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Tv
Tv/Rc/O
Gt
Gh/O
Tv/Rc
Tv/R
CfCv/RcTv
Cv/Rc
Tb/OTv/Rc/R
Tv/CvTv/Rr
Rc/Tv
R
Tb//O
ObTv/Cv//R
TvG
Tv/Rc/RCv
Cv
Cv R//Tv
Tv/Cv
Tv/Rrc/TbTb
Tb/O
Rrc/Rr/Tv
Tb/Tv/O
Tv//Rc
GhTb/OOpRc/Tv
Tb
Tv
Tv/R//Tb
Tv
Gt/Ge
Tv
TbTv//O
Tv/O
Gh/O/R
Rc/Tv/RRrc/Tv/RrCvCv
Tb/Tv/OGv/R
Gv/RcTv/Rc
Tv/R G/R/O
Cv
Cv
Tv/Rc/OTb/O
Tv//R
Gh
Tv/Cv
Tb/Tv
CvTvTv/Rrc/Tb
Rc/TvR
Tb/OGb/Gv
Fp
Gh Gb Tb//OGr/Gk
Tv/Rc//R GbR
Rc/R/Tv
Tv/Rc/R-O
R/Gv
Rc/Tv/RTe/Tv/Rc
Tb/Rrc
Rc/R/Tv
Tp//O
OpTe/Re
Rc/Tv/O
Tb/TvTv//O
Gh/R
Tv//R
Rc/R/TvTv
Tv
Cv
Tv/O
Tv
Tv
O/TCv
Tv/RcTv
Tb/Te
Tb
TbCb/Cv/R
Tv/Rc/RRe
Tv/Rc/R Gh
Tv/O
TbTv/R
Tb/Tv/OGb//Gr
Tb
GtTv
Gt
CvTv/RR/Rc/Tv
Tb
Tv/CvTv
Tv/Rc
Tv/Cv/R Tv/Rc/R Tv/RcGb ThTb
Cv/Tv
Tv
TbGb TvTbRTv/Rc/R
GbCv/RcTb Tv//R
Tv/Rc
Tv/Rc Tv/Rc/Tb Tv//OTh Tb/Tv
Gp
R//Tv-O
Tv/Rc
R/Rc/Tv
R/Rc/Tv
Gb
Gb
Gb
Gb
Lp
Rrc/Rc/Tv
Tv/Rc/R
Tv/Rc/R
Gb//O
Tv//Rc
Tv//Rc
Gp//O
Tv
TV/Rc/ORc/Tv/R
Tb/Tv
Tv/RcRc/Tv/R
Rc/Tv/OG/Gt
R/Tv/Rc
R/Tv/Rc
Rc/R/Tv
Tv/Rc
Tv/Rc
Tv
TV/Rc/O
Tv//Rc
Rr//Tv
Tv/Rc
Tv/Rc
Tv/R
Tv/Rc/Rr
Tv/Rc
Tv/R
Tv/Rrc/Rr
Tv/Rrc
Tv/Rc/O Rrc/Tv//O
Rc/R/TvR/Tv/Rc
Tv/Rc
Te/TbTv/Rc/O
TbTb
Tv/Rc/OTv
Cv
Fp
Fp
Tb Tb
Tb
Tb
Tb
Tb
Rc/Tv
Tv/G//OTv
Tv/G//OTv/G//O
Tv//R
Tv//R
TbTr
Tr
TrTr
Th//O
Th
Th
Th
Th
Th
Th
Cv/TvR
Tv/Rc
Tv/Tb
Tv/R
Tv//Rc
Gt
R
R//Tv
Tv/Rc
Tv/R
Tv/Rc
Tv//O
Rc/Tv/R Tv/Rc//O
Gr
Rc/R/Tv
Tv
Tv/O/Rc
Tv/Rr
Cv/Rc
O/Tv
Tv/Rc
Tb
Gb
RTb
FpGp
Tb/O
Tv/Rc/R
Tv Tv/Rc/O
Tv/Rc
Tv/Rc/O
Tv
Th Th
CaCa
CaTv//R
Tb/O
Tb
Rc/Tv
Rc/Tv/R
Tv/O
Rc/R/Tv
Rc/R/Tv
Tv//Tb
Tb/Tv
Tb/Tv/O
Rc/R/Tv
R//Tv
R//Tv
Rc/Tv/R-O
Rc/R/Tv
Tv/Cv Tv//O-Tb
Tb
TbTb
Ge
GeGt//Ge
Ff
Ge
Gt//Ge
TbTb
Tb
Gh/Gk
Rc/Tv/R
Tv/Tb/O
Tb//O
LrFp
Fp
Gt
Gt/Ge
Ge
Ge
Tv
Tv Tv/Rc/R
Tv/Rc
TvRc/Tv/R
Tv
Tv
Tv
Gp
Gp
Th/Lp
Gb
Gb
LpLp Lp
LpLp
Tv
TbTh
Tv
Gt/Ge
Gh Gh Tb/O
Tb
Th
Th
Tb//O Tv/RcRc/R/Tv
Lp/T//R
Lp
TvTv/Rc
Tb
Gh
Tv/R
Tv/Rc
Tv/Rc
Tv/Rc
Tb
Tb/Tv/OTv/R
Tb/TvTv/Rc
Tv/Rc//R
Tv
Tv/Rc/R
Th
Rc/Tv/R
Rc/Tv/R
Tb/Tv/O
Tb/Fp
Rc/Tv/R
Te
Tb
Tb/Tv-O
Tv
Gh/O
Tb/Tv/O
Tv/Tb/Rc
Tv
Tv/Rc
54o45'61o30'
54o45'61o00'
54o30'61o00'61o30'
54o30'
MISTINIPPI LAKES
N E
G A
M O O
K
L A K E
K A N A I R I K T O K
R I V E R
1
2
2
21
1
LEGENDEach outlined area is assigned a classification consisting of up to three genetic categories and modifiers that designate the types ofdeposits within each area. Each category within a classification is listed in order of dominance and is separated from the other categories bya slash (e.g., Tv/R). Generally, the areas are divided so that up to three landforms or deposit types are identified within a given area. Theclassification system is also used to denote the approximate percentage of landforms occurring within an outlined area, but those whichform less than 5 percent of the area are not included in the classification. Four variations of the landform system are as follows:
Where three different landforms are included in a single map unit they are each separated by a single slash (/) and their relativepercentages are (60 - 80), (15 - 35), and (5 - 15).Where two landforms are included in a single map unit, a double slash (//) or single slash (/) is used to separate them, and theirrelative percentages are (85 - 95) // (5 - 15) for double slash, or (60 - 85) / (15 - 40) for a single slash.A hyphen between two landform types indicates that they are approximately equal in area. For example, Tv-Rc indicates that tillveneer and rock concealed by vegetation or a thin regolith are equal in area.A composite symbol is used to show combinations of the above cases. For example, indicates that about 60 - 85 percent of thearea is covered by fluvial sediment, 15 - 40 percent by glaciofluvial sediments, and is underlain by till.
