|  | Gentleman's Magazine 1760 p.522 where it run with the greatest rapidity at the foot of the  
mountain.
 The effects of the brooks of Hopebeck and  
Habcorton need not to be so particularly described,  
being of the same kind with the other, only inferior in  
degree, both on account of their being swelled by one of the 
spouts only, & their channels being deeper. However, the 
damage done by those, tho' inferior to the other, was by no  
means inconsiderable. One circumstance relative to that of  
Hopebeck may perhaps deserve to be mentioned: having  
burst its banks just at the place of crossing the highway,  
it continued its course along a lane to a considerable  
distance before it found a passage into the fields; and when 
the brook subsided, and the supply failed, much water  
remained stagnant in the hollows of the lane, particularly  
one before the door of a house, situated on the road. At  
this the people, not knowing how it could possibly come  
there, were greatly surprized; but much more, when they  
found in it a very fine dish of trout.
 With regard to the physical cause of this uncommon  
phaenomenon, there are some circumstances preceding it which 
seem irrenconcileable with either of the two theories I have 
seen. The cause assigned in the first theory, viz.  
various and contrary winds, could not be the real cause, as  
there was very little wind all the day preceding the event;  
what there was came constantly from the same quarter, and it 
entirely ceased in the evening. Neither was there more  
probability in the other cause's operation, viz. an  
extraordinary rarefraction of the air by igneous meteors, as 
there was not the least lightning seen, or thunder heard,  
nor any other diagnostic of the atmosphere's being charged  
with a more than ordinary stock of sulphureous exhalations,  
and nitrous acids at that time.
 ROB. DIXON.
 
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