Granitic rocks are generally favoured for aggregate production due to the relative ease <strong>of</strong> crushing andshape characteristics (Brand et ai, 1984). Problems, however, have been experienced with poor asphaltadhesion when these materials are used for road pavement This is primarily due to the high free quartzcontent. Rock types such as monzonite and the Tai Po Granodiorite, which have a significantly lower quartzcontent and similar crushing characteristics, may be more suitable for this purpose and should be consideredfor quarrying.From a planning point <strong>of</strong> view, granitic rocks are generally favoured. <strong>The</strong>y require more site formationcompared to the flat superficial deposits, but the moderate slope angles, ease <strong>of</strong> excavation, high yield <strong>of</strong> filland general stability <strong>of</strong> slopes is reflected in the extensive development which already exists on these rocks.3.1.6 Characteristics <strong>of</strong> the Volcanic Rocks<strong>The</strong> location and type <strong>of</strong> volcanic and volcaniclastic rocks found in the study area are discussed in Section2.3.3 and in Appendix C.1.1. Excluding the minor sedimentary member, these rocks tend to have similarmaterial characteristics.<strong>The</strong> engineering behaviour <strong>of</strong> the rock mass is controlled by a combination <strong>of</strong> factors. <strong>The</strong> major factorsare: the frequency, orientation and roughness <strong>of</strong> joints and other discontinuities; the degree and extent <strong>of</strong>weathering; cleft water pressures and permeability characteristics.<strong>The</strong> volcanic rocks <strong>of</strong> the Repulse Bay Formation are generally well jointed. Joint spacing (GeologicalSociety <strong>of</strong> London, 1977) commonly ranges from 'moderately narrow' (20 to 60 mm) to 'wide' (200 to 600mm) or, more rarely, Very widely' spaced (600 to 2 000 mm). Small outcrops that have a joint spacing <strong>of</strong>greater than 2 m tend to stand out on hillsides and ridges as tors. Locally, the joint spacing is very variable,<strong>of</strong>ten ranging from wide to narrow over distances <strong>of</strong> less than 10 m. Most exposures contain several sets <strong>of</strong>joints, each set exhibiting a range <strong>of</strong> orientations. This range is generally related to the persistence <strong>of</strong> thejoints, with less persistent joints being the most variable in orientation. Joints can sometimes be seen tocurve in larger exposures. Persistent joints which exist in well-defined sets tend to be fairly smooth, althoughthey are occasionally striated. Smaller, discontinuous joints are <strong>of</strong>ten irregular and stepped and are <strong>of</strong> lessengineering significance. Many <strong>of</strong> the joints are steeply inclined and may result in 'unfavourable' orientationsin relation to construction. Small wedge and joint controlled failures are visible along the Tsing Yi Road. Siteinvestigations for projects involving rock cut slopes should be designed to identify and define the dominantjoint sets prior to engineering design.In these rocks, weathering tends to be relatively shallow, with average depths in the order <strong>of</strong> 8 to 10 m. <strong>The</strong>volcaniclastic rocks are generally more deeply weathered, and up to 20 rn <strong>of</strong> weathered material is common.As discussed in Section 3.1.1, the depth <strong>of</strong> weathering is largely dependent on the joint spacing. Alongphotolineaments (shown on the Engineering Geology Map), very close jointing may be encountered whichlocally depresses the weathering pr<strong>of</strong>ile. This effect increases the credibility <strong>of</strong> the material by streams. <strong>The</strong>sestreams tend to preferentially follow such lines <strong>of</strong> weakness and can be seen on aerial photographs aslineaments. A major lineament in this study area passes through Tide Cove from Lai Chi Kok and correspondswith a major valley, now filled with alluvium and marine deposits. Characteristics <strong>of</strong> other lineaments arerevealed by tunnelling records and many faults and crushed seams encountered in these excavations can berelated to surface photogeological lineaments. In addition, there are a number <strong>of</strong> hydrothermally alteredzones <strong>of</strong> white clay (kaolinite) and green mica (chlorite). Although the hydrothermally altered zones are notthe result <strong>of</strong> weathering but rather the product <strong>of</strong> the granite batholith emplacement into the volcanic countryrock, the effect is to produce a zone <strong>of</strong> weak erodible material similar to a joint controlled weathering pr<strong>of</strong>ile.Very little water inflow has been reported along these altered zones.On weathering, the volcanic rocks tend to produce a clayey silt with minor sand and a fairly uniform pr<strong>of</strong>ile.