ITCZ) or equatorial trough. This line of convergence near the equator is also discernible in a map of streamlines (Figure 12.2; Note 12.A). It is actually a band a few hundred kilometres wide, enclosing places where winds flow inwards (are 'confluent') and subsequently rise convectively.he movement of the ITCZ across South Africa (Figure 12.1) is complicated by the land's shape, elevation and location, and there is a southerly spur called the Zaire Air Boundary (ZAB). Similarly, there is a spur over South America.
C. horst. D. mountain belt. Weegy: A downwarped structure with a circular shape is a basin. Expert answered|debnjerry|Points 32701|User: Faults are generally closely associated with A. monoclines. B. anticlines. C. synclines. D. symmetrical folds. Weegy: Faults are generally closely associated with monoclines.. horst. D. mountain belt. Weegy: A downwarped structure with a circular shape is a basin. Expert answered|debnjerry|Points 32701|User: Faults are generally closely associated with A. monoclines. B. anticlines. C. synclines. D. symmetrical folds. Weegy: Faults are generally closely associated with monoclines.
Now research presented this week at the fall meeting of the American Geophysical Union in San Francisco that will be published in the December 12 issue of Science indicates that earthquakes along one type of fault in the area could trigger temblors along other faults.