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Source: The Open Library
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1E&G – Quaternary Science Journal Vol. 58 No 2
By DEUQUA

“E&G – Quaternary Science Journal Vol. 58 No 2” Metadata:
- Title: ➤ E&G – Quaternary Science Journal Vol. 58 No 2
- Author: DEUQUA
- Publisher: Geozon Science Media
- Publish Date: 2010
“E&G – Quaternary Science Journal Vol. 58 No 2” Subjects and Themes:
- Subjects: ➤ Carpathian Basin - Pomerania - Coast - Evolution - Holocene - Geology - Niederösterreich - Vegetation History - production of neolithic ceramic - Lengyel Culture - Lower Austria - Loess - Paleosol - Micromorphology - Amphibolite - Langenlois - Quaternary - Palaeosols - Biomarkers - Alkanes - Palaeovegetation - aeolian sands - Finow Soil - fossil soils - Late Glacial - Holocene dune formation - Geschiebedecksand (GDS) - Baltic Sea - Rügen - sea-level rise - coastal evolution - barrier - lagoon - vienna - Wien - environment - Umwelt
Edition Identifiers:
- The Open Library ID: OL24335319M
Access and General Info:
- First Year Published: 2010
- Is Full Text Available: No
- Is The Book Public: No
- Access Status: No_ebook
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Wiki
Source: Wikipedia
Wikipedia Results
Search Results from Wikipedia
Aeolian harp
An Aeolian harp (also wind harp) is a musical instrument that is played by the wind. Named after Aeolus, the ancient Greek god of the wind, the traditional
Wadi Rum
Sandstone, separated by flat-bottom valleys of alluvial sediments, aeolian sands, and salt pans. The Umm Ishrin is the thickest formation in the Lower
Soil conditioner
application is limited by the soil conditions and whilst ideal in the aeolian sands, it may not be appropriate in the fluvial deposits which are richer
The Pinnacles (Western Australia)
in quantities greater than that needed for plant growth. In coastal aeolian sands that consist of large amounts of calcium (derived from marine shells)
Deriba (caldera)
are in part covered by the Nubian Sandstones of Cretaceous age and aeolian sands, and by the Jebel Marra massif which occupies a surface of 13,000 square
Bayonne
the sub-soil of Bayonne beneath the surface accumulations of silt and aeolian sands. The drainage network of the western Pre-Pyrenees evolved mostly from
Hunter Region
Woodland Lower Hunter Valley Dry Rainforest Warkworth Sands Woodland. This EEC occurs on aeolian sands, south east of Singleton (but may occur elsewhere in
Hinchinbrook Island
200 metres (330 to 660 feet). The barrier, which consists mainly of aeolian sands, extends more than 30 metres (98 feet) below the present sea level in
Booti Booti National Park
southern end. The three areas are connected by low–lying estuarine and aeolian sands. The stretch of land between Cape Hawke and Booti Hill is around 10
Madhurawada
sediments, and their cultural remains were subsequently covered by the aeolian sands as revealed by studies at Ramayogi Agraharam, Paradesipalem, Madhurawada