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! DEPARTMENT OF NATURAL RESOURCES OF NATURAL DEPARTMENT > > Digital elevation model (DEM) from Shuttle Radar Topography Mission (SRTM) data of the of data (SRTM) Mission Topography Radar Shuttle from (DEM) model elevation Digital surface additional provides image The north-east). the from (shaded area map Lamaline information not readily illustrated on the variabilitysurficial map. isTerrain evident, with areas of bedrock highlighted rougher as textured higher, areas (consistent with surficial map), andareas constructional oriented north-south Similarly, areas. textured as smoother shown till thicker of surficial the on identified features to correspond also and evident, are ridges) (till landforms map. 2007: 2007: Surficial Geology of the Lamaline map sheet (NTS 1L/13). Government Department of Newfoundland of Natural and Labrador, Resources,Map 2007-14, Geological Open Survey, File 001L/13/0189. 2001: 2001: Carbon-14 date list for NewfoundlandNewfoundland Geological Department and Labrador, Survey, Open Minesof and Energy, [http://gis.geosurv.gov.nl.ca] 2. File NFLD/2190, Version 2001: 2001: Newfoundland and Labrador Striation Database, Newfoundlandversion 4. and Geological Department Labrador Survey, of Mines Open File NFLD/2195. [http://gis.geosurv.gov.nl.ca] Energy, and Taylor, D.M.and Batterson, M.J. Taylor, Taylor, D.M. Beach ridges . . ridges Beach Geological boundary ...... Geological . boundary . . . . Scarp face at edge of fluvial terrace . Cirque ...... Esker (flow direction known or . . unknown) assumed, Meltwater channel (small, large) . . . . . ridge moraine major of Crestline ribbed of or minor Trend moraineridges ...... ridge fill Crevasse Sand dunes ...... All symbols Note: and classifications may not occur on this map. Elevationinsea feet above mean level. Contour interval50 feet. Geology by M.J. Batterson.Taylor. editing Map by D.M. Paltanavage. digital / T. GIS cartography by Digital elevation Mission data aand the (SRTM), National partnershipsupplied Geo by between the NASA Shuttle RadarTopography Additional informationavailable February 2000). Space ShuttleAgency Endeavor(NGA). (11-22 aboard FlownNASA theIntelligence http://edc.usgs.gov/products/elevation/srtmbil.html DepartmentobtainedtheN mayof Geoscience be mapfromCopies this Publications of InformationSection, and Geological Survey, Box8700, St. John’s,A1BResources, 4J6 NL, Canada,P.O. Department: http://www.nr.gov.nl.ca/nr/ Geological Survey: http://www.nr.gov.nl.ca/mines&en/geosurvey/ e-mail: [email protected] OPEN FILE 001L/13/0189 This map supercedes Map 2005 - 010, Open File NFLD 001L/13/0182 PUBLISHED 2007 References: Note: FilereportsissuedOpenand maps Geological by the Survey Division Newfoundland the of Natural and LabradorDepartmentof Reso made made available for public use without being formally edited or peer reviewed. They are based upon preliminary data and evaluati agrees not to provide a digital reproduction or copy of this product Derivative to a thirdproducts shouldparty. acknowledge t Disclaimer: a division ofThe Geological the Department Survey, of Natural Resources (the “authors and publishers”), retains sole the right and information found in any product produced.The authors and publishers assume no legal liability or responsibility for any alterations, changes or misrepresentations made by third parties with respect to these products or the original data. Furthermore,the Geological Su liabilitywith respectto digital reproductions or copiesoriginal of products or for derivative productsby made third parties. Please consult with the Geological Survey in order to ensure originality and correctness of data and/or products. Recommended citation: Recommended D.M