GENETIC CLASSIFICATION
Rock
Alluvium consisting of silt and clay to bouldery gravel, forms terraces and plains associated withmodern stream channels, their floodplains and deltas; usually less than 1 m thick; deposited byfluvial action at or below maximum flood levelsCoarse-grained bedrock derived materials; may include sand, silt or clay; accumulates on the lowerparts, or at the base of steep rock faces; transported by gravity
Medium-to fine-grained sand and silt, well sorted, poorly compacted; commonly forms as dunes upto 10 m high; transported and deposited by wind
Fine-grained sand to coarse-grained cobbly gravel; forms plains, ridges (eskers), hummocks,terraces and deltas; generally greater than 1 m thick; deposited as outwash in an ice-contact orproglacial positionSilt, clay, gravel and sand; forms as plains and blankets; silt and clay is deposited in freshwaterlakes from suspension, sand and silt by lake-floor currents, gravel and sand by shoreline waveactionClay, silt, gravel and diamicton; sand is present in some places, generally moderately to well sortedand commonly stratified, but may be massive; forms beach ridges, deltas, terraces and barsdeposited in a marine environment; gravel and sand are formed by shoreline wave action; mayinclude shells, clay and silt deposited from suspension and turbidity currents; gravel is generally awavewashed lag
Includes all types of till; composed of diamicton; transported and subsequently deposited by/or fromglacier ice with no significant sorting by water. These include relatively thin (Tv) or thicker (Tb, Te,Tp, T) till with little or no surface expression; features produced by actively flowing ice (Td, Tl, Tr) orsediment deposited through ice disintegration (Th, Tk)
Bedrock, either exposed (R) or concealed by vegetation (Rc)
MORPHOLOGY
SymbolDepositionalEnvironments Origin and Characteristics of Materials
Symbol Morphology Description
a A relatively gentle slope at the foot of a steeper slope, commonly used to describe colluvium at thebase of a rock escarpment; consists of materials derived from the usually steeper upper slopeAny deposit greater than 1.5 m thick; minor irregularities of the underlying unit are masked but themajor topographic form is still evidentVegetation mat developed on either colluvial surfaces or a thin layer of angular frost-shattered andfrost-heaved rock fragments overlying bedrock; includes areas of shallow (less than 1 m),discontinuous overburdenElongate ridge(s) between 1.5 and 20 m high, 20 and 300 m wide, and 200 to 5000 m long; ridgeshave a rounded end pointing in the up-ice direction and gently curving sides that taper in the down-ice direction; exhibit a convex longitudinal profile, commonly with a steeper slope in the up-icedirection; consist of subglacially formed deposits shaped in a streamlined form parallel to thedirection of glacial flow; commonly consist of till, although some may contain stratified drift; mayhave a rock coreA series of closely spaced gullies or deeply incised channels; can have a dendritic pattern or may bea single straight or arcuate channel; gullies and channels may contain underfit streamsA gently sloping accumulation of debris deposited by a stream issuing from a valley onto a lowland;has its apex at the mouth of the valley from which the stream issues; the fan shape