,jasmin_name,name,ID,country,geodetic_measurements,deformation_observation,duration_of_observation,characteristics_of_deformation,latitude,longitude,measurement_methods,inferred_causes,references,Area,frames,Review needed,date_edited,owner_id,subset
0,hekla,Hekla,372070,Iceland,Yes,Yes,Continuous,"<p><span style=""color: #2e2e2e;"">Sturkell et al. (2013) studied Hekla&#8217;s last eruption in 2000 using </span>campaign GPS; an InSAR interferogram; dry tilt data, and borehole strain data. They found the presence of a dike that &#8220;causes surface fissuring extends no more than ~ 0.5 km in depth, and the reservoir depth is ~ 10 km. These are connected by a conduit of small lateral extent. Data for previous eruptions are consistent with this model&#8221;.<br />
There are numerous studies based on deformation datasets published on Hekla and yield estimated reservoir depths from<span style=""color: #2e2e2e;""> 5 to 10 km (Sturkell et al. 2013 and references therein). In general &#8220;Hekla shows a few long-term precursors to eruptions: optical tilt, GPS and InSAR give indications of upcoming eruptions&#8221; (Sturkell et al. 2013).</span><br />
&nbsp;</p>
",63.983000000000004,-19.666,"InSAR, GPS - continuous, GPS - campaign, Levelling, Strainmeter, Tiltmeter, EDM",Magmatic,"['Sturkell, E., K Ágústsson, A. T. Linde, S. I. Sacks, P. Einarsson, F. Sigmundsson, H. Geirsson, R. Pedersen, Peter C. LaFemina, H. Ólafsson, New insights into volcanic activity from strain and other deformation data for the Hekla 2000 eruption, JVGR, http://dx.doi.org/10.1016/j.jvolgeores.2013.02.001', 'Smithsonian Institution Global Volcanism Program<br />\nhttp://www.volcano.si.edu/volcano.cfm?vn=372070']",Iceland and Arctic Ocean,"{'region': 'iceland', 'frames': [{'id': '009D_02597_080910', 'track': '9'}, {'id': '016A_02562_091313', 'track': '16'}]}",,,,N