Batterson, M.J. Taylor, and l eir ive the ypes of ypes se which r categories ows: a givenThe area. o o o o o 48 50 49 47 51 0 5 1K 2C 1N 2F o 54 o T 54 F/G Kilometres act of land; materials are either till, glaciofluvial, 1L 01 NEWFOUNDLAND 2D 1M 2L 2E 2M o o 56 56 11I 12I 11P 12H 12A 12P o o 58 58 LEGEND 12G 12B 11O MORPHOLOGY o o o o o 51 50 49 48 47 GENETIC CLASSIFICATION Alluvium consisting siltof and clay boulderyto gravel, forms terraces and plains associated with streammodern channels, their floodplains and deltas; usuallym less than thick; deposited 1 by fluvial action at or below maximum flood levels Coarse-grained bedrock derivedmaterials; may include sand, silt or clay; accumulates lower on the parts, 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 up to 10 m high; transported and deposited by wind Fine-grained sandto coarse-grained cobblygravel; forms plains, ridges(eskers), hummocks, terraces and deltas; generally greater than 1 m thick; deposited as outwash in an ice-contact or proglacial position gravel and sand; forms as plainsSilt, clay, and blankets; siltand clay is deposited freshwater in lakes from suspension, sand and silt by lake-floor currents, gravel and sand by shoreline wave action silt, gravel and diamicton;Clay, sand is present in some places, generally moderately to well sorted and commonly stratified, but may be massive; forms beach ridges, deltas, terraces and bars deposited in a marine environment; gravel and sand are formed by shoreline wave action; may include shells, clay and silt deposited from suspension and turbidity currents; gravel is generally a wavewashed lag Includes all types of till; composed of diamicton; transported and subsequently deposited by/or from glacier ice with no significantThese include sorting relativelyby water. thin (Tv) or thicker (Tb,Te, tillT) with Tp, little orno surface expression; features produced or by actively flowingTr) Tl, ice (Td, sediment deposited through ice disintegration Tk)(Th, Poorly drained accumulations peat, of peat moss and other organic matter; developed in areas of poor drainage A relatively gentleslopeat foota steeper the of slope, commonly A describe used to colluvium the at base of a rock escarpment; consists of materials derived from the usually steeper upper slope Any deposit greater than 1.5 m thick; minor irregularities of the underlying unit are masked but the evident still is form topographic major matdeveloped on either colluvial surfacesthinlayerVegetation angular or a of frost-shattered and frost-heaved rock fragments overlying bedrock; includes areas of shallow (less than 1 m), discontinuous overburden Elongate ridge(s) between 1.5high, and 20 m 20 and 300 wide, m and 200 to 5000 m long; ridges have a roundedend pointing in up-ice the direction and gently curvingsides that taperthe in down- ice direction; exhibit a convex longitudinal profile, commonly with a steeper slope in the up-ice direction; consist of subglacially formed deposits shaped in a streamlined form parallel theto directionof glacial flow; commonlyconsist till, of although some may contain stratifieddrift; may rockhave a core series of closely spaced A gullies or deeplyincised channels; can have a dendritic patternor may a single straightbe or arcuate channel; gulliesandchannelscontain may underfit streams sloping gentlyaccumulation debrisstreamdeposited of valley issuinglowland; by a onto from a a A has its apex at the mouth of the valley from which the stream issues; the fan shape results from the deposition of material as the stream swings back and forth across the lowland; fluvial fans are usually derived from eroded glacial and glaciofluvial deposits; glaciofluvial fans (deltas) are depositedstanding in water rather in than a terrestrial environment; colluvial