Water deposits the clay particles in thin, flat layers.
If you make the modeling clay into a bowl shape, it should float
Clay is a very distinctive type of soil that feels "sticky" as well as "gooey". There is some water content, but it is not water-logged. It is difficult to dig in, and does not support plant-life very easily. It can become rock when it is fired up. It is basically made from fine-grained minerals as natural materials. Clay is made by particles being mixed with water and materials from the surrounding soil. Clay can also be formed from when weathered rock is carried from a place from where they were formed such as streams of water. Note that there are different colors of clay, depending on the region of the US.
unfortunately you can't. no matter how much you try and rehydrate clay, it has already started a process of chemically changing in the absence of water. after a certain amount of water has evaporated from it, it will turn hard, and eventually without proper firing will become crumbly and very dusty. keep clay wrapped well and it will keep for years!
You can make clay without cream of tartar by using BAKING SODA instead of cream of tartar.Take 2 cups flour, 1 cup salt, 2 Tbsp vegetable oil and 1 cup water. Mix salt and flour well. Add oil and then slowly add water until you get nice clay consistency. That is when your clay is ready.
Water deposits the clay particles in thin, flat layers.
Soil deposited by water is known as alluvium. This type of soil is typically made up of silt, clay, sand, and gravel deposits that have been carried and deposited by streams, rivers, and other bodies of water.
Rocks and soil deposited by streams are called alluvium. Alluvium consists of a mixture of gravel, sand, silt, and clay that is transported and deposited by flowing water.
Heavier particles such as gravel and sand are deposited first as the water slows down. Finer particles like silt and clay settle later and further downstream due to their lighter weight.
Boulders-cobbles-pebbles-sand-silt-clay
Sediment is a fine powdery material that is transported and deposited by water. It can consist of particles such as sand, silt, and clay that settle out of suspension in bodies of water like rivers, lakes, and oceans. Sedimentation plays a key role in shaping landscapes and creating geological formations.
A floodplain is the land that is covered by water when a river overflows it's banks. When this happens, silt and clay are deposited over time and the land on either side of the river flattens out. Any depressions in the land will hold water when the river level returns to normal after flooding and therefore more clay and silt will be deposited there filling it up.
Sediments such as sand, silt, and clay are deposited by running water. This sediment deposition occurs when the water's velocity decreases, causing it to drop its sediment load. Over time, these sediments can accumulate and form various landforms such as deltas, alluvial fans, and floodplains.
Sediment
Silt is fine sand, clay, or other material carried by running water and deposited as a sediment, especially in a channel or harbor.
clay
Normally consolidated clay refers to a type of clay sediment that has experienced sufficient pressure over time to reach a stable state of compaction. This means that any additional loading on the clay will not cause further compaction. Normally consolidated clay typically has higher strength and lower compressibility compared to overconsolidated clay.