulnerability in the Nyiragongo Volcano Crisis Democratic Republic of Congo 2002
    Human Health and Vulnerability in the Nyiragongo Volcano Crisis Democratic Republic of Congo 2002 Final Report to the World Health Organisation Dr Peter J Baxter University of Cambridge Addenbrooke’s Hospital Cambridge, UK Dr Anne Ancia Emergency Co-ordinator World Health Organisation Goma Nyiragongo Volcano with Goma on the shore of Lake Kivu Cover : The main lava flow which shattered Goma and flowed into Lake Kivu Lava flows from the two active volcanoes CONGO RWANDA Sake Munigi Goma Lake Kivu Gisenyi Fig.1. Goma setting and map of area and lava flows HUMAN HEALTH AND VULNERABILITY IN THE NYIRAGONGO VOLCANO CRISIS DEMOCRATIC REPUBLIC OF CONGO, 2002 FINAL REPORT TO THE WORLD HEALTH ORGANISATION Dr Peter J Baxter University of Cambridge Addenbrooke’s Hospital Cambridge, UK Dr Anne Ancia Emergency Co-ordinator World Health Organisation Goma June 2002 1 EXECUTIVE SUMMARY We have undertaken a vulnerability assessment of the Nyiragongo volcano crisis at Goma for the World Health Organisation (WHO), based on an analysis of the impact of the eruption on January 17/18, 2002. According to volcanologists, this eruption was triggered by tectonic spreading of the Kivu rift causing the ground to fracture and allow lava to flow from ground fissures out of the crater lava lake and possibly from a deeper conduit nearer Goma. At the time of writing, scientists are concerned that the continuing high level of seismic activity indi- cates that the tectonic rifting may be gradually continuing. Scientists agree that volcano monitoring and contingency planning are essential for forecasting and responding to fu- ture trends. The relatively small loss of life in the January 2002 eruption (less than 100 deaths in a population of 500,000) was remarkable, and psychological stress was reportedly the main health consequence in the aftermath of the eruption.
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  • Democratic Republic of the Congo | Mount Nyiragongo Eruption
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  • Recent Activity at Nyiragongo and Lava-Lake Occurrences
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  • The Tragedy of Goma Most Spectacular Manifestation of This Process Is Africa’S Lori Dengler/For the Times-Standard Great Rift Valley
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