fans are derived from bedrock and are usually steeper (i.e., cone shaped) apparentlyAn random assemblage of knobs, mounds, ridges and depressions without any pronounced parallelism, significant form or orientation; formed by glacial melting during ice stagnation and disintegration. Includes subglacial,englacial, supraglacialandstratified materials basin or bowl-shaped closed depression or hollow glacialA in drift;resultsfrom the melting a of buried or partly buried detachedblock or lensof glacier ice; commonly occurs in association with hummocks Elongate spindle-shaped ridge(s) between 6 and 60 high,m 75 and 300 m wide and up to 4000 m long; ridges are commonlystraightlongitudinalbotha flatandhavesided, ends, one or at taper profile; consist of subglacially formed deposits shaped in a streamlined form parallel to the direction iceof flow; consist commonly although of till, contain stratified may some may drift; have a rock core. Includes slope lineated bogs (Ol) flat,comparatively level, or slightly undulating tr A alluvial, marine, lacustrine or organicsediments; bedrock features are commonly masked by the overlying sediments elongated and commonly steep-sidedNarrow, feature thatrises above surrounding the terrain; materials are either rock, till, glaciofluvial, fluvial, marine, lacustrine, aeolian, or organic sediments. Includes string bogs (Or) level or gently Long, narrow, inclined step-like surface, bounded along one edge by a steeper descending slope or scarp and along the other by a steeper ascending slope or scarp; materials are glaciofluvial andfluvial by formed generally sediments; or lacustrine fluvial glaciofluvial, till, either erosionactionwave or marine depositAny lessm1.5 thanthick; morphology underlying the of evident unit is generallythin lesslayer, th Bedrock, either exposed (R) or concealed by vegetation (Rc) Origin and Characteristicsof Materials n Morphology Description a plain apron blanket concealed by vegetation Rock drumlinoid eroded and dissected hummock kettle lineated ridge terrace veneer weathered complex Fluvial Colluvial Aeolian Glaciofluvial Lacustrine Marine Glacial Bog Depositional Environments C F L E O G R M Tv Rc Where three differentWhere landforms are included in a single map unit they are each separated by a single slash (/) and their relat percentages are (60 - 80), (15 - 35), and (5 - 15). two landformsWhere are included in a single map unit, a double slash (//)or single slashis (/) used to separate them, and th 15)percentagesforrelative95)//slash. doublea single (5 - (15 - 40) for slash,or(60- 85) / are (85 - between hyphen two landform types indicatesA that they are approximately equal in area. Tv-RcFor example, indicatestil that and veneer rock concealed by vegetation or a thin regolith are equal in area. composite symbol isusedshow to combinations ofA above the cases.indicates For example, that about 60 - 85 percent of till. by is underlain and sediments, glaciofluvial by 40 15 - percent sediment, fluvial by covered is area Th, Tk Td, Tl, Tr Tb, Te, Tp, T Tb, Te, b c d e Each outlinedEach areais assigned a classification consisting of three up to genetic categories and modifiers that designate the t deposits within each area. Each category within a classification is listed in order of dominance and is separated from the othe by a the areasslashTv/R). are (e.g., divided Generally, so that up to three landforms or deposit types are identified within classification system is also used to denote the approximate percentage of landforms occurring within an outlined area, but tho form less 5 than percent of the area are not included in the classification. Four variations of the landform system are as foll 1. 2. 3. 4. Symbol a ff h k l p r t v w x Symbol 45' o 00' o 46 47 30'

