where you would be most likely to find sediments that would lithify to become a conglomerate?

Conglomerates are a type of sedimentary rock that are formed from the cementing of rounded pebbles, cobbles, and boulders. Here are the steps to answer where you would most likely find sediments that would lithify to become a conglomerate:

1. Identify the type of sediments that form conglomerates: Conglomerates are formed from rounded pebbles, cobbles, and boulders. These sediments are usually transported by water, and they become rounded as they roll along the river or stream bed.

2. Identify where these sediments are found: These types of sediments are typically found in river and stream beds, where the water can transport them and cause them to become rounded. They can also be found in glacial till, or the sediment left behind by a retreating glacier, and on beaches, where the action of the waves can round the sediments.

3. Identify where lithification occurs: Lithification, the process of turning sediments into rock, typically occurs underground. The weight of the overlying sediments and the minerals in the groundwater help to cement the sediments together to form rock.

So, you would be most likely to find the sediments that would lithify to become a conglomerate in river and stream beds, glacial till, and on beaches. These sediments would then be buried and lithified to become conglomerate rock.