(TFT) The Conjurers' Crooked Cottage

["Jay Carlisle" <Jay_Carlisle@charter.net>]

The following is the background for the little cabin on top of a hill I 
talked about awhile back.
This was all done as a "collapsible" HTML doc (the little lodge is 
collapsible too) for the webspace that Charter Communications can't manage 
to keep running so I throw it up like this for now sans Maps and images.
The actual location of the house is in Marion County Oregon, but by 
includeing this "broad background" on the surounding region I can handel 
"open-ended player Actions" MUCH easier in play.

Wanna be a jerk and ignore my little cabin and just start walking?
I'm not lost.

Wanna "start digging"?
I've got that.

There is obviously quite a bit more to do, but bear in mind that this whole 
structure collapses to 8 nodes, only one of which is the actual cottage 
itself.
If you just want to run the thing as a traditional module then thats the 
only node you'll need to click.
Another bonus, anything else I write-up for this geographical region uses 
this same background.

I'd be quite curious to hear what y'all think of the structure... IMHO this 
is the kind of info one needs to actually implement "War" (the 'Goblin' port 
is still just a little north and west of Hull in east central Britan by the 
by, but the gunpowder stuff is still centered around New Zeland.)




All + All -
The Conjurers' Crooked Cottage

- Geographical Locations
- Geography & Geology
- Log. & Lat.
The Pacific Northwest is located in the northern and western hemispheres 
encompassed by a box from ~40 to 50 degrees north to south by ~110 to 125 
degrees east to west.

- Soils/Subsoils
Entisols
Vertisols
Inceptisols
Aridisols
Mollisols
Spodosols
Alfisols
Ultisols
Oxisols
Histolsols
Soil Orders and Sub-Orders Regions Map

- Landforms

- Major Tectonic Features
Anticline
Syncline
Thrust Fault
Normal Fault
Transcurrent Fault
Volcanic Cone
Calderia
Structural Basin
+ Hypothetical Cross Section
Major Tectonic Feature Map

- Glacial
Wisconsin Continental Glaciation
Wisconsin Alpine Glaciation
Glacial Outwash
Pleistocene Lakes
Wisconsin Loess Deposits >32 feet
Existing Glaciers
Glacial and Periglacial Feature Map

- Regions
- Pacific Border Province
- Klamath - Siskiyou Mtns.
The Klamath Mountains section is defined on a partially geologic and 
partially topographic basis. The steep topography, dense vegetation, and 
structural complexity have produced a confusing geologic record. Metamorphic 
recrystallization masks much of the deposition history of the ancient 
sedimentary and volcanic strata of the region. This section has been folded, 
uplifted a few thousand feet, and dissected by erosion. Topographically 
these mountains merge with the younger Coast Range to the north and with the 
southern end of the Cascade Range.

- Coast Range
The Coast Range of Oregon and Washington consists of moderately folded 
marine tuffaceous sandstones and shales together with basaltic volcanic 
rocks and related intrusive. These have been uplifted 1000 to 2000 feet or 
more, and then eroded by streams to a generally submature stage. Resistant 
igneous rocks account for certain summits and for several capes projecting 
seaward. Sea terraces, sand dunes, and other shore features occupy narrow 
strips along the coast. Drowned valleys provide many harbors and the drowned 
lower course of the Columbia River offers a route through the Coast Range.

- Olympic Mtns.
The Olympic Mountains consist of a mass of folded and metamorphosed rocks 
eroded into sharp, steep-sided ridges that stand 4000 to 8000 feet above sea 
level. The highest peaks bear perpetual snowbanks and several small 
glaciers. The mountains were severely glaciated during the ice age.

- Willamette - Puget Lowland
The Willamette and Cowlitz Lowlands are primarily stream valleys eroded to 
low elevations in belts of relatively nonresistant tilted or folded Tertiary 
rocks. Resistant rocks locally form hills and watergaps. Both valleys 
contain alluvial terraces. The Puget Lowlands, eroded by streams and 
Pleistocene glaciers, is a partially drowned system of valleys. Bordering 
Puget Sound are hummocky plains of till and fairly smooth sheets of 
glaciofluvial gravel.

