Above Ground – EXTRUSIVE – Formed when volcanoes erupt. This causes the magma to rise above the earth’s surface. When magma appears above the earth, it is called lava. When the lava cools above ground, it forms Igneous Rocks.

Igneous rocks

Sedimentary rocks are formed on or near the Earth’s surface, in contrast to metamorphic and igneous rocks, which are formed deep within the Earth. The most important geological processes that lead to the creation of sedimentary rocks are erosion, weathering, dissolution, precipitation, and lithification.

Bedrock is the hard, solid rock beneath surface materials such as soil and gravel. Bedrock also underlies sand and other sediments on the ocean floor. Bedrock is consolidated rock, meaning it is solid and tightly bound. Overlying material is often unconsolidated rock, which is made up of loose particles.

The definition of bedrock means the layer of solid rock below the soil. Unbroken solid rock found at the bottom during an archaeological dig is an example of bedrock. The solid rock that lies beneath the soil and other loose material on the Earth’s surface.

What is another word for bedrock?

Bedrock, a deposit of solid rock that is typically buried beneath soil and other broken or unconsolidated material (regolith). Bedrock is made up of igneous, sedimentary, or metamorphic rock, and it often serves as the parent material (the source of rock and mineral fragments) for regolith and soil.

The gold is found not only in the bedrock, but in gravels as much as two feet above the bedrock. In the original pay-streak on Wade Creek, gold is found as deep as 1 1/2 feet into the bedrock. The origin of the gold is supposed to have been from the quartz stringers in the schists.

The reason diamond is so hard has to do with the arrangements of carbon atoms in its crystalline form, which has a very high packing factor. Bedrock can be made from many different substances, with a hardness anywhere from 1 to 9. So even the hardest bedrock is still not as hard as diamond.

Under the action of heat, cold, rain, wind, and other atmospheric factors, the rock breaks down physically into small fragments that become the parent material of the soil. The rock also chemically changes as the compounds in the rock dissolve in rain or react with air.