FREE BOOKS

Author's List




PREV.   NEXT  
|<   67   68   69   70   71   72   73   74   75   76   77   78   79   80   81   82   83   84   85   86   87   88   89   90   91  
92   93   94   95   96   97   98   99   100   101   102   103   104   105   106   107   108   109   110   111   112   113   114   115   116   >>   >|  
tany, as indicated in the table, also in Normandy and Maine; in the Boulonnais district only the middle and upper divisions are known. In south France in the neighbourhood of Cabrieres, about Montpellier and in the Montagne Noire, all three divisions are found in a highly calcareous condition. Devonian rocks are recognized, though frequently much metamorphosed, on both the northern and southern flanks of the Pyrenees; while on the Spanish peninsula they are extensively developed. In Asturias they are no less than 3280 ft. thick, all three divisions and most of the central European subdivisions are present. In general, the Lower Devonian fossils of Spain bear a marked resemblance to those of Brittany. _Asia._--From the Ural Mountains eastward, Devonian rocks have been traced from point to point right across Asia. In the Altai Mountains they are represented by limestones of Coblentzien age with a fauna possessing Hercynian features. The same features are observed in the Devonian of the Kougnetsk basin, and in Turkestan. Well-developed quartzites with slates and diabases are found south of Yarkand and Khotan. Middle and Upper Devonian strata are widespread in China. Upper Devonian rocks are recorded from Persia, and from the Hindu Kush on the right bank of the Chitral river. _England._--In England the original Devonian rocks are developed in Devon and Cornwall and west Somerset. In north Devonshire these rocks consist of sandstones, grits and slates, while in south Devon there are, in addition, thick beds of massive limestone, and intercalations of lavas and tuffs. The interpretation of the stratigraphy in this region is a difficult matter, partly on account of the absence of good exposures with fossils, and partly through the disturbed condition of the rocks. The system has been subdivided as shown in Table III. TABLE III. +-----------------------------+-------------------------------+ | North Devon and West | | | Somerset. | South Devon. | +-----------------------------+-------------------------------+ / | Pilton group. Grits, slates | Ashburton slates. | U | | and thin limestones. | Livaton slates. | P | | Baggy group. Sandstones | Red and green Entomis slates
PREV.   NEXT  
|<   67   68   69   70   71   72   73   74   75   76   77   78   79   80   81   82   83   84   85   86   87   88   89   90   91  
92   93   94   95   96   97   98   99   100   101   102   103   104   105   106   107   108   109   110   111   112   113   114   115   116   >>   >|  



Top keywords:

Devonian

 

slates

 

developed

 

divisions

 

condition

 

limestones

 

Somerset

 

England

 

partly

 
fossils

Mountains
 

features

 

original

 
consist
 

Devonshire

 

Cornwall

 
Sandstones
 

Middle

 
strata
 

widespread


Khotan
 

Yarkand

 

Entomis

 

diabases

 

sandstones

 

Chitral

 

recorded

 

Persia

 

limestone

 

Livaton


subdivided

 

system

 

exposures

 
disturbed
 

Pilton

 

Ashburton

 

interpretation

 
intercalations
 

massive

 
addition

stratigraphy
 
matter
 

account

 

absence

 

difficult

 

region

 

quartzites

 

frequently

 
metamorphosed
 

recognized