- Cascade Mtns.
The Cascade Mountains of Oregon and the southern half of Washington are a 
broad upwarp composed of (1) a basal portion of early Tertiary tuffs, 
breccias , lavas, and mudflows, exposed in the Columbia River Gorge and 
other deep valleys; (2) a thick middle section of middle Tertiary basalts 
that form the deeply eroded Western Cascades; and (3) an upper section of 
late Tertiary and Quaternary andesites and basalts that form the less 
dissected High Cascades lava platform, which is generally 15 to 25 miles 
wide and 4000 to 6000 feet high along the crest of the range. Crowning the 
range are a number of well-known, snowcapped volcanic peaks in various 
stages of dissection - Mt. Rainier, Mt. St. Helens, Mt. Adams, Mt. Hood, Mt. 
Jefferson, Three Sisters, Mt. Loughlin, and others. Crater Lake occupies a 
caldera which resulted from the eruptive collapse of the summit of Mt. 
Mazama about 6,600 years ago. The northern half of the Cascade Range of 
Washington is a maturely dissected upland underlain by ancient sediments 
that have been folded, metamorphosed, and intruded by granites. The more or 
less accordant ridges rise to elevations of 6000 to 8000 feet. Above them 
rise several volcanic cones (Mt. Baker, Glacier Peak, others) The northern 
Cascades were extensively glaciated, and the mountains now harbor many small 
glaciers.

- Columbia Intermontane
- Columbia Basin
The Columbia Basin is an irregular structural and topographic basin 
underlain by middle Tertiary basalt flows that have been depressed below sea 
level in the Pasco area and upwarped on the flanks of the surrounding 
mountains. Fluvial, lacustrine, eolian, and glacial sediments overlie much 
of the basalt, and locally form terraces or other subordinate physiographic 
fearures. The portion in north central Oregon is partly a plateau incised by 
canyons and partly a low plain of sand and gravel. The portion in south 
central Washington comprises a series of anticlinal ridges (partly faulted) 
and synclinal valleys. The outstanding features include Horse Heaven Hills, 
Yakima Valley, Saddle Mountain (one of several), Kittitas Valley, and the 
Wenatchee Mountains - Frenchman Hills, Columbia and Yakima rivers cross 
several of these ridges in watergaps. Most of the remainder is a plateau in 
varying but generally youthful stages of dissection. Noteworthy are the 
Waterville Plateau, Quincy Basin (alleviated), Palouse Hills (loess 
covered), and Tristate Upland (on the southeast). The northern edge of the 
plateau was glaciated and the channeled scablands reflect the drainage ways 
of ice age floods. The Grand Coulee is the most spectacular of these 
channels.

- Central Mtns.
The Central Mountains comprise a complex group of folded and faulted uplifts 
including the Seven Devils, Wallowa, Elkhorn, Greenhorn, Aldrich, and Ochoco 
mountains. They rise 2000 to 5000 feet above their surroundings and reach 
elevations of 6000 to 10,000 feet. They include various rocks of differing 
resistance to erosion. Because of orographic rainfall, the mountains are 
well dissected. The higher portions, especially the Wallowa Mountains, were 
glaciated. Alluviated fault troughs occur within the mountains, as at La 
Grande, Oregon.

- Harney High Lava Plains
The Harney High Lava Plains are situated between the Central Mountains, the 
Basin and Range area, the Cascade Mountains, and the Malheur-Owyhee Upland. 
They are mainly a flattish youthful tract of late Cenozoic lavas, ranging in 
elevation generally from about 4000 to 5000 feet. The surface is lower near 
the Deschutes River canyon, the only major stream in the area. Volcanoes are 
abundant in the western portion. Chief among them is Newberry Volcano 
(Paulina Mountain), with its breached caldera. Hundreds of faults, mostly of 
small throw, are present; they become more pronounced southward toward the 
Basin and Range Province.

- The Malheur-Owyhee Upland
The Malheur-Owyhee Upland occupies parts of southeastern Oregon and 
southwestern Idaho. It is a partly dissected, warped plateau, mostly 4000 to 
8000 feet high and underlain mainly by Cenozoic lava flows, tuffs, and 
lakebeds. Most of the area is unmapped and little studied. The Owyhee River 
and its tributaries drain much of the area in deeply incised canyons.

