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A monocline (or, rarely, a monoform) is a step-like fold in rock strata consisting of a zone of steeper dip within an otherwise horizontal or gently dipping sequence. Formation [ edit ]
The term 'fold' is used in geology when one or more originally flat sedimentary strata surfaces are bent or curved as a result of plastic (i.e. permanent) deformation. A monocline is a step-like fold, in which one limb is roughly horizontal. The Purbeck Monocline was formed during the late Oligocene and early Miocene epochs, about 30 million ...
Observational study, can be naturalistic (see natural experiment), participant or controlled. Program evaluation; Quasi-experiment; Self-report inventory; Survey, often with a random sample (see survey sampling) Twin study; Research designs vary according to the period(s) of time over which data are collected:
The Jones Child Study Center has a special relationship with the Institute of Human Development as a site for research, training and outreach to the community, parents, and teachers. The Institute of Human Development's fundamental mission is to study evolutionary, biological, psychological, social, and cultural factors that affect human ...
A 1996 study claiming a connection in men [399] has not been verified by subsequent studies, including a 2013 study that found no correlation. [400] The menstrual cycles of women who live together do not tend to synchronize. A 1971 study made this claim, but subsequent research has not supported it. [401] [402]
Oblique aerial photo of a hogback located between Gallup and Ramah in western New Mexico.. In geology and geomorphology, a hogback or hog's back is a long, narrow ridge or a series of hills with a narrow crest and steep slopes of nearly equal inclination on both flanks.
In structural geology, a syncline is a fold with younger layers closer to the center of the structure, whereas an anticline is the inverse of a syncline. A synclinorium (plural synclinoriums or synclinoria ) is a large syncline with superimposed smaller folds. [ 1 ]
The Waterpocket Fold is a geologic landform that extends from southern Wayne through Garfield and ending in northern Kane counties of southern Utah, United States. [1] The geologic structure, formed during the Laramide orogeny , is a south-southeast trending fold in which the east side is dropped relative to the west side.