| Terms |
Definitions |
|
Limestone
|
|
|
Sandstone
|
|
|
angular
|
negligible transport
|
|
coprolite
|
fossilized excrement
|
|
Rock Salt
|
crystalline, cpo
|
|
Surfaces
|
smooth/polished to "frosted", etched
|
|
dynamic metamorphism
|
shear stress predominant
|
|
Chemical Limestone
|
Fine Crystalizing
Calcite
Chemical Evaporite
|
|
sedimentary environments: Evaproite
|
chemical sediments
|
|
flat face
|
attack from 1 direction
|
|
Nonclastic
|
a pattern of interlocking crystals
|
|
two chemical sedimentary rocks
|
tufa,rock salt
|
|
coquina
|
shell fragments cemented by calcite/beach
|
|
Coquina
|
soft porous limestone, composed essentially of fragments of shells and coral,
|
|
Sedimentary contact
|
Transitional with other deposits
|
|
cementation
|
The process by which dissolved minerals crystalize and glue particles of sediment together into one mass.
|
|
erosion
|
removal of sediment grains from rock
|
|
Ironstone
|
Grey and red layers, streaks brows
|
|
Conglomerate
|
sedimentary rock composed largely of gravels.
|
|
Ice wedging
|
Mechanical weathering process that occurs when water freezes in the cracks of rocks and expands, causing the rock to break apart
|
|
sediment
|
matter deposited by some natural process
|
|
fossils
|
remains or traces of acient life
|
|
precipitation
|
process of forming a chemical precipitate
|
|
Unsorted
|
no order of layering or size
|
|
coastal beaches
|
surf zone; sediment constantly being processed by wave attack; well-sorted
|
|
Stratification
|
The layering of sedimentary rock. Also called bedding.
|
|
cement
|
the minerals that fill sediment pores and cement the rock together
|
|
Types of Cement
|
A) Quartz
B) Calcite
C) Hematite
D) Barite
|
|
Climate
|
Average weather pattern in an area over a long period of time; can be classified by temperature, humidity, precipitation, and vegitation
|
|
cross bedding
|
inclined layer of sediment deposite across hoorizontal surface
formed on sandy beaches, migrating sand dune
|
|
sedimentary structures: cross bedding
|
indicates current direction
wind, water
|
|
clastic and chemical
|
two groups of sedimentary rocks
|
|
Greywacke
|
- Fine grained Matrix
- Usually from turbidity currents
|
|
Deposition
|
dropping of sediments. Occurs when agents of erosion(water, wind, glacier) can no longer carry the sediment.
|
|
James Hutton
|
father of modern geology; principle of uniformitarianism
|
|
mud crack
|
a feature in some sedimentary rocks that forms when wet mud dries out, shrinks, and cracks
|
|
Mudstone
|
a rock that breaks into chunks or blocks.
|
|
Texas State Capitol
|
-Made of granite
-Almost made of limestone
-Paid for with 3 million acres of land
-That land became XIT ranch
|
|
Longshore current
|
current that runs parallel to the shore line at slight angels, and moves tons of loose sediments
|
|
grain size:medium
|
made of sand, form sandstone (pure quartz sand) arkose (sand size quartz plus feldspar makes it pink) graywacke (mixture of different clast sizes), tend to be 2-.063mm
|
|
shale
|
only rock that does not cement because the pore spaces are too small
|
|
Clay
|
so small, its too fine to even "feel"
|
|
Where are calcerous deposits found?
|
From the Northern Hemisphere's perspective, the southern oceans.
|
|
Particle size
|
Refers to diameter of clasts making up a rock. Names used for clast size from coarsest to finest are: boulder, cobble, pebble, sand, silt, and clay.
|
|
Mass movement
|
Ant type of erosion that occurs as gravity moves materials down slope
|
|
Sedimentary Rocks
|
Rocks that are mostly found on the exposed surface of Earth, made of sediments, and form in layers
|
|
fossil, p 23
|
the remains or traces of organisms preserved from the geologic past
|
|
Bioclastic sedimentary rock
|
made by living organisms or composed mostly of materials from life forms. Also called organic sedimentary rock.
|
|
clastic sedimentary rocks
|
made of weathered bits of rocks and minerals: (conglomerate, breccia, sandstone, stiltstone, shale)
|
|
environment of deposition, p 228
|
a geographic setting where sediment accumulates. Each site offers a unique combination of geologic processes and environmental conditons.
|
|
what are Steno's four laws?
|
law of original horrizontality, law of cross cutting relationships, superposition, lateral contituity
|
|
nonclastic texture, p 228
|
a term for the texture of sedimentary rocks in which the minerals form a pattern of interlocking crystals.