- The Snake River Lava Plain
The Snake River Lava Plain is an arcuate downwarp 30 to 60 miles wide and 
about 400 miles long. It descends gently from an elevation of about 6000 
feet above sea level at its east end to about 2,200 feet on the west. The 
eastern part is a more or less silt-covered youthful lava plain, almost 
featureless except for low lava domes and occasional cinder cones. Very 
young lavas occur at Craters of the Moon, Hell's Half Acre, and elsewhere. 
The western part of the plain is underlain by lakebeds and alluvium as well 
as lava, and is partly dissected to terraces, box canyons, and open valleys.

- Rocky Mtns.
- Northern Rockies
The Northern Rocky Mountains section includes parts of northeastern 
Washington. Northern and central Idaho, and western Montana. It is 
characterized by high mountain ridges and deep intermontane valleys eroded 
from rocks of moderately complex structure. Where the rocks have been folded 
and faulted, the ridges are aligned as in the Whitefish, Mission, Selkirk, 
and San Poil ranges. Some valleys (e.g., Deer Lodge, Bitterroot, Flathead, 
and Purcell) are 10 to 20 miles wide and favor settlement and 
transportation. The mountains of central Idaho, developed by erosion of 
massive granite rocks, are irregular and resist exploration and settlement. 
Most of the province drains into the Columbia River and its tributaries, 
although the eastern part drains into the headwaters of the Missouri River 
system, and the extreme northeast corner drains toward Hudson Bay. Although 
much of this section is well dissected, as seen in the Soldier Mountains, 
Pleistocene glaciation has produced some of the North American continents 
most spectacular mountain scenery.

- Middle Rockies
A part of the Middle Rocky Mountains section extends into southeastern 
Idaho, where northerly to northwesterly trending mountain ranges and valleys 
have eroded from folded, thrust-faulted, or tilted rocks. The valleys are 
about 6000 feet above sea level, and the ridges reach 2000 to 4000 feet 
higher. Blockfaulting, characteristic of the Basin and Range Province, 
extends into this area also; therefore, the boundary is somewhat arbitrary. 
The northern part of the area lies in the Snake River drainage basin, 
whereas Bear River on the south, following a circuitous route, eventually 
drains into Great Salt Lake, as does Malad Valley. The summits of many of 
the ranges are ancient, beveled, erosional surfaces. More recent uplift has 
caused modern streams to dissect and often cut across these ranges, creating 
gorges and 'watergaps' that connect the valleys between the range.

- Basin and Range
The northern edge of the Great Basin section of the Basin and Range Province 
extends into south central Oregon and into southern Idaho. The part in Idaho 
consists of a series of tilted fault blocks and parallel stream valleys 
developed in a region of folded rocks. By contrast, the part in Oregon is a 
youthful high lava plain by fault block mountains and by fault thoughs. 
Representative of the high-standing blocks are Steens Mountain, Hart 
Mountain, Abert Rim, and Winter Ridge. Typical fault troughs are Alvord 
Basin, Warner Valley, and the basins of Abert, Summer, Goose, and Klamath 
lakes. The western part of this province is covered by the ash and pumice of 
the Mt. Mazama and Mt. Newberry eruptions, which greatly alter the 
appearance, drainage, and vegetation of the area. The presence of so many 
young faults attests to the recency of tectonic activity in the region, as 
do the numerous hot springs and geothermal areas.

Landform Regions Map

- Water
- Surface & Runoff Basins
Spokane
Upper Columbia
Yakima
Upper Snake
Central Snake
Lower Snake
Mid Columbia
Lower Columbia
Willamette
Coastal
Puget Sound
Oregon Closed Basin
northern most areas of Klamath and Bear basins
Drainage Basins and Sub-Basins Map
Major Surface Waters and Runoff Map
- Aquifers
Major Aquifers Map
- Withdrawals
Water Withdrawals Map
Electric Generating Facilities (favorable locations for watermills)

- Land Capability Classes
Class I = level grade with little erosion potential, deep soil depth with 
good structure, good drainage and moisture capacity, and no stones.

Class II = gentle grade with moderate erosion potential, moderate soil depth 
with unfavorable structure, correctable drainage with fair moisture 
capacity, and few stones.

Class III = moderate slope with high erosion potential, shallow soil depth 
with moderate salinity, moderately wet soils with low moisture capacity, and 
few stones.

Class IV = moderately steep slope with severe erosion potential, shallow 
soil depth with severe salinity, wet soils with low moisture capacity and 
few stones.

Class V = level grade with little erosion potential, variable soil depth 
with poor structure, no drainage, and areas with stones present.

