Early human settlements in Northern Africa: paleomagnetic evidence from the Ain Hanech Formation (northeastern Algeria)

2014 ◽  
Vol 99 ◽  
pp. 203-209 ◽  
Author(s):  
J.M. Parés ◽  
M. Sahnouni ◽  
J. Van der Made ◽  
A. Pérez-González ◽  
Z. Harichane ◽  
...  
1974 ◽  
Vol 111 (2) ◽  
pp. 149-155 ◽  
Author(s):  
D. Vass ◽  
G. P. Badgasarjan ◽  
S. Bajanik

SummaryFour volcanic rocks from northern Tunisia and a syntectonic granite from northeastern Algeria were dated by the K—Ar method. The stratigraphic position of the dated rocks is determined mainly by their relationship to biostratigraphically calibrated Miocene tectonism. The K—Ar age of the granite, which is younger than latest Burdigalian and older than Early Tortonian, is 16.8 m.y. (*15.8 m.y. calculated with western decay constants). Rhyodacite at 10.9 (*10.4), rhyolite at 8.8 (*8.3), basalt at 7.3 (*6.9) and adesite at 7.0 (*6.7) m.y. are all apparently younger than Lower Tortonian.


2013 ◽  
Vol 303 ◽  
pp. 93-106 ◽  
Author(s):  
A. Amorosi ◽  
M. Bini ◽  
S. Giacomelli ◽  
M. Pappalardo ◽  
C. Ribecai ◽  
...  

Radiocarbon ◽  
2007 ◽  
Vol 49 (2) ◽  
pp. 527-542 ◽  
Author(s):  
P M Dolukhanov ◽  
A M Shukurov ◽  
Kh A Arslanov ◽  
D A Subetto ◽  
G I Zaitseva ◽  
...  

Newly obtained radiocarbon measurements are used to suggest that the initial settlement of the northeastern Baltic area was largely controlled by the Ladoga-Baltic waterway in the north of the Karelian Isthmus, which emerged ∼11,500 cal BP and remained in action for ∼7000 yr. The transgression of Ladoga Lake started ∼5000 cal BP and reached its maximum at ∼3000 cal BP (∼1100–1000 cal BC). The formation of a new outlet via the Neva River led to a rapid regression of the lake that stimulated the spread of farming populations.


Author(s):  
Thomas S. Bianchi

Humans have had a long relationship with the ebb and flow of tides on river deltas around the world. The fertile soils of river deltas provided early human civilizations with a means of farming crops and obtaining seafood from the highly productive marshes and shallow coastal waters associated with deltas. However, this relationship has at times been both nurturing and tumultuous for the development of early civilizations. The vicissitudes of seasonal changes in river flooding events as well as frequently shifting deltaic soils made life for these early human settlements challenging. These natural transient processes that affect the supply of sediments to deltas today are in many ways very similar to what they have been over the millennia of human settlements. But something else has been altered in the natural rhythm of these cycles. The massive expansion of human populations around the world in both the lower and upper drainage basins of these large rivers have changed the manner in which sediments and water are delivered to deltas. Because of the high density of human populations found in these regions, humans have developed elaborate hydrological engineering schemes in an attempt to "tame" these deltas. The goal of this book is to provide information on the historical relationship between humans and deltas that will hopefully encourage immediate preparation for coastal management plans in response to the impending inundation of major cities, as a result of global change around the world.


2016 ◽  
Vol 416 ◽  
pp. 5-11 ◽  
Author(s):  
C. Falguères ◽  
F. Sémah ◽  
H. Saleki ◽  
S. Hameau ◽  
H. Tu ◽  
...  

2017 ◽  
Vol 164 ◽  
pp. 168-186 ◽  
Author(s):  
Xuefeng Sun ◽  
Huayu Lu ◽  
Shejiang Wang ◽  
Liang Yi ◽  
Yongxiang Li ◽  
...  

1988 ◽  
Vol 42 (3) ◽  
pp. 519-520
Author(s):  
Maurice Kirk
Keyword(s):  

2007 ◽  
Vol 109 (1) ◽  
pp. 202-204
Author(s):  
EDWARD SWENSON
Keyword(s):  

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