TEM Expanded Legend and Report (el)

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ECOSYSTEM UNITS OF THE ITCHA / ILGACHUZ AREA
AND THE CHARLOTTE ALPLANDS
Volume 1 - Expanded Legend
Prepared for: Wildlife Branch
Ministry of Environment, Lands and Parks
Williams Lake, B.C.
Prepared by: Chris Clement, A.Sc.T., R.P.F., R.P.Bio.
and Rod Dalziel
Shearwater Mapping Ltd.
Victoria, B.C.
January 2000
ECOSYSTEM UNITS OF THE ITCHA / ILGACHUZ AREA
AND THE CHARLOTTE ALPLANDS
Volume 2 - Data Synthesis Tables
Prepared for: Wildlife Branch
Ministry of Environment, Lands and Parks
Williams Lake, B.C.
Prepared by: Chris Clement, A.Sc.T., R.P.F., R.P.Bio.
and Rod Dalziel
Shearwater Mapping Ltd.
Victoria, B.C.
January 2000
TABLE OF CONTENTS
1.
INTRODUCTION
1.1
1.2
Introduction ................................................................................................ 1
Study area.................................................................................................. 1
2.
METHODOLOGY .................................................................................................. 7
3.
ECOSECTIONS AND BIOGEOCLIMATIC UNITS ................................................. 9
4.
ECOSYSTEM UNITS ............................................................................................ 11
IDFdk4 01 LP ....................................................................................................... 11
04 DS ...................................................................................................... 11
05 DW ..................................................................................................... 12
07 DM ..................................................................................................... 12
08 SS ...................................................................................................... 12
00 ND...................................................................................................... 12
00 WM .................................................................................................... 12
IDFdw 01 DP ...................................................................................................... 12
00 AT ...................................................................................................... 12
00 BP ...................................................................................................... 12
00 CR...................................................................................................... 12
00 DB ...................................................................................................... 12
00 DK ...................................................................................................... 12
00 DS ...................................................................................................... 13
00 LK ...................................................................................................... 13
00 SG...................................................................................................... 13
00 SH ...................................................................................................... 13
00 SS ...................................................................................................... 13
00 ST ...................................................................................................... 13
SBPSxc 01 LK ....................................................................................................... 13
02 LC ...................................................................................................... 13
03 SB ...................................................................................................... 13
04 SF ...................................................................................................... 14
05 SH ...................................................................................................... 14
06 SM ..................................................................................................... 14
00 BS ...................................................................................................... 14
CF ...................................................................................................... 14
00 TS ...................................................................................................... 14
00 WB ..................................................................................................... 14
00 WT ..................................................................................................... 14
SBPSdc 01 LJ ....................................................................................................... 14
02 LC ...................................................................................................... 14
03 LF....................................................................................................... 14
04 BF ...................................................................................................... 14
05 SB ...................................................................................................... 14
06 SM ..................................................................................................... 14
07 BB ...................................................................................................... 14
00 BS ...................................................................................................... 14
00 WT ..................................................................................................... 14
SBPSmc 01 LF ...................................................................................................... 15
02 LC ...................................................................................................... 15
03 BF ...................................................................................................... 15
04 SB ...................................................................................................... 15
05 SO...................................................................................................... 15
06 SH ...................................................................................................... 15
07 BB ...................................................................................................... 15
00 BS ...................................................................................................... 15
00 WB ..................................................................................................... 15
00 WT ..................................................................................................... 15
SBSmc2 01 SB ..................................................................................................... 15
02 PH ...................................................................................................... 15
04 HB ...................................................................................................... 15
08 ST ...................................................................................................... 15
11 HG ..................................................................................................... 15
00 BS ...................................................................................................... 15
MSdc2 01 SF ...................................................................................................... 15
02 DS ...................................................................................................... 16
03 DK ...................................................................................................... 16
04 PK ...................................................................................................... 16
06 ST ...................................................................................................... 16
07 SG...................................................................................................... 16
08 SH ...................................................................................................... 16
00 AW ..................................................................................................... 16
00 SS ...................................................................................................... 16
MSxv
01 LG ...................................................................................................... 16
02 LF....................................................................................................... 16
03 LK ...................................................................................................... 16
04 GK...................................................................................................... 16
06 SC ...................................................................................................... 17
07 SG...................................................................................................... 17
08 SH ...................................................................................................... 17
00 BP ...................................................................................................... 17
00 BS ...................................................................................................... 17
00 FC ...................................................................................................... 17
00 LB ...................................................................................................... 17
00 TB ...................................................................................................... 18
00 TF ...................................................................................................... 18
00 WG .................................................................................................... 18
00 WS ..................................................................................................... 18
ESSFmw 01 FR ................................................................................................................ 18
02 LJ ...................................................................................................... 18
03 DF ..................................................................................................... 18
04 FH ..................................................................................................... 18
05 FA ..................................................................................................... 18
06 FV ..................................................................................................... 18
07 FO ..................................................................................................... 18
08 FG ..................................................................................................... 18
00 AV ..................................................................................................... 18
00 BS ..................................................................................................... 18
00 DG .................................................................................................... 18
00 SS ..................................................................................................... 18
00 TW .................................................................................................... 19
00 WS .................................................................................................... 19
ESSFxv1 01 AC ..................................................................................................... 19
02 WJ .................................................................................................... 19
03 LC ..................................................................................................... 19
04 JG ..................................................................................................... 19
05 AT ..................................................................................................... 19
06 FR ..................................................................................................... 19
07 FV ..................................................................................................... 20
08 FH ..................................................................................................... 20
08 AF ..................................................................................................... 20
00 AV ..................................................................................................... 20
00 BP ..................................................................................................... 20
00 BS ..................................................................................................... 20
00 BV ..................................................................................................... 20
00 DG .................................................................................................... 20
00 FC ..................................................................................................... 20
00 LB ..................................................................................................... 20
00 SS ..................................................................................................... 20
00 TB ..................................................................................................... 21
00 WG ................................................................................................... 21
00 AF ..................................................................................................... 21
00 LB ..................................................................................................... 21
00 TF ..................................................................................................... 21
00 SS ..................................................................................................... 21
00 WS .................................................................................................... 21
ESSFmwp and ESSFxvp1
00 AF .................................................................................................... 21
00 CS .................................................................................................... 21
00 DG .................................................................................................. 21
00 FB .................................................................................................... 21
00 FC .................................................................................................... 21
00 FM.................................................................................................... 21
00 HT .................................................................................................... 22
00 PC .................................................................................................... 22
00 SF .................................................................................................... 22
00 SS .................................................................................................... 22
00 TW ................................................................................................... 22
AT
00 AF ................................................................................................... 22
00 CS ................................................................................................... 22
00 FC ................................................................................................... 23
00 HT ................................................................................................... 23
00 MW ................................................................................................. 23
00 PC ................................................................................................... 23
00 SF ................................................................................................... 23
00 SM .................................................................................................. 23
00 SS ................................................................................................... 23
00 TW .................................................................................................. 23
5.
GLOSSARY ........................................................................................................... 24
6.
REFERENCES ...................................................................................................... 27
APPENDICES - A: Plant Species List
EXPANDED LEGEND ITCHA / ILGACHUZ AND CHARLOTTE ALPLANDS
1INTRODUCTION
1.1 Introduction
In the summer of 1996 and 1997 Shearwater Mapping Ltd. was contracted by the
Wildlife Branch of the Ministry of Environment, Lands and Parks to produce Terrestrial
Ecosystem maps at a scale of 1:50 000 for the Itcha / Ilgachuz study area. Additionally
a map of ecosystem units at a scale of 1:20 000 was produced for the Punkutlaenkut
Creek drainage. In the summer of 1998 the project was expanded to include the
Charlotte Alplands. The 1996, 1997 and 1998 study areas are depicted in Figure 1 on
page 3. NTS map sheets covered included 92N 13 (n. half) and 14 (n. half), 93 C 3, 4
(e. half), 5 (portions of),6, 7, 8, 9, 10, 11, 12 (east half), 13 (east half), 14, 15 and 16
(see Figure 1. Study Area).
Following the standards for Terrestrial Ecosystem Mapping in British Columbia
(Resources Inventory Committee 1995 for Itcha/Ilgachuz and 1998 for Charlotte
Alplands) 471 plots, and 287 ground visual records were located and sampled. In
addition 677 quick visual records were obtained. There are thirteen Biogeoclimatic Units
in the study area, including IDFdk4, IDFdw, SBPSxc, SBPSdc, SBPSmc, SBSmc2,
MSdc2, MSxv, ESSFmw, ESSFmwp, ESSFxv1, ESSFxvp1 and AT. See the
Biogeoclimatic Unit section (page 7) for a detailed description of biogeoclimatic units.
1.2 Study Area
Most of the study area lies within the Western Chilcotin Upland (WCU) Ecosection with
only the southwestern corner occuring in the Chilcotin Plateau (CHP) Ecosection and a
small northern portion occuring in the Nazko Upland (NAU) Ecosection. Elevations
range from approximately 1120m (Anahim Lake) to 2400m (Far Mountain in the
Ilgachuz Range) with the entire area primarily a gently sloping plateau with the Itcha
Range, Ilgachuz Range, Rainbow Range and Pacific Ranges being prominent
mountainous areas. Major drainages which bissect the area include the Dean River
(draining the western portion) and the Chilcotin River (draining the eastern portion).
Draining into the Dean River are Holtry Creek, Nimpo Creek, Dagg Creek, Holte Creek,
Lehman Creek, Corkscrew Creek, Beeftrail Creek, Festuca Creek and Obsidian Creek.
Draining into the Chilcotin River are Punkutlaenkut Creek, Palmer Creek, Jorgensen
Creek, Clusko Creek, and Downton Creek. The northern part of the study area is
drained by the Blackwater, Kushya, Coglistiko and Baezaeko Rivers. The Hotnarko
River drains east of Anahim Lake into the Atnarko River. Prominent lakes within the
study area include Chilcotin, Nimpo (northern part), Anahim, Kappan, Abuntlet, Lessard,
Tezla, Gatcho, Eliguk, Tsibekuz, Stuyvesant, Itcha and Narcosli.
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The Itcha - Ilgachuz study area is part of the Fraser Plateau which has a flat and gently
rolling topography having large areas of undissected upland lying between 1200 and
1525 meters (Holland 1964). A large part of the study area is underlain by flat or gently
dipping late Miocine or Pliocine olivine basalt flows. On the western edge of the study
area the Rainbow Range, peaking at 2478m. at Tsitsult Peak, projects above the
plateau as do the other Miocine shield volcanoes of the Ilgachuz and Itcha Ranges all
composed mainly of andesite and dacite. Much of the plateau is covered with glacial
drift composed of basal till modified in places by drumlins and glacial grooves
interspersed by occasional areas of shallow materials overlying bedrock and exposed
bedrock (Tipper 1970). The Anahim valley and Coglistiko River areas have extensive
areas of ablation till, eskers and meltwater channels. Isolated areas of glaciolacustrine
occur in Holtry Creek and in the Baezaeko River drainage.