30' v

o T

55 0 O/Or 0 O/Tv 5 R Tl/Te Th/Or O/Or Or/Th Or Ge/G Tv//Rc-O Tb//Rc Tv/Rc Th/Or

 Tb/Tv/O

 Tl



Tv/Rc

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5 0

 0 5 O

Tb//Rc

5 2 5 Tl/Tb 2 O/Or

Tv/Rc

Or/O Tb/O  Tb/O Rc//Tv Tb/Tv/O Tl/Tb

 Tv/Rc/O

Gv/Gt Or//Th

O Tb/O

| | Te/Tb

0 b 5 2

T |

/ >

Tb/O | |

v O/Or/Tb

T Tv/Rc |

/ Tb b

| T

Tv/Rc | Tb Tb/O/Th

Th/O |

| |

Te/Tb | | Tl/Te |

 Gv/Gt Rc/Tv Rc//Tv

 Tv//Rc Rrc/Tv

1L/13 0

0 5 Te/O Tv/Rc Or//Th Tv/Rc Tb//Rc

Fv/Rc 0 O 5 Or/Tb/O 0 Tl/Te

25  Tb/Tv/O Tv/Rc/Tb

Tb 0 5 2 Gv/Gt

Tl/Tb Tb/Te |

 | Tv/Tb Tb/Te Or

Or/Tb/O 0 Tv/Rc/Tb 25 |

Tv/Tb/Rc

Tb > |

 5 v

 Lawn T

/ Tb/Rc 0

Tb /

 25 c  Rc/Tv R O/Or Tl Rc//Tv Gf

Tv/Rc/O 0

5 ½

O/Or 2

Mr/Mv

1.2 m?1.2 r

½ u

Tb b

balsamea) r

a 4 m 4 m

Peat Peat

Wood (Abies Wood H

Tb/Tv n

Tb/O/Or w

Tv/Rc a

Tb//Te L Te/Or/O

t a

e r  G /O Te/Tb 970

0 m

Tb/Tv/O Te/Tb  Ov GSC-4670 Tb//Te Tv//Rc 

1850

 Modern 0 0  5 GSC-6117

5 GSC-6075 Gv//Rc 2 2 1 O/Tb

 Tb/Tv/O Tv/Tb/Rc Or 1 O T T Tv/Rc Ov 8100 T Fv/Rc Ov Fv/Rc Tv//Rc Ov

 GSC-6105

O/Or Gv//Rc

Tv/Tb/Rc O/ 0

5 | Tv/O/Rc 2 Tb/

| Tv/Tb/Rc

| |

| | 0

2 |

O Fv/R |



Tb/Tv/O >

Tv/Rc/O

Tv/Tb/O 0 Fv//Rc

Tv/O/Rc 5

Tv/Rc/O 0 >

Tv/Rc



5 Tve//Tb-Rc | Or 2

O |

½ >

| Tv//Rc

Fv/R ½½½½ Mr L A W N A Y A BL Or/O

Tve//O Tv/Rc-O Tv/O/Rc Rc/Tv/O > > Tv/Rc

Tv//Rc > > |

Fv/Rc | |

| | |  Tv/Rc-O | Rc

Tv//O |

 Rc//Tv-O Wood Wood Wood m 0.7 Wood m 0.5 0.75 m 0.85 m Tv/Rc/O Tl Tv/Rc-O Rc/Tv/O

Tv/Rc-O  Tv/O/Rc 0

 Tv/Rc/O 0

5 Fv/R Tb//Te 380 560 910 940 GSC-5728 GSC-5717 GSC-5708 GSC-5706 O/Or Rc//Tv-O Or//O Tv/Rc/O Tv/Rc/O Tl



 Tv/O/Rc c  1

R 

/ O//Or Tv//Rc 2 /O Tv//Rc O/Tv/Or v Tv/O/Rc T Tv/Rc/O Rc/Tv/O Or Tv/Rc-O O Or/O Tv/Rc/O Tb/O/Tv

