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.
Three principal types of faults are present in the Teton region: normal faults, reverse faults, and thrust faults. A normal fault (fig. 16A) is a steeply dipping (steeply inclined) fault along which rocks above the fault have moved down relative to those beneath it. A reverse fault (fig.