Channel-levee evolution in combined contour current-turbidity current flows from flume tank experiments: REPLY
Channel-levee evolution in combined contour current–turbidity current flows from flume-tank experiments: COMMENT
Late Ordovician mass extinction caused by volcanism, warming, and anoxia, not cooling and glaciation
Persistence of Grenvillian dominance in Laurentian detrital zircon age systematics explained by sedimentary recycling: Evidence from detrital zircon double dating and detrital monazite te...
A sub-centennial-scale optically stimulated luminescence chronostratigraphy and late Holocene flood history from a temperate river confluence
Late Ordovician mass extinction caused by volcanism, warming, and anoxia, not cooling and glaciation: COMMENT
Late Ordovician mass extinction caused by volcanism, warming, and anoxia, not cooling and glaciation: REPLY
COVER: A tsunami hit the coastline of Tanzania 1000 yr ago, destroying an ancient Swahili fishing village whose ruins were found close to the modern town of Pangani. The human skull in the image, one of many remains found at the site, testifies to the unexpected destruction that occurred during the tsunami. These remains represent the oldest tsunami victims thus far found in East Africa. See “A 1000-yr-old tsunami in the Indian Ocean points to greater risk for East Africa” by Maselli et al., p. 808–812.
Photo by: Vittorio Maselli
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