The bulk of the study area occurs as SBPSxc (SubBoreal Pine-Spruce Very Dry Cold
Subzone) and MSxv (Montane Spruce Very Dry Very Cold Subzone) biogeoclimatic
subzones. In the SBPSxc an intensive fire history combined with a dry, cold climate
results in the development of very open forests of lodgepole pine with only occasional
occurrences of hybrid white spruce (Engelmann x white) and subalpine fir. Understory
vegetation of zonal sites is dominated by soopolallie, kinnikinnick, twinflower and
Pleurozium schreberi. Typical surficial materials are sandy gravelly and gravelly muddy
morainal blankets; characteristic soil developments are Orthic Dystric Brunisol, Orthic
Gray Luvisol and Brunisolic Gray Luvisol. On sites with coarse-textured soils terrestrial
lichens such as Cladonia and Cladina species often proliferate. In the MSxv, which
occurs above the SBPSxc up to an elevation of about 1500m, lodgepole pine still
dominates forests on mesic sites. Hybrid white spruce is occasionally present both in
the tree and shrub layers. Common in the understory of zonal sites are grouseberry,
crowberry, twinflower, Dicranum species and Cladonia ecmocyna. Typical surficial
materials are sandy, gravelly morainal blankets, with Eluviated and Orthic Dystric
Brunisol soils.
Also occuring with limited geographic range are the SBPSdc (SubBoreal Pine-Spruce
Dry Cold Subzone), SBPSmc (SubBoreal Pine-Spruce Moist Cold Subzone),SBSmc2
(SubBoreal Spruce Moist Cold Subzone Babine Variant) and IDFdk4 (Interior DouglasFir Dry Cool Subzone Chilcotin Variant). In the Charlotte Alplands area isolated pockets
of IDFdw (Interior Douglas-fir Dry Warm Subzone) and MSdc2 (Montane Spruce Dry
Cold Subzone Tatlayoko Variant) occur at low elevations of valleys abutting the Pacific
Ranges.
Occuring above the MSxv are the ESSFxv1 (Engelmann Spruce-Subalpine Fir Very Dry
Very Cold Subzone West Chilcotin Variant) and the Alpine Tundra Zone (AT).
Occurring sporadically and transitionally between ESSFxv1 and AT is a parkland unit of
the ESSFxv1, (ESSFxvp1) which is characterized by the presence of stunted tree
islands interspersed with dry and moist meadows. Along the western boundary of the
study area the ESSFmw and ESSFmwp occur sporadically (Engelmann Spruce Subalpine Fir Moist Warm Subzone and Engelmann Spruce - Subalpine Fir Moist Warm
Parkland Subzone). Typical vegetation on mesic sites in the ESSFxv1 consists of open
lodgepole pine forests, usually with a component of Engelmann spruce and subalpine
fir. Common species include grouseberry, heart-leaved arnica, Dicranum species,
Barbilophozia species and Cladonia ecmocyna. A diversity of non-forested ecosystems
occur in the ESSFxv1 including dry and moist meadows, shrub carrs, riparian
shrublands, talus slopes, rock outcrops, fens, and dry grasslands. The Alpine Tundra
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varies depending on the type of underlying bedrock. In the Itchas / Ilgachuz area where
bedrock is predominantly basaltic mesic alpine vegetation is dominated by scrub birch or
Altai fescue. In the Charlotte Alplands where bedrock types are mostly acidic the mesic
vegetation is dominated by scrub birch, dwarf snow willow and sedges.
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2. METHODOLOGY
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A total of 471 full plots (FS882) were located and sampled, as well as 287 ground
inspection records and 677 quick visual records. Plots were selected to characterize the
range of ecosystems and structural stages occurring on the various surficial materials.
The existing Site Series classification (Steen and Coupe 1997) was utilized, except for
non-forested units which were named according to RIC standards.
ITCHA / ILGACHUZ AND CHARLOTTE ALPLANDS FIELD SAMPLE MATRIX
BIOGEO
UNIT
IDFdk4
PLOTS
QUICK
VISUALS
2
TOTAL
4
GROUND
VISUALS
5
IDFdw
7
5
26
38
SBPSxc
98
97
126
321
SBPSdc
4
4
7
15
SBPSmc
25
8
29
62
SBSmc2
2
2
3
7
MSdc2
3
2
7
12
135
95
99
329
ESSFmw
0
0
0
0
ESSFmwp
0
0
0
0
ESSFxv1
67
33
184
284
ESSFxvp1
53
15
62
130
AT
73
21
132
226
TOTAL
471
287
677
1435
MSxv
11
Note: Quick visuals include those done on ground and from helicopter
At each plot location Ecosystem Field Forms (FS882) were completed according to
Luttermerding et al. (1990). For the Charlotte Alplands new standards were followed
(MOF and MOELP 1998). A complete list of vascular plants was made and percent
cover estimates were recorded for each species entry. Dominant mosses, lichens and
liverworts were also recorded. Soils were described in terms of horizons, texture,
percentage of coarse fragments and presence of roots, with classifications conforming
to the Canadian System of Soil Classification (1987). Humus forms were also classified
(following Klinka et al. 1981) and described. Surficial geology terminology is after
Howes and Kenk (1997). Unknown or dubious plant specimens were collected and
identified (by J. Penny, B.C. Conservation Data Centre(vascular plants), Trevor Goward
(lichens) and Terry
McIntosh (mosses and liverworts). Nomenclature of vascular plants follows Douglas
(1997); mosses after Crum et al. (1973); lichens according to Hale and Culberson
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(1970); and liverworts after Stotler and Crandall-Stotler (1977). Also recorded at each
plot location were information on coarse woody debris (following RIC standards), wildlife
species ratings (capability and suitability), scat information (primarily caribou), wildlife
trees and aboreal lichen loading ratings.
For ground inspections the following parameters were recorded: surveyors, date,
mapsheet, aerial photo number, elevation, slope, aspect, slope position, soil moisture
regime, soil nutrient regime, soil drainage, soil texture, soil classification, terrain unit, site
series, structural stage, site modifier, and Ecosection. In addition a brief summary list of
plant species and wildlife ratings was recorded. Quick visual records consisted only of
date, surveyors, mapsheet, terrain unit site series (observations were often made by
helicopter) and biogeoclimatic subzone.
During field sampling the variation in structural stages was sampled. Structural stages
sampled, and also mapped, are:
1a
1b
2
3
3a
3b
4
5
6
7
Non-vegetated (<5% total cover)
Sparsely vegetated (<10% vascular plants, up to 100% bryophytes /
lichens)
Herb (wetlands, grasslands, tundra or recently logged)
Shrub / Herb (early successional stage or disclimax / communities
dominated by shrubby vegetation <10m tall <20 years for normal forest
succession, up to 100+ years for disclimax / climax communities)
Low Shrub (disclimax / climax communities dominated by shrubby
vegetation <2m tall).
Tall Shrub (disclimax / climax communities dominated by >2m tall and
<10m).
Pole Sapling (trees greater than 10m tall, <40 years for normal
succession or up to 100 years for stagnant stands
Young Forest (40 to 80 years)
Mature Forest (80 to 140 years)
Old Forest (>140 years)
Note: for the Charlotte Alplands mapping structural stage 2 (for non-forested units) was
often mapped as 2a (Forb-dominated) or 2b (Graminoid-dominated).
Office work consisted of data synthesis (see Volume 2 for environmental and vegetation
data synthesis tables), ecosystem description and ecosystem mapping. Mapping was
done on 1:60 000 (1987) black and white aerial photos. (Punkutlaenkut Creek was also
mapped on 1:15 000 (1991) colour aerial photographs). Ecosystems were mapped
within a bioterrain framework. Map symbols representing the site series are subdivided,
based on site conditions such as depth of soil, aspect, soil texture and landform
(subdivisions are represented by the addition of site modifier symbols).
These site modifiers (Resources Inventory Committee 1998) which are attached to
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the site series symbols on the maps, are as follows:
a - active floodplain
the site series occurs on an active fluvial floodplain (level or very gently
sloping surface bordering a river that has been formed by river erosion and
deposition), where evidence of active sedimentation and deposition is
present.
c - coarse-textured soil
the site series occurs on soils with a coarse texture, including sand and
loamy sand; and also sandy loam, loam, and sandy clay loam with greater
than 70% coarse fragment volume.
d - deep soil
the site series occurs on soils greater than 100 cm to bedrock.
f - fine-textured soil
the site series occurs on soils with a fine texture including silt and silt loam
with less than 20% coarse fragment volume; and clay, silty clay, silty clay
loam, clay loam, sandy clay and heavy clay with less than 35% coarse
fragment volume.
k - cool, northerly aspect
the site series occurs on gently sloping topography (less then 25% in the
interior, less than 35% in the CWH, CDF, and MH zones).
n - fluvial fan
the site series occurs on a fluvial fan (most common), or on a colluvial fan or
cone.
p - peaty soil
the site series occurs on deep organics or a peaty surface (15-60 cm)3 over
mineral materials (e.g., on organic materials of sedge, sphagnum, or
decomposed wood).
r - ridged
the site series occurs throughout an area of ridged terrain, or it occurs on a
ridge crest.
s - shallow soil
the site series occurs where soils are considered to be shallow to bedrock
(20-100 cm).
t - fluvial terrace
the site series occurs on a fluvial or glaciofluvial terrace, lacustrine terrace, or
rock cut terrace.
v - very shallow soil
the site series occurs where soils are considered to be very shallow to
bedrock (less than 20 cm).
w- warm, southerly aspect
the site series occurs on warm, southerly or westerly aspects (1350 - 2850),
on moderately steep slopes (25%-100% slope in the interior and 35%-100%
slope in the CWH, CDF and MH zones).
Definitions are from standard for Terrestrial Ecosystem Mapping in British Columbia
(Resources Inventory Committee 1998).
Map symbols consist of a site series, site modifier (if applicable) and structural stage.
For example:
LGf5
(LG)Pl - Crowberry - Feathermoss site series, (f)fine-textured (site modifier), (5)young
forest (structural stage). Up to two site modifiers can be attached to a site series.
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Complex (2 or 3 part) map symbols are utilized where landscape, site or vegetation
conditions are diverse. For example:
8 LGf5 - 2 SGp5
Eighty percent Pl - Crowberry - Feathermoss site series, fine-textured, young forest with
twenty percent Sxw - Horsetail - Crowberry site series, peaty, young forest. Note that
for complex map symbols deciles are placed before the site series symbols, and deciles
must always total 10 (10 = 100%). A maximum of three site series are allowed for any
one polygon, with a minimum of 10% for any one component.
