Agricultural geology . Fie. 7. Stratified rocks folded into a series of anticlines and Fig. S. A recumbent fold. All of these varieties are most easily imderstood from the term commonly employed is isochnal folding, whereboth limbs of an overturned fold dip in the same again may be complex; that is a number of smallfolds may be combined into the general form of one largefold, as shown in the figure of an anticlinorium (Fig. 9). Anexaggerated form of an anticlinorium is the fan-structure of

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Keywords: ., bookcentury1900, bookdecade1910, bookidcu3192, booksubjectgeology