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Lamaline Map Sheet the Lamaline Map of > ! | > ! | 56o 00' 55o 30' o o 47 00' | 47 00' LEGEND | | Rc/Tv/O Rc/Tv | Tv/O/Rc Or Tb Tv/Rc/O | O/Or Rc/Tv/O Fv/R Tb Or Tb/Tv/O O/Tb Tb/Tv Tv/Tb/O Tv/O/Rc Tb/O Th/Or 500 | Tl//O Tv/O-Rc Tv//Rc-O Tv//Rc-O O//Or Tv//Rc-O !! !! Tv//Rc-O Fv/R Tb/Tv/O 5 > O/Tv !! 0 O/Te Ov Rc/Tv/O O/Or/Tb Or//Th Tl !! 5 0 O/Or Th//O-Tb T !! 2 Tv//Rc Tv//O-Rc 0 Tb/Ov O/Rc Tl 0 Te/Tb Tv/O/Rc / G Tv/O/Rc Tv//Rc-O 0 Tv/O/Rc O Each outlined area is assigned a classification consisting of up to three genetic categories and modifiers that designate the types of Tb/Tv Tv/Tb/Rc 5 /R Tb/O 50 Tb/Tr/O Rc/Tv/O Th Tv//Rc-O c Tv/Tb/O Fv/Rc Tv/Tb Te/Tv/Rc Tve/Rc/O Te/Tb Tb Th Tv//Rc-O O//Or-Rc Te/Or/O deposits within each area. Each category within a classification is listed in order of dominance and is separated from the other categories | Tv/Rc/O | | O//Tv | Tv//Tb-O Fv//Rc Fv/R Te/Tb/O | > 2 Or 50 Tv/Rc by a 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. The | O/Or Tv//Rrc 0 | Tv/Rc/O 5 Tv/Rc-O Fv/Rc 2 > b Tb/O/Th Tv/O/Rc Tb/O O/Or/Tb O//Or-Rc Tb/Tv/O Te/O Or//Th Ge/G classification system is also used to denote the approximate percentage of landforms occurring within an outlined area, but those which | T Tv/Rc/O Tv/O/Rc O/Or 0 > / O O//Tb Rrc/Tv/O e 5 Tv/O/Rc O//Tb-Or / | 0 Tb/Te Tb/Tv/O b | 5 v 7 form less than 5 percent of the area are not included in the classification. Four variations of the landform system are as follows: | > Tb/O/Tv O/Or Tv/Rc-O Or/Tb/O T | 2 Tv//Rc-O T Ge/Ev Tb/O / | v Tv//Rc-Te O/Or/Tv Tl T > | Tv/Rc-O | Te/Tv | 7 Rc/Tv Tv/Rc/O | 5 | | Tv/O-Rc O | | 0 > O/Or 2 > Fp | | | | | | | Te/Tb Rc/Tv 5 1. Where three different landforms are included in a single map unit they are each separated by a single slash (/) and their relative 0 | | | Tr//O O//Tb-Or > | Tv/Rc/O | 0 Te/Tb/O | 0 O O/Tv | | O | Te/Tb Tb/O Tv//O Tv/Rc 5 0 percentages are (60 - 80), (15 - 35), and (5 - 15). | Ov | 0 5 Tl/Te | 0 Tv/O/Tb Tv/Rc/O | Te//Rc-O 5 2 Tv/O/Rc Tv/Rc Tv/O-Rc > | T 2 O/Tb/Or | O/Or Tb/O/Or 0 | Gv/Gt Ov | O//Or-Rc Tl/Te | Te/O | Ov 0 Tl/Te Ov /Tb 0 Tv//Rc O/Or 5 Rc 5 //Rc O Tb/O 2. Where two landforms are included in a single map unit, a double slash (//) or single slash (/) is used to separate them, and their | T T O//Or O/Or/Rc Rc//Tv-O > 2 | Tv//Rc | Te/Tb/O | | Ov Tv//Rc-O | | | | Tv//Rc-O Or//O Te/Tb Tb/Te relative percentages are (85 - 95) // (5 - 15) for double slash, or (60 - 85) / (15 - 40) for a single slash. | Fv/Rc T 1 O > Tv/O/Rc Th/Or Tb/Te / | Tv/O/Rc > R Tv/Rc-O Tb/O/Th Y O c | Tv/Rc Tv/Rc/O / | Tv Tv/O/Rc O/Or Th/O/Or Mr | Tb/Tv Tv/Rc/O Gv//Rc | Gv/Gt | Te/Gv O 3. A hyphen between two landform types indicates that they are approximately equal in area. For example, Tv-Rc indicates that till A Tb/Tv/O O/Or | | Rc/Tv | O/Or Tb/Tv/O Rc/Tv Ov 0 O/Or/Tb O/Or Or/Th | | | veneer and rock concealed by vegetation or a thin regolith are equal in area. 0 O/Or/Rc O/Or/Rc O//Tb O O Or Tb/ > | 5 Tv/O/Rc O//Tb | | | 7 O/Or/Tb DEPARTMENT OF NATURAL RESOURCES B | Tl T | | 5 O/Or O/Or | | O/Rc/TV 0 0 O F/G Tb/O/Tv | Tv/Rc Ov 5 /Tb 2 | O Ov Or/Tb/O Tv//Rc-O Rc/Tv Rc/Tv T O/Tv O/Tb/Or /O 4. A composite symbol is used to show combinations of the above cases. For example, T indicates that about 60 - 85 percent of the GEOLOGICAL SURVEY | Ov Tv/Rc/O Tv/O/Tb | | T Ov Tb/ Tv//Rc-O Th/Te/O Tv/Rc/O Tb//Rc | Fv/Rc | c area is covered by fluvial sediment, 15 - 40 percent by glaciofluvial sediments, and is underlain by till. T O Tv/O/Tb | | R T / 5 Tv/Rc/O Fv/Rc | Ov O Tl Tb/O ICAL S 0 O/Or / 0 G U | Ov Tb Tb O R 0 Te/ v Rc/Tv 5 L V | T 5 /O/Rc 2 O//Or Tv/O/Rc Ov O 2 E 5 > 0 O E | T 0 T Tv/Tb/Rc Tv/Rc Tb/ / Y Th//Gr-Rc 0 | Tv//Rc-O G Ov T b O/Or E > O/Or/Tb N /Tb O/Tb/Or O T 0 / R O E Gv//Rc Tb//Tv-Or l T > < Tb/Tv/O O//Tv Tv/Rc-O 5 Tb/Te Gv/Te Tv//Rc 2 T W O < Tb/O/Tv Te/Tb/Tv D Ov > Tv//Rc GENETIC CLASSIFICATION F Tv//Rc O A Ov | 0 < Rc/Tv/O Tv/Rc/O N 0 > O/Or Tv//Rc-O U R 2 5 Tv/O O/Tb B Tb/Te N | Tv/Rc/O 5 T < > Tv//Rc-O D 1864 A Gr/Rc L 0 Te/Gv Te O/Or LA D | ND AN > Fv//Rc Tl/Tb Depositional < Tb/Rc | | Tb/Tv/O O//Tv Or/O U Ov Tb/O/Tv | Tv/O/Rc Or Te/ O/Or | Tv//Rc-O Tv/Rc/O O//Tb Symbol Environments Origin and Characteristics of Materials 2 Tb/Tv/O > T | 5 Tv/Rc/O Gv/Gt > Or/O T Ov 0 | | Tb//Rc-O Tv/Rc SURFICIAL GEOLOGY | | Te/ > Fv/Rc | Tb/Te T Tv/Rc/O Tb/Tv Tv/Tb/Rc Tb/Te/O Ov Tv//Rc-O R Tb/ /Rc Tb/O/Tv Tb/O/Rc O//Or Ov | T O O Tv/Rc/O Tv/O/Rc O Te/Tb OF THE LAMALINE MAP SHEET | Tb/O/Tv Tb Bog Poorly drained accumulations of peat, peat moss and other organic matter; developed in areas of | Rc/Tv Tl O > Ov Ov | > Ov/Tv Gv//Rc Tb//Rc | Tb/ Tv/O/Rc poor drainage /Tb | Ov Tv/Rc 0 Tv//Rc O (NTS 1L/13) T | | Gv/Te Tb/ /Rc 0 O/Or/Tb 0 T Tv/O/Rc Rc/Tv Th/O | 5 5 Ov Tv/O/Rc F O/Tv/Or 2 T 2 Tb/ O Tb//Te 5 Tb/Tv/O O/Or/Tb O/Te/Tb 0 | Ov T Tv/O/Rc 2 | Tv/Rc/O Tl/Tb 50 | Rc/Tv/O Tv/Rc/O Tb/ Tv//Rc Ov > | | T Tb/Te | Tb/O/Tv Tv/Tb/Rc Or/O Tv/Rc/O Fluvial Alluvium consisting of silt and clay to bouldery gravel, forms terraces and plains associated with T Tv/Rc/O O//Tb Tv//Rc-O Tv/Tb/Rc Gv/Gt 00 5 Gve/Rc Tv/Rc Tv/Tb/Rc Ov Tb/Rc 2 MAP 2007-14 Ov | modern stream channels, their floodplains and deltas; usually less than 1 m thick; deposited by 2 5 F Ov Tv/ Ov | | Tb// /Rc O/Or Tb//Te Ov Tb/ /Tv 5 Tv/ /Tb 0 v 0 T > T Tv/Rc O/Or | O O//Rc | Tb/O/Tv T T T Tb/O/Rc // Tb//Rc fluvial action at or below maximum flood levels | Ov | Tv/O/Rc T Ov R/Rc | > c /O/Rc | | Te/ Tv/Rc/O O/Or > Ov R 0 Te/Gv | 25 | T Tv//Rc-O Tv T Gv//Rc Ov Ov | >Tve//O T Rc//Tv Tv/Rc | /Tb Tv/O Tb/O/Rc Fv//Rc Tb//Te Or Tb//Te | 50 Te/Tb Th/O //Tv 00 Colluvial Coarse-grained bedrock derived materials; may include sand, silt or clay; accumulates on the lower SYMBOLS | 5 Tb Ov T Te Tv/Rc/O O/Or/Rc T Tv/O/Rc | | Te/ O//Rc | Ov Ov 500 C parts, or at the base of steep rock faces; transported by gravity //Tb-Rc | Ù Ov T 0 O//Or O//Rc-Or ½ ! Tb/ /Tv 5 Tv/Rc ! | O Tv/ /Rc Gv//G T 2 Geological boundary . Drumlin (direction known, | 0 Tv/Rc/O O O/Or Tv/Rc/O O/Or/Tv 8100 v 0 Te/O T Rc//Tv | T Tv/O/Rc T Tb//Te 5 Tb/Tv/O 2 T Tv/Rc/O / Tv/Rc 5 O unknown).
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