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3. ECOSECTIONS AND BIOGEOCIMATIC UNITS
The Western Chilcotin Upland (WCU) Ecosection occupies approximately 90% of the
study area, while the Chilcotin Plateau (CHP) Ecosection occurs around Chilcotin Lake,
and lower Chilcotin River and Palmer Creek. The Nazko Upland (NAU) Ecosection
occupies a small area in the northwest corner; the Western Chilcotin Ranges (WCR)
occurs in the southwest corner of the study area. Information contained in the
biogeoclimatic unit descriptions is taken from Steen and Coupe (1997).
IDFdk4 - Interior Douglas-Fir Dry Cool Subzone Chilcotin Variant
The IDFdk4 occurs within the Chilcotin Plateau below approximately 1250m in the
southeast corner of the study area. The typical zonal climax sites in this zone are
dominated by multiaged Douglas-fir while most seral stands are dominated by lodgepole
pine. Due to and extensive fire history, most stands are dominated by lodgepole pine;
small stands of trembling aspen occur throughout this zone as well. The dominant
understory of zonal sites include soopolallie, kinnikinnick, prickly rose, pinegrass, redstemmed feathermoss and Peltigera species.
IDFdw - Interior Douglas - fir Dry Warm Subzone
The IDFdw occurs below 1000m in the Klinaklini River valley and the Atnarko River
valley. In the Hotnarko River Valley the IDFdw extends from the valley bottom up to
1200m. Climax forests are dominated by open stands of Douglas-fir; seral stands may
have a consideral component of lodgepole pine and trembling aspen. Typical
understory plants on zonal sites include prickly rose, soopolallie, birch-leaved spirea,
pinegrass, showy aster, kinnikinnick and wild strawberry.
SBPSxc - Sub-Boreal Pine-Spruce Very Dry Cold Subzone
The SBPSxc occurs below 1300m in the southeast and southwest portions of the study
area. Fire history has resulted in extensive lodgepole pine stands with hybrid white
spruce occurring in regeneration layers on gentle slopes and on moist sites with medium
to fine-textured soils. Trembling aspen occurs throughout this zone in small stands or
scattered amongst the lodgepole pine. On zonal sites, the low-growing understory is
dominated by soopolallie, kinnikinnick, twinflower, pinegrass and Cladonia species with
lesser amounts of prickly rose and common juniper and a sparse moss cover.
SBPSdc - Sub-Boreal Pine-Spruce Dry Cold Subzone
The SBPSdc occurs as two small lobes east of Mount Sheringham and around Narcosli
Lake in the northeast, below 1250m. Fire history maintains lodgepole pine as the
dominant overstory species with hybrid spruce rarely surpassing the understory except
on moist sites. Level to gently sloping sites, sometimes have small locally occuring
aspen stands while the majority have moderately open to closed canopies of lodgepole
pine. Kinnikinnick, pinegrass and red-stemmed feathermoss dominate the understory
with various herbs and scattered shrub species also occuring.
SBPSmc - Sub-Boreal Pine-Spruce Moist Cold Subzone
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The SBPSmc occurs in the lower Dean River and Blackwater River valleys below
1250m. Zonal sites in this subzone occur on level to mid-slope positions and soil types
dominated by even-aged lodgepole pine in the tree canopy. Hybrid white spruce is a
commonly abundant in the regeneration layer with soopolallie, prickly rose, birch-leaved
spirea and common juniper present in the shrub layer. The sparse to moderate herb
layer includes bunchberry, twinflower, dwarf blueberry and kinnikinnick with Peltigera
species, Cladonia species and red-stemmed feathermoss common.
SBSmc2 - Sub-Boreal Spruce Moist Cold Subzone Babine Variant
The SBSmc2 occurs as a small lobe east of Narcosli Lake between 1200 and 1350m.
Loamy soils occuring on gentle to moderately steep slopes dominated by lodgepole pine
are characteristic of the zonal site in this subzone. (On upper slopes a shallow soil
phase (25-50cm) sometimes occurs over bedrock while all other zonal sites are in the
deep soil phase). Fire history prevents the majority of the stands from reaching their
climax where they would be dominated by hybrid white spruce and subalpine fir. Stands
are characterized by a nearly continuous moss layer with an understory dominated by
black huckleberry, green alder, bunchberry, queen's cup and twinflower.
MSdc2 - Montane Spruce Dry Cold Subzone Tatlayoko Variant
The MSdc2 has a limited occurrence in the Klinaklini and Atnarko River valleys between
1000 and 1670m. Climax forests are dominated by subalpine fir and hybrid white
spruce. Douglas-fir and lodgepole pine are sometimes present in climax stands and
lodgepole pine usually dominates seral stands. Typical shrubs and herbs include
soopolallie, green alder, birch-leaved spirea, twinflower, one-sided wintergreen, heartleaved arnica and bunchberry.
MSxv - Montane Spruce Very Dry Very Cold Subzone
The MSxv occurs as an extensive belt below the ESSFxv1 and above the SBPS units
with an elevational range of 1250 to 1700m. The climax forest of hybrid white spruce
and subalpine fir is rarely present due to slow succession and frequent fire history.
Lodgepole pine usually dominates these stands with hybrid white spruce, lodgepole pine
and occasional subalpine fir regenerating beneath. The understory is commonly made
up of crowberry, grouseberry and twinflower with lesser amounts of heart-leaved arnica
and bunchberry and a continuous layer of Dicranum species, red-stemmed
feathermoss, knight's plume and Cladonia species on the forest floor.
ESSFmw - Engelmann Spruce - Subalpine Fir Moist Warm Subzone
The ESSFmw is confined to a small area in the southwest corner of the study area. The
presence of amabilis fir with subalpine fir is indicative of a coastal climatic influence.
Common shrubs and herbs on zonal sites include white-flowered rhododendron, Sitka
alder, black huckleberry, Sitka valerian, five-leaved bramble and one-sided wintergreen.
ESSFmwp - Engelmann Spruce - Subalpine Fir Parkland Moist Warm Subzone
The ESSFmwp occurs as discontinuous patches above the upper limits of the ESSFmw
proper, typically becoming part of the alpine / subalpine mosaic. Elevations range from
1750 to 2100m. Parkland landscapes are typically composed of tree islands
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EXPANDED LEGEND ITCHA / ILGACHUZ AND CHARLOTTE ALPLANDS
interspersed with dry grasslands and rich herbaceous meadows. Tree islands are
composed of stunted, wind-blown subalpine fir, and meadows are commonly dominated
by Altai fescue, dwarf blueberry, globeflower, subalpine daisy, arrow-leaved groundsel
and mountain sagewort.
ESSFxv1 Engelmann Spruce-Subalpine Fir Very Dry Very Cold Subzone
West Chilcotin Variant
The ESSFxv1 occurs as a horizontal band around all mountains above the MSxv;
approximate elevational range is 1650 to 1750m. The ESSFxv1 zonal site series most
commonly occurs on mid slopes and on upper or lower slopes to a lesser extent.
Lodgepole pine dominates the majority of stands where forest fires have occurred, with
subalpine fir and Engelmann spruce dominating climax stands. Stands on zonal sites
typically have a sparse shrub layer and low covers of heart-leaved arnica, heathers,
grouseberry and Arctic lupine with scattered Dicranum and Cladonia species in the
moss/lichen layer.
ESSFxvp1 Engelmann Spruce - Subalpine Fir Parkland Very Dry Very
Cold Subzone West Chilcotin Variant
The ESSFxvp1 occurs as discontinuous patches above the upper limits of the ESSFxv1
proper, typically becoming part of the alpine / subalpine mosaic. Elevations range from
1750 to 2100m. Parkland landscapes are typically composed of tree islands
interspersed with dry grasslands and rich herbaceous meadows. Tree islands are
composed of stunted, wind-blown subalpine fir, and meadows are commonly dominated
by Altai fescue, dwarf blueberry, globeflower, subalpine daisy, arrow-leaved groundsel
and mountain sagewort.
AT
Alpine Tundra Zone
The Alpine Tundra Zone occurs on all mountain tops at elevations above approximately
1820m. Elevation varies depending on aspect, wind exposure and landform. Mesic
alpine ecosystems (on rich bedrock types) are dominated by either scrub birch or Altai
fescue, typically on subdued slopes of morainal or colluvial material. Other consistently
present herbs include alpine fescue, white mountain-avens, kinnikinnick, mountain
sagewort and northern goldenrod. The patchy moss layer is dominated by Flavocetraria
nivalis, Stereocaulon spp., and Cetraria species. On poor bedrock types (which are
prevalent in the Charlotte Alplands) typical species on mesic sites are scrub birch, dwarf
snow willow, sedges, Altai fescue, ragged snow and Cladina arbuscula.
4. ECOSYSTEM UNITS
An ecosystem unit incorporates site series, site modifiers and structural stage. Site
series are named according to the plant association they belong to; for forested site
series usually one or two tree species and one or two of a shrub, herb, moss, lichen or
liverwort; non-forested site units two or three of any of shrub, herb, moss, lichen and
liverwort species. Two letter site series symbols are now standardized for all
biogeoclimatic units in the province (Resource Inventory Committee 1998). A summary
of all ecosystem units is provided in Table 1.
