Figure 2
From: Continuous, semi-automatic monitoring of ground deformation using Sentinel-1 satellites
TS anomalies classified according to the driving force as at Update #19. Anomalies related to slope instabilities are widespread in most of the mountain areas of the region. Anomalies related to subsidence phenomena are identified in the alluvial plains, along with two uplifting areas within the province of Grosseto and Firenze. Anomalies linked to geothermal activities straddle the provinces of Pisa, Siena and Grosseto. TEA (Tuscan-Emilian Apennines); AA (Apuan Alps); SV (Serchio Valley); LAV (Lower Arno Valley); CH (Chianti Hills); CRV (Chiana River valley); AM (Amiata Mountain); CV (Cornia Valley); OV (Ombrone Valley). Maps were generated using ESRI ArcGIS 10.3 platform (https://www.esri.com/en-us/home).
