FREE BOOKS

Author's List




PREV.   NEXT  
|<   215   216   217   218   219   220   221   222   223   224   225   226   227   228   229   230   231   232   233   234   235   236   237   238   239  
240   241   242   243   244   245   246   247   248   249   250   251   252   253   254   255   256   257   258   259   260   261   262   263   264   >>   >|  
e needle is so mounted that it only moves freely in the horizontal plane, and therefore the horizontal component of the earth's force alone directs it. The direction assumed by the needle is not generally towards the geographical north, but diverges towards the east or west of it, making a horizontal angle with the true meridian, called the magnetic variation or declination; amongst mariners this angle is known as the variation of the compass. In the usual navigable waters of the world the variation alters from 30 deg. to the east to 45 deg. to the west of the geographical meridian, being westerly in the Atlantic and Indian oceans, easterly in the Pacific. The vertical plane passing through the longitudinal axis of such a needle is known as the magnetic meridian. Following the first chart of lines of equal variation compiled by Edmund Halley in 1700, charts of similar type have been published from time to time embodying recent observations and corrected for the secular change, thus providing seamen with values of the variation accurate to about 30' of arc. Possessing these data, it is easy to ascertain by observation the effects of the iron in a ship in disturbing the compass, and it will be found for the most part in every vessel that the needle is deflected from the magnetic meridian by a horizontal angle called the deviation of the compass; in some directions of the ship's head adding to the known variation of the place, in other directions subtracting from it. Local magnetic disturbance of the needle due to magnetic rocks is observed on land in all parts of the world, and in certain places extends to the land under the sea, affecting the compasses on board the ships passing over it. The general direction of these disturbances in the northern hemisphere is an attraction of the north-seeking end of the needle; in the southern hemisphere, its repulsion. The approaches to Cossack, North Australia; Cape St Francis, Labrador; the coasts of Madagascar and Iceland, are remarkable for such disturbance of the compass. [Illustration: FIG. 2.--Admiralty Compass (Frame and Needles).] [Illustration: FIG. 3.--Thomson's (Lord Kelvin's) Compass (Frame and Needles).] [Illustration: FIG. 4.--Section of Thomson's Compass Bowl. C, aluminium cap with sapphire centre; N, N', needles; P, pivot stem with pivot.] The compass as we know it is the result of the necessities of navigation, which have increased from century to century. It
PREV.   NEXT  
|<   215   216   217   218   219   220   221   222   223   224   225   226   227   228   229   230   231   232   233   234   235   236   237   238   239  
240   241   242   243   244   245   246   247   248   249   250   251   252   253   254   255   256   257   258   259   260   261   262   263   264   >>   >|  



Top keywords:

needle

 

variation

 
compass
 

magnetic

 

meridian

 
horizontal
 

Compass

 

Illustration

 

Thomson

 

called


Needles

 

directions

 
disturbance
 

passing

 
hemisphere
 
geographical
 
direction
 

century

 

compasses

 

affecting


extends

 

result

 
northern
 

disturbances

 

places

 

general

 
necessities
 

navigation

 

increased

 

adding


subtracting

 

observed

 

repulsion

 

needles

 

deviation

 

centre

 

Admiralty

 
remarkable
 

sapphire

 

Section


aluminium

 

Kelvin

 
Iceland
 
Madagascar
 

approaches

 

Cossack

 

southern

 
seeking
 

Australia

 

Labrador