 O Tv/Rc-O Tv/O/Rc T Tb/O O/Rc Ov Tv/Rc Tv/O/Rc

Tv/O/Tb Tv/Rc-O Tl/O/Tv

Tb/O

0  Tv//Rc-O 0

O/Tve/Or 5 Rc/Tv O//Rc-Or 5

 Tv/Rc/

 O//Rc-Or Tb/O Rc//Tv-O Or Tv/Rc Tv//Rc-O Tv//Rc  Rc/Tv/O Rc O/Tv/Or Tb/Rc

 O/Or Tv/O/Rc O/Or/Tv Tv/Rc

½ ½½ 0 Tv//Rc-O T

Ov 5 Rc/Tv

 O//Or Tv//Rc-O 50

 Tv/O/Rc //Tv Tv/Rc/ Tv/Rc 0 T Tv/Rc/O 5 Ov

2 Mr/Mv Gyttja m 115 m 115 115 m 115 Gyttja Gyttja O//Or-Rc Tv//Rc-O Tl O/Or/Tv Te/O

 O//Tb

Tv/Rc/O Tv/Rc/O Tv/O/Tb Tv//Rc-O

0 5 11300 13400 10700

Tv/Rc

GSC-3649

GSC-3559 GSC-3572 c

/  R/Rc

O Tv/O/Rc /

O/Or/Rc v Tv/Rc/O T T Ov O O T Ov

^ Rc/Tv/O O//Tv T Tv//Rc E Ov Tb/ O Tb/Tv Tv//Rc-O Tv/Rc/ Tv/Rc O//Or

Tv/O/Tb Tv/ /Tb Tv/  0

Tv/Rc/O ^

Tl/Rc 5 Tv Or/O E Tv/Rc/O O/Or

 Tv/Rc/O /Rc/O Tv 

O//Or 0

/Or/Tb 5 Tb/O/Rc Fv//Rc

Tv//Rc 2 Tb T O//Or-Rc Ov Tv//Rc-O

Tv/O/Rc Tv/Rc

Tv/Rc/O O  Tv/Rc Rc/Tv

 1 O/Tb/Or

 /Tb/O O//Tv Tv/Rc/O Tv/O/Rc O//Or

0 Tv/Rc/O Tv/Rc

5   2 O 2 T Ov O//Or-Rc Fv/Rc Tv//Rc Tb/O/Rc

O//Rc

/Tv

0 O 0 5 O/Or T



Ov O

 Tv/Rc Tv/Rc/O O/Tb

0 Rc/Tv

2 0

Tv/Rc/O Tv//Rc 5 Tv/Rc/O 2 Tv/Rc/O Fv/Rc Tv O//Tb Rc/Tv/O O Tv/Tb/Rc Mr Tb/Rc O Ov/Tv Tb/Or /Tb Tv//Rc

 O/Tb/Or Tve/Rc/O O//Rc

T | O

Ov ^

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> O O Tv/O Tv O /Tb

 T O//Tb  Ov /Tb Tv/O/Rc

T 0 Rc/Tv Tv//Rc-O Ov

Tv//Rc 5 O//Tv T Cove Lord's Tv/Tb/Rc Tb/ Ov O O Rc/Tv Or Tv/Tb/Rc O/Tv T O/Tb Ov Tv/ 1 Tv/Tb/Rc O//Tb-Or 2 O

T  Tv/Tb/Rc O Tb/Tv/O O Ov  Rc/Tv O Tv//Rc-O T Ov O Tv/Rc

O c

b/R /Rc Tb/ O

Tb/Tv/O v/T

Tv/Rc/O O//Tb-Or T

^ 

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O 2 5 2 Tv/O/Rc Tv/Rc/O

Tv/O/Rc Tl

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O | ^ > O O//Tb

| E T

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Ov Tb/ Tb/ /Rc Tl//Rc O/Or /Tb T O  Ov  Tv/Rc Tv/O Tl//Rc Tv/Rc Tv/ T

Tv/Rc/O

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Tb/ > |

^ T Tv/Rc/O

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| 2 1

 O//Tv Tv/ /Rc

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//Tb-Rc 5

Tv//Rc-O 2

Tv/Rc/O ^ T E Tv/O-Rc Ov Tv/Rc/O <

Tv//Rc-O ^

Tl//Rc O Tv < E Mr O/Or /Tb

> Tv/Rc

T < T

0 Ov Ov Tv/Rc/O

5 Tv/O/Rc >

2 T Tv//Rc-O Ov O/Or T Te Tv/Rc/O Ov Tb/ Tb/ /Rc O//Tv Tl//Rc Tv/O-Rc O//Tb Tv/Rc Tv//Rc-O O

O ^

Tb/ Tl/Rc E T Tb/O Ov

O/Or ^ O/Or Tb/Tv

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0 Tb/Te/O O T

5 /Rc Tb/ 0 2 Tv/Rc Ov

Tb/O O 5 Th

O/Tb/Or Tv/O-Rc 2

O ^ Tv//Rc-O

Tb/ Tb/ /Tv 50 O/Or

E Tl//Rc

0 O Ov

5 Tv/Rc/O Tv/Rc/O /Or/Tb 2 Th

 Tb/ T T /Tv Te/Tb/Tv Ov Ov O Tv//Rc T

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0 5

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| Ov

| 

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Fv/Rc O/Or | > Tv/O/Rc T Tb/

