FREE BOOKS

Author's List




PREV.   NEXT  
|<   283   284   285   286   287   288   289   290   291   292   293   294   295   296   297   298   299   300   301   302   303   304   305   306   307  
308   309   310   311   312   313   314   315   316   317   318   319   320   321   322   323   324   325   326   327   328   329   330   331   332   >>   >|  
vered and exposed to the action of the atmosphere, while farther down it may yield very good coal. It is probable besides that the layers of shale, which often surround the coal seams, have in this case been mistaken for the true coal. For those who are inexperienced in coal-mining to make such a mistake is the rule and not the exception. ] [Footnote 209: In order not to write without due examination about figures which have been written about a thousand times before, I have, with the help of Petermann's map of North and Middle Asia in Stieler's Hand-Atlas, calculated the extent of the areas of the Siberian rivers, and found them to be:-- Square Geographical kilometres. square miles. River area of the Ob (with the Tas) 3,445,000 62,560 River area of the Yenisej 2,712,000 49,250 River area of the Lena 2,395,000 43,500 Of these areas 4,966,000 square kilometres, or about 90,000 geographical square miles, lie south of 60 deg. N.L. ] [Footnote 210: For the northern hemisphere it is the general rule that where rivers flow through loose, earthy strata in a direction deviating considerably from that of the parallels of latitude, the right bank, when one stands facing the mouth of the river, is high, and the left low. The cause of this is the globular form of the earth and its rotation, which gives rivers flowing north a tendency towards the east, and to rivers flowing south a tendency to the west This tendency is resisted by the bank, but it is gradually eaten into and washed away by degrees, so that the river bed, in the course of thousands of years, is shifted in the direction indicated. ] [Footnote 211: As specimens of the sub-fossil mollusc fauna of the _tundra_ some of the common species are delineated on the opposite page. These are:--1. _Mya arenaria_, Lin. 2/3 of natural size. 2. _Mya truncata_, Lin. var. _Uddevallensis_, Forbes. 2/3 3. _Saxicava pholadis_, Lin. 2/3. 4. _Tellina lata_, Gmel. 2/3 5. _Cardium ciliatum_, Fabr. 2/3. 6. _Leda pernula_, Muell. var. _buccata_, Steenstr. Natural size. 7. _Nucula expansa_, Reeve. Nat. size. 8. _Fusus Kroyeri_, Moell. 2/3. 9. _Fusus fornicatus_, Reeve. 1/2. 10. _Fusus tornatus_, Gould. 2/3. 11. _Margarita elegantissima_, Bean. Natural size. 12. _Pleurotoma plicifera_, Wood. Natural size. 13. _Pleurotoma pyramidalis_, Stroem. 1-1/2. 14. _Trichotropis
PREV.   NEXT  
|<   283   284   285   286   287   288   289   290   291   292   293   294   295   296   297   298   299   300   301   302   303   304   305   306   307  
308   309   310   311   312   313   314   315   316   317   318   319   320   321   322   323   324   325   326   327   328   329   330   331   332   >>   >|  



Top keywords:

rivers

 

square

 
Footnote
 

tendency

 
Natural
 

direction

 

Pleurotoma

 
flowing
 

kilometres

 

specimens


globular

 

mollusc

 

tundra

 
fossil
 

resisted

 

gradually

 
rotation
 

thousands

 

shifted

 

washed


degrees
 

truncata

 
fornicatus
 
tornatus
 

Kroyeri

 
Steenstr
 

Nucula

 

expansa

 

pyramidalis

 

Stroem


Trichotropis

 

plicifera

 

Margarita

 
elegantissima
 

buccata

 

arenaria

 

natural

 

Uddevallensis

 

opposite

 

common


species

 

delineated

 
Forbes
 

Saxicava

 

ciliatum

 

pernula

 

Cardium

 

pholadis

 

Tellina

 
hemisphere