chemical weathering
Water seeping into cracks in a rock will freeze and expand when the water becomes frozen in winter.
This expansion will cause the crack to become wider until the rock splits.
Weathering and erosion occur all the time even when mountains are forming
No
Yes
The agents of "weathering" is both the agents of the physical and the chemical weathering combined. Agents of physical weathering can be: wind, water, sun, ice, gravity, rain, etc. Agents of chemical weathering may be: acid from roots, acid rain, oxidation/reduction (rusting), carbon dioxide, etc. They are the same because both physical and chemical weathering lead to erosion of rocks. In other words, both help rocks break down into smaller pieces. They are also the same because both physical and chemical weathering can occur with the same agent. For example, TREES. The roots of trees release acid to break down rocks (chemical weathering) while the roots of trees also grow into the cracks of rocks and help break them apart (physical weathering). Note that weathering is just the beginning process of erosion. Erosion is when stuff actually breaks down into smaller pieces.
Although sedimentary rocks form in a variety of processes, the first process that would occur in the formation of the most common sedimentary rocks would be that of weathering, which is the breakdown of rocks into smaller pieces through chemical or mechanical means by nature.
weathering could occur and the rock would break apart.
Weathering and erosion occur all the time even when mountains are forming
mechanical weathering
In the Stratosphere
Weathering of rocks occur on the outer surface.
Mechanical and chemical weathering both occur.
Physical weathering, such as cracks, creates more surface area for chemical weathering to occur on.
Chemical weathering in the warm, wet season and mechanical weathering in the cool, dry season.
No
Yes
weathering occurs faster at high elevations because
Weathering by living organisms is possible practically anywhere.