﻿<?xml version="1.0" encoding="utf-8"?><rss xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:xsd="http://www.w3.org/2001/XMLSchema"><channel><totalitems>275</totalitems><casualities>22</casualities><lasthour>0</lasthour><title>GDACS EMM News Feed</title><description>
                                                        Europe Media Monitor (EMM) reads and analyses around 40.000 new news items per day from around 1000 sites worldwide. The text of the items, extracted using EMM's own text extraction algorithm, is indexed using Lucene (see http://lucene.apache.org). Please make sure your area of interest is not already covered by one of the pre-defined categories (alerts). If it is, we kindly ask you to use the feed from that category as this significantly reduces the load on our system. This site is a joint project of DG-JRC and DG-COMM. The information on this site is subject to a disclaimer (see http://europa.eu/geninfo/legal_notices_en.htm). Please acknowledge EMM when (re)using this material
                                                    </description><item><title>Long-lived shallow slow-slip events on the Sunda megathrust</title><link>https://www.nature.com/articles/s41561-021-00727-y</link><description>During most of the time between large earthquakes at tectonic plate boundaries, surface displacement time series are generally observed to be linear. This linear trend is interpreted as a result of steady stress accumulation at frictionally locked asperities on the fault interface.</description><pubDate>Mon, 03 May 2021 18:46:00 +0200</pubDate><guid>nature-ngeo-80355d01587efcf4cad249bf2ad0a277</guid><sortelement xmlns="emm">20210503184600</sortelement></item><item><title>Long-lived shallow slow-slip events on the Sunda megathrust</title><link>https://www.nature.com/articles/s41561-021-00727-y</link><description>During most of the time between large earthquakes at tectonic plate boundaries, surface displacement time series are generally observed to be linear. This linear trend is interpreted as a result of steady stress accumulation at frictionally locked asperities on the fault interface.</description><pubDate>Mon, 03 May 2021 17:28:00 +0200</pubDate><guid>nature-Earth-and-Environmental-Sciences-2fc7e45cad594c3b65e91146cd21940d</guid><sortelement xmlns="emm">20210503172800</sortelement></item><item><title>Magnitude 4.5 earthquake strikes near Palu, Central Sulawesi, Indonesia</title><link>https://www.volcanodiscovery.com/earthquake/news/129067/Magnitude-45-earthquake-strikes-near-Palu-Central-Sulawesi-Indonesia.html</link><description>The United States Geological Survey reported a magnitude 3.4 quake in the United States near Carlsbad, Eddy County, New Mexico, only 16 minutes ago. The earthquake hit early morning on Monday 3 May 2021 at 5:46 am local time at a very shallow depth of 3.1 miles.</description><pubDate>Mon, 03 May 2021 17:04:00 +0200</pubDate><guid>volcanodiscovery-e689805bb7fdcf9182e69c7122eec11d</guid><sortelement xmlns="emm">20210503170400</sortelement></item><item><title>Moderate mag. 4.5 earthquake - SULAWESI, INDONESIA, on Monday, 3 May 2021 at 14:40 (GMT)</title><link>https://www.volcanodiscovery.com/earthquakes/quake-info/6229904/mag4quake-May-3-2021-SULAWESI-INDONESIA.html</link><description>A magnitude 4.5 earthquake near Palu, Central Sulawesi, Indonesia, was reported only 17 minutes ago by Indonesia's Meteorology, Climatology, and Geophysical Agency, considered the main national agency that monitors seismic activity in Indonesia. The earthquake occurred at a shallow depth of 10 km....</description><pubDate>Mon, 03 May 2021 17:04:00 +0200</pubDate><guid>volcanodiscovery-0d43497a353b169c9b3c868e18ff46c8</guid><sortelement xmlns="emm">20210503170400</sortelement></item></channel></rss>