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EXPANDED LEGEND ITCHA / ILGACHUZ AND CHARLOTTE ALPLANDS
Table 1. Ecosystem Units of the Itcha / Ilgachuz Area
IDFdk4
01
LP
LPf
LPfs
04
DS
DScs
DSv
FdPl - Pinegrass - Feathermoss, typic (gentle mesic slopes, deep, medium-textured moraine)
FdPl - Pinegrass - Feathermoss, fine-textured soil
FdPl - Pinegrass - Feathermoss, fine-textured soil, shallow soil
Fd - Juniper - Pasture sage,typic (deep soil,medium-textured moraine,warm aspect)
Fd - Juniper - Pasture sage, coarse-textured and shallow soil
Fd - Juniper - Pasture sage, very shallow soil
05
DW
DWf
DWs
Fd - Bluebunch wheatgrass - Pinegrass,typic(warm aspect, deep,medium-textured moraine)
Fd - Bluebunch wheatgrass - Pinegrass, fine-textured soil
Fd - Bluebunch wheatgrass - Pinegrass, shallow soil
07
DM
DMs
DMf
Fd - Feathermoss - Stepmoss,typic (deep soil, cool aspect, medium-textured moraine)
Fd - Feathermoss - Stepmoss, shallow soil
Fd - Feathermoss - Stepmoss, fine-textured soil
08
SSf
SS
Sxw - Scrub birch - Feathermoss, typic (lower moist slopes, deep, coarse-textured soil)
Sxw - Scrub birch - Feathermoss, fine-textured soil
00
ND
Needlegrass meadow, typic(deep soil, gentle slope, medium-textured soils)
00
WM
Wet meadow, typic (deep soil, gentle slope, fine-textured soils)
IDFdw
01
DP
DPc
DPk
DPks
DPs
DPw
Fd - Prickly rose - Pinegrass, typic (gentle mesic slopes, deep, medium-textured moraine)
Fd - Prickly rose - Pinegrass, coarse-textured soil
Fd - Prickly rose - Pinegrass, cool aspect
Fd - Prickly rose - Pinegrass, cool aspect, shallow soil
Fd - Prickly rose - Pinegrass, shallow soil
Fd - Prickly rose - Pinegrass, warm aspect
00
AT
ATn
Trembling aspen - Thimbleberry - Sarsaparilla, typic (deep, medium-textured soil, gentle slope)
Trembling aspen - Thimbleberry - Sarsaparilla, fan
00
BP
BPc
BPs
FdBl - Prickly rose - Pinegrass, typic (deep, medium-textured soil, cool aspect)
FdBl - Prickly rose - Pinegrass, coarse-textured soil
FdBl - Prickly rose - Pinegrass, shallow soil
00
CR
Black cottonwood - Red-osier dogwood floodplain, typic
(active floodplain, coarse-textured soil, terrace)
00
DB
00
DK
DKc
DKs
Fd - Prickly rose - Bluebunch wheatgrass, typic (not mapped)
(deep, medium-textured moraine, warm aspect)
Fd - Soopolallie - Kinnikinnick, typic (deep, medium-textured soil, warm aspect)
Fd - Soopolallie - Kinnikinnick, coarse-textured soil
Fd - Soopolallie - Kinnikinnick, shallow soil
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00
DS
DSk
DSkv
DSv
Fd - Saskatoon - Snowberry, typic (shallow soil, warm aspect)
Fd - Saskatoon - Snowberry, cool aspect
Fd - Saskatoon - Snowberry, cool aspect, very shallow soil
Fd - Saskatoon - Snowberry, very shallow soil
00
LK
Pl - Kinnikinnick - Cladonia, typic (deep, coarse-textured soil, gentle slope)
00
SG
SGa
Sxw - Twinberry - Gooseberry, typic (deep, moist medium-textured moraine, gentle slope)
Sxw - Twinberry - Gooseberry, active floodplain
00
SH
SHa
SHc
SHp
Sxw - Horsetail, typic (deep wet, medium-textured soil)
Sxw - Horsetail, active floodplain
Sxw - Horsetail, coarse-textured soil
Sxw - Horsetail, peaty soil
00
SS
SSa
Scrub birch - Sedge - Sphagnum fen, typic (peaty soil)
Scrub birch - Sedge - Sphagnum fen, active floodplain
00
ST
Sxw - Soopolallie - Twinberry, typic (deep,fine-textured soil, moist gentle slope)
STc
Sxw - Soopolallie - Twinberry, coarse-textured soil
STg
Sxw - Soopolallie - Twinberry, gullied
STgk Sxw - Soopolallie - Twinberry, gullied, cool aspect
STgw Sxw - Soopolallie - Twinberry, gullied, warm aspect
STk
Sxw - Soopolallie - Twinberry, cool aspect
STn
Sxw - Soopolallie - Twinberry, fan
SBPSxc
01
LK
Pl - Kinnikinnick - Feathermoss, typic (gentle mesic slopes, deep, medium-textured soil)
LKc
Pl - Kinnikinnick - Feathermoss, coarse-textured soil
LKck
Pl - Kinnikinnick - Feathermoss, coarse-textured soil, cool aspect
LKf
Pl - Kinnikinnick - Feathermoss, fine-textured soil
LKfk
Pl - Kinnikinnick - Feathermoss, fine-textured soil, cool aspect
LKfs
Pl - Kinnikinnick - Feathermoss, fine-textured and shallow soil
LKfw Pl - Kinnikinnick - Feathermoss, fine-textured soil, warm aspect
LKk
Pl - Kinnikinnick - Feathermoss, cool aspect
LKks
Pl - Kinnikinnick - Feathermoss, cool aspect, shallow soil
LKkv
Pl - Kinnikinnick - Feathermoss, cool aspect, very shallow soil
LKs
Pl - Kinnikinnick - Feathermoss, shallow soil
LKsw Pl - Kinnikinnick - Feathermoss, shallow soil, warm aspect
LKw
Pl - Kinnikinnick - Feathermoss, warm aspect
02
LC
Pl - Kinnikinnick - Cladonia, typic (coarse-textured glaciofluvial, deep soil, gentle slope)
LCk
Pl - Kinnikinnick - Cladonia, cool aspect
LCks
Pl - Kinnikinnick - Cladonia, cool aspect, shallow soil
LCkv Pl - Kinnikinnick - Cladonia, cool aspect, very shallow soil
LCr
Pl - Kinnikinnick - Cladonia, ridged
LCs
Pl - Kinnikinnick - Cladonia, shallow soil
LCsw Pl - Kinnikinnick - Cladonia, shallow soil, warm aspect
LCv
Pl - Kinnikinnick - Cladonia, very shallow soil
LCvw Pl - Kinnikinnick - Cladonia, very shallow soil, warm aspect
LCw
Pl - Kinnikinnick - Cladonia, warm aspect
03
SB
SBc
SBf
SBp
Sxw - Scrub birch - Fenmoss, typic (moist cold air depressions, deep soil,gentle slope,medium-textured)
Sxw - Scrub birch - Fenmoss, coarse-textured soil
Sxw - Scrub birch - Fenmoss, fine-textured soil
Sxw - Scrub birch - Fenmoss, peaty soil
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EXPANDED LEGEND ITCHA / ILGACHUZ AND CHARLOTTE ALPLANDS
04
SF
SFc
SFf
SFgk
SFp
SFs
Sxw - Scrub birch - Feathermoss,typic (moist cold air depressions, deep soil, gentle slope, medium-textured)
Sxw - Scrub birch - Feathermoss, coarse-textured soil
Sxw - Scrub birch - Feathermoss, fine-textured soil
Sxw - Scrub birch - Feathermoss, gullied, cool aspect
Sxw - Scrub birch - Feathermoss, peaty soil
Sxw - Scrub birch - Feathermoss, shallow soil
05
SH
SHc
SHf
SHn
SHp
Sxw - Horsetail - Glow moss, typic (moist gentle slopes and depressions, medium-textured soil)
Sxw - Horsetail - Glow moss, coarse -textured soil
Sxw - Horsetail - Glow moss, fine-textured soil
Sxw - Horsetail - Glow moss, fan
Sxw - Horsetail - Glow moss, peaty soil
06
SM
SMa
SMc
SMn
SMp
Sxw - Horsetail - Meadowrue, typic (deep, medium-textured soil, depressions and gentle slopes)
Sxw - Horsetail - Meadowrue, active floodplain
Sxw - Horsetail - Meadowrue, coarse-textured fluvial terrace
Sxw - Horsetail - Meadowrue, fan
Sxw - Horsetail - Meadowrue, peaty soil
00
BS
BSc
BSf
Sedge - Bluejoint fen, typic (peaty)
Sedge - Bluejoint fen, coarse-textured soil
Sedge - Bluejoint fen, fine-textured soil
00
TS
TSf
TSp
Timber oatgrass - Sedge dry meadow, typic (level deep, medium-textured moraine)
Timber oatgrass - Sedge dry meadow, fine-textured soil
Timber oatgrass - Sedge dry meadow, peaty soil
00
WB
WBc
WBf
Willow - Scrub birch shrub carr, typic (deep, medium-textured soil, gentle slope)
Willow - Scrub birch shrub carr, coarse-textured soil
Willow - Scrub birch shrub carr, fine-textured soil
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00
WBp
Willow - Scrub birch shrub carr, peaty soil
WT
WTa
Willow - Sedge fen, typic (organic over floodplain)
Willow - Sedge fen, active floodplain
SBPSdc
01
LJ
LJf
LJk
LJks
LJs
LJw
Pl - Juniper - Feathermoss, typic (deep soil, gentle slope, medium-textured moraine)
Pl - Juniper - Feathermoss, fine-textured soil
Pl - Juniper - Feathermoss, cool aspect
Pl - Juniper - Feathermoss, cool aspect,shallow soil
Pl - Juniper - Feathermoss, shallow soil
Pl - Juniper - Feathermoss, warm aspect
02
LC
Pl - Kinnikinnick - Cladonia, typic (coarse-textured, deep soils on upper slopes)
LCk
Pl - Kinnikinnick - Cladonia, cool aspect
LCr
Pl - Kinnikinnick - Cladonia, ridged
LCs
Pl - Kinnikinnick - Cladonia, shallow soil
LCsw Pl - Kinnikinnick - Cladonia, shallow soil, warm aspect
LCvw Pl - Kinnikinnick - Cladonia, very shallow soil, warm aspect
LCw
Pl - Kinnikinnick - Cladonia, warm aspect
03
LFc
Pl - Kinnikinnick - Feathermoss, typic (coarse-textured)(not mapped)
04
BF
PlSb - Feathermoss, typic (deep soil, gentle slope, medium-textured moraine)
05
SB
SBf
Sxw - Scrub birch - Feathermoss, typic (deep soil, gentle slope,medium-textured moraine)
Sxw - Scrub birch - Feathermoss, fine-textured soil
06
SMa
SMc
