Oil Painting, Sculpture, Mural, and Ceramics.
While it is still setting up, it can be carved to get a general shape, then it is sanded. Apply in thin layers up to 1/4 inch for large areas. To fill in large gaps or to build shapes it can be put on a sheet of plastic or cardboard and held in place until it sets. There are epoxy fillers for bumpers, but if there is much damage it is usually better to replace the cover.
Two readily available building materials come to mind: Bales of straw, and large pieces of cardboard. You can get straw through a feed store, possibly a garden store could order it. The cardboard could be found at appliance stores, or anyplace that unpacks large boxes. It really depends on where you want to make it, and how much you want to spend.
a large area of often with a large house on it
Architects usually use CAD software on computers. Some use the old method of large, well-lit drafting boards with drafting machines. As far as materials, they use plenty of rulers, T-squares, manifolds and speciality paper and pens.
Layers of rocks can curve downward due to tectonic forces. When two tectonic plates collide, the pressure and compression can cause the rocks to fold and bend. This folding can create downward curves known as synclines, where the youngest rocks are exposed in the center and older rocks are found on the sides.
they have thicker skin so the desert temperature changes do not affect them
A fault block mountain occurs when rock layers are pulled from opposite directions, large blocks slide downward, creating peaks and valleys. See Link edited by ERIC: To make it easier (SHEARING)
What causes an avalanche?An avalanche occurs when the snowpack - or the layers of accumulated snow - on the side of a mountain is in some way disturbed, leading to a fracturing of the top layer and a downward torrent of a large mass of the white stuff.
Landslide
Avalanche
A large sphere rolls without slipping because the friction between the sphere and the surface it is rolling on allows it to rotate and move forward at the same time. This means that the sphere's surface is not sliding against the ground, but rather gripping it as it rolls.
Raw materials and a large workforce for those of you on study island
Anticlinorium folds are large-scale upward-arching folds in rock layers, with older rocks at the core and younger rocks towards the edges. Synclinorium folds are large-scale downward-arching folds with younger rocks at the core and older rocks towards the edges. Both anticlinorium and synclinorium folds are common in mountain-building processes and structural geology.
they are called layers
Reverse Grading.
Stratus Clouds are clouds that cover large areas and form in layers.