Die Vektordaten / Geometrien enthalten Kitastandorte der Stadtgemeinden Bremen und Bremerhaven, sowohl öffentlicher wie auch privater Träger. In den Attributdaten sind Informationen zur Art der Einrichtung hinterlegt (wie z.B. Adressdaten, Betreuungs- bzw. Einrichtungsart, Trägern, ISCED-2011 Level, etc.).
Kindertageseinrichtungen - Kindergärten, Kinderkrippe, Hort - im Landkreis Diepholz ---- Den Downloadservice zu diesem Thema (shp, dxf, dwg) finden Sie unter DOWNLOAD-LINKS ----
INSPIRE-Datensatz zum Annex3-Thema Versorgungswirtschaft und staatliche Dienste für das Bundesland Sachsen-Anhalt. Der Datensatz wurde aus den Daten des Ministeriums für Arbeit, Soziales, Gesundheit und Gleichstellung (MS) sowie der Apothekerkammer Sachsen-Anhalt abgeleitet und INSPIRE-konform transformiert. Die Krankenhausstandorte entsprechen dem Krankenhausplan vom 01.12.2019. Die Daten der Standorte der Kindertageseinrichtungen sind vom September 2021. Die Apothekenstandorte der Apothekerkammer Sachsen-Anhalt haben den Stand 27.03.2025. Der Download der Krankenhausstandorte ist beschränkt. Für die vollumfängliche Nutzung dieses Downloaddienstes wenden Sie sich bitte an den Ansprechpartner. Der Download der Apothekenstandorte ist ebenfalls beschränkt. Für die vollumfängliche Nutzung dieses Downloaddienstes wenden Sie sich bitte an die Apothekerkammer Sachsen-Anhalt.
Der Dienst stellt für das INSPIRE-Thema Versorgungswirtschaft und staatliche Dienste aus den Daten des Ministeriums für Arbeit, Soziales, Gesundheit und Gleichstellung sowie der Apothekerkammer Sachsen-Anhalt (Krankenhausstandorte entsprechend Krankenhausplan und Kindertageseinrichtungsstandorte entsprechend Kifoeg.web sowie Apothekenstandorte) umgesetzte Daten bereit. Der Download der Krankenhausstandorte ist zugangsbeschränkt. Für die vollumfängliche Nutzung dieses Downloaddienstes wenden Sie sich bitte an den Ansprechpartner. Der Download der Apothekenstandorte ist ebenfalls beschränkt. Für die vollumfängliche Nutzung dieses Downloaddienstes wenden Sie sich bitte an die Apothekerkammer Sachsen-Anhalt.
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In January 2020, a swarm of earthquakes started under Thorbjorn volcano, Reykjanes, SW Iceland, associated to the uplift of up to 0.5 cm per day. Concern in Iceland was growing and the Iceland Meteorological Office suggested at that time that possibly magma intruded in the crust at shallow depth (3 to 9 km). The first eruption occurred on 19.03.2021, followed by many others in the foolwing years. The GFZ started a seismological Hazard and Risk Team (HART), as soon as February 2020 in cooperation with IMO, ISOR and the University of Iceland. The interrogator was located in Grindavik and was connected to a standard telecom cable. The full data dataset of this 5J network comprise 250 Tb of raw data. The standard infrastructure is not designed for such large data set. Therefore, we implement here several datasets, corresponding to several processing and associated publications. Specific full data set is available upon request to the authors. In Flovenz et al., 2022, the data subset comprise a selection of wave-forms recorded along an optical fibre of 21 km length. The subset consists of 40 channels at 100 Hz (spatially stacked 9x). The whole time period from January until August 2020 is covered, with a total size of 496 GB. The data is MiniSEED at 4096 bytes record length with STEIM2. In Maass et al., 2024, the data subset consists of two sections of contiguous channels (1701-2000 and 3921-4218, spatial sampling 4 meters) of dynamic strain rate down sampled at 5 Hz. The whole time period from January until August 2020 is covered, with a total size of 340 GB. The data is MiniSEED at 4096 bytes record length with STEIM2.
Following a sequence of seismic events detected by the National Geographic Institute (IGN Spain), on 13.09.2021 the new volcano Cumbre Vieja initiated an eruption, located on the mid-western flank at a location just to the north of the 1949 eruption site. The eruption fed a lava flow that buried already some hundreds of houses, with a high economic estimated loss. Previous studies have shown that La Palma was the source of 3 or 4 large sector collapses associated with avalanches under see and tsunami generation. This volcanic activity is accompanied with an increased seismic activity. The GFZ contributes to the monitoring of the seismic activity by sending experts in the frame of a Hazard and Risk Team (HART). Our partner is the National Geographic Institute. Besides tiltmeters, a temporary 4 station seismic network with TrilliumCompact 20 sec posthole seismometers, D-Cube digitisers (100 sample/sec) and C-Cubes LTE communication for real-time data transmission is being deployed near the Cumbre Vieja volcano, increasing the station density of the IGN network. Data access is being restricted for some time.
Standorte der Kindertagesstätten unterteilt in Krippen, Kindergärten, Horte Alterserweiterte Kindergärten und Kindertagespflege.
The Sarez Pamir aftershock seismic network was installed two months after the 7 December 2015, Mw7.2 Sarez Pamir earthquake in the eastern Pamir highland of Tajikistan. In the first recording period until September 2016, the stations were distributed along the Sarez-Karakul fault system. In September 2016 part of the stations were moved into the southern Pamir. In total the network consisted of eight stations on 13 sites, equipped with broad band, 3-component seismometers of type Trillium Compact. The data were recorded using Earth Data recorders (EDR), recording was continuous at a sample rate of 100Hz.The principal aim of the network was to record the aftershock sequence of the Sarez earthquake and to augment the coeval East Pamir China seismic network and the earlier TIPAGE and TIPTIMON seismic networks. Waveform data are available from the GEOFON data centre, under network code 9H.
Strong earthquakes cause transient perturbations of the near Earth’s surface system. These include the widespread landsliding and subsequent mass movement and the loading of rivers with sediments. In addition, rock mass is shattered during the event, forming cracks that affect rock strength and hydrological conductivity. Often overlooked in the immediate aftermath of an earthquake, these perturbations can represent a major part of the overall disaster with an impact that can last for years before restoring to background conditions. Thus, the relaxation phase is part of the seismically induced change by an earthquake and needs to be monitored in order to understand the full impact of earthquakes on the Earth system. Early June 2015, shortly after the April 2015 Mw7.9 Gorkha earthquake, we installed an array of 12 seismometers and geophones and 6 weather stations in the upper Bhotekoshi catchment, covering an area of ~50 km2. The seismic network was optimized for the monitoring of Earth surface processes (landsliding, mass wasting river processes, debris flows) and for the monitoring of properties of the shallow subsurface by coda analysis. To achieve the latter aim and to probe different scales and depths, seismometers were installed with inter-station distances from about 80m to 9km. In particular, in each of two locations close to the Bhotekoshi river, three seismometers were installed in small arrays with inter-station distances of about 100m. The seismic array is part of a wider data acquisition strategy including hydrometric measurements and high resolution optical (RapidEye) and radar imagery (TanDEM TerraSAR-X). Waveform data is available from the GEOFON data centre, under network code XN.
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