Which type of stress produces folds and reverse faults?

Compression (squeezing together)

A normal fault forms when the hanging wall:

Moves down relative to the footwall, under tension

A joint has no movement along it; a fault has movement that offsets the rocks

Cooling and contraction of the lava

A buried erosion surface and a gap in time between older rocks below and younger rocks above

The beds below sit at a different angle from the flat-lying beds above

The angle the bed makes with the horizontal, down the line of steepest slope

At right angles (perpendicular) to it

Gentle dips give wide outcrops; steep dips give narrow ones

Were deposited horizontally and tilted or folded afterwards

Younger than the granite the pebbles came from

Deposition, then deformation (tilting or folding), then intrusion, erosion (unconformities) and faulting, using a principle at each step

14questions. Pick an answer and you'll see why right away.

Which type of stress produces folds and reverse faults?
In an anticline, where are the oldest beds found?
A normal fault forms when the hanging wall:
What is the key difference between a joint and a fault?
The hexagonal columns of the Giant's Causeway are joints formed by:
An unconformity records:
On a cross-section, how is an angular unconformity recognised?
What does the dip of a bed describe?
Strike is always oriented how, relative to the dip direction?
How does the angle of dip affect the width of a bed's outcrop on a map?
By cross-cutting relationships, a fault or intrusion is:
The principle of original horizontality tells you that tilted or folded beds:
A conglomerate containing granite pebbles is, by the principle of included fragments:
When reading the order of events from a cross-section, in which general order are events worked out?