Quaternary geology of the upper sabinal River Valley, Uvalde and Bandera counties, Texas

1995 ◽  
Vol 10 (6) ◽  
pp. 457-480 ◽  
Author(s):  
Charles E. Mear
Keyword(s):  
River Valley ◽  
Quaternary Geology

Testing the perspectives for discovery of the Paleolithic sites in the northern portion of the Ob river valley: Quaternary geology, paleogeography, and geomorphology

2019 ◽  
Vol 17 ◽  
pp. 109-116
Author(s):  
Ivan D. Zolnikov ◽  
Anton V. Vybornov ◽  
Alexander V. Postnov ◽  
Andrey G. Rybalko ◽  
Andrei A. Kartoziia
Keyword(s):  
River Valley ◽  
Quaternary Geology ◽  
Ob River ◽  
Northern Portion

scholarly journals The Initial Period of the Investigation of the Relief and Landscape of the Oka River Valley (the 19th Century — the 1940s)

2021 ◽  
pp. 130-139
Author(s):  
А.Ю. Воробьев
Keyword(s):  
19Th Century ◽  
Initial Period ◽  
River Valley ◽  
Quaternary Geology ◽  
Moscow Region ◽  
The South ◽  
River Terraces ◽  
Vladimir Region ◽  
The 19Th Century

Рассматриваются изданные с середины XIX века до 1940-х годов работы, посвященные физико-географическим исследованиям в пределах долины средней Оки в Рязанской области, юго-востока Московской области и юга Владимирской области. Отмечен повышенный интерес к вопросам четвертичной геологии и распределения высот в террасовом комплексе долины. Выделены достижения в области разработки вопросов типизации археологических памятников и геоморфологического районирования. Обозначены тенденции, существовавшие в распределении акцентов в физико-географических исследованиях региона за период с середины XIX века по 40-е годы ХХ столетия. Определены главные методологические черты исследовательской работы, осуществлявшейся ведущими и региональными научными физико-географическими школами в обозначенный период и предметом которой были современное состояние долинных геокомплексов средней Оки и их облик в древности. The article treats research works published in the period between the mid 19th century and the 1940s and devoted to the investigation of the Oka river valley in the Ryazan region, the southeast of the Moscow region and the south of the Vladimir region. The article underlines that the issues of quaternary geology and architecture of river terraces have been investigated by many researchers. The article analyzes works devoted to the classification of archeological and geomorphological structures. It investigates tendencies associated with geographic research of the region during the mid 19th century – the 1940s. It identifies major methodological characteristics of the research of the architecture of the Oka river valley performed by leading and local geographic societies.

scholarly journals Quaternary geology, geomorphology and tectonics in the Ogosta river valley system, the Danubian plain (Bulgaria)

2001 ◽  
Vol 34 (1) ◽  
pp. 55 ◽  
Author(s):  
D. ANGELOVA
Keyword(s):  
River Valley ◽  
Quaternary Geology ◽  
Iron Hydroxides ◽  
Quaternary Sediments ◽  
Local Data ◽  
Genetic Types ◽  
Quaternary Base

The Quaternary in the Ogosta River valley system (the Danubian plain) is represented by various genetic types of continental Quaternary sediments (eolian, alluvial, deluvial, proluvial). They lie on a diverse pre-Quaternary base. It is uneven and with various denudation. The accepted correlation schemes are based on local data in which the tectonic factor and duration of deformation have not been accounted for. The present work considers the complex results obtained during the investigation of the Quaternary sediments and formations. The filling consists of clayey-sandy or calcareous-sandy materials, coloured in rusty nuances by iron hydroxides. Their age has been determined on the basis of the found fauna: Elephas meridionalis Nesti,Anancus arvernensis Cr. et Gob (Bakalov, Nikolov, 1962).

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