1 1 10 MOIST 2026-04-07T09:38:05+00:00 0.058 sec MOIST Multidisciplinary Oceanic Information SysTem (MOIST) MOIST has been the contribution of INGV to the data dissemination within the ESONET NoE EC project (2007-2011) and is the web interface for the management of the seafloor marine multidiscinary data and metadata related to GEOSTAR-type observatories used in the ESONET Demonstration Mission. MOIST also include the seafloor data acquired by the observatories by INGV from 1998. MOIST allows the access through the following selection criteria: site; time interval; instrument / sensor / parameter; project / campaign. The web interface allows the submissions of queries for data download. MOIST intends to host all the data and metadata coming from EMSO ESFRI and hopefully all collaborating projects. Current areas with data: East Sicily, East Sicily, Greek, Gulf of Cadiz, Marmara Sea, Marsili Basin, Weddell Sea. POLYGON((-9.518245 -69.404917,-9.518245 40.729087,29.398833 40.729087,29.398833 -69.404917,-9.518245 -69.404917)) marine metadata 1 Creative Commons Attribution 4.0 International License (CC BY 4.0) 2026-04-07T09:38:05+00:00 2026-04-07T09:38:05+00:00 EPSG:4326 2002-10-09T00:00:00+00:00 2026-04-07T09:38:05+00:00 moist..testsite.emso-miur.2019.nemo-sn1.vector_magnetometer.72 TestSite: SN1 2020 - Vector Magnetometer Platform or instrument orientation 2019-10-12T00:00:00+00:00/ This sensor provides the three components of the magnetic induction vector in the directions N-S, E-W and Z (vertical). It is a fluxgate prototype developed at INGV laboratories equipped with an inertial platform for levelling control. It provides continuous seafloor magnetic data which are important for two main reasons: a) they extend the magnetic observations from land to the seafloor, improving the spatial distribution in the Italian territory; b) these data are important for the study of short and long magnetic field time variations. The variational data allow us to estimate the resistivity structure underneath the area of observations and possibly to detect some magnetic variations related to some geo-hazards, such as earthquakes and tsunamis. The main aim is the continuous and almost real-time measurement of the three components of the Earth?s magnetic field in a very peculiar environment which in fact has a favorable impact on the quality of the measurements: first, the temperature is more stable at the sea bottom, especially in deep sea sites, so the instrumental drift due to temperature variations is absent or negligible. Second, the water column acts as a natural "shield" to the highest frequencies of the iono- and magnetosphere inducing fields. Public POINT(15.397500 37.547650) 2019-10-12T00:00:00+00:00