Title: Identification and Classification of rock
1Identification and Classification of rock
- Part 1
- Rock Identification and Description
2Classification and Engineering Description of
Rock
- Introduction Eurocode 7 EN ISO 14689
and BS5930 - Primary concept Rock Material v Rock Mass
- Identification of Rock type (lithology)
- What should be included in a rock description
- Discontinuities and structure
3Definitions
- Rock
- - Eurocode 7 naturally occurring assemblage
of - minerals, consolidated, cemented or bonded
so as to - form material of generally greater
strength or - stiffness than soils
-
- Geoguide 3 (HK) any naturally formed earth
material which cannot be broken down by hand into
its constituent grains, or may only be partially
broken down by hand depending on its weathering
condition - Our definition Cannot be worked with hand tools
4Definitions
- Rock material (part a)
- the rock which makes up the blocks within the
framework of discontinuities - Rock Mass (part b)
- the rock together with its discontinuities and
weathering profile
5Rock Material and Rock Mass
- Describe the material and identify rock type
this can be done from hand specimens or in the
field - Describe the rock mass characteristics - this
includes the orientation, nature and condition of
the discontinuities which separate the rock
blocks. Best done in the field but some
quantification can be made from rock core
extracted from a borehole
6The Engineering Description
- Formal system of rock description
- Conveys a sense rock strength, condition and
possible susceptibility to future changes - Provides a set of terms with defined meaning
- Comprehensive,
- meaningful concise
- Its good news
7Identification and Description of Rock
- Description of rock
- A statement describing the physical nature,
composition - and state of the rock
- Visual examination
- Simple tests in the field
- in situ or hand specimen
- Observation of site conditions, geological
history. - Classification (Identification of rock type)
- Assigning the correct petrological name (see
Table A.1 ) - Usually from hand specimen, but may require thin
section for specialist engineering applications
(e.g. tunnelling)
8Petrological Classification of Rock
- ROCK NAME always in CAPITALS
- (Refer Simplified Classifications and Table A.1)
- Based on geological origin, mineralogy and grain
size - Often of some engineering significance e.g.
- -SLATE cleavage imparts strength anisotropy
- -GRANITE strong when fresh but weathers to a
residual soil - -LIMESTONE soluble in water, may contain karst
features -
9Rock Identification (rock name)
- See Aide memoirs for identification
- Genetic group Igneous plutonic volcanic
Metamorphic - Sedimentary clastic, chemical, organic
- Grain size
- Minerals composition
- Texture and Fabric
- Other (voids )
10General Description Description of Rock Material
- Description of Rock Material
- Colour
- Grain size
- Matrix
- ROCK NAME (in CAPITALS)
- Weathering or alteration
- Carbonate content
- Stability when exposed to a new water or
atmospheric environment - Strength
-
- Eurocode 7 BS5930
-
11Description of Rock colour
- Systematic approach to colour descriptions
- Colour charts are useful as everyone sees colours
differently
12Description of Grain Size
- Key parameter in petrological classifications
- (See Table A.1 Aid to rock Identification)
- Grain size influences engineering behaviour
- Predominant grain size of the minerals or rock
fragments - May be necessary to describe both the clasts
(grains) - and the matrix (ground mass)
13Description of Grain Size
- Grain size
- very coarse grained
- 63mm ----------------------------------
- coarse grained
- 2mm ----------------------------------
- Medium grained
- 0.063mm ----------------------------
- Fine grained
- 0.002mm ---------------------------
- Very fine grained
14Description of Rock Material texture
- Texture refers to individual grains and
- their relationship or arrangement
15Description of matrix
- Definition relatively fine grained material in
which the coarser fragments or crystal are
embedded - - describe particle size and mineralogical
composition. - e.g. - Very fine grained argillaceous
- - orangey brown ferruginous
- - grey micritic calcareous
- - siliceous
16Carbonate Content
- Carbonate content determined by reaction to
dilute HCL - Carbonate free no effervescence
- Calcareous clear, but not sustained
effervescence - Highly Calcareous strong and sustained
effervescence - Note Wet or moist surfaces delay the reaction
- Dolomitic rocks will react when grains
are crushed
17Stability of rock material
- Degradation of rock material when exposed to a
new water or atmospheric environment - Stable no change
- Fairly stable specimen surface crumbles
- Unstable specimen disintegrates
- This highlights the inter-grain bond strength.
So friable - sandstones, sedimentary rocks with some clay
content - and weathered igneous and metamorphic rocks may
crumble. - Rocks containing swelling clay minerals may
adsorb moisture - from the air and spall.
18Stability of rock material in water
- After soaking for 24 hours
- Term Description Grade
- Stable No Changes 1
- Fairly stable A few fissures, surface crumbles
slightly 2 - Many fissures, breaks into small lumps, surface
crumbles highly 3 - Unstable Disintegrates ,or most of the surface
crumbles 4 - Whole specimen becomes muddy or disintegrates
into sand 5
19Description of Rock Material Strength
- Unconfined Compressive
- Strength (MPa)
- Extremely weak Indented by thumb nail (soils)
lt1 - Very Weak crumbles under firm blows with point
of geological hammer 1 5 - Can be peeled by a pocket knife
-
- Weak difficult to peel with a pocket knife,
shallow indentations made by 5 - 25 - firm blows with pointed end of geological
hammer - Medium strong Cannot be peeled or scraoed by a
pocket knife 25 50 - Can be fractured by single firm hammer
blow - Strong Requires more than one firm hammer blow
to fracture 50 100 - Very strong Requires many blows to fracture
100 250
20General Description General Information
- Additional information and minor constituents
- Abnormal minerals, vugs or voids with description
of size and mode of origin - Fossils
- Other
- Geological Formation From geological maps or
memoirs - Prefer to put this in brackets
- May or may not indicate some engineering
characteristics - Only use if confident
- The Geological Formation or stratigraphic name
- e.g. Sherwood Sandstone
- Woolwich and Reading Formation
21General Description Description of Rock Mass
- Types of rock
- Structure Larger scale interrelations of
geological features and associations between
rock types in-situ. - Discontinuities
- Weathering
- Fracture State
- Groundwater
- Eurocode 7 BS5930
22Description of Rock Mass Structure
- Descriptive terms for sedimentary rocks
- Bedded (well, poorly)
- Interbedded (with.)
- Laminated
- Graded
- Massive (ambiguous term)
- Folded (post-depositional)
23Description of Rock Mass Structure
- Descriptive terms for
- Metamorphic rocks
- Cleaved
- Foliated
- Schistose
- Banded
- Lineated
- Gneissose
- Folded
24Description of Rock Mass Structure
- Descriptive terms for intrusive and extrusive
igneous rocks - - Massive
- - Flow banded
- - Lineated
- - Layered
- - Folded
25Classification and Engineering Description of Rock
- Examples material description
- Very strong, light pinkish white, porphyritic,
coarse grained, slightly weathered to fresh
GRANITE, with feldspar phenocrysts gt6mm. - Strong, thickly bedded, dark grey, medium
grained, crystalline, oolitic LIMESTONE with
micritic matrix and occasional fossils.
Burrington Oolite, Carboniferous. - Very weak to weak, orangey brown, medium grained,
inequigranular, micaceous, friable SANDSTONE.
Quartz grains sub-rounded.