Sxw - Horsetail - Meadowrue, active floodplain (deep, gentle slope, medium-textured fluvial)
Sxw - Horsetail - Meadowrue, typic
07
BB
Sb - Scrub birch - Sedge, typic (forested bog, peaty)
00
BS
Sedge - Bluejoint fen, typic (peaty)
00
WT
WTa
Willow - Sedge fen, typic (organic over floodplain)
Willow - Sedge fen, active floodplain
SBPSmc
01
LF
LFk
LFks
LFs
LFw
Pl - Feathermoss - Cladonia, typic (gentle mesic slopes, deep, medium-textured moraine)
Pl - Feathermoss - Cladonia, cool aspect
Pl - Feathermoss - Cladonia, cool aspect, shallow soil
Pl - Feathermoss - Cladonia, shallow soil
Pl - Feathermoss - Cladonia, warm aspect
02
LC
Pl - Kinnikinnick - Cladonia, typic (deep coarse-textured glaciofluvial, gentle slope)
LCk
Pl - Kinnikinnick - Cladonia, cool aspect
LCkv
Pl - Kinnikinnick - Cladonia, cool aspect, very shallow soil
LCr
Pl - Kinnikinnick - Cladonia, ridged
LCrv
Pl - Kinnikinnick - Cladonia, ridged, very shallow soil
LCs
Pl - Kinnikinnick - Cladonia, shallow soil
LCsw Pl - Kinnikinnick - Cladonia, shallow soil, warm aspect
LCvw Pl - Kinnikinnick - Cladonia, very shallow soil, warm aspect
LCw
Pl - Kinnikinnick - Cladonia, warm aspect
03
BF
BFk
SbPl - Feathermoss, typic (gentle slope, deep soil, medium-textured moraine)
SbPl - Feathermoss, cool aspect
04
SB
Sxw - Scrub birch - feathermoss, typic (flat, deep soil,medium-textured moraine)
05
SO
SOa
SOn
Sxw - Horsetail, typic (riparian forests and receiving, gentle slopes, deep soils, medium-textured moraine)
Sxw - Horsetail, active floodplain
Sxw - Horsetail, fan
06
SH
SHa
SHc
Sxw - Horsetail - Glow moss, typic (wet toe slopes and depressions, deep soil, medium-textured moraine)
Sxw - Horsetail - Glow moss, active floodplain
Sxw - Horsetail - Glow moss, coarse-textured soil
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07
BB
Sb - Scrub birch - Sedge, typic (peaty)
00
BS
Sedge - Bluejoint fen, typic (peaty)
00
WB
WBf
WBn
WBp
Willow - Scrub birch shrub carr, typic (gentle slope, deep medium-textured moraine)
Willow - Scrub birch shrub carr, fine-textured soil
Willow - Scrub birch shrub carr, fan
Willow - Scrub birch shrub carr, peaty soil
00
WT
WTa
Willow - Sedge fen, typic (organic over floodplain)
Willow - Sedge fen, active floodplain
SBSmc2
01
SB
Sxw - Huckleberry, typic (mesic medium-textured moraine, deep soil, gentle slope)
SBk
Sxw - Huckleberry, cool aspect
SBks
Sxw - Huckleberry, cool aspect, shallow soil
SBsw Sxw - Huckleberry, shallow soil, warm aspect
SBw
Sxw - Huckleberry, warm aspect
02
PH
Pl - Huckleberry - Cladonia, typic (gentle sloping coarse-textured glaciofluvial terrace, deep soil)
PHsw Pl - Huckleberry - Cladonia, shallow soil, warm aspect
PHw Pl - Huckleberry - Cladonia, warm aspect
04
HB
HBks
Sxw - Huckleberry - Dwarf blueberry, typic (moist medium-textured morainal, deep soil, gentle slope)
Sxw - Huckleberry - Dwarf blueberry, cool aspect, shallow soil
08
ST
Sxw - Twinberry - Oak fern, typic (deep soil, gentle receiving slope, medium-textured)
11
HG
HGf
HGp
Sxw - Horsetail - Glow moss, typic (gentle slope and depression, deep, medium-textured moraine)
Sxw - Horsetail - Glow moss, fine-textured soil
Sxw - Horsetail - Glow moss, peaty soil
00
BS
Sedge - Bluejoint fen, typic (peaty)
MSdc2
01
SF
SFk
SFks
SFw
Sxw - Wintergreen - Feathermoss, typic (deep, medium-textured moraine, gentle slope)
Sxw - Wintergreen - Feathermoss, cool aspect
Sxw - Wintergreen - Feathermoss, cool aspect, shallow soil
Sxw - Wintergreen - Feathermoss, warm aspect
02
DS
FdBl - Spirea - Stonecrop, typic (shallow soil, ridgetops)
DSk
FdBl - Spirea - Stonecrop, cool aspect
DSkv FdBl - Spirea - Stonecrop, cool aspect, very shallow soil
DSvw FdBl - Spirea - Stonecrop, very shallow soil, warm aspect
DSw
FdBl - Spirea - Stonecrop, warm aspect
03
DK
FdBl - Soopolallie - Kinnikinnick, typic (deep medium-textured soil, warm aspect)
DKc
FdBl - Soopolallie - Kinnikinnick, coarse-textured soil
DKkv FdBl - Soopolallie - Kinnikinnick, cool aspect, very shallow soil
DKs
FdBl - Soopolallie - Kinnikinnick, shallow soil
04
PK
PlBl - Soopolallie - Kinnikinnick, typic (deep, coarse-textured soil, gentle slope)
06
ST
STg
Sxw - Twinberry - Reedgrass, typic (deep, fine-textured soil, moist lower slopes and flats)
Sxw - Twinberry - Reedgrass, gullied
07
SG
Sxw - Gooseberry, typic (deep, fine-textured soil, gentle slopes with seepage)
SGa
Sxw - Gooseberry, active floodplain
SGg
Sxw - Gooseberry, gullied
SGgk Sxw - Gooseberry, gulled, cool aspect
SGgw Sxw - Gooseberry, gullied, warm aspect
SGk
Sxw - Gooseberry, cool aspect
SGn
Sxw - Gooseberry, fan
SGw
Sxw - Gooseberry, warm aspect
08
SH
SHa
Sxw - Horsetail, typic (deep, fine-textured soil with near-surface water tables)
Sxw - Horsetail, active floodplain
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00
AW
AWk
Sitka alder - Willow - avalanche tract, typic (deep, medium-textured soil)
Sitka alder - Willow - avalanche tract, cool aspect
00
SS
Scrub birch - Sedge fen, typic (peaty soil)
MSxv
01
LG
LGc
LGck
LGf
LGfk
LGfs
LGfw
LGk
LGks
LGkv
LGs
LGw
Pl - Crowberry - Feathermoss, typic (deep soil, gentle slope, medium-textured moraine)
Pl - Crowberry - Feathermoss, coarse-textured
Pl - Crowberry - Feathermoss, coarse-textured soil, cool aspect
Pl - Crowberry - Feathermoss, fine-textured soil
Pl - Crowberry - Feathermoss, fine-textured soil, cool aspect
Pl - Crowberry - Feathermoss, fine-textured and shallow soil
Pl - Crowberry - Feathermoss, fine-textured soil, warm aspect
Pl - Crowberry - Feathermoss, cool aspect
Pl - Crowberry - Feathermoss, cool aspect, shallow soil
Pl - Crowberry - Feathermoss, cool aspect, very shallow soil
Pl - Crowberry - Feathermoss, shallow soil
Pl - Crowberry - Feathermoss, warm aspect
02
LF
LFs
03
LK
Pl - Kinnikinnick - Cladonia, typic (shallow soil, ridgetop, gentle slope, medium-textured soil)
LKc
Pl - Kinnikinnick - Cladonia, coarse-textured soil
LKk
Pl - Kinnikinnick - Cladonia, cool aspect
LKkv
Pl - Kinnikinnick - Cladonia, cool aspect, very shallow soil
LKv
Pl - Kinnikinnick - Cladonia, very shallow soil
LKvw Pl - Kinnikinnick - Cladonia, very shallow soil, warm aspect
LKw
Pl - Kinnikinnick - Cladonia, warm aspect
04
GK
Pl - Grouseberry - Kinnikinnick, typic (deep, medium-textured soil, gentle slope)
GKc
Pl - Grouseberry - Kinnikinnick, coarse-textured glaciofluvial
GKk
Pl - Grouseberry - Kinnikinnick, cool aspect
GKks Pl - Grouseberry - Kinnikinnick, cool aspect, shallow soil
GKkv Pl - Grouseberry - Kinnikinnick, cool aspect, very shallow soil
GKr
Pl - Grouseberry - Kinnikinnick, ridged
GKs
Pl - Grouseberry - Kinnikinnick, shallow soil
GKsw Pl - Grouseberry - Kinnikinnick, shallow soil, warm aspect
GKv
Pl - Grouseberry - Kinnikinnick, very shallow soil
GKvw Pl - Grouseberry - Kinnikinnick, very shallow soil, warm aspect
GKw
Pl - Grouseberry - Kinnikinnick, warm aspect
06
SC
SCc
SCf
SCfk
SCfs
SCk
SCp
SCs
07
SG
SGc
SGf
SGp
08
00
SH
Pl - Fescue - Stereocaulon, typic (deep, coarse-textured glaciofluvial soil, gentle slope)
Pl - Fescue - Stereocaulon, shallow soil
Sxw - Crowberry - Knight's plume, typic
(deep soil, level to gentle slope, medium-textured moraine wit intermittent seepage)
Sxw - Crowberry - Knight's plume, coarse-textured soil
Sxw - Crowberry - Knight's plume, fine-textured soil
Sxw - Crowberry - Knight's plume, fine-textured soil, cool aspect
Sxw - Crowberry - Knight's plume, fine-textured soil, shallow soil
Sxw - Crowberry - Knight's plume, cool aspect
Sxw - Crowberry - Knight's plume, peaty soil
Sxw - Crowberry - Knight's plume, shallow soil
Sxw - Crowberry - Glow moss, typic
(deep soil, gentle slope with seepage, medium-textured moraine adjacent to wetlands)
Sxw - Crowberry - Glow moss, coarse-textured soil
Sxw - Crowberry - Glow moss, fine-textured soil
Sxw - Crowberry - Glow moss, peaty soil
SHa
SHc
SHf
SHn
SHp
Sxw - Horsetail - Crowberry, typic
(toe slopes, deep medium-textured soil, with near surface water table)
Sxw - Horsetail - Crowberry, active floodplain
Sxw - Horsetail - Crowberry, coarse-textured soil
Sxw - Horsetail - Crowberry, fine-textured soil
Sxw - Horsetail - Crowberry, fan
Sxw - Horsetail - Crowberry, peaty
BP
Scrub birch - Small-flowered penstemon shrub carr,typic
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(deep coarse-textured soil, level to gently sloping cold air basins)