Class VI = steep slope with severe erosion potential, shallow soil depth 
with salinity, poor drainage with low moisture capacity, and stones present.

Class VII = very steep slope with severe erosion potential, shallow soil 
depth with salts, low moisture capacity, and severe stones.

Class VIII = Unsuitable for cultivation, grazing, or forestry.

Land Capability Classes Regions Map

- Rock
- Sedimentary
- Quaternary
Recent & Pleistocene
- Upper Tertiary
Pliocene and Miocene including Recent & Pleistocene
- Lower Tertiary
Oligocene, Eocene, & Paleocene
- Cretaceous
In sections of Region M includes Jurassic & Triassic
Jurassic & Triassic
- Upper Paleozoic
Permian, Pennsylvania, & Mississipian - In sections of Region M includes 
Middle & Lower Paleozoic
- Middle Paleozoic
Devonian & Silurian
- Lower Paleozoic
Ordovician & Cambrian
Younger Precambrian
- Older Precambrian
Metamorphic & Igneous rocks
- Volcanic
- Quaternary & Tertiary
Includes small areas of Intrusive rocks
- Intrusive
- Lower Tertiary & Mesozoic
Chiefly granitic rocks
Dominant Rock Types Map

- Special
- Natural Wonders
Crater Lake
Craters of the Moon
Three Sisters
Fort Rock
Parks
Trails
Campgrounds

- Major Settlements
Aberdeen
Bellingham
Boise
Bremerton
Chehalis/Centralia
Coos Bay
Eugene
Idaho Falls
Klamath Falls
Lewiston
Longview
Medford
Mt. Vernon
Pasco
Pendleton
Pocatello
Port Angeles
Portland
Richland
Roseburg
Salem
Seattle
Spokane
Tacoma
Walla Walla
Wenatchee

- Technology
- General Building Practices
Monument
Public
Upper
Middle
Lower
Wonders of the World

- Environment
- Flora
- Vegetation Zones
- Forrest Province
- Sitka Spruce Zone
Confined to coastal hexes, this coniferous zone extends from Alaska to 
southwesternmost Oregon. Extensively altered by logging and fire, Sitka 
spruce (Picea sitchensis) characterizes the zone although in many places 
western hemlock (Tsuga heterophylla) and Douglas-fir Pseudotsuga menziesii) 
dominate. Red alder (Alnus rubra) often forms patches in disturbed areas and 
riparian situations, while western redcedar (Thuja plicata) characterizes 
swampy habitats. Besides stabilized dune communities in which shore pine 
(Pinus contorta) is a prominent successional species, there are salt marsh 
communities in estuaries and communities associated with shifting dunes. The 
Sitka Spruce Zone grades into the Western Hemlock Zone with which it bears 
close relationship.

- Western Hemlock Zone
Mantling both the Coast Range and the western slopes of the Cascades, this 
zone is one of the most extensive in the region, streching from British 
Columbia to California. Although named for the shade-tolerant western 
hemlock (Tsuga heterophylla) characterizing the persistent vegetation, the 
dominate tree is often the seral Douglas-fir (Pseudotsuga menziesii) in 
drier climes. In disturbed moist sites, red alder (Alnus rubra) and bigleaf 
maple (Acer macrophyllum) are common and as elevation increases Pacific 
silver fir (Abies amabilis) replaces western hemlock.

- Cascade Subalpine Forest Zone
A complex group of zones developing under heavy snow flanks the Cascades and 
Olympics and extends into British Columbia. This group includes the Pacific 
Silver Fir Zone marked by Abies amabilis At higher elevations, silver fir 
gives way to a more stunted forest of mountain hemlock (Tsuga mertensiana) 
and subalpine fir (Abies lasiocarpa) and forms a parklike pattern of open 
meadow and forest stringers. In areas of volcanic ash or areas recently 
disturbed by fire, even-aged stands of lodgepole pine (Pinus contorta var. 
murrayana) prevail. In southern Oregon, the zones bear close relationship to 
the California red fir forest.

