FACULTY : CIVIL & ENVIRONMENTAL ENGINEERING
NO. OF PAGES:
1/2
DEPARTMENT : INFRASTRUCTURE & GEOMATIC ENGINEERING
EDITION: NO. OF CHECKING:
LAB 2a
EFECTIVE DATE :
8/1/2007
AMENDMENT DATE:
4/9/2016
LABORATORY : ENGINEERING GEOLOGY & GEOPHYSICS TOPIC : INCLINED BEDDING - FOLD ( LAB L AB 2a)
1.0 OBJECTIVE To plot ground profile and rock formations from geological map – inclined beddings.
2.0 LEARNING OUTCOMES a) b) c)
Students should able to plot subsurface profile. Students should able to understand the geological structure in subsurface profile. Students should able to understand a history of the geological area.
3.0 THEORY
A geological map is one, which shows in the first place, the occurrence and distribution of the rocks at the surface of the ground. Conventional sign may show certain facts of observation about them. The geological map allows the geological structure of the country to be inferred. Beds of rocks are bounded by bedding surfaces, which may be horizontal, tilted or bent in any form or direction. A series of beds which ha ve been laid down regularly one on the t he other, and which may be treated as a whole, form a conformable series. It follows that the lower beds are the older. In such a series of bedding surfaces are parallel. Each bedding surface is usually common to two beds of rock, being the top of one and the bottom of the one next above. In the simplest case, these surfaces are planes: bedding planes.
Prepared by
:
Lecturer
Name
:
Assoc. Prof. Dr. Aziman Bin Madun / Mohd Hazreek Bin Zainal Abidin
Signature
:
Date
:
4 September 2016
FACULTY : CIVIL & ENVIRONMENTAL ENGINEERING
NO. OF PAGES:
2/2
DEPARTMENT : INFRASTRUCTURE & GEOMATIC ENGINEERING
EDITION: NO. OF CHECKING:
LAB 2a
EFECTIVE DATE :
8/1/2007
AMENDMENT DATE:
4/9/2016
LABORATORY : ENGINEERING GEOLOGY & GEOPHYSICS TOPIC : INCLINED BEDDING - FOLD ( LAB 2a )
4.0 EQUIPMENT AND MATERIALS 1. 2. 3. 4. 5.
Geological Map ( Map 7 – Appendix B ) Graph paper/drawing paper - A4 size Ruler Pencils Colour pencils (optional)
5.0 PROCEDURE 5.1
Plot the cross-section with the horizontal and vertical scales accordingly to the scale of the geological map on a piece of graph paper or blank sheet. Refer Figure 1.1. The vertical scale is normally exaggerated to improve visibility of the profile.
5.2 Draw a line to join the line of cross-section on the map, says A - B. 5.3 Using a blank piece of paper, mark the points of intersection accordingly between the lines with the contours respective to its heights. 5.4 Transfer the points to the cross-section profile respective to the heights of the contours. 5.5 Join the points to form the profile of the ground elevation.
6.0 RESULT AND ANALYSIS By referring to Map 7,
Highlights the rock boundary to focus for determination of strike line. Select two pints within the marked boundary of similar heights. Draw the line between the two points to indicate the first strike line. Its value corresponding to two value of the contour. Select another point (of ascending @ descending contour value). Draw a line that touches the parallel the select point to the first strike line. Measure the distance (say, d1) cut at right angles to the parallel lines. Determine the angle of dip of the fold. Similarly, repeat similar procedure to the other wings of the fold. Identify the thickness of the outcrop.
7.0 QUESTIONS Explain types of fold (with the aid of diagram) and discuss how this structure occurred.
8.0 CONCLUSION Conclude your results especially by rate its effect on outcrop layer in relation to the civil engineering or construction
industry etc.
FACULTY : CIVIL & ENVIRONMENTAL ENGINEERING
NO. OF PAGES:
1/2
DEPARTMENT : INFRASTRUCTURE & GEOMATIC ENGINEERING
EDITION: NO. OF CHECKING:
LAB 2b
EFECTIVE DATE :
8/1/2007
AMENDMENT DATE:
4/9/2016
LABORATORY : ENGINEERING GEOLOGY & GEOPHYSICS TOPIC : FAULT BEDDING ( LAB 2b )
1.0 OBJECTIVE To plot ground profile and rock formations from geological map – faulted bedding.
2.0 LEARNING OUTCOMES a) Students should able to plot subsurface profile. b) Students should able to understand the geological structure in subsurface profile. c) Students should able to understand a history of the geological area.
3.0 THEORY A geological map is one, which shows in the fi rst place, the occurrence and distribution of the rocks at the surface of the ground. Conventional sign may show certain facts of observation about them. The geological map allows the geological structure of the country to be inferred.
Beds of rocks are bounded by bedding surfaces, which may be horizontal, tilted or bent in any form or direction. A series of beds which have been laid down regularly one on the other, and which may be treated as a whole, form a conformable series. It follows that the lower beds are the older. In such a series of bedding surfaces are parallel. Each bedding surface is usually common to two beds of rock, being the top of one and the bottom of the one next above. In the simplest case, these surfaces are planes: bedding planes.
Prepared by
:
Lecturer
Name
:
Assoc. Prof. Dr. Aziman Bin Madun / Mohd Hazreek Bin Zainal Abidin
Signature
:
Date
:
4 September 2007
FACULTY : CIVIL & ENVIRONMENTAL ENGINEERING
NO. OF PAGES:
2/2
DEPARTMENT : INFRASTRUCTURE & GEOMATIC ENGINEERING
EDITION: NO. OF CHECKING:
LAB 2b
LABORATORY : ENGINEERING GEOLOGY & GEOPHYSICS
EFECTIVE DATE :
8/1/2007
TOPIC : FAULT BEDDING ( LAB 2b )
AMENDMENT DATE:
4/9/2016
4.0 EQUIPMENT AND MATERIALS 1. 2. 3. 4. 5.
Geological Map ( Map 14 – Appendix C ) Graph paper/drawing paper - A4 size Ruler Pencils Colour pencils (optional)
5.0 PROCEDURE 5.1 Plot the cross-section with the horizontal and vertical scales accordingly to the scale of the geological map on a piece of graph paper or blank sheet. Refer Figure 1.1. The vertical scale is normally exaggerated to improve visibility of the profile. 5.2 Draw a line to join the line of cross-section on the map, says A - B. 5.3 Using a blank piece of paper, mark the points of intersection accordingly between the lines with the contours respective to its heights. 5.4 Transfer the points to the cross-section profile respective to the heights of the contours. 5.5 Join the points to form the profile of the ground elevation.
6.0 RESULT AND ANALYSIS By referring to Map 14,
Determine the dip and strike of the coal seams. Determine the thickness of sandstone outcrop. Determine the dip and strike of the fault. Plot the rock outcrop and fault on the cross-section profile.
7.0 QUESTIONS AND DISCUSSION Explain types of fault (with the aid of diagram) and discuss how this structure occurred.
8.0 CONCLUSION Conclude your results especially by rate its effect on outcrop layer in relation to the civil engineering or construction
industry etc.
APPENDIX B SEMESTER/SESSION : SUBJECT :
ENGINEERING GEOLOGY
COURSE CODE
: :
BFF BFC 21303
y al C
D L O D F N E G E el L a h S
e n ot s d 7 n a p S a M
DO NOT CHANGE THE SIZE
APPENDIX C SEMESTER/SESSION : SUBJECT :
MAP 14
COURSE CODE
ENGINEERING GEOLOGY
: :
BFF BFC 21303
FAULT
F
F
LEGEND Sandstone
Clay F
Shale
F
Fault
DO NOT CHANGE THE SIZE
