Stratigraphy: The Study of Rocks And Their Location Relative To Each Other
Stratigraphy (noun, “Strah-TIG-grah-fee”)
This is a branch of geology that focuses on geological strata, or rock layers. The ground beneath your feet is not one solid mass. It has layers, like the layers of an onion, on its outer crust. These layers build up over time. Dust settles, and organisms die and turn to mud. That dust, mud and other material eventually turns into rock. The composition of that rock is different depending on what has gone into making it.
Scientists study how these layers were made and how they are organized. That’s because stratigraphy can hint at Earth’s past. For example, studying layers of rock can show when an area changed from a sandy seabed to a muddy swamp. Examining the fossils in the rock layers can show what kinds of ancient creatures lived together at the same time. Rock layers can even provide clues about dramatic events — like the asteroid that helped to wipe out the dinosaurs.
In a sentence
Some scientists who study stratigraphy think that people have altered the Earth’s layers enough that it might be a sign of a new unit of geologic time — the Anthropocene.
Anthropocene: Term coined by scientists to describe the age in which humans have been the strongest force of change on the planet. It is generally believed to date from at least the dawn of the Nuclear Age (in the middle 1940s), and possibly even earlier — from the beginning of the Industrial Revolution in the early 1800s.
asteroid: A rocky object in orbit around the sun. Most asteroids orbit in a region that falls between the orbits of Mars and Jupiter. Astronomers refer to this region as the asteroid belt.
crust: (in geology) Earth’s outermost surface, usually made from dense, solid rock.
dinosaur: A term that means terrible lizard. These ancient reptiles lived from about 250 million years ago to roughly 65 million years ago. All descended from egg-laying reptiles known as archosaurs. Their descendants eventually split into two lines. For many decades, they have been distinguished by their hips. The lizard-hipped line are believed to have led to the saurichians, such as two-footed theropods like T. rex and the lumbering four-footed Apatosaurus (once known as brontosaurus). A second line of so-called bird-hipped, or ornithischian dinosaurs, appears to have led to a widely differing group of animals that included the stegosaurs and duckbilled dinosaurs. But a new 2017 analysis now calls into question that characterization of relatedness based on hip shape.
fossil: Any preserved remains or traces of ancient life. There are many different types of fossils: The bones and other body parts of dinosaurs are called “body fossils.” Things like footprints are called “trace fossils.” Even specimens of dinosaur poop are fossils. The process of forming fossils is called fossilization.
geologic: An adjective that refers to things that are related to Earth’s physical structure and substance, its history and the processes that act on it. People who work in this field are known as geologists.
geological: Adjective to describe things related to Earth’s physical structure and substance, its history and the processes that act on it. People who work in this field are known as geologists.
geology: The study of Earth’s physical structure and substance, its history and the processes that act on it. People who work in this field are known as geologists. Planetary geology is the science of studying the same things about other planets.
organism: Any living thing, from elephants and plants to bacteria and other types of single-celled life.
solid: Firm and stable in shape; not liquid or gaseous.
strata: (singular: stratum) Layers, usually of rock or earthen materials, whose structure tends to vary little. It is usually different from layers above and was produced at a different period of time using different ingredients.
stratigraphy: The study of geological strata — how they were made and what they were made from, their arrangement in the ground and what it tells scientists about the conditions on Earth when these layers were created.