 Ov O/Tb/Or Tb

 Tb/Tv/ Tv/Rc/Tb Tb// Mr Tv//Rc-O

 Mv Tv//O-Rc T T Fv/Tb Ov Tb//Tv-Or Ov km

Tv//Rc 50

Fv/Rc

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5 0 > 2 5 | 2 T Tb/ Tb/ Tb/ /Tv T Ov

Ov Tb

| > O/Or/Tb Tb/O

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T | Tv/ /Rc Ov Tb T | T Ov Er

Tb/ Fv/Tb | Ov

| Tb/ /Tv Tb/

Map 2007-14 | Tv/ /Rc Tv/ /Tb O Tl//O  | Tb | |  T

| | Mr/Mv

Tv/Rc/O | NEWFOUNDLAND

| Tv/Rc | |  Point au Gaul

 LAMALINE Tv/O/Rc

O/Or > O/Or T Ov T Tv/Tb/Rc Tb/O/Rc Ov Te/Tb/O Tv/ /Rc Tv/ /Tb/Rc Tb/ /Rc Tb/ Fv/Tb O/Or /Tb Gv//Rc Tv/Tb/Rc T Gv//Rc T 0.3 m 0.3 Th//O-Tb Ov Ov T Ov Basal peat O/Or

Mr//Rr

Tb/O/Th

Te/ /Rc Te/ 0 0 5 25 2 Tb

 Tb/O/Tv Fv/Tv Tv/Rc/O Tv/O/Rc Tv/Rc/O

 0.5 Rc/R 3080 Fv/Tb

 T

 GSC-6113 Ov Tb/O/Tv O/Or Tv/Rc/O

 O/Tb T Tb/ Ov T Th/O/Or

101234 Ov

B A B A Y

O/Te/Tb |

5 T | Te/ /Rc Te/

Ov Tv/ /Rc Tv/

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5 A MALL I N E

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| | | T Tv/Rc/O T Ov Tr//O

Ov > T N A E C O C I T N A L T A Rc/R O/Or/Tb Ov  Tb/ /Tv Tb/ Allan's Island Tb/ T Ov Tve/Rc/O O Tb Tb/O/Tv Te/ /Rc Te/

 Tb/O/Tv

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0  0  5 O/Or/Tb Mr Allan's Island Allan's Tv//Rc  T Ov T T Tv/O/Rc Ov Ov Th/O

Rc/Tv Tv//Rc

Th/Te/O  0 5 7 Tb Te/ /Rc Te/ Tv/ /Rc Tv/ Te// -Rc Te// Tv//Rc Fv//Rc Mr T  Ov Tb/O/Tv Tb O/Or/Tb