00
BS
BSc
BSf
Sedge - Bluejoint fen, typic (peaty soil)
Sedge - Bluejoint fen, coarse-textured soil
Sedge - Bluejoint fen, fine-textured soil
00
FC
Altai fescue - Cladonia dry grassland,typic
(deep coarse-textured glaciofluvial soil, in cold-air basins)
00
LB
LBc
Pl - Scrub birch - Altai fescue, typic (deep soil, gentle slope, medium-textured moraine)
Pl - Scrub birch - Altai fescue, coarse-textured soil
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00
TB
TBf
TBp
00
TF
Timber oatgrass - Sedge - Herb wet meadow, typic
(coarse glaciofluvial, deep soil, gentle slopes)
Timber oatgrass - Sedge - Herb wet meadow, fine-textured soil
Timber oatgrass - Sedge - Herb wet meadow, peaty soil
TFc
Timber oatgrass - Altai fescue cold dry meadow, typic
(gentle slope, deep, medium-textured moraine, cold-air basins)
Timber oatgrass - Altai fescue cold dry meadow, coarse-textured soil
00
WG
Willow - Glow moss shrublands,typic (active fluvial, coarse-textured soils, level)
00
WS
WSa
Willow - Scrub birch - Sedge fen, typic (organic over floodplain)
Willow - Scrub birch - Sedge fen, active floodplain
ESSFmw
01
FR
FRc
FRk
FRks
FRsw
FRw
02
LJ
LJv
LJvw
LJw
BlBa - Rhododendron, typic (deep, medium-textured soil, gentle slope)
BlBa - Rhododendron, coarse-textured soil
BlBa - Rhododendron, cool aspect
BlBa - Rhododendron, cool aspect, shallow soil
BlBa - Rhododendron, shallow soil, warm aspect
BlBa - Rhododendron, warm aspect
BlPl - Juniper - Racomitrium, typic (gentle slope, ridgetop, shallow soil)
BlPl - Juniper - Racomitrium, very shallow soil
BlPl - Juniper - Racomitrium, very shallow soil, warm aspect
BlPl - Juniper - Racomitrium, warm aspect
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03
DF
DFkv
DFsw
DFvw
Fd - Falsebox - Pinegrass, typic (deep, medium-textured soil, gentle upper slope)
Fd - Falsebox - Pinegrass, cool aspect, very shallow soil
Fd - Falsebox - Pinegrass, shallow soil, warm aspect
Fd - Falsebox - Pinegrass, very shallow soil, warm aspect
04
FH
FHc
FHcw
FHks
FHsw
FHw
Bl - Huckleberry - Falsebox, typic (deep, medium-textured soil, gentle upper slopes)
Bl - Huckleberry - Falsebox, coarse-textured soil
Bl - Huckleberry - Falsebox, coarse-textured soil, warm aspect
Bl - Huckleberry - Falsebox, cool aspect, shallow soil
Bl - Huckleberry - Falsebox, shallow soil, warm aspect
Bl - Huckleberry - warm aspect
05
FA
BlBa - Azalea - Pipecleaner moss, typic
(deep, medium-textured soil, lower receiving gentle slopes)
06
FV
FVc
FVgw
Bl - Gooseberry - Valerian, typic (deep, medium-textured soil, lower receiving gentle slopes)
Bl - Gooseberry - Valerian, coarse-textured soil
Bl - Gooseberry - Valerian, gullied, warm aspect
07
FO
FOa
FOn
BlBa - Oak fern - Lady fern, typic (deep, medium-textured soil, lower receiving gentle slopes)
BlBa - Oak fern - Lady fern, active floodplain
BlBa - Oak fern - Lady fern, fan
08
FG
Bl - Gooseberry - Horsetail, typic
(treed swamp, deep, medium-textured, poorly drained soil)
Bl - Gooseberry - Horsetail, fan
FGn
00
AV
AVk
AVks
AVsw
AVw
Sitka alder - Willow - Sitka valerian avalanche tract, typic
(deep, medium-textured soil)
Sitka alder - Willow - Sitka valerian avalanche tract, cool aspect
Sitka alder - Willow - Sitka valerian avalanche tract, cool aspect, shallow soil
Sitka alder - Willow - Sitka valerian avalanche tract, shallow soil, warm aspect
Sitka alder - Willow - Sitka valerian avalanche tract, warm aspect
00
BS
Sedge - Bluejoint fen, typic (peaty soil)
00
DG
Subalpine daisy - Arrow-leaved groundsel wet meadow,typic
(deep, medium-textured soil, gentle slope)
Subalpine daisy - Arrow-leaved groundsel wet meadow, peaty soil
Subalpine daisy - Arrow-leaved groundsel wet meadow, warm aspect
DGp
DGw
00
SS
SSks
Scrub birch - Ragged snow shrub steppe, typic
(deep, medium-textured soil, gentle slope)
Scrub birch - Ragged snow shrub steppe, cool aspect, shallow soil
00
TW
Two-toned sedge - Dwarf snow willow tundra, typic
(deep, medium-textured soil, gentle slope)
00
WS
WSa
WSn
Willow - Scrub birch - Sedge fen, typic (peaty soil)
Willow - Scrub birch - Sedge fen, active floodplain
Willow - Scrub birch - Sedge fen, fan
ESSFxv1
01
AC
ACc
ACcs
ACk
ACks
ACs
ACsw
ACw
02
WJ
WJd
WJdk
WJdw
WJk
WJkv
WJv
WJvw
Bl - Arnica - Cladonia, typic (deep soil, gentle slope, medium-textured moraine)
Bl - Arnica - Cladonia, coarse-textured soil
Bl - Arnica - Cladonia, coarse-textured, shallow soil
Bl - Arnica - Cladonia, cool aspect
Bl - Arnica - Cladonia, cool aspect, shallow soil
Bl - Arnica - Cladonia, shallow soil
Bl - Arnica - Cladonia, shallow soil, warm aspect
Bl - Arnica - Cladonia, warm aspect
BlPa - Juniper - Cladonia, typic (shallow soil, gently sloping ridgetops)
BlPa - Juniper - Cladonia, deep soil
BlPa - Juniper - Cladonia, deep soil, cool aspect
BlPa - Juniper - Cladonia, deep soil, warm aspect
BlPa - Juniper - Cladonia, cool aspect
BlPa - Juniper - Cladonia, cool aspect, very shallow soil
BlPa - Juniper - Cladonia, very shallow soil
BlPa - Juniper - Cladonia, very shallow soil, warm aspect
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WJw
BlPa - Juniper - Cladonia, warm aspect
03
LC
LCk
LCks
LCkv
LCr
LCs
LCsw
LCv
LCvw
LCw
Pl - Cladonia - Stereocaulon, typic (coarse-textured glaciofluvial, deep soil, gentle slope)
Pl - Cladonia - Stereocaulon, cool aspect
Pl - Cladonia - Stereocaulon, cool aspect, shallow soil
Pl - Cladonia - Stereocaulon, cool aspect, very shallow soil
Pl - Cladonia - Stereocaulon, ridged
Pl - Cladonia - Stereocaulon, shallow soil
Pl - Cladonia - Stereocaulon, shallow soil, warm aspect
Pl - Cladonia - Stereocaulon, very shallow soil
Pl - Cladonia - Stereocaulon, very shallow soil, warm aspect
Pl - Cladonia - Stereocaulon, warm aspect
04
JG
JGm
JGms
JGs
JGv
BlPa - Juniper - Grouseberry, typic (coarse-textured, deep soil, warm aspect)
BlPa - Juniper - Grouseberry, medium-textured soil
BlPa - Juniper - Grouseberry, medium-textured soil, shallow soil
BlPa - Juniper - Grouseberry, shallow soil
BlPa - Juniper - Grouseberry, very shallow soil
05
AT
ATs
ATv
BlPa - Arnica - Twinflower, typic (coarse-textured, deep soil, cool aspect)
BlPa - Arnica - Twinflower, shallow soil
BlPa - Arnica - Twinflower, very shallow soil
06
FR
Bl - Rhododendron - Crowberry, typic
(coarse-textured, deep soil, gentle slopes with intermittent seepage)
Bl - Rhododendron - Crowberry, cool aspect
Bl - Rhododendron - Crowberry, cool aspect, shallow soil
Bl - Rhododendron - Crowberry, shallow soil
FRk
FRks
FRs
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07
FV
FVc
FVg
FVgk
FVgw
FVk
FVp
FVs
FVw
08
FH
Bl - Valerian - Arnica, typic
(moisture-receiving lower gentle slopes, deep medium-textured moraine)
Bl - Valerian - Arnica, coarse-textured soil
Bl - Valerian - Arnica, gullied
Bl - Valerian - Arnica, gulled, cool aspect
Bl - Valerian - Arnica, gulled, warm aspect
Bl - Valerian - Arnica, cool aspect
Bl - Valerian - Arnica, peaty soil
Bl - Valerian - Arnica, shallow soil
Bl - Valerian - Arnica, warm aspect
FHa
FHc
FHks
FHn
FHp
FHw
Bl - Horsetail - Glow moss, typic
(cold, moist valley floor, medium-textured, deep level to gently sloping moraine)
Bl - Horsetail - Glow moss, active floodplain
Bl - Horsetail - Glow moss, coarse-textured soil
Bl - Horsetail - Glow moss, cool aspect, shallow soil
Bl - Horsetail - Glow moss, fan
Bl - Horsetail - Glow moss, peaty soil
Bl - Horsetail - Glow moss, warm aspect
00
AF
AFw
White mountain-avens - Altai fescue tundra, typic (shallow soils and gentle slopes)
White mountain-avens - Altai fescue tundra, warm aspect
00
AV
Sitka alder - Willow - Sitka valerian avalanche, typic
(deep, medium-textured soil)
Sitka alder - Willow - Sitka valerian avalanche, cool aspect
Sitka alder - Willow - Sitka valerian avalanche, cool aspect, shallow soil
Sitka alder - Willow - Sitka valerian avalanche, shallow soil, warm aspect
Sitka alder - Willow - Sitka valerian avalanche, warm aspect
AVk
AVks
AVsw
AVw
00
BP
Scrub birch - Small-flowered penstemon shrub carr, typic
(deep soil, gentle slopes in cold air basins, medium-textured moraine)
00
BS
Sedge - Bluejoint fen, typic (peaty)
BSc
Sedge - Bluejoint fen, coarse-textured soil
00
BV
Bluejoint - Sitka valerian avalanche tract, typic (deep, peaty soil)
Note: This unit was not mapped.
