Horizon A
horizontal bedding is sedimentary rock structure in which layers of rocks lies horizontally.
Foot wall
The crust alone contains millions of different layers of sedimentary rock. For the layers of the Earth, some of which are rock and some of which are not, see the related link below.
Least likely to break from fracture, generally speaking, would be unweathered igneous rock.
That the one below the other is generally older.
It is the bedrock.
Unweathered rock.
No it is definitely not.
Limestone is the youngest since it's at the top
Every layer of rock, as one moves up from the core, is younger than the one below it. This means that the layers of rock above and below the coal are different ages, with the one above younger and the one below older.
Due to faulting or folding.
Tension in Earth's crust pulls rock apart, causing hanging walls. In a normal fault, the fault is at an angle, so one block of rock lies above the fault while the other block lies below the fault. The block of rock that lies above is called the hanging wall. The rock that lies below is called the footwall.
Five steps: weathering, erosion transportation, deposition, and lithification
horizontal bedding is sedimentary rock structure in which layers of rocks lies horizontally.
solid rock baby
Every layer of rock, as one moves up from the core, is younger than the one below it. This means that the layers of rock above and below the coal are different ages, with the one above younger and the one below older.
Foot wall