3IO 



STEPHEN TABER 



erable distance on both sides. Water-pipes at a distance of several 

 hundred feet from the fauk-line have been pulled apart, telescoped, 

 or bent in the direction of the movement, and fences formerly straight 



Dam af Crysia] .Sprinqs Lcxke 

 showing cracks formed by the displacemenf 

 Fig. 7. 



have been bent into a slight curve for a distance of 200 or 300 yards 

 from the fracture. 



The intensity of the shock v^as greatest along the line of faulting, 

 and decreases as one goes away from this line. In comparing the 



