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A B C D E F G H I J K L M N O P Q R S T U V W X Y Z
A lava flow with a smooth, ropy surface.
The science that studies the past distribution of plants and animals.
The study of how global climate has changed through time.
Natural magnetism is acquired by some rocks, especially igneous rocks that are rich in iron, as they solidify. As the rocks cool, iron-bearing minerals are 'frozen' into position. The orientation of iron-bearing magnetic minerals record the location of the Earth's magnetic poles and the latitude of the rock at the time of cooling.
The study of ancient seismic (earthquake) events.
Includes the time from about 570-245 million years ago.
The study of pollen, living and fossil.
The supercontinent which formed at the end of the Paleozoic Era and began breaking up about 200 million years ago to form today's continents.
A radioactive isotope that changes to a different, daughter isotope when its nucleus decays.
The preexisting rock from which a metamorphic rock forms.
A tectonically inactive continental margin characterized by a lack of earthquakes and volcanic activity.
A bare rock surface that provides a protective rock cover over the material beneath it.
A sloping bedrock surface at the base of a mountain, formed when erosion removes much of the mountain's mass.
Loose particles of rock or mineral (sediment) that range in size from 2 - 64 millimeters in diameter. Pebbles are the smallest type of gravel.
A very coarse-grained igneous rock, commonly with a granitic composition. Usually forms from molten rock rich in water or other volatiles that facilitate the growth of large crystals. Forms sills and dikes.
A stream that runs continuously throughout the year.
The ability of a rock or other material to allow water to flow through its interconnected spaces. Permeable bedrock makes a good aquifer, a rock layer that yields water to wells. See porosity. (3 MB porosity animation available)
The study of rocks.
Lover of rocks. May be a petrologist, a stone mason, a rock climber.
An igneous rock texture in which the mineral grains are large enough to be seen with the unaided eye and are of approximately equal size.
The eon beginning about 570 million years ago and continuing to the present. The portion of Earth history with rocks containing abundant fossils.
A magnesium-rich member of the mica mineral family. Phlogopite is a yellowish-brown to coppery-colored mica. Like all micas, phlogopite forms flat, plate-like crystals that cleave into smooth flakes.
A very fine-grained, foliated metamorphic rock, generally derived from shale or fine-grained sandstone. Phyllites are usually black or dark gray; the foliation is commonly crinkled or wavy. Differs from less recrystallized slate by its sheen, which is produced by barely visible flakes of muscovite (mica).
A member of the feldspar mineral family. Plagioclase feldspars are silicates that contain considerable sodium and calcium. Feldspar crystals are stubby prisms, generally white to gray and a glassy luster.
Generally tiny animals or plants that live floating in water.
Permanent deformation (change in size or shape) of soft, but solid rock by folding or flowing without fracturing.
The theory that the Earth's outer shell is made up of about a dozen lithospheric plates that move about and interact at their boundaries.
Playas are shallow, short-lived lakes that form where water drains into basins with no outlet to the sea and quickly evaporates. Playas are common features in arid (desert) regions and are among the flattest landforms in the world.
The earliest Epoch of the Quaternary Period, beginning about 1.6 million years ago and ending 10,000 years ago. Commonly known as the 'Ice Age', a time with episodes of widespread continental glaciation.
The latest Epoch of the Tertiary Period, beginning about 5.3 million years ago and ending 1.6 million years ago.
Any igneous rock that cools beneath the surface. (=intrusive rock).
A lake formed in a land-locked basin during a period of increased rainfall associated with glacial advance elsewhere.
The percentage of open spaces (pores) in rock or soil. When these spaces are interconnected, water, air, or other fluids can migrate from space to space. Interconnected spaces make the soil or bedrock permeable.
An igneous rock texture characterized by larger crystals (phenocrysts) in a matrix of distinctly finer crystals (groundmass).
Large mineral grains that grow during metamorphism.
The 'unofficial' time period that encompasses all time from the Earth's formation, 4.55 billion years ago to 570 million years ago, the beginning of the Paleozoic Era.
A large rock resting on another in an unstable position. Precarious boulders may remain in place for thousands of years until an earthquake or human-caused tremor dislodges them.
The process that separates solids from a solution.
Mineral precipitate. A mineral deposited from a water solution in pores or other openings in rocks. Chemical reaction with the surrounding rock, changes in pressure or temperature, or just drying up (evaporation) can cause a mineral to precipitate out of solution. Quartz veins are common products of mineral precipitation.
The 'Precambrian' time interval from 2.5 billion to 570 million years ago.
A light-colored, frothy, glassy volcanic rock. The texture is formed by rapidly expanding gas in erupting lava.
Iron sulfide mineral (FeS). Forms silvery to brassy metallic cubes or masses. Common in many rocks. Known as fool's gold. Weathered pyrite produces limonite (iron oxide) that stains rock brown. or yellow.
An igneous rock texture produced from consolidation of fragmented volcanic material ejected during a violent eruption. Also used to describe ash, bombs and other material forcefully ejected during a volcanic eruption (=tephra)
A volcanic eruption that produces a large volume of solid volcanic fragments (pyroclastics) rather than fluid lava. This type of eruption is typical of volcanoes with high silica, viscous, gas-rich magma.
Family of silicate minerals containing iron, magnesium, and calcium in varying amounts. Differ from amphibole family by lack of water in the crystals. The most common variety, augite, contains aluminum as well. Generally forms very dark green to black stubby prisms.