00
DG
Subalpine daisy - Arrow-leaved groundsel wet meadow, typic
(deep moist soil, gentle slope, medium-textured moraine and fluvial)
Subalpine daisy - Arrow-leaved groundsel wet meadow, coarse-textured soil
Subalpine daisy - Arrow-leaved groundsel wet meadow, cool aspect
Subalpine daisy - Arrow-leaved groundsel wet meadow, peaty soil
Subalpine daisy - Arrow-leaved groundsel wet meadow, shallow soil
DGc
DGk
DGp
DGs
00
FC
FCsw
FCv
Altai fescue - Cladonia dry grassland, typic
(deep, coarse-textured soil, gentle slope in cold-air basins)
Altai fescue - Cladonia dry grassland, shallow soil, warm aspect
Altai fescue - Cladonia dry grassland, very shallow soil
00
LB
Pl - Scrub birch - Altai fescue, typic
(deep soil, gentle slope, medium-textured moraine adjacent to shrub carrs and meadows)
00
SS
Scrub birch - Ragged snow, shrub steppe, typic
(deep, medium-textured soil, gentle slope)
Scrub birch - Ragged snow, shrub steppe, cool aspect
Scrub birch - Ragged snow, shrub steppe, cool aspect, shallow soil
Scrub birch - Ragged snow, shrub steppe, shallow soil, warm aspect
SSk
SSks
SSsw
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00
TB
Timber oatgrass - Sedge - Herb wet meadow, typic
(deep, coarse-textured soil, gentle slopes in moist cold air basins)
Timber oatgrass - Sedge - Herb wet meadow, peaty soil
TBp
00
TF
TFc
Timber oatgrass - Altai fescue cold dry meadow, typic
( deep soil, gentle slope, medium-textured moraine cold-air basins)
Timber oatgrass - Altai fescue cold dry meadow, coarse-textured soil
00
WG
WGn
Willow - Glow moss shrublands, typic (active floodplain)
Willow - Glow moss shrublands, fan
00
WS
WSa
Willow - Scrub birch - Sedge fen, typic (peaty)
Willow - Scrub birch - Sedge fen, active floodplain
ESSFmwp and ESSFxvp1
00
AF
*
AFk
AFks
AFkv *
AFs
AFsw
AFv *
AFvw
AFw
White mountain-avens - Altai fescue tundra, typic
(deep, medium - textured soil, gentle slope)
White mountain-avens - Altai fescue tundra, cool aspect
White mountain-avens - Altai fescue tundra, cool aspect, shallow soil
White mountain-avens - Altai fescue tundra, cool aspect, very shallow soil
White mountain-avens - Altai fescue tundra, shallow soil
White mountain-avens - Altai fescue tundra, shallow soil, warm aspect
White mountain-avens - Altai fescue tundra, very shallow soil
White mountain-avens - Altai fescue tundra, very shallow soil, warm aspect
White mountain-avens - Altai fescue tundra, warm aspect
00
CS
CSa
CSn
Cottongrass - Sedge - Sphagnum fen, typic (peaty soil)
Cottongrass - Sedge - Sphagnum fen, active floodplain
Cottongrass - Sedge - Sphagnum fen, fan
00
DG *
Subalpine daisy - Arrow-leaved groundsel wet meadow, typic
(deep, medium-textured soil, moist gentle slope)
Subalpine daisy - Arrow-leaved groundsel wet meadow, cool aspect
Subalpine daisy - Arrow-leaved groundsel wet meadow, cool aspect, peaty soil
Subalpine daisy - Arrow-leaved groundsel wet meadow, peaty soil
Subalpine daisy - Arrow-leaved groundsel wet meadow, shallow soil
Subalpine daisy - Arrow-leaved groundsel wet meadow, warm aspect
DGk
DGkp
DGp
DGs
DGw
00
FB *
Bl - Dwarf blueberry - Dicranum parkland, typic
(deep, medium-textured soil, gentle slope)
FBc
Bl - Dwarf blueberry - Dicranum parkland, coarse-textured soil
FBk
Bl - Dwarf blueberry - Dicranum parkland, cool aspect
FBks* Bl - Dwarf blueberry - Dicranum parkland, cool aspect, shallow soil
FBkv
Bl - Dwarf blueberry - Dicranum parkland, cool aspect, very shallow soil
FBs *
Bl - Dwarf blueberry - Dicranum parkland, shallow soil
FBsw * Bl - Dwarf blueberry - Dicranum parkland, shallow soil, warm aspect
FBvw
Bl - Dwarf blueberry - Dicranum parkland, very shallow soil, warm aspect
FBw
Bl - Dwarf blueberry - Dicranum parkland, warm aspect
Note - * indicates units occurring in both ESSFmwp and ESSFxvp1; all others occur only in the
ESSFxvp1
00
FC
00
FCc
FCks
FCs
FCsw
FCw
Altai fescue - Cladonia grassland, typic
(deep, medium-textured soil, gentle slope, rich bedrock types)
Altai fescue - Cladonia grassland, coarse-textured soil
Altai fescue - Cladonia grassland, cool aspect, shallow soil
Altai fescue - Cladonia grassland, shallow soil
Altai fescue - Cladonia grassland, shallow soil, warm aspect
Altai fescue - Cladonia grassland, warm aspect
FM *
FMk *
FMks
FMs
FMsw
FMw*
Bl - Heather parkland, typic (deep, medium-textured soil, gentle slope)
Bl - Heather parkalnd, cool aspect
Bl - Heather parkland, cool aspect, shallow soil
Bl - Heather parkland, shallow soil
Bl - Heather parkland, shallow soil, warm aspect
Bl - Heather parkland, warm aspect
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00
HT *
HTk *
HTks
HTs
HTsw
HTw
Heather - Mountain sagewort tundra, typic
(deep, medium-textured soil, gentle slope)
Heather - Mountain sagewort tunda, cool aspect
Heather - Mountain sagewort tundra, cool aspect, shallow soil
Heather - Mountain sagewort tundra, shallow soil
Heather - Mountain sagewort tundra, shallow soil, warm aspect
Heather - Mountain sagewort tundra, warm aspect
00
PC
PCk
PCw
Pa - Crowberry krummholz, typic (gentle slope, shallow soil)
Pa - Crowberry krummholz, cool aspect
Pa - Crowberry krummholz, warm aspect
00
SF
Scrub birch - Altai fescue shrub steppe, typic
(deep, medium-textured soil, gentle slope, rich bedrock types)
Scrub birch - Altai fescue shrub steppe, cool aspect
Scrub birch - Altai fescue shrub steppe, cool aspect, shallow soil
Scrub birch - Altai fescue shrub steppe, shallow soil
Scrub birch - Altai fescue shrub steppe, shallow soil, warm aspect
Scrub birch - Altai fescue shrub steppe, warm aspect
SFk
SFks
SFs
SFsw
SFw
00
SS
00
TW *
AT
00
AF
00
*
Scrub birch - Ragged snow shrub steppe, typic
(deep, medium-textured soil, gentle slope, poor bedrock types)
SSk * Scrub birch - Ragged snow shrub steppe, cool aspect
SSks * Scrub birch - Ragged snow shrub steppe, cool aspect, shallow soil
SSs
Scrub birch - Ragged snow shrub steppe, shallow soil
SSsw Scrub birch - Ragged snow shrub steppe, shallow soil, warm aspect
SSw
Scrub birch - Ragged snow shrub steppe, warm aspect
Two-toned sedge - Dwarf snow willow tundra, typic
(deep, medium-textured soil, gentle slope, poor bedrock types)
TWk * Two-toned sedge - Dwarf snow willow tundra, cool aspect
TWks* Two-toned sedge - Dwarf snow willow tundra, cool aspect, shallow soil
TWs * Two-toned sedge - Dwarf snow willow tundra, shallow soil
TWsw Two-toned sedge - Dwarf snow willow tundra, shallow soil, warm aspect
TWw
Two-toned sedge - Dwarf snow willow, tundra, warm aspect
AFd
AFdk
AFk
AFkv
AFv
AFvw
AFw
White mountain-avens - Altai fescue tundra, typic
(shallow soil, gentle slope)
White mountain-avens - Altai fescue tundra, deep soil
White mountain-avens - Altai fescue tundra, deep soil, cool aspect
White mountain-avens - Altai fescue tundra, cool aspect
White mountain-avens - Altai fescue tundra, cool aspect, very shallow soil
White mountain-avens - Altai fescue tundra, very shallow soil
White mountain-avens - Altai fescue tundra, very shallow soil, warm aspect
White mountain-avens - Altai fescue tundra, warm aspect
CS
CSn
Cottongrass - Sedge - Sphagnum, typic (peaty soil)
Cottongrass - Sedge - Sphagnum, fan
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00
FC
FCk
FCks
FCkv
FCs
FCsw
FCw
00
HT
HTk
HTks
HTs
HTsw
HTw
Altai fescue-Cladonia grassland, typic
(deep soil, medium-textured soil, gentle slope, rich bedrock types)
Altai fescue-Cladonia grassland, cool aspect
Altai fescue-Cladonia grassland, cool aspect, shallow soil
Altai fescue-Cladonia grassland, cool aspect, very shallow soil
Altai fescue-Cladonia grassland, shallow soil
Altai fescue-Cladonia grassland, shallow soil, warm aspect
Altai fescue-Cladonia grassland, warm aspect
Heather - Mountain sagewort tundra, typic
(deep, medium-textured soil, gentle slope, poor bedrock types)
Heather - Mountain sagewort tundra, cool aspect
Heather - Mountain sagewort tundra, cool aspect, shallow soil
Heather - Mountain sagewort tundra, shallow soil
Heather - Mountain sagewort tundra, shallow soil, warm aspect
Heather - Mountain sagewort tundra, warm aspect
00
MW
Moss campion-Spiked wood-rush tundra, typic (shallow soils, gentle slope)
(Note: MW is mapped as part of AF unit)
00
PC
PCk
PCw
Pa - Crowberry krummholz, typic (shallow soil, gentle slope)
Pa - Crowberry krummholz, cool aspect
Pa - Crowberry krummholz, warm aspect
00
SF
SFk
SFks
SFkv
SFs
SFsw
SFw
Scrub birch - Altai fescue shrub steppe, typic
(deep, medium-textured soil, gentle slope, rich bedrock types)
Scrub birch - Altai fescue shrub steppe, cool aspect
Scrub birch - Altai fescue shrub steppe, cool aspect, shallow soil
Scrub birch - Altai fescue shrub steppe, cool aspect, very shallow soil
Scrub birch - Altai fescue shrub steppe, shallow soil
Scrub birch - Altai fescue shrub steppe, shallow soil, warm aspect
Scrub birch - Altai fescue shrub steppe, warm aspect
00
SM
Sedge - Mountain sagewort wet meadow, typic (deep moist, medium-textured soil, gentle slope)
00
SS
Scrub birch - Ragged snow, shrub steppe, typic
(deep, medium-textured soil, gentle slope, poor bedrock types)
Scrub birch - Ragged snow, shrub steppe, cool aspect
Scrub birch - Ragged snow, shrub steppe, cool aspect, shallow soil
Scrub birch - Ragged snow, shrub steppe, cool aspect, very shallow soil
Scrub birch - Ragged snow, shrub steppe, shallow soil
Scrub birch - Ragged snow, shrub steppe, shallow soil, warm aspect
Scrub birch - Ragged snow shrub steppe, warm aspect
SSk
SSks
SSkv
SSs
SSsw
SSw
00
TW
TWk
TWks
TWs
TWsw
TWw
Two-toned sedge - Dwarf snow willow tundra, typic
(deep, medium-textured soil, gentle slope, poor bedrock types)
Two-toned sedge - Dwarf snow willow tundra, cool aspect
Two-toned sedge - Dwarf snow willow tundra, cool aspect, shallow soil
Two-toned sedge - Dwarf snow willow tundra, shallow soil
Two-toned sedge - Dwarf snow willow tundra, shallow soil, warm aspect
Two-toned sedge - Dwarf snow willow tundra, warm aspect
Each ecosystem is described in terms of dominant and associated plant species for each vegetation layer (trees, shrubs, herbs
and mosses / lichens / liverworts). Dominant species have a frequency of 75% or greater, combined with a mean cover of at
least 5%. Associated species have a frequency of less than 75% (with any mean cover value) or frequency of 75% or greater
combined with mean cover of less than 5%. Frequency is the number of plots (within the sample group) that a species occurs in,
expressed as a percentage. Mean cover is the mean of all percent cover ratings for specific plants within an ecosystem unit.
For site series with less than 3 samples, information provided in the field guide (Steen and Coupe 1997) is used to derive
descriptions of site conditions and vegetation.
A number of anthropogenic and sparsely vegetated units were mapped:
BF,BFk,BFs,BFw
Blockfield
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Angular blocks of rock derived from underlying bedrock or drift.
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CF
ES,ESw
GB
GL
LA
OW
PD
RI
RO,ROk,ROw
RR
Cultivated field
Exposed soil
Gravel bar
Glacier
Lake
Open water
Pond
River
Rock outcrop
Rural
TA,TAk,TAw
Talus slope
UR
Urban
Area subject to human agricultural processes.
Any area of exposed soil that is not included in any of the other
Un-vegetated wave and current formed bar in larger rivers.
