Send the link below via email or IMCopy
Present to your audienceStart remote presentation
- Invited audience members will follow you as you navigate and present
- People invited to a presentation do not need a Prezi account
- This link expires 10 minutes after you close the presentation
- A maximum of 30 users can follow your presentation
- Learn more about this feature in our knowledge base article
Do you really want to delete this prezi?
Neither you, nor the coeditors you shared it with will be able to recover it again.
Make your likes visible on Facebook?
You can change this under Settings & Account at any time.
Mechanical and Chemical Weathering
Transcript of Mechanical and Chemical Weathering
The roots of some plants will weather as they grow.
Especially the roots of strong trees, plants growing in rocky soil will break up the rocks with their growing roots.
Even the strongest rocks can be broken by some trees' roots.
The roots of plants produce weak acids (acids that react to water). These acids can weather limestone and marble easily.
Chemical weathering also requires water. Rainfall provides water needed for chemical changes.
Acid rain is made of water.
Sulfur, carbon, and nitrogen mix with rainwater in the clouds, and create acid rain when it precipitates.
This rain can weather marble and limestone.
Chemical weathering breaks down the rock through chemical changes. Rocks that undergo chemical changes may have a different mineral composition in the result, unlike mechanical weathering.
Mechanical and Chemical Weathering
Both types of weathering include plants in their processes.
Both types of weathering are supported by wet climates.
Ice-wedging, also known as frost-wedging, requires water.
Water is pooled inside the crevices of rocks
The water freezes, and expands
The rock splits from the ice expansion
The mechanical weathering process occurs differently than chemical weathering.
This statue has gone through chemical weathering and developed rust, a material different from the original.
Mechanical weathering physically breaks the rocks into smaller pieces. Because of this, the mineral makeup of the new rock is the same as the original.
A tree is weathering a rock.
Different temperatures will encourage a different type of weathering to occur.
Cold temperatures will more likely cause mechanical weathering to take place.
Ice wedging requires the cold for the water to freeze inside rocks.
Cold temperatures cause many things to expand, which will aid mechanical weathering more than hot temperatures.
On the other hand, hot temperatures increase the potential of chemical activity.
Warm temperatures also make evaporation possible, a key step to creating acid rain.
Heat quickens the rate at which the particles are moving, thus making the bonds between particles easy to break and reconnect to different ones, all the while increasing the chemical action.
The water weathers the rocks as it flows.
The outcome will still be the same as the original rock.
By Tian Wells
Here are some elements that cause chemical weathering:
Here are some types of mechanical weathering:
Ice or frost wedging
mechanical exfoliation (the release of pressure above a rock)
the growth of plants
animals (animals that burrow in the ground will sift soil and break up rocks)
a process that physically breaks rocks apart
a process that breaks rocks apart through chemical changes.
the gradual process of wearing away and breaking down rocks
: where ice, wind, water, gravity, or waves wear or rub away material by friction
: a mechanical weathering process which removes overlying layers and pressure of rock and causes the underlying layers to be weathered in a dome shape
: a chemical change in which a substance combines with oxygen, forming rust