## When rock layers bend and buckle but do not break what term is used?

Ch. 3 Science Test on: The Rock and Fossil Record

Occurs when rock layers bend and buckle from Earth’s internal forces Folding
Occurs when internal forces in the Earth slant rock layers without folding them Tilting
A surface that represents a missing part of the geologic column Unconformity

## What happens when bending of the rocks become too much?

Answer: If a rock bends and stays bent after stress is released, it is said to undergo plastic behavior. A combination of elastic and brittle behavior causes earthquakes. Rocks get bent in an elastic fashion until they reach their limit, then they break in brittle fashion.

## What causes rock layers to bend?

Tectonic plate motions deform Earth’s crust. Deformation causes rock layers to bend and break and causes mountains to form. It is the amount of force per unit area on a given material. The bending of rock layers in response to stress is called folding.

## What causes the materials to bend and break?

The report suggests that, when compressed, layered materials — everything from sedimentary rocks, to beyond-whisker-thin graphite — will form a series of internal buckles, or ripples, as they deform. Every material can bend and break.

## What does bend mean?

transitive verb. 1 : to constrain or strain to tension by curving bend a bow. 2a : to turn or force from straight or even to curved or angular bend a pipe. b : to force from a proper shape Her bicycle’s back wheel got bent in the crash.

## What do you call the deformation in rocks layers where there is a change in shape without breaking?

4. Fig. 10.7c: At higher confining pressures, a similarly directed external force will cause the deeply buried rock to actually flow and deform without fracturing. This is known as ductile deformation and the rock is said to behave plastically.

## What do we call a downward fold in rock layers?

Synclines are typically a downward fold (synform), termed a synformal syncline (i.e. a trough), but synclines that point upwards can be found when strata have been overturned and folded (an antiformal syncline). …

## What is syncline anticline?

Anticlines are folds in which each half of the fold dips away from the crest. Synclines are folds in which each half of the fold dips toward the trough of the fold. This intensely folded limestone from Highland County shows how anticlines and synclines typically occur together.

## How is syncline formed?

Synclines are formed when tectonic plates move toward each other, compressing the crust and forcing it upward.

## What is a plunging syncline?

A plunging anticline or a plunging syncline is one that has its axis tilted from the horizontal so that the fold is plunging into the earth along its length. A cross-section at a right angle to the axis of a plunging anticline looks the same as an anticline.

## How is a Monocline formed?

A monocline is a simple bend in the rock layers so that they are no longer horizontal. Anticlines are folded rocks that arch upward and dip away from the center of the fold. When rocks arch upward to form a circular structure, that structure is called an adome.

## What is the difference between a joint and a fault?

Joints and faults are types of fractures. A joint is a fracture along which no movement has taken place, usually caused by tensional forces. A fault is a fracture or break in the rock along which movement has taken place.

## How do you recognize faults in the field?

How do you recognize faults in the field? slickensides (polished fault surfaces) are all clues used to identify faults. Describe the differences among an anticline, a syncline, and a monocline.

## Where do most earthquakes happen?

Where do earthquakes occur?

• The world’s greatest earthquake belt, the circum-Pacific seismic belt, is found along the rim of the Pacific Ocean, where about 81 percent of our planet’s largest earthquakes occur.
• The Alpide earthquake belt extends from Java to Sumatra through the Himalayas, the Mediterranean, and out into the Atlantic.

## Is Focus and epicenter the same Why?

The focus is the place inside Earth’s crust where an earthquake originates. The point on the Earth’s surface directly above the focus is the epicenter. When energy is released at the focus, seismic waves travel outward from that point in all directions. It’s these waves that you feel during an earthquake.