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.
they are deposited by sediment
Larger particles are deposited first as a stream loses velocity. Gravel would be deposited first, since it is the largest (out of Clay, Silt, Sand, and Gravel)
Boulders-cobbles-pebbles-sand-silt-clay
In a sediment collecting basin, clay is typically deposited closest to the shore. This is because clay particles are very fine and can remain suspended in water for longer periods, allowing them to settle out in calmer, shallow areas near the shore. Sandstone and siltstone, which are composed of larger particles, tend to be deposited further offshore where water energy is higher and sediment transport is more vigorous.
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