results from thedeposition of material as the stream swings back and forth across the lowland; fluvial fans areusually derived from eroded glacial and glaciofluvial deposits; glaciofluvial fans (deltas) aredeposited in standing water rather than in a terrestrial environment; colluvial fans are derived frombedrock and are usually steeper (i.e., cone shaped)An apparently random assemblage of knobs, mounds, ridges and depressions without anypronounced parallelism, significant form or orientation; formed by glacial melting during icestagnation and disintegration. Includes subglacial, englacial, supraglacial and stratified materials
A basin or bowl-shaped closed depression or hollow in glacial drift; results from the melting of aburied or partly buried detached block or lens of glacier ice; commonly occurs in association withhummocksElongate spindle-shaped ridge(s) between 6 and 60 m high, 75 and 300 m wide and up to 4000 mlong; ridges are commonly straight sided, taper at one or both ends, and have a flat longitudinalprofile; consist of subglacially formed deposits shaped in a streamlined form parallel to the directionof ice flow; commonly consist of till, although some may contain stratified drift; may have a rockcore. Includes slope lineated bogs (Ol)A comparatively flat, level, or slightly undulating tract of land; materials are either till, glaciofluvial,alluvial, marine, lacustrine or organic sediments; bedrock features are commonly masked by theoverlying sedimentsNarrow, elongated and commonly steep-sided feature that rises above the surrounding terrain;materials are either rock, till, glaciofluvial, fluvial, marine, lacustrine, aeolian, or organic sediments.Includes string bogs (Or)Long, narrow, level or gently inclined step-like surface, bounded along one edge by a steeperdescending slope or scarp and along the other by a steeper ascending slope or scarp; materials areeither till, glaciofluvial, fluvial or lacustrine sediments; generally formed by fluvial and glaciofluvialerosion or marine wave actionAny deposit less than 1.5 m thick; morphology of the underlying unit is evidentA thin layer, generally less than 1 m thick, of frost-heaved and frost-shattered bedrock fragmentsCommonly used to indicate numerous esker ridges that are closely spaced; can be used where anygenetic category exhibits numerous surface expressions in a small area, and in which no singleelement can be defined at this scale
SURFICIAL GEOLOGYSNEGAMOOK LAKE MAP SHEET
(NTS 13K/11MAP 2007-03
Geology by S.J. McCuaigGIS / digital cartography by T.J. Sears.Digital elevation data supplied by the Shuttle Radar Topography Misssion (SRTM) , a partnership between NASA and the National Geospatial-Intelligence Agency (NGA). Flown aboard the NASA Space Shuttle Endeavour (11-22 February 2000). Additional information availablefrom:.http://edc.usgs.gov/products/elevation/srtmbil.htmlCopies of this map may be obtained from the Geoscience Publications and Information Section, Geological Survey, Department of NaturalResources, P.O. Box 8700, St. John’s, NL, Canada, A1B 4J6Department: http://www.nr.gov.nl.ca/nr/Geological Survey: http://www.nr.gov.nl.ca/mines&en/geosurvey/e-mail: [email protected] FILE 013K/11/0291
PUBLISHED 2007References:McCuaig, S.J. and Smith, J.S.
2005: Quaternary Geology of the Snegamook Lake Area, Central Mineral Belt, Labrador. In Current Research, Newfoundland andLabrador Department of Natural Resources, Geological Survey, Report 05-1, 15-26.
