A Deep-Water Glauconitization Process on the Ivory Coast-Ghana Marginal Ridge (ODP Site 959): Determination of Fe3+-Rich Montmorillonite in Green Grains

2001 ◽  
Vol 49 (6) ◽  
pp. 540-558 ◽  
Author(s):  
A. Wiewióra
Keyword(s):  
2008 ◽  
Vol 109 (1) ◽  
pp. 81-87 ◽  
Author(s):  
Asli Cadun ◽  
Duygu Kışla ◽  
Şükran Çaklı

Author(s):  
Maria Rucińska-Zjadacz ◽  
Stanisław Rudowski

AbstractThe Hel Peninsula is a 35 km long spit that extends into water depths of almost 60 m. Unlike most sandy barriers, the distal end of the Hel Peninsula is prograding into the deep water. This affects unique conditions for the evolution of this section of the Peninsula. The aim of this study is to determine the morpholithodynamic changes on the tip of the Hel Peninsula. Shore studies were performed in 2006-2008 and 2012. Measurements included: beach profiling, determination of shoreline and dune base line positions, and collection of sediment samples. The different nature of the eastern, central and western part of the Hel tip is evident. The eastern part is accumulative, the central part is variable with the general nature of strong and differently directed redeposition and accumulative periods, while the western part is highly erosive.


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