The law of superposition states that rock strata (layers) farthest from the ground surface are the oldest (formed first) and rock strata (layers) closest to the ground surface are the youngest (formed most recently). A fossil is the remains or traces of plants and animals that lived long ago.
The igneous rock layer is younger than the sedimentary layers under it and older than the sedimentary layers that form on top of it. Why is igneous rock always younger than any rock it cuts through? Fossils contained within sedimentary rock can offer clues about the age of the rock.
It’s firm and hard like other rock, but it’s actually flowing very slowly, about as slowly as your fingernails grow. The outer core is a liquid layer, made mostly of iron and nickel, that moves around the inner core. This motion causes Earth to act like a giant magnet.
Rocks never die, they just change form. So they don’t have a lifespan. Rocks are always changing form, but too slowly to notice with you’re eyes. In fact; rocks aren’t even classified as living things.
A rock is the hard, solid part of the Earth that is not soil or metal. Rocks can be different colors. Some rocks are smooth. Other rocks are very rough.
The cycle has no beginning and no end. Rocks deep within the Earth are right now becoming other types of rocks. Rocks at the surface are lying in place before they are next exposed to a process that will change them. Several processes can turn one type of rock into another type of rock.
Weathering describes the breaking down or dissolving of rocks and minerals on the surface of the Earth. Water, ice, acids, salts, plants, animals, and changes in temperature are all agents of weathering. Once a rock has been broken down, a process called erosion transports the bits of rock and mineral away.
Rock cycle:The cycle in which rocks transform between Igneous, Sedimentary, and Metamorphic via the processes of the earth. Sedimentary Rock: Sedimentary rocks are formed from pre-existing rocks or pieces of once-living organisms. They form from deposits that accumulate on the Earth’s surface.
A crystal is just a mineral that is not part of an aggregated solid, like a rock, but instead stands on its own. Structured lattice-like lattices are used to make crystals. The outcome is an inorganic, geometric structure.
Most minerals can be characterized and classified by their unique physical properties: hardness, luster, color, streak, specific gravity, cleavage, fracture, and tenacity.