McCuaig, S.J. and Taylor, D.M.2005: Till geochemistry of the Snegamook Lake area. Newfoundland and Labrador Department of Natural Resources, GeologicalSurvey, Open File 013K/0283, 134 pages.
Recommended citation:McCuaig, S. J.
2007: Surficial Geology of the Snegamook Lake Map Sheet (NTS 13K/11). Geological Survey, Department of Natural Resources,Government of Newfoundland and Labrador, Map 2007 - 03 Open File 013K/11/0291
Note:Open File reports and maps issued by the Geological Survey Division of the Newfoundland and Labrador Department of Natural Resources aremade available for public use without being formally edited or peer reviewed. They are based upon preliminary data and evaluation.The purchaseragrees not to provide a digital reproduction or copy of this product to a third party. Derivative products should acknowledge the source of the data.Disclaimer:The Geological Survey, a division of the Department of Natural Resources (the “authors and publishers”), retains the sole right to the original dataand information found in any product produced. The authors and publishers assume no legal liability or responsibility for any alterations, changesor misrepresentations made by third parties with respect to these products or the original data. Furthermore, the Geological Survey assumes noliability with respect to digital reproductions or copies of original products or for derivative products made by third parties. Please consult with theGeological Survey in order to ensure originality and correctness of data and/or products.
Tv
Tb, Te, Tp, T
Th, Tk
Td, Tl, Tr
F/GT
25A
24P 14M
24I 14L
24H 14E 14F
24A 14D 14C
23O 23P 13M 13N 13O
23J 23I
23G 23H
23B 23A
22P
13L 13K 13J
13E 13F 13G
13D 13C 13B
13I
13H
13A
12P
3E
3D
2M
62o
62o
60o
58o
56o
54o
60o
59o
57o
56o
55o
54o
53o
51o
60o
58o
59o
58o
57o
56o
55o
54o
53o
61o61o
52o
60o
54o64o66o
68o
64o66o
68o
51o51o
LABRADOR0 100 200 300
km
Index Map
M
L
G
E
C
FFluvial
Colluvial
Aeolian
Glaciofluvial
Lacustrine
Marine
Glacial
Rc
R
b
apron
blanket
c concealed byvegetation
d drumlinoid
e eroded anddissected
f fan
hummockh
kettlek
lineatedl
plainp
ridger
terracet
veneervweatheredcomplex
wx
Poorly drained accumulations of peat, peat moss and other organic matter; developed in areas ofpoor drainageO
Bog
1.
2.
4.
3.
Text
Text
Taylor, D.M.2001: Newfoundland and Labrador Striation Database, Version 4. Newfoundland and Labrador Department of Natural Resources,Geological Survey, Open File NFLD/2195.
GEOLOGICAL
SURVEY
NEWFOUNDLAND
AND LABRADOR
1864
Department of Natural ResourcesGeological Survey
10123
Kilometres
MAP 2007-03
SNEGAMOOK LAKENEWFOUNDLAND & LABRADOR
SYMBOLSGeological boundary . . . . . . . . . . . .
Scarp face at edge of terrace . . . . . .
Cirque . . . . . . . . . . . . . . . . . . . . . . . .
Esker (flow direction known orassumed, unknown) . . . . . . . . . . . . .
Meltwater channel (small, large) . . . .
Crestline of major moraine ridge . . . .
Trend of ribbed or minormoraine ridges . . . . . . . . . . . . . . . . .
Beach ridges . . . . . . . . . . . . . . . . . .
Crevasse fill ridge . . . . . . . . . . . . . .
Sand dunes . . . . . . . . . . . . . . . . . . .
Drumlin (direction known,unknown). . . . . . . . . . . . . . . . . . . . . .
Crag-and-tail hill . . . . . . . . . . . . . . . . .
Fluting . . . . . . . . . . . . . . . . . . . . . . . .
Rôche moutonnée . . . . . . . . . . . . . . .
Striation (direction known, unknown)(numbers indicate relative age) . . . . .
Avalanche track . . . . . . . . . . . . . . . . .
Kettle hole (small, large) . . . . . . . . . .
Sinkhole (small, large) . . . . . . . . . . . .
Observation site . . . . . . . . . . . . . . . .
Delta . . . . . . . . . . . . . . . . . . . . . . . . .
Note: All symbols and classifications may not occur on this map.Elevation in metres above mean sea level. Contour interval 20 metres.
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