TORONTO, June 07, 2022 Labrador Gold Corp. is pleased to announce results from seven drill holes, including the first hole drilled at the Golden Glove Target in the south end of its 100% owned. | June 7, 2022
Fuelled by psychedelic counterculture, the Californian university has nurtured Steve Reich, Laurie Anderson and more – and caused riots at its concerts. But can it survive?
The Mills College Music Department and Center for Contemporary Music presents Music in the Fault Zone: Experimental Music at Mills College (1939 to the present) a four-day festival, April 21–24, 2022, celebrating its extraordinary musical legacy. It brings together musical luminaries from Mills’s past, present, and future during four days of concerts featuring music by Darius Milhaud, Lou Harrison, John Cage, Anthony Braxton, Robert Ashley, Terry Riley, Steed Cowart, and Henry Cowell.
The Mills College Music Department and Center for Contemporary Music presents Music in the Fault Zone: Experimental Music at Mills College (1939 to the present) a four-day festival, April 21–24, 2022, celebrating its extraordinary musical legacy. It brings together musical luminaries from Mills’s past, present, and future during four days of concerts featuring music by Darius Milhaud, Lou Harrison, John Cage, Anthony Braxton, Robert Ashley, Terry Riley, Steed Cowart, and Henry Cowell.
Upper-plate normal faults along forearcs often accumulate slip during > Mw 6 earthquakes. Such normal faults traverse the forearc of the Hellenic Subduction System (HSS) in Greece and are the focus of this study. Here, we use detailed field-mapping and analysis of high-resolution Digital Elevation Models (DEMs) to study 42 active normal faults on the islands of Kythira and Antikythira in the Aegean Sea. Onshore fault kinematic data are complemented by seabed bathymetry mapping of ten offshore faults that extend along the Kythira-Antikythira Strait (KAS). We find that normal faults in the KAS have lengths of ~1-58 km and scarps ranging in height from 1.5 m to 2.8 km, accommodating, during the Quaternary, trench-orthogonal (NE-SW) extension of ~2.46 ± 1.53 mm/a. Twenty-eight of these faults have ruptured since the Last Glacial Maximum, with their postglacial (16±2 ka) displacement rates (0.19-1.25 mm/a) exceeding their Quaternary (≤ 0.7-3 Ma) rates (0.03-0.37 mm/a) by more