- Grand Fir & Douglas-fir Zones
Mesic coniferous forests occur in interiour areas and exhibit a broad 
distribution. Often both grand fir (Abies grandis) and Douglas-fir 
(Pseudotsuga menziesii) occur in mixed stands, although Douglas-fir tends to 
be more prevalent in Idaho.Other trees of importance, in order of increesing 
moisture tolerance, are ponderosa pine (Pinus ponderosa), western larch 
(Larix occidentalis), and lodgepole pine (Pinus contorta var. murrayana); 
the later two species are fire-responsive pioneers. In northern Idaho, 
western redcedar (Thuja plicata) and western hemlock (Tsuga heterophylla) 
are prominent. Oregon boxwood (Tsuga heterophylla) and common snowberry 
(Symphoricarpos albus) dominate two prevalent understory communities.

- Ponderosa Pine Zone
In a broad belt below the Grand fir and Douglas-fir Zones is an open 
coniferous forest dominated by ponderosa pine (Pinus ponderosa). Understory 
vegetation varies from shrubby mats of bitterbrush (Purshia tridentata) and 
snowbrush (Ceanothus velutinus) in central Oregon to meadows of Idaho fescue 
(Festuca idahoensis) further to the east.

- Western Redcedar Zone
At moderate altitudes in moist locales in the northeastern portion of the 
region, this zone occurs between the more xeric Grand fir and Douglas-fir 
Zones and the spruce-fir type. Dominant trees include western redcedar 
(Thuja plicata), western hemlock (Tsuga heterophylla), and western white 
pine (Pinus monticola), but grand fir (Abies grandis) and western larch 
(Larix occidentalis) are found in drier sites. Understory unions in this 
zone are often similar to those of the Grand Fir and Douglas-fir Zones.

- Engelmann Spruce & Subalpine Fir Zones
Confined to higher elevations to the east, this type is the counterpart of 
the Cascade Subalpine Forest. Varying from dense to open, parklike stands of 
subalpine fir and Engelmann spruce, the zone has occasional intrusions of 
subalpine larch (Larix lyallii) and whitebark pine (Pinus albicaulis) at 
higher elevations and Douglas-fir (Pesudotsuga menziesii) at lower 
elevations.

- Mixed Needleleaf-Broadleaf Forest Zones
A highly complex set of zones closely related to plant communities in 
California, this evergreen forest straddles the Siskiyou Mountains in 
southwest Oregon. Edaphic, fire history, and climatic contrasts lead to 
sharp breaks in plant cover. Douglas-fir (Pseudotsuga menziesii) dominates 
the upper canopy, but various sclerophyllous trees and shrubs are found in 
the understory including tanoak (Lithocarpus densiflourus), canyon live oak 
(Quercus chrysolepis), Pacific madrone (Arbutus menziesii), and golden 
chinquapin (Castanopsis chrysophylla). Serpentine soil bears a distinctive 
flora and a sparse vegetation, and other dry rocky areas support a 
sclerophyllous broadleaf chaparral.

- Rogue-Umpqua Forest-Shrub Zones
Occupying valleys in the rainshadow of the Siskiyou Mountains is a 
vegetation mosaic exhibiting many xeric characteristics. Woodlands are 
dominated by Oregon white oak (Quercus garryana), with Califorina black oak 
(Q. kelloggii)  on mesic sites. Pacific madrone (Arbutus menziesii), 
ponderosa pine (Pinus ponderosa), sugar pine (Pinus lambertiana), and 
incense cedar (Calocedrus decurrens), distinguish this zone from from 
Willamette Valley forest. On shallow soils, south slopes, and recently 
burned areas, sclerophyllous shrub communities are found with narrow-leaved 
buckbrush (Ceanothus cuneatus) and white-leaved manzanita (Arctostaphylos 
viscida).

- Willamette Forest-Prairie Zones
Confined to bottomland and adjacent slopes of the Willamette Valley is a 
mosaic of forest, woodland, open savana, and prairie. Praire and oak savanna 
at the time of first settlement was maintained by aboriginal burning. 
Woodlands dominated by Oregon white oak (Quercus garryana) have since been 
invaded by Douglas-fir (Pseudotsuga menziesii) and grand fir (Abies 
grandis), with bigleaf maple (Acer macrophyllum) important on north-facing 
slopes. Grasslands maintained by grazing include many introduced species and 
occupy direr sites. Lacing this mosaic of forest and prairie are bands of 
riparian woodland in which Oregon ash (Fraxinus latifolia), black poplar 
(Populus trichocarpa), and willow (Saliz spp.) are prominet.