Tb/O/Tv 50 Tv/Rc Tv O/Or Tb/ Lamaline Tv/O/Rc Tb//Tv T

| T Rc/Tv/O |

| | > Ov T Ov Tb/ T Ov Mv/Mr

750 Te/

Tb/ 0

O/Or/Tb 5

2 Rc//Tv-O 5 Mt O/Tv O/Or

0 Tv/Tb/O 75 Tb O/Or T  Tv/Rc

Ov  Tb/Tv/O

 1 Tv/Rc/O Rc/Tv/O T Tv//Rc Rc Ov Te/ Tv/O/Rc 2

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0 /Rc Te/

0 0 5 5 O/Or/Rc Mr/Mv Tv/O/Rc T Te/O Ov Tb/Rc T Fv/Rc O Ov Tv/Rc/O Tv//Rc-O

Te/ Rc

/O/Rc 0 5 2  T Tve/ /Rc Tve/ Ov Tv/Rc Tb/Tv O/Or/Tv Tv/Rc Tv//Rc-O

O/Or/Rc 0

Rc/Tv/O 0

Rc/Tv 5 /O/Rc T Tv//Rc-O /Tv Ov /O T O

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Ov O |

T | T T Ov

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| Mr/Mv | T Tv/Rc / Tv/O/Rc

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5 Tv/Rc/Tb

Tv/Rc/O Gve/Rc Tv/Rc/O

Rc/Tv 0

Tv Rc/Tv/O 0 > 5 Tv < O

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c Gv/Rc >< 0

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>< Fv/Ff >< > Rc/Tv/O

< /Tv O Tv//Tb-O Tv//Rc-O T Ov O Tv/O/Tb Tv/Rc/O  O Tv/O/Rc

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Tv/Tb/O

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c Mv/Tv/O

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0 Tv//Rc-O /Tv

Rc/Tv/O 5 Tv/Rc O/Tv /Tv T T T Ov Ov Ov Tv/Tb/Rc Tv/O/Rc O//Or Tb/O/Tv Tb/ /Rc Tb/  Tv/Rc

 T Ov G Ov Te Mv/Tv/O Ov

Tv//Rc

0 5 0 /Tv

0 Tv/Rc/O

5 T Rc/Tv Ov Ge/Ev Mr/Mv Te//Rc-O Fv/Rc T

Mr Ov

Tv/Rc 0

T 2

Tv//Rc-O T Ov / Te/

Tv//Rrc c

0 T 5 Ov 0

Tb/ /Rc 5 R/Rc /O Mr

//Rc 500 T T Ov Ov T Ov Te/Tb

Tv/Rc Mr/Mv Tb/ |



0 |

0 | | Tv//Rc-O 5 > Rc/Tv

Fv//Rc | |

Gv//G | T

 T Ov

| Ov > /Tb Tb/Te/O | Mr | Te/Tb T | Te/

Tv/Rc/O

Ov Te/Tb

O T O 0 >

| Ov 5

T Rc/Mv O/Te Fp > | Ov

| Tb/ /Rc

Tv/Rc

b Tb/

T T

/ Ov

e Mr

v T T Ov Tb/Tv Tb/ Tv/Rc Te/O Gv//G T  T Ov Ov Tb/ Tv Gv//G

Tve/Rc/O Te/ > Tb/Te

|  Te/Tb

Ov | Tv/Rc/O 

 | Gv/Te Mv/Tv Mr 500 

| 2 T /Tb 1 T Ov Ov T Rrc/Tv/O Rc/Tv Ov Tb/ T T

 Tb/

/Tb Ov Ov

| Tb/Te Te/Tv/Rc 0 5

> 2

| Ov | /Rc Tv/ Mr Tv/ /Rc Tv/ Tb/Te

 Te/Gv Mr Tb/Rc

 T Tv//Rc Ov Tv/Tb/Rc

/Tb

| T | | Ov

Tv//Rc-O T

| T Point May

| Ov O | Ov Ov

| | |

0 Gv/Te

| Te/ Te/Tb/ | Tb/Tv | 5

   Tb/Te

2 0

| 1 

5 Tb/

| 0

| 2 

|  | >

| | |  >  Tb/Tv/O

| | Te/Tb/ Rc/Tv | 2 Ov >  1

Te/Tv | | |

 1 > > | | 2 | Tb/Te O

> 2

Te/Tb |



|  |  T

Ov 0 |

| | 5

Tv//Rc-O |

Te/Tb/O Tb/Tv T | T Ov

 |

Te/Gv Ov Gv/Gt

| !!

| |

| | | >

| | | !! >

| | | |

> 

| T | | | !!

Ov | |

| T Te/Tb

O/Tb | |

> | | | Ov T  Tb//Te !! 

Ov |

| | | | |

| Tv/Rrc/

!! | |

| 1 Gv/Te

| | |

|  |

| |

0 | 2 |

| >

5 /Tb |

Tv//Rc-O | | |

2 |

Tb/Tr/O | 0

5 |  | Te/Tb/ T |

Ov | |

T | > O//Tb > 

> 

1 Ov 

0 |

 |

| |

| T |

Tb/ | 

1 Ov O

| >

| 2

> | Te/Tb/O | | ½

> Mr

| Te/Tb/ Tb/Tv/O |

 Tb//Te

T 0 | Ov 5 Tb

2 Te/Gv

 Te/ Mr Tv//Rc-Te Peat 1.2 m 1.2

5360

GSC-2613

T T

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