answersLogoWhite

0


Best Answer

When rock layers bend and buckle it creates mountains. For example, the Rocky Mountains in the west are millions of years younger than the Appalachian Mountains in the east forming from two separate incidents of buckling.

User Avatar

Wiki User

9y ago
This answer is:
User Avatar
More answers
User Avatar

AnswerBot

5mo ago

Tension between rock layers can lead to fractures or faults forming as the rocks are pulled apart. This creates pathways for fluids like water or magma to flow through, potentially leading to geological events such as earthquakes or volcanic activity.

This answer is:
User Avatar

User Avatar

Wiki User

12y ago

a normal fault

This answer is:
User Avatar

User Avatar

Wiki User

11y ago

a mftr is form #x

This answer is:
User Avatar

Add your answer:

Earn +20 pts
Q: What results from tension between rock layers?
Write your answer...
Submit
Still have questions?
magnify glass
imp
Related questions

What results from compression between rock layers?

it forms a sedimentary rock


What is an unconformity between parallel rock layers?

An unconformity between parallel rock layers is a gap in the geologic record where erosion has removed some rock layers before new ones were deposited on top. This results in a lack of continuity in the rock record, representing a period of geologic time that is not preserved in the sequence of rock layers.


When rock layers bend and buckle in results in a?

Fols


When rock layers bend and buckle it results in what?

When rock layers bend and buckle, it results in the formation of folds in the Earth's crust. This folding occurs due to tectonic forces that compress and deform the rock layers, leading to the creation of structures such as anticlines and synclines. These folded rock layers can be seen in mountain ranges and other tectonically active regions.


What is a slab of volcanic rock formed when magma squeezes between layers of rock?

A sill is a slab of volcanic rock formed when magma squeezes between layers of rock. It is typically horizontal and parallel to the surrounding rock layers. Sills are distinguishable from dikes, which cut across the rock layers.


What are formations that are sandwiched between layers of existing rock formations?

The formations that are sandwiched between layers of existing rock formations called sills. Another formation between layers is called laccoliths.


What is a slab of rock when magma squeezes between layers of rock?

sill


What fault Rock layers are placed under compressional stress?

When rock layers are placed under compressional stress, faults like reverse or thrust faults are commonly formed. In these faults, the rock layers are pushed together and the hanging wall moves up relative to the footwall. This results in shortening and thickening of the rock layers.


What type of stress occurs when layers of rock are pulled apart?

Tensional stress occurs when layers of rock are pulled apart. This type of stress results in the stretching and thinning of rock layers, leading to the formation of features like rift valleys or normal faults.


What are formations that are sandwiched between layers of existing rock formations called?

Formations that are sandwiched between layers of existing rock formations are called interbedded formations. These formations are typically deposited in between layers of pre-existing rocks due to changes in sedimentation patterns or depositional environments over time.


What is the difference between a sill and a laccolith?

A sill is a horizontal sheet of igneous rock that is intruded between existing rock layers, while a laccolith is a dome-shaped intrusion that causes the overlying rock layers to arch upwards. Sills are flat and parallel to existing rock layers, while laccoliths are typically lens-shaped and create bulges in the rock layers above them.


Which igneous feature is formed when magma is forced into layers parallel to the surrounding rock layers?

A sill is formed when magma is forced into layers parallel to the surrounding rock layers. Sills are characterized by their tabular shape and are often found intruding between rock layers.