|  
 |  
 
 
 
| Below 500 ft., | 16 stations, | mean fall | 87  
inches. |   
 
| 500 to 1000 ft., | 10 |  | 79 |   
 
| 1000 to 1500  
ft., | 10 |  | 100 |   
 
| 1500 to 2000  
ft., | 4 |  | 92 |   
 
| 2000 to 2500  
ft., | no |  |  |   
 
| 2500 to 3000  
ft., | 2 |  | 75 |   
 
| 3000 to 3500  
ft., | 2 |  | 68 |   
  
 |  
 
 
|  
 |  
 
This would indicate that the maximum occurs at nearer 1,000  
ft. than 2,000 ft; and the same indication results from  
grouping the stations having 100 in. and upwards, according  
to their amounts. There are 14 such stations; their mean  
fall is 128 in., and mean altitude 785 ft. There are 5  
stations having more than 128 in., and their mean altitude  
is 789ft; and there are 9 having between 100 in. and 128  
in., and their mean altitude is 782 ft., thus showing how  
slight is the effect of altitude. Lastly, the wettest spot  
known is at 1,077 ft., the next wettest at 422 ft., and  
there is only one station above 1,500 ft. which has a fall  
of even 100 in. 
  
The slight effect of altitude is evident all through the  
table - for instance, Skiddaw (18) is 1,400 ft. above  
Keswick (17), yet the amounts only differ by one inch.  
Again, Wythburn (20), and Birkside (21), differ by 1,200  
ft., and in amount only by 4 in. Sometimes the amount is  
largely in excess at the lower station; as with Elterwater  
(23), at the foot of Loughrigg and Loughrigg Fell-top (24),  
a difference of 850 ft., and a deficiency of 15 in. at the  
greater elevation. 
  
Concerning the distribution of rain in the district, the  
following appear indisputable facts:- 
  
 
1. That there are various spots in the district at which the 
true mean annual rainfall is above 100 in. 
  
 
2. That true mean falls of 125 in. and upwards are at  
present only known to occur at the head of Borrowdale. 
  
 
3. That in the greater part of the district the fall is 80  
in. or 90 in., and that these heavy falls occur almost as  
far to the east as Shap; but that the amount in the  
north-eastern parts decreases with great rapidity, the  
clouds having been previously condensed by contact with the  
mountain-tops, until a few miles N.E. of Penrith is probably 
almost as dry as Bedford. 
  
 |