|
|
What is a fossil and what types of things become fossils?
|
evidence of ancient life; animal bones, shells, plant remains
|
|
Lignite
|
|
|
Rock gypsum
|
|
|
organic
|
carbon-based compound
|
|
chemical
|
evaporites
calcite, halite, gypsum
|
|
Sediments
|
solid particles (clasts)
|
|
Meander
|
curve in a river
|
|
Compaction
|
Accumulation of sediments, usually deltas in rivers
|
|
Wentworth Scale
|
List of Rock Sizes:
-Boulder...Foot
-Cobble
-Pebble...Thumb
-Gravel
-Sand...Sugar
-Silt
-Clay...Flour
|
|
detrial
|
mineral/rock fragments produced by mechanical weathering or erosion
shale, sandstone, and mudstone
|
|
Breccia
|
rock composed of sharp-angled fragments embedded in a fine grained matrix
|
|
geographic locations
|
Formations were named after
|
|
fine clastics
|
composed of silt and clay
|
|
formation
|
strata recognized on a regional scale
|
|
Coquina (hash of fossil fragments)
|
clastic, cpo
|
|
Streams
|
the second most powerful erosional force on Earth
|
|
Conglermerate
|
-large fragments ranging from gravel to boulders,
-any mineral composition
-porosity and permeability depend on degree of cementation
|
|
chalk
|
soft compact calcite, CaCO3, with varying amounts of silica, quartz, feldspar, or other mineral impurities, generally gray-white or yellow-white and derived chiefly from fossil seashells
|
|
Aridisol
|
Low in organic matter, has carbonate horizons. Forms in arid environments (e.g. Western US)
|
|
well sorted clast
|
uniform grain size, steady energy
|
|
Sorting
|
Indicates the degree to which the clasts in a rock are all the same size or include a variety of sizes. Well-sorted sediment consists entirely of sediment of the same size, where poorly sorted sediment contains a mixture of more than one grain size.
|
|
Inorganic Limestone
|
tan to gray, fizzes in acid
|
|
Moraine
|
Large ridge of rocks and soil deposited by a glacier when it stops moving forward
|
|
organic rock
|
sedimentary rock that forms from remains of organisms deposited in thick layers
|
|
ripple marks
|
sedimentary rock sometimes record the motion of wind and water waves on lakes, oceans, rivers, and sand dunes in features
|
|
coarsed grained detrital sedimentary rocks
|
conglomerate and breccia
|
|
biochemical rocks
|
sedimentary rocks that consist of shell material
|
|
Laminations/laminae
|
Layers within the horizontal beds that may be a different angles/ inclined as cross beds
|
|
Fossil
|
remains, imprints, or traces of a living thing that lived long ago
|
|
Sedimentary rock that can form by both chemical and biochemical processes
|
Limestone
|
|
Conglomerate (texture, type, grain size)
|
Clastic, detrial, coarse grain
|
|
Sed Features: Nodules
|
Rounded rocks of DIFFERENT composition to host rock
Examples: Flint Nodules, Septarian Nodules, Pyrite Nodules, Geodes
|
|
Abrasion
|
A type of erosion that occurs when wind blown sediments strike rocks and sediments, polishing and pitting their surface
|
|
chemical sedimentary rocks
|
formed by precipitation of minerals out of water solutions. this occurs without life activity of organisms.
|
|
chemical weathering
|
minerals in rocks change into new substances
|
|
Claystone
- Fine grained rock
|
clay sized particles, they're smooth
|
|
Deposition (clastic sedimentary process)
|
Settling out of the transporting fluid.
|
|
What are sedimentary rocks?
|
- solidification of loose sediments
- from weathering of preexisting rocks
|
|
the correct sequence of rock forming
|
erosion,deposition compactation and cementation
|
|
Where would you go today to find andhydrite forming?
|
Persian Gulf
|
|
Compare differences between a conglomerate and a breccia
|
Breccia consists of angular fragments(rubble) while in conglomerate the particles show obvious signs of wear(gravel)The difference is the roundness of grains. Conglomerates are more rounded
|
|
Erosion, transportation, deposition, and lithification
|
What are the four major sedimentary processes?
|
|
How are clastic rocks formed?
|
from sediments that have been weathered, transported, or deposited
|
|
Mudstone
- Fine grained rock
|
kinda variation of shale with less sorting (I wouldn't use this term)
|
|
graded bed, p 237
|
a layer of sediment that has larger particles on the top and smaller particles on the bottom. Graded beds change gradually in grain size from top to bottom.
|
|
What does rock salt form from?
|
It forms from halite which is salt in solution.
|