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Chapter 5 Sedimentary Archives

Name:___________________________
Across
Covers parts of the crystalline rock on the stable area of the continent
Type of sandstone composed of ~30% fined grained matrix of mud and 70% quartz, feldspar and other rock particles. Deposited in tectonically active area.
Deformation or structural activity of a large part of the Earth's lithosphere over long period of time.
The collective term for the size, shape and arrangement of clasts in sedimentary rocks.
Fan shaped accumulation of sediments that occurs where a stream or river flows into a large body of water.
Large areas of exposed cryrstalline on on the stable are of a continent.
Underwater plain on the deep ocean floor.
The specific depositional setting of a particular sedimentary rock, unique in terms of physical, chemical, and biological characteristics.
Geologic term for sea level fall.
The glue that holds sediments in sedimentary rocks together.
Layered sedimentary rock composed of silicate minerals that absorbs lots of water. Weathering product of feldspars and micas.
Geologic term for mountain building.
The degree for which particle size is uniform, can be poor or well.
Relating to or arising from the action of the wind
Coursening upward of sediments in the rock record, recording shallow water sediments covering deep water sediments.
Area where sediments accumulate at a great rate than sediments of the same age in neighboring areas.
Sedimentary rock type expressed by its formation, composition, and fossil content.
Down
The color of a shale that has been deposited under anoxic conditions and contains carbon and/or reduced iron.
The gradual slope at the base of the steep slope that connects the continental shelp and the deep ocean floor.
Sedimentary envrionments that started out side-by-side will end up overlappin one another over time due to sea level change. The vertical sequence of facies represents facies that were once laterally continuous.
Geologic term for the rise of sea level.
The gradual sinking of an area of land, geologically due to the accumulation of sediments.
The color of sediments deposited under oxidizing conditions (typically continental deposits), color is due to the presence of oxidized iron.
Erosional or non-depositional surface separating two rock masses or strata of different ages, indicating that sediment deposition was not continuous.
The steep slope between the outer edge of the continental shelf and the deep ocean floor.
Type of biochemical sedimentary rock made of calcium carbonate.
Stable area of a continent.
Type of sandstone containing 25% or more of feldspar, an igneous mineral. Typically pink or red. Deposited in tectonically active area.