Learn More About the Science of Geology

Learn More About the Science of Geology What is geology? It is the study of the Earth, its substances, shapes, processes, and history. There are several different components that geologists study with regard to this fascinating field. Minerals Minerals are natural, inorganic solids with a consistent composition. Each mineral also has a unique arrangement of atoms, expressed in its crystal form (or habit) and its hardness, fracture, color, and other properties. Organic natural substances, like petroleum or amber, are not called minerals. Minerals of exceptional beauty and durability are called gemstones (as are a few rocks). Other minerals are sources of metals,  chemicals  and fertilizers. Petroleum is a source of energy and chemical feedstocks. All of these are described as mineral resources. Rocks Rocks are solid mixtures of at least one mineral. While minerals have crystals and chemical formulas, rocks instead have textures and mineral compositions. On that basis, rocks are divided into three classes reflecting three environments: igneous rocks come from a hot melt, sedimentary rocks from accumulation and burial of sediment, metamorphic rocks from altering other rocks by heat and pressure. This classification points to an active Earth that circulates matter through the three rock classes, on the surface and underground, in what is called the rock cycle. Rocks are important as ores- economic sources of useful minerals. Coal is a rock that is a source of energy. Other rock types are useful as building stone, crushed stone and raw material for concrete. Still others serve for toolmaking, from the stone knives of our prehuman ancestors to the chalk used by artists today. All of these, too, are considered mineral resources. Fossils Fossils are signs of living things that are found in many sedimentary rocks. They may be impressions of an organism, casts in which minerals have replaced its body parts, or even remnants of its actual substance Fossils also include tracks, burrows, nests, and other indirect signs. Fossils and their sedimentary environments are vivid clues about the former Earth and what living there was like. Geologists have compiled a fossil record of ancient life stretching hundreds of millions of years into the past. Fossils have practical value because they change throughout the rock column. The exact mix of fossils serves to identify and correlate rock units in widely separated places, even in the grit pumped up from  drill holes. The geologic time scale is based almost entirely on fossils supplemented with other dating methods. With  it,  we can confidently compare sedimentary rocks from everywhere in the world. Fossils are also resources, valuable as museum attractions and as collectibles, and their commerce is increasingly regulated. Landforms, Structures and Maps Landforms in all their variety are products of the rock cycle, built of rocks and sediment. They were shaped by erosion and other processes. Landforms give testimony of the environments that built and altered them in the geologic past, such as ice ages. From mountains and water bodies to caves to the sculpted features of the beach and seafloor, landforms are clues into the Earth beneath them. Structure is an important part of studying rock outcrops. Most parts of the Earths crust are warped, bent and buckled to some extent. The geologic signs of this jointing, folding, faulting, rock textures, and unconformities help in assessing structure, as do measurements of the slopes and orientation of rock beds. Structure in the subsurface is important for water supply. Geologic maps are an efficient database of geologic information on rocks, landforms and structure.   Geologic Processes and Hazards Geologic processes drive the rock cycle to create landforms, structures and fossils. They include erosion, deposition, fossilization, faulting, uplift, metamorphism, and volcanism. Geologic hazards are powerful expressions of geologic processes. Landslides, volcanic eruptions, earthquakes, tsunamis, climate change, flooding and cosmic impacts are extreme examples of ordinary things. Understanding the underlying geologic processes is a key part of mitigating geologic hazards.   Tectonics and Earth History Tectonics is geologic activity on the largest scale. As geologists mapped the worlds rocks, untangled the fossil record and studied geologic features and processes, they began to raise and answer questions about tectonics the life cycle of mountain ranges and volcanic chains, motions of continents, the rise and fall of the ocean, and how the mantle and core operate. Plate-tectonic theory, which explains tectonics as the motions in Earths outer broken skin, has revolutionized geology, enabling us to study everything on Earth in a unified framework. Earth history is the story that minerals, rocks, fossils, landforms, and tectonics tell. Fossil studies, in combination with gene-based techniques, yield a consistent evolutionary history of life on Earth. The Phanerozoic Eon (age of fossils) of the last 550 million years is well mapped as a time of expanding life punctuated by mass extinctions. The previous four billion years, the Precambrian time, is being revealed as an age of enormous changes in the atmosphere, oceans and continents. Geology Is Civilization Geology is interesting as a pure science, but Professor Jim Hawkins at Scripps Institution of Oceanography tells his classes something even better: Rocks are money! What he means is that civilization rests on rocks: Society relies on a good supply of Earth products.For every structure we build, we need to know about the ground it sits on.Our food and fiber come from soil, a thin biogeochemical layer of incredible complexity.Protection against geologic hazards depends on our understanding of them.