ATTITUDE OF BEDS Flashcards

(33 cards)

1
Q

Is the study of factors such as origin, occurrence, classification, type and effects of various secondary structures like folds, faults, joints, rock cleavage and are different from those primary structures such as bedding and vesicular structure, which develop in rocks at the time of their formation.

A

STRUCTURAL GEOLOGY

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2
Q

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

A

ROCK MECHANICS

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3
Q

It is that branch of mechanics concerned with the response of rock to the force fields of its physical environment.

A

ROCK MECHANICS

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4
Q

It is an important field in civil engineering as it applies in the majority of infrastructure projects including dams, roads, tunnels, bridges, buildings, and protection of slopes.

A

ROCK MECHANICS

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5
Q

Two important principle components of planar:

A

strike and dip

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5
Q

A general term for the orientation of a line or plane. ______ refers to the three-dimensional orientation of planar and linear features such as a bed, joint or a fold

A

Attitude

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5
Q

A compass direction of the line
measured in degree (0-360)
clockwise from north with
north=0, east=90, south=180,
west=270. Expressed In Three
Digits (000).

A

AZIMUTH

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6
Q

A compass direction
measured 0-90 degrees
from north or south.

A

QUADRANT

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7
Q
  • Also known as top
    view.

-It is the bird’s eye
point of view of the
earth surface.

A

MAP VIEW

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7
Q

Representation of a geometry on
a plane perpendicular to the
earth’s surface.

A

CROSS-SECTIONAL
VIEW

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8
Q

METHODS IN DETERMINING
THE ATTITUDE of planar:

A
  1. Strike and Dip
  2. Right Hand Rule
  3. Dip-Line Trend and Plunge
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8
Q

Sedimentary beds are deposited in

A

horizontal layers,

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9
Q

-Geologic structures: beddings, joints,
faults, axial planes, etc.

A

PLANAR

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10
Q

-This system is used to describe the orientation of inclined
bedding which is named after the two important principal
components in describing 3D spatial orientation.

A

strike and dip

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11
Q

if the layers are no longer horizontal,

A

they have been affected by tectonic forces and have become either tilted, or folded.

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12
Q

-The azimuth direction line formed by the intersection of
horizontal plane and the plane intersect.

A

strike and dip

13
Q

The maximum slope of a plane, measured from horizontal. The ______
direction is always perpendicular to strike.

14
Q

Dip values are always in the range of 0-90. A dip angle of 0 defines horizontal plane with 90 describes a vertically oriented plane

A

0-20 – shallow

20-50 – moderate

50-90 – steep

15
Q

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

16
Q

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

17
Q

Direction of a line of intersection
between a tilted plane and a horizontal
plane.

18
Q

geologist use this instrument to measure strike and dip.

A

BRUNTON OR CLINO COMPASS

18
Q

parts of the brunton compass

A

-mirror
-lift pin for needle
-compass card
-sighting arm
- needle
-bull’s eye level
- clinometer level

19
Q

-This rule is followed by most geologist in the world for
consistency. The azimuth direction of the strike is recorded
such that true dip is inclined to the right of the observer. In
this case, the strike azimuth could be to any quadrant.

A

the right-hand rule

20
-As the name suggests, this method is similar to the method trend and plunge of in determining linear attitude. This method relies on the implicit 90 degrees angle between true dip azimuth and the strike.
DIP-LINE TREND AND PLUNGE
20
is when your are facing the strike direction and your right side is dipping downward.
the right-hand rule
21
-In this method, the observer measures the dip azimuth and then the true dip angle. Because strike of a plane always has a trend of 90 degrees form the dip trend, one may simply record the dip trend and the angle of a plane.
DIP-LINE TREND AND PLUNGE
22
-Two important principle components: trend and plunge -Geologic structures: folds, hinges, elongated minerals, cleavage, bedding intersection, etc.
LINEAR
23
METHODS OF DETERMINING THE ATTITUDE OF LINEAR
1. Trend and Plunge 2. Pitch/Rake
24
-Meanwhile, plunge is the angle of inclination of a line measured in a vertical plane. It is the angle from the horizontal line to the line itself. It shows how the particular line dips with respect to the horizontal line. And plunge ranges from 0-90 degrees.
TREND AND PLUNGE
24
-Is the projecting line onto the horizontal plane. It is the azimuth direction of a line in map view (top view). Since trend is measured in top view, vertical line has no definable trend.
TREND AND PLUNGE
25
This method is used when it is difficult to measure the trend due to the steepness of the plunge.
PITCH RAKE
26
is the angle between the line and the strike of the plain that contains the line.
PITCH RAKE