Well... This Is Haveing Sex With Your Cat. Sorry, I Meant Your Racoon.
In planer bedding Surfaces are without cross lines, but cross-bedding is inclined.
Deltas
Surfaces between layers of sediments (bedding planes) are usually deposited in horizontal sheets, but cross-bedding is inclined. Graded beds are horizontal and are usually sorted from coarse at the bottom to fine at the top.
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deltas
Absolutely: there are many possibilities. The only issue is that as the cross-bedding is often not on a massive scale, this may cause graded bedding to become unnoticeable. It is clearer in a rock with only graded bedding. As the beds are often quite shallow, grading is often unnoticeable, yet it still may exist on a slight scale.
The wavy line between layers of rock is called a "cross bedding." Cross bedding forms when sediments are deposited at an angle due to currents, resulting in distinct layers that intersect at an angle to the horizontal bedding.
A common variety of cross bedding. Generally at a relatively low angle it resembles scooped grooves. It is formed by sand dune migration (large or small scale)
Cross bedding
Where only one of both bounding surfaces are curved.
Absolutely: there are many possibilities. The only issue is that as the cross-bedding is often not on a massive scale, this may cause graded bedding to become unnoticeable. It is clearer in a rock with only graded bedding. As the beds are often quite shallow, grading is often unnoticeable, yet it still may exist on a slight scale.
what is a cross connection in plumbing