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111 Cards in this Set

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is the study of factors such as origin, occurrence, classification, type and effects of various secondary structures

Structural Geology

is the theoretical and applied science of the mechanical behavior of rock.

Rock Mechanics

is the use of elevation contour lines to show the shape of the Earth's surface.

Topographic Map

are imaginary lines connecting points having the same elevation on the surface of the land above or below a reference surface

Elevation Contours

make it possible to show the height and shape of mountains, the depths of the ocean bottom, and the steepness of slopes

Contours

represent the distribution of different types of rock and surficial deposits, as well as locations of geologic structures such as faults and folds

Geologic Maps

are the primary source of information for various aspects of land-use planning, including the siting of buildings and transportation systems

It is the birds eye view of the earth surface

Map View

Also known as top view

A geologic cross-section shows geologic features from the side view

Cross-Sectional View

Geologic Age Symbol: Q

Quaternary

Geologic Age Symbol: T

Tertiary

Geologic Age Symbol: K

Cretaceous

Geologic Age Symbol: J

Jurassic

Geologic Age Symbol: Tr

Triassic

Geologic Age Symbol: P

Permian

Geologic Age Symbol: |P

Pennsylvanian

Geologic Age Symbol: M

Mississippian

Geologic Age Symbol: D

Devonian

Geologic Age Symbol: S

Silurian

Geologic Age Symbol: O

Ordovician

Geologic Age Symbol: -C

Cambrian

Geologic Age Symbol: p-C

Pre-Cambrian

Youngest to Oldest Geologic Time Period

Quaternary


Tertiary


Cretaceous


Jurassic


Triassic


Permian


Pennsylvanian


Mississippian


Devonian


Silurian


Ordovician


Cambrian


Pre-Cambrian

these folds have the oldest beds in the middle, with beds dipping away from the axis

Anticlines

plunge towards the closed end of the V

Plunging Anticlines

these folds have the youngest beds in the middle, with beds dipping towards the axis

Synclines

plunge towards the open end of the V

Plunging Synclines

is a general term for the orientation of a line or plane.

Attitude

refers to the three dimensional orientation of a planar and linear features such as bed, a joint, a hornblende needle or a fold.

The attitude of planar structure is defined by ..

Strike and dip

describe the orientation of a plane in a space.

Strike and Dip

is the azimuth direction line formed by the intersection of horizontal plane and the plane of interest.

Strike

is the inclination of the plane measured down.

Dip

is a vector—gives the direction and the amount of dip of the plane

examples of planar structure

bedding


fault


fold axial plane


layering of lava


cleavages


schistosity

The attitude of linear structure is defined by ..

Trend and plunge

is the bearing of the line

Trend

is the inclination of the line

Plunge

The acute angle between the line and strike of the plane on which the line lies.

Pitch / Rake

Examples of Linear Structures

Fold axis


hingeline


intersection of two planes


stretched pebbles


other lineations

In this method the compass dial is divided into four quadrants, namely NE, SE, SW, and NW.

Quadrant Bearings

Degrees North and south are at

A compass direction of a line measured in degrees (0-360 degrees) clockwise from north

Azimuth

Brunton Compass properly known as ..

Brunton Pocket Transit

Essential tool for field geologists, environmental engineers, and surveyors

Brunton Compass

The compass was made by ..

Brunton Inc. of Riverton, Wyoming

The year and patent of compass

David Brunton, 1987

Degrees of a Shallow Dip Angle

0°-20°

Degrees of a Moderate Dip Angle

20°-50°

Degrees of a Steep Dip Angle

50°-90°

Types of Dip

True Dip


Apparent Dip

is the inclination of a plane measured in a plane that is not perpendicular to the strike

Apparent Dip

is the inclination of a plane measured in a plane trending perpendicular to the strike

True Dip

This rule is followed by most geologist in the world for consistency

Right Hand Rule

The azimuth direction of the strike is recorded such that true dip is inclined to the right of the observer.

this method is similar to the method trend and plunge of in determining linear attitude.

Dip-line Trend and Plunge

This method relies on the implicit 90 degree angle between true dip azimuth and the strike.

Strike and Dip

Vertical Strata/Bedding

Horizontal Strata/Bedding

Anticline Axis

Syncline Axis

Plunging Anticlines

Plunging Synclines

Strike-Slip Fault

Inclined Bedding

Overturned Bedding

are most effectively displayed on 3D Block diagrams because they display the interpretation of the structure in the subsurface.

Fold Structures

a stack of originally planar surfaces, such as sedimentary strata, that are bent or curved during permanent deformation.

Fold

Metamorphic fabrics

Foliation


Cleavage

points of maximum curvature within a single folded surface.

Hinge

a line when moved parallel to itself “sweeps out” a folded surface.

Axis

The fold axis and fold hinge line have the same attitude.

the plane or surface defined by connecting fold hinge lines in multiple folded surfaces

Axial Plane/Surface

the area of a folded surface between hinge points.

Fold Limbs

a point on a folded surface where the curvature changes direction.

Inflection Point

This is half the distance between hinge points.

highest elevation point on a folded surface.

Crest

lowest elevation point on a folded surface.

Trough

Concave-down folds

Antiforms

Concave-up folds

Synforms

Anticline

Oldest Middle

Synformal Anticlines

Oldest Middle

Syncline

Youngest Middle

Antiformal Syncline

Youngest Middle

Axial Surface


Hinge Line


Hinge Zone


Fold Axis


Hinge Points


Axial Trace


Inflection Point


Limb


Inflection Line


Amplitude


Wavelength


Non-cylindrical Fold


Interlimb Angle


Cylindrical Fold

In the map view a non-plunging fold will have .. .. .. ..

Straight, parallel, contact lines

are produced by geologically significant intervals of time marked by uplift and erosion, or by non- deposition.

Unconformable contacts

contain oldest strata in the core (center) of the structure

Domes

Anticlines

contain younger strata in the core of the structure

Basins

Synclines

have one limb containing overturned strata- otherwise they follow the rules discussed above for anticlines and synclines.

Overturned folds

Overturned Synclines

Overturned Anticlines

Unconformable Contact

simply defined as an exposure of a solid rock on the surface of the earth.

Outcrop

commonly called stereonets, we are just concerned with orientations, alone

Sterographic projections

a diagrammatic representation of the earth's surface or part of it, showing the geographical distributions, positions, etc., of natural or artificial features such as roads, towns, relief, rainfall, etc.

Map

Should include concise information related to geographic information and theme of the map's content

Title

refers to the relationship (or ratio) between distance on a map ang a corresponding distance on the ground

Scale

Should include a north arrow and corner coordinates information

Orientation

Explanation of symbols used in a map including, colors, lines, icons, and symbols

Legend

Selected reference locations or features for orientation

Reference features

Authors, publisher, associated publications; complete bibliographic information

Source information

What was the base source of geographical information if a map, such as a USGS topographic map or satellite image? What was the map projection?

Base map information

What year was the map release? Is the data old or new data?

Date published

Is there a publication associated with this map?

Written text

preserves the same scale in every direction, locally, thus maintaining the correct shape of the features

Conformal

preserves the area throughout, but distorts the shape

Equal Area

depicts the correct distance between a point at the center of the projection and points in any direction away from the center

Equidistant

Shows true angles or bearings, locally

Equal angles

Normal fault

Strike and Dip


Inclined Bedding


Inclined at an Angle

Dome

Basin

Reverse Fault


Thrust Fault

Contact Certain

Contact Inferred

Contacts Inferred Beneath Sedimentary Cover