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.
Fault Classification. Faults and fault zones are classified by how the rocks on each side of the fault or fault zone move past each other. There are two main types of movement along faults: 1) a sideways movement called strike slip, and 2) an up or down movement called dip slip. Strike-Slip Faults The movement along a strike-slip fault is approximately parallel to the strike of the fault, meaning the rocks move past each other horizontally.