Sediments at location L might exhibit which FOUR of the following characteristics?Group of answer choicesangular clastscross-beddingcurrent ripple-marksgraded beddingmoderately thick bedding (10-100 centimeters thick)mudcrackspoorly-sortedrounded claststhick-massive bedding (>1 meter thick)thin bedding / laminations (<3 centimeters thick)wave ripple markswell-sorted - moderately well sorted

The characteristics of sediments at location L can vary greatly depending on the specific environmental conditions and geological processes at play. However, here are four possible characteristics that sediments at location L might exhibit:

1. Angular Clasts: These are fragments of rock that have sharp, angular edges. They are typically formed by physical weathering processes such as freeze-thaw cycles or mechanical erosion.

2. Cross-Bedding: This is a geological structure where layers of sediment or sedimentary rock are inclined or horizontal. It often forms in environments with varying energy conditions, such as rivers or wind-blown dunes.

3. Mudcracks: These are patterns of cracks caused by the drying out of wet clay or mud. They are often found in environments where sediment is periodically exposed to the air, such as river banks or tidal flats.

4. Poorly-Sorted: This refers to a sediment sample that contains a wide range of grain sizes. It often indicates a high-energy depositional environment, such as a glacier or a fast-flowing river, where there is not enough time for the sediment to be sorted by size.

Remember, these are just possibilities. The actual characteristics of the sediments at location L would depend on a variety of factors, including the local climate, the types of rock in the area, and the specific geological processes at work.