1) The most obvious is that a boulder is significantly larger than a pebble or smaller boulder or rock. This would give the illusion of a smaller pebble weathering quiker than a boulder, when they are actually weathering at the same rate
2) The way they are being weather can be a factor. If you have a boulder being hit by only water or air while a pebble is all over the river bottom and sand than the pebble will weather quicker because there are more forces acting on it than the boulder.
Igneous rocks that cooled slowly are intrusive. Igneous rocks that cooled quickly are extrusive. Intrusive rocks form larger crystals, because the crystals have a longer time to grow. Extrusive rocks have small to no crystals, because they had little or no time to grow/form.
The boulder rolled down the hill with a mighty force, scattering smaller rocks in its path.
Intrusive rocks cool more slowly than extrusive rocks because they are formed beneath the Earth's surface. This slower cooling allows for larger mineral crystals to form within the rock.
Small rocks have a higher surface area to volume ratio, which exposes more of their surface to weathering processes like erosion and chemical reactions. This increased exposure makes them more prone to breaking down or weathering quickly compared to larger rocks.
No, extrusive rocks cool quickly because they form on the Earth's surface or in shallow depths where the temperature is lower. This rapid cooling results in small mineral crystals or a glassy texture in the rock.
After lava cools down and solidifies, it forms rocks. These rocks can then weather and erode into small fragments called boulders.
No. Intrusive igneous rocks have large crystals because they cool slowly.
Most do, however some do not, for instance a pseudotachylyte cools quickly.
Igneous rocks that cooled slowly are intrusive. Igneous rocks that cooled quickly are extrusive. Intrusive rocks form larger crystals, because the crystals have a longer time to grow. Extrusive rocks have small to no crystals, because they had little or no time to grow/form.
The boulder rolled down the hill with a mighty force, scattering smaller rocks in its path.
Basalt cools off quickly because it is formed under water.
boulder holder
The phenomenon in which hard rocks weather more slowly than softer rocks under the same climatic conditions is known as differential weathering. This occurs because softer rocks are more susceptible to physical and chemical weathering processes, such as erosion and chemical reactions, which break them down more quickly. Hard rocks, being more resistant to these processes, tend to maintain their structure and form for a longer period, leading to variations in landscape features. Consequently, this differential erosion can create distinct geological formations.
Intrusive rocks cool more slowly than extrusive rocks because they are formed beneath the Earth's surface. This slower cooling allows for larger mineral crystals to form within the rock.
boulder holder
Boulder.
a boulder