- Western Juniper Zone
This open woodland is the northern counterpart of the Pinyon-Juniper type of 
the Great Basin. Shrub-steppe dominated by big sagebrush (Artemisia 
tridentata) and Idaho fescue (Festuca idahoensis) typically comprises the 
understory of this zone. Throughout the arid regions of interior Oregon, 
juniper woodland characterizes rimrock habitat where local moisture supplies 
permit establishment of this xerophytic tree.

- Shrub-Steppe Province
- Steppe Zones
Grassland without shrubs mantles areas of north-central Oregon and the 
Palouse of south-eastern Washington and adjacent Idaho. Much of this 
grassland is converted to farming with settelment. Among the various 
communities within this grassland is the Agropyron-Festuca type 
characterized by bluebunch wheatgrass (Agropyron spicatum) and Idaho fescue 
(Festuca idahoenis). In moister situations, Sandberg's bluegrass (Poa 
sandbergii) and Idaho fescue are prominent together with many forbs and 
shrubby common snowberry (Symphoricarpos albus). The steppe type is 
intermediate between ponderosa pine forest and more xeric shrub-steppe, and 
the communities of the Steppe Zones form understory unions in these adjacent 
vegetation types.

- Big Sagebrush Zone
The most widespread vegetation zone in the Pacific Northwest extends from 
Canada to Nevada and from the Cascades to the Rockies. Dominated by big 
sagebrush, the zone intermingles with juniper woodland in central Oregon. 
The type supports nonintensive grazing. Plant communities have been 
identified based on understory grasses, shrub cover, soils, and slope. Two 
prominent communities are Artemisia tridentata/Festuca idahoensis and 
Artemisia tridentata/Agropyron spicatum associations, the former with 
greater moisture requirements. Low sagebrush (Artemisia arbuscula) 
frequently replaces big sagebrush in eastern Oregon on shallow stony soils. 
Other prominet shrubs include several species of sagebrush and rabbit brush 
(Chrysothamnus spp.). Commonly referred to as "high desert," the 
shrub-steppe in this zone consists of nondesert species and exhibits a 
shrub-grass structure which is distinct from true desert.

- Desert Shrub Zones
Occupying pockets within the Big Sagebrush Zone. Desert Shrub Zones are the 
most xeric of the region. Frequently the type occupies playas where saline 
conditions prevail, but the type also occupies the rainshadow of several 
mountian ranges in southeastern Oregon and southern Idaho. Important shrubs, 
most of which are halophytic, include shadscale (Atriplex confertifolia), 
salt sage (A. nuttalli), greasewood (Sarcobatus vermiculatus), and spring 
hopsage (Grayia spinosa). Grasses and forbs are occasionally found in this 
open vegetation.

- Alpine Province
Found near and above the tree line, these zones are narrowly represented in 
the Cascades and more extensively in the Rocky Mountains. Mainly comprised 
of herbaceous plants and low shrubs, these zones contain a few trees 
displaying krummholtz form and occupying protected habitats. Alpine heath 
communities of the subalpine park land extend into the alpine zones, and 
glaciers, permanent snow fields, and extensive areas of talus and rock over 
much of the area.

Ponderosa Pine Regions Map
Shore Pine/Lodgepole Pine Regions Map
Quaking Aspen Regions Map
Oregon White Oak Regions Map
Engelmann Spruce Regions Map
Western Juniper Regions Map
Western Hemlock Regions Map
Douglas-fir Regions Map

Fauna

- Climate
- General
Extremes, as well as moderation, are the hallmarks of the climates of the 
Pacific Northwest. These extremes are induced by mountains which shield an 
elevated interior from moderating, moistening winds from the Pacific Ocean. 
Sharp climatic gradients are also induced by these ranges. It is the 
Cascades which create the major precipitation divide in the Pacific 
Northwest. To the west of the Cascades, with several topographically created 
exceptions, annual precipitation is always over 15 inches per year, while 
ares to the east, again excepting mountain zones, recieve less than 15 
inches of precipitation durring most years. Frequent fogs occur west of the 
Cascades with maxima along the coast, while to the east of the Cascades fogs 
are much less common. These climatic conditions control the varied character 
of agriculture and natural vegetation across the region. However, seasional 
variations in atmospheric flow create marked reorganizations of climates 
across the Pacific Northwest.

Freeze-Free Period Map

Days