answersLogoWhite

0

Rocks expand and contract depending on the temperature. After repeated exposure to temperature cycles, the surface of a rock may experience weakness in the bonds between crystals or particles, causing a delamination of the outer layer.

User Avatar

Wiki User

15y ago

What else can I help you with?

Related Questions

Describe how changes in the temperature cause rock fragmentation?

Changes in temperature cause thermal stress on rocks. When rocks heat up, they expand, and when they cool down, they contract. These repeated cycles of expansion and contraction can lead to the fragmentation of rocks due to internal stresses, ultimately causing them to break apart.


What do changes in temperature cause rock to do?

Changes in temperature cause rock to expand and contract. This may cause them to crack, and pieces may break off.


How can changes in temperature cause rocks to erode?

The temperature heats the rock and breaks it (erodes).


Why does temperature weather rocks?

Temperature can weather rocks through a process called thermal weathering, where rocks expand and contract due to heating and cooling cycles. This constant expansion and contraction weakens the rock structure, leading to breakdown and fragmentation over time. Additionally, extreme temperature changes can cause thermal stress, leading to fracturing and eventual disintegration of the rock.


Breaking down rock by physical force?

The process of breaking down rock by physical force is known as mechanical weathering. This can be caused by factors such as temperature changes, pressure changes, or the action of ice and water in cracks and crevices. Over time, this can lead to the fragmentation and breakdown of rocks into smaller pieces.


Does temperature changes cause chemical weathering?

Yes, temperature changes can cause chemical weathering by expanding and contracting rock materials, leading to the breakdown of minerals and weakening of rocks. For example, freezing and thawing cycles can cause rocks to crack and break apart, accelerating the chemical weathering process.


Describe how temperature changes can make cracks form in rocks?

Temperature changes cause rocks to expand and contract, leading to stress within the rock. Over time, repeated expansion and contraction can weaken the rock and lead to the formation of cracks. Additionally, differential rates of expansion and contraction in different parts of the rock can cause internal forces that contribute to crack formation.


How is a fragmentation clastic sedimentary rock produced?

Fragmentation clastic sedimentary rock is formed by the lithification of inorganic and/or organic sediments.


How do sudden temperature changes cause weathering of rock?

Sudden temperature changes can cause thermal stress on rocks, leading to expansion and contraction. This repeated stress can cause the rocks to weaken and eventually break apart through a process known as thermal weathering. Additionally, frost wedging can occur when water enters cracks in the rock, freezes, and expands, further contributing to the weathering process.


Why is sedimentary rock converted into metamorphic rock?

Sedimentary rock is formed generally at low temperature and pressure conditions.Therefore a change in this conditions to higher levels triggers mineralogical change.The driving forces for metamorphism are changes in temperature, pressure, and composition of the environment or strong deformation.These changes cause recrystallization in the solid state as the rock changes toward equilibrium with the new environment.Hence, formation of metamorphic rocks.


How do changes in temperature cause rocks to break down?

Changes in temperature cause rocks to undergo thermal expansion and contraction. When rocks heat up, they expand; likewise, when they cool down, they contract. Over time, this repeated expansion and contraction weaken the rock structure, creating cracks and fractures that eventually lead to rock breakdown.


What changes as a parent rock becomes a metamorphic rock?

When a parent rock undergoes metamorphism, changes such as increased temperature and pressure cause its mineral composition and texture to rearrange. This process can lead to the formation of new minerals, foliation (alignment of minerals), and a different overall appearance compared to the original parent rock.