A mass of perennial ice and snow with definite lateral limits.
Water body >2m deep and >50ha in area.
Wetland of standing water <2m deep.
A small body of water >2m deep, but less then 50ha.
Watercourse formed when water flows between continuous,
Gentle to steep, bedrock escarpment or outcropping.
Any area in which residences and other human developments are scattered and
intermingled with forest, range, farmland and native vegetation or cultivated crops
Angular rock fragments of any size accumulated at the foot of steep
rock slopes as a result of successive rock falls.
An area in which residences and other human developments form an
No detailed descriptions are provided for these units (except for CF in SBPSxc, TA in ESSFxv1, RO in MSxv, and BF in AT).
For site descriptions, surficial material, soil development and humus forms are listed in order of frequency of occurrence. See
Glossary for definition of technical terms. Arboreal lichen ratings (ALR) are provided for all forested site series. Where data was
available the ratings are linked to specific structural stages, otherwise a general rating is given to the entire site series.
5. GLOSSARY (Footnotes denote sources)
bog1
Nutrient - poor peatlands (pH <4.5) characterized by plant communities with a large component of ericaceous shrubs and
Sphagnum mosses.
blanket2
A mantle of unconsolidated materials thick enough to mask minor irregularities of the surface, but still conforming to underlying
topography; greater than 1 metre thick.
Brunisolic Gray3
A luvisolic soil (clay enriched Bt horizon) that has a Luvisol weakly developed mineral soil horizon (Bm) on the surface.
Cumulic Regosol3
A soil lacking development which forms through periodic repeated inundation as evidenced by buried thin humus layers.
dry meadow
Typically developed on well-drained mineral materials; diverse community of upland herbs, grasses and sedges.
Eluviated Dystric3
A weakly-developed acidic soil lacking a well-developed
Brunisol
mineral-organic surface horizon, which has an eluviated horizon (Ae).
fan2
A relatively smooth segment of a cone with a slope gradient of up to 26%. Typically applied to fluvial fans, colluvial fans or
glaciofluvial fans.
fen1
A wetland dominated by sedges and grasses where the main source of water is through-flowing (groundwater).
Fibric Humisol3
A humic (well decomposed) organic soil with a sub- dominant Fibric (poorly decomposed) layer.
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fluvial2
Materials transported and deposited by streams and rivers.
glaciofluvial2
Materials that exhibit clear evidence of having been deposited by glacial meltwater in front of or in contact with glacial ice.
Gleyed Dystric
Differs from Eluviated Dystric Brunisol by having mottles Brunisol 3
that indicate gleying.
Gleyed Gray3
A luvisolic soil (Clay enriched Bt horizon) with distinct Luvisol mottling within 50cm of the mineral surface or prominent mottles at
depths of 50 - 100 cm
Gleyed Humo-Ferric3
Differ from Orthic Humo-Ferric Podzol by having Podzol mottles that indicate gleying.
Gleyed Regosol3
They differ from Orthic Regosol by having faint to distinct mottles that indicate gleying within 50 of the mineral surface.
Lacustrine2
Sediments that have settled from suspension, in bodies of standing fresh water.
Mesic Fibrisol3
A fibric (poorly decomposed) organic soil with a subdominant mesic layer (moderately decomposed) layer.
Mesic Humisol3
A humic (well decomposed) organic soil with a subdominant mesic layer (moderately decomposed) layer.
Moder4
Humus form having F and H humus horizons which have been fragmented through faunal activity.
Mor4
Humus form having the least level of decomposition with fungi dominant in the F horizon (fermented).
morainal2
Material deposited directly by glacier ice without modification by any other agent of transportation.
organic2
Sediments composed largely of organic materials resulting from the accumulation of vegetative matter.
Orthic Dystric3
Weakly - developed acidic soils lacking a well-developed Brunisol mineral-organic surface horizon.
Orthic Gleysol3
Soils having strongly gleyed B and C horizons and may have organic surface horizons and an eluvial horizon.
Orthic Gray3
A soil usually derived from fine-textured parent material, Luvisol with a clay-enriched B horizon (Bt).
Orthic Humic3
Gleyed soils (subject to fluctuating water tables as Gleysol evidenced by strong mottling in the soil profile) with an organic
enriched surface horizon (Ah).
Orthic Humo-Ferric3
Soils having a Bhf horizon at least 10cm thick, usually Podzol having an Ac horizon.
Orthic Regosol3
A soil lacking development, with no horizon differentiation in the soil profile.
plain2
A level or very gentle sloping, unidirectional surface. (0 to 5% slope).
Rego Gleysol3
A gleysolic soil lacking a B horizon at least 10 cm thick.
Rego Humic3
Differs from an Orthic Humic Gleysol by lacking a B Gleysol horizon at least 10cm thick.
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shrub carr1
Low shrub-dominated ecosystem in frost-prone basins; never inundated and seasonally saturated; usually has extremely
mounded shrubs on elevated sites; herb and moss layers diverse, often dominated by forbs and grasses.
terrace2
A single or assemblage of step-like form(s) where each step-like form consists of a scarp face and a horizontal or gently inclined
surface above it.
Terric Fibrisol3
A fibric (poorly decomposed) organic soil with at least 40 cm of organic material over mineral soil.
Terric Humisol3
A humic (well decomposed) organic soil having at least 40 cm of organic matter (of which at least 12 cm is humic) over mineral
soil.
Terric Mesisol3
A moderately well decomposed (mesic) organic soil with mineral soil contact within 40 cm of the soil surface.
Typic Humisol3
Organic soils having the most advanced stage of decomposition (humic).
Typic Mesisol3
Organic soils having a moderate level of decomposition (mesic).
veneer2
A mantle of unconsolidated materials too thin to mask minor irregularities of the surface of the underlying materal; thickness
ranges from 10 cm to 1 metre.
wet meadow1
Developed on mineral materials; periodically saturated, seldom inundated; diverse community of grasses, low sedges, rushes
and forbs.
1.
2.
3.
4.
Field Manual for Describing Ecosystem 1998.
Howes and Kenk 1997.
Canadian System of Soil Classification 1987.
Klinka et al. 1981.
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6. REFERENCES
Agriculture Canada Expert Committee on Soil Survey. 1987. Canadian system of soil classification. 2nd edition.
Agriculture Canada Publication 1646. 164 p.
B.C. Ministry of Environment, Lands and Parks and B.C. Ministry of Forests. 1998. Field manual for describing terrestrial
ecosystems, Victoria, B.C.
Crum, A.H., W.C. Steer, and L.E. Anderson. 1973. A new list of mosses for North America north of Mexico. Bryologist
76:83-130.
Hale, M.E., and W.L. Culberson. 1970. A second checklist of the lichens of the continental United States and Canada.
Bryologist 63:137-172.
Douglas, G.W., G.B. Straley, and D. Meidinger. 1989, 1990, 1991, 1994. The Vascular Plants of British Columbia. Parts
1-4. Special Report Series Nos. 1-4. Research Branch, B.C. Ministry of Forests, Victoria, B.C.
Holland, S.S. 1976. Landforms of British Columbia. A physiographic outline. Bulletin 48. British Columbia Department of
Mines and Mineral
Resources, Victoria. 138 p.
Howes, D.E., and E. Kenk. 1997. Terrain classification system for British Columbia (revised edition). MOE Manual 10.
Recreational Fisheries Branch, Ministry of Environment, and Surveys and Resource Mapping Branch, Ministry of Crown Lands,
Province of British Columbia, Victoria, B.C. 90 p.
Klinka, K., R.N. Green, R.L. Trowbridge, and L.E. Lowe. 1981. Taxonomic classification of humus forms in ecosystems of
British Columbia. First Approximation. Land Management Report 8. British Columbia Ministry of Forests, Victoria. 54 p.
Luttmerding, H.A., D.A. Demarchi, E.C. Lea, D.V. Meidinger and T. Vold (editors). 1990. Describing ecosystems in the
field (2nd edition). MOE Manual II. Ministry of Environment, Lands and Parks, in cooperation with Ministry of Forests, Victoria,
B.C. 213 p.
Meidinger, D. 1987. Recommended vernacular names for common plants of British Columbia. B.C. Ministry of Forests
and Lands, Research Report RR8702-HQ. Victoria. 64 p.
Resources Inventory Committee. 1998. Standard for terrestrial ecosystem mapping in British Columbia. Ministry of
Environment, Lands and Parks. Victoria, B.C.
Steen, O.A. and R.A. Coupe. 1997. A field guide to forest site identification and interpretation for the Cariboo Forest
Region. B.C. Ministry of Forest, Victoria, B.C. Land Mangement Handbook 39 p. (Ports 1 and 2).
Taylor, R.L., and B. MacBryde. 1977. Vascular plants of British Columbia: a descriptive resource inventory. Technical
Bulletin 4. University of British Columbia, Vancouver.
Tipper, H.W. 1970. Glacial geomorphology and pleistoncene history of central British Columbia. Geological Survey of
Canada, Bulletin 196. Department of Energy, Mines and Resources, Ottawa, Canada.
Armleder, H.M., S.K. Stevenson and S.D. Walker. 1992. Estimating the abundance of arboreal forage lichens. Land
Management Handbook Field Guide Insert 7. B.C. Ministry of Forests, Victoria, B.C.
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Figure 1. Study Area
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SBPSxc / 02 - Plot 9628105, logged
SBPSxc / 02 - Plot 9620058, pole sapling stage.
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Plot 9628195 - SBPSxc / 06 active floodplain.
Plot 9628194 - SBPSxc / 06
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open shrubby / herb site.
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Plot 9620061 - MSxv / 01, shrub stage.
Plot 9614544 - MSxv / 01, pole sapling stage.
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Typical parkland (FB) interspersed with FC and AF (both pictures).
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Rock unit in ESSFxv1.
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Typical barren talus is ESSFxv1.
No data was obtained for the ESSFmwp units (only in the Charlotte Alplands). Refer to
the appropriate ESSFxvp1 description; plant species may differ slightly from those in the
ESSFxvp1. The following map units occur in both ESSFxvp1 and ESSFmwp:
AF, AFkv, AFv
DG
FB, FBks, FBs, Fbsw
FM, FMk, FMw
HT, HTk
SS, SSk, SSks
TW, TWk, TWks, TWs
Descriptions for the following site series can be found as follows:
SS, SSk, SSks, SSs, SSsw, SSw
TW, TWk, TWks, TWs, TWsw, TWw
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AT
AT
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Logged mesic (01) site in ESSFxv1, Plot 9801266
Sedge - Bluejoint fen in ESSFxv1, Plot 9801371
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Typical FB parkland (Plot 9801255)
PC krummholz slope in alpine transition (Plot 9801298)
Typical rich fen in Alpine Tundra Zone.
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Windswept AF ridge, in Charlotte Alplands.
APPENDIX A
Plant Species List
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ECOSYSTEM DESCRIPTIONS
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