980 resultados para Lennep, Jakob van, 1802-1868


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"La 1re exécution de cette oeuvre a eu lieu ... à Gand, le 14 septembre 1863, jour de l'inauguration de la statue de Jacques van Artevelde."

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[v.19] 1657. Koning Davids Harpzangen.--[v.20] 1657-1660. Koning Davids Harpzangen. Jeptha.--[v.21] 1660. Koning Edipus. Koning David in ballingschap. Koning David herstelt.--[v.22-23] 1660. Publius Virgilius Maroos Wercken in Nederduitsch dicht vertaelt.--[v.24] 1660-1662. Samson. Adonias. Bespiegelingen.--[v.25] 1662. Bespiegelingen. Joannes de Boetgezant.--[v.26] 1663. Batavische Gebroeders. De Heerlyckheit der Kercke. Faëton.--[v.27] 1664-1667. Adam in Ballingschap. Ifigenie in Tauren. Zungchin.--[v.28] 1667-1671. Noah. Feniciaensche. Herkules in Trachin. Ovidius Herscheppinge.--[v.29-30] 1671-1679. Ovidius herscheppinge.

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Deel 1. Beschouwingen van den sterrenhemel geheel vernieuwd door F. Kaiser. Natuurk. beschrijving van onzen aardbol bewerkt door E.M. Beima.--Deel 2. Over de lucht en den dampkring geheel verniuwd door C.J. Matthes.--Deel. 3. Behelzende natuurlijke geschiedenis van het dierenrijk nieuw bewerkt door J. van der Hoeven.--Deel 4. Natuurlijk geschiedenis van het plantenrijk door H.C. van Hall.--Deel 5. Over de delfstoffen en de geschiedenis der aarde door F.A.W. Miquel.

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Vit het Tijdschrift voor Nat. gesch. en physiol. VIIIste deel ...

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Translated from the 2d Dutch ed. by Rev. William Clark.

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Coastal subsidence causes sea-level rise, shoreline erosion and wetland loss, which poses a threat to coastal populations. This is especially evident in the Mississippi Delta in the southern United States, which was devastated by Hurricane Katrina in 2005. The loss of protective wetlands is considered a critical factor in the extensive flood damage. The causes of subsidence in coastal Louisiana, attributed to factors as diverse as shallow compaction and deep crustal processes, remain controversial. Current estimates of subsidence rates vary by several orders of magnitude. Here, we use a series of radiocarbon-dated sediment cores from the Mississippi Delta to analyse late Holocene deposits and assess compaction rates. We find that millennial-scale compaction rates primarily associated with peat can reach 5mm per year, values that exceed recent model predictions. Locally and on timescales of decades to centuries, rates are likely to be 10 mm or more per year. We conclude that compaction of Holocene strata contributes significantly to the exceptionally high rates of relative sea-level rise and coastal wetland loss in the Mississippi Delta, and is likely to cause subsidence in other organic-rich and often densely populated coastal plains.