<strong>The</strong> coarse tuffs, if widely jointed, may produce corestones and boulders in a similar manner to granitic rocks.<strong>The</strong> higher clay contents <strong>of</strong> the weathered materials tend to reduce the incidence <strong>of</strong> erosion in these rockseven though they occur on steep slopes. <strong>The</strong> GEOTECS data in Tables B10 and B11 and Figures 4 and 8indicate that, except for the more deeply weathered coarse tuffs, the Repulse Bay Formation rocks show ageneral trend <strong>of</strong> relatively low incidence <strong>of</strong> erosion. Due to the large statistical sample and the relative lack <strong>of</strong>major urban development on these rocks, this is probably a good reflection <strong>of</strong> the erodibility <strong>of</strong> thesematerials. <strong>The</strong> incidence <strong>of</strong> instability, as measured by GEOTECS, is slightly above the average compared tothe mean for the insitu terrain in the study area. <strong>The</strong> morphological forms associated with slope failure involcanics are similar to those in colluvium, in that they are characterised by small landslip scars with extensivedebris deposits. That is, they are characterised by large length to width ratios (4 or5:1).When fresh, these rocks generally have a high strength, but the presence <strong>of</strong> joints substantially reduces theeffective mass strength. Due to their fine grain and relatively high strength, these rocks are difficult to crushand are not currently used for aggregate production. <strong>The</strong> narrow joint spacing in many <strong>of</strong> the volcanic rocksmay produce fragments unsuitable for aggregate when crushed. <strong>The</strong> weathered mantle may be suitable fors<strong>of</strong>t borrow, but the shallow weathering depths will limit the potential yield from most sites.33
<strong>The</strong> steep terrain and thin weathered mantle may make many areas <strong>of</strong> volcanic rock unsuitable forintensive development. Large volumes <strong>of</strong> excavation, much <strong>of</strong> it requiring blasting, would be necessary forsite formation, and the resulting slopes may be subject to joint-controlled instability. However, where theserocks occur on flat to gently sloping terrain, their foundation depths are fairly shallow. Recent developmentson Tsing Yi Island have been carried out partly in coarse tuff and shallow stripping depths have beenencountered.Site investigations in the volcanic rocks should be designed to determine the depth and degree <strong>of</strong>weathering, the frequency and orientation <strong>of</strong> jointing and the position and seasonal fluctuations <strong>of</strong> the watertable. <strong>The</strong> Standard Penetration Test can be a useful indicator <strong>of</strong> the depth <strong>of</strong> successive zones <strong>of</strong>decomposition <strong>of</strong> the rock mass. Direct shear tests on the discontinuities <strong>of</strong> Zone C/D rocks, and direct shearand triaxial tests on Zone A/B rocks, can be used to determine the shear strengths <strong>of</strong> joints and soil matrix. Itshould be noted that, because most failures <strong>of</strong> insstu material are shallow, the overburden pressure on a failureplane is probably quite low. Representative shear strength parameters should therefore be obtained fromlaboratory triaxial tests carried out at appropriately low confining pressures.3.1H Characteristics <strong>of</strong> the Metamorphic RocksVery Sittle is known about these rocks within the study area. Dark metamorphosed sulphurous shales andquartzites occur <strong>of</strong>fshore in an area planned for reclamation. <strong>The</strong>se rocks are deeply weathered and occurbeneath, up to 40 m <strong>of</strong> marine deposits and old alluvium. <strong>The</strong>y decompose to a very dense clayey silt that hasSPT values ranging from 20 up to 120. <strong>The</strong> upper value indicates that driven piles may terminate within it.It should be noted that the sulphur derived from pyrites may produce an acid groundwater that could reactwith steel piles or concrete. Chemical analysis <strong>of</strong> the groundwater may indicate the nature and extent <strong>of</strong> thispotential problem.34
- Page 2 and 3: THE UNIVERSITY OF HONG KONGLIBRARY
- Page 5 and 6: Map of the Territory of Hong Kong S
- Page 7 and 8: CONTENTSPageFOREWORD 31. INTRODUCTI
- Page 9 and 10: PageA.8 Engineering Geology Map 111
- Page 11 and 12: List of FiguresFigure TitlePage1 Lo
- Page 13 and 14: 1.1.1 The Centra! New Territories G
- Page 15 and 16: 1.5.4 Erosion Map (EM)This map is t
- Page 17 and 18: Table 1.3 GLUM Classes and Landslip
- Page 19 and 20: The geological boundaries for the b
- Page 21 and 22: (a) Volcanic coiluvium (Cv)—This
- Page 23 and 24: The most common occurrence of this
- Page 25 and 26: Areas subject to erosion are classi
- Page 27 and 28: SquattersSquatters appear to be loc
- Page 29 and 30: 3. ASSESSMENT OF3.1 Description and
- Page 31 and 32: material density but undisturbed sa
- Page 33 and 34: Table 3.1Description and Evaluation
- Page 35: As with the volcanic rocks, the fre
- Page 40 and 41: Reference should be made to the Geo
- Page 42 and 43: Area 6Area 7Area 8Area 9Tai Mo Shan
- Page 44 and 45: The area is entirely underlain by v
- Page 46 and 47: Approximately 5% of the terrain has
- Page 48 and 49: Most of the ridgecrest terrain fall
- Page 50 and 51: 5.The findings reached during the C
- Page 52 and 53: 6.Addison, R. (1986). Geology of Sh
- Page 54: So, C. L (1971). Mass movements ass
- Page 57 and 58: ~?m^^iz$$m&' f ; v> ;,'2r„' •;
- Page 59 and 60: CLASS IV (26.0%) /UNCLASSIFIED (2.0
- Page 61 and 62: F F A R Rx, v v R R flv A >- ( R R
- Page 63 and 64: 4?s*-# ••*••••• #rf
- Page 65 and 66: + + ® m+ *-*=[_! 5-Bailie]*;*- + *
- Page 67 and 68: O)44 • • •4 • 4 • +++ •
- Page 70 and 71: I1 Fig. 1Location map ofthe Central
- Page 72 and 73: W TP flj? W-fi I OIM INUIIixTYa-n'
- Page 74 and 75: Scale1:20 000Example of the Geotech
- Page 76 and 77: Scale1.20 000Example of the Physica
- Page 78 and 79: Scale1:20 000Example of the Enginee
- Page 80 and 81: Scale1:20 000Example of the General
- Page 82 and 83: Example of the Landform Map (LM)Sca
- Page 84: Scale1:20 000Example of the Erosion
- Page 87 and 88:
Plate 2.Oblique Aerial Photograph L
- Page 89 and 90:
Plate 4. Oblique Aerial Photograph
- Page 92 and 93:
Plate 6.Oblique Aerial Photograph o
- Page 94 and 95:
Plate 8.Oblique Aerial Photograph o
- Page 96 and 97:
Plate 10. Low Level Oblique Aerial
- Page 98 and 99:
Plate 12. Ridgecrest Erosion on the
- Page 100 and 101:
1 S';: ; f -;,Plate 14.Low Volcanic
- Page 102 and 103:
Plate 16.Upper Sideslope and Ridgec
- Page 104 and 105:
BBBBI BHHH........ ... :,.;, • Il
- Page 106 and 107:
AOF EVALUATION ASSOCIATED TECHNIQUE
- Page 108 and 109:
GeneralisedLimitations andEngineeri
- Page 110 and 111:
In this study, all the footsSope an
- Page 112 and 113:
A.7 Geotechrsical Land Use MapThe G
- Page 114 and 115:
(b) Records of a limited amount of
- Page 116 and 117:
A.9 Generalised Limitations and Eng
- Page 118 and 119:
Table A4Criteria for Initial Assess
- Page 120 and 121:
The information presented in the GL
- Page 122 and 123:
APPENDIX BTableDATA TABLES FOR THE
- Page 124 and 125:
Table B4 Aspect and Slope GradientA
- Page 126 and 127:
Table B8Geology and GLUM ClassGeolo
- Page 128 and 129:
Table B10Slope Gradient, Aspect Geo
- Page 130 and 131:
Table B12Existing Land Use (From ae
- Page 132 and 133:
cINFORMATIONPageC.1 Description of
- Page 134 and 135:
Jointing within this rock type is u
- Page 136 and 137:
6040Marine deposit - sands, silts a
- Page 139 and 140:
The rock is pale grey or pink when
- Page 141 and 142:
Within Tide Cove itself, this basal
- Page 143 and 144:
of Reports4 - 6per §riil black hel
- Page 145 and 146:
RAINFALL(mm)ro14s*en c33Q)CD3O 3339
- Page 147 and 148:
Table C2Selection of Aerial Photogr
- Page 149 and 150:
DOF AND CHARACTERISTICS ONIN HONG K
- Page 151 and 152:
The more randomly oriented, smoothe
- Page 153 and 154:
ROCKMASSCHARACTERISTICSJOINTSFAULTS
- Page 155 and 156:
D.2.5FaultsA fault is a fracture in
- Page 157 and 158:
(e) Basements—these require tanki
- Page 159 and 160:
(iv) S/te InvestigationIn heterogen
- Page 161 and 162:
D.3.11Site InvestigationA 'desk stu
- Page 163 and 164:
Irregularities in slope profile can
- Page 165 and 166:
CHUNAMCement-lime stabilised soil u
- Page 167 and 168:
INCISED DRAINAGE CHANNELTerrain com
- Page 169 and 170:
SHEETING JOINTDiscontinuity produce
- Page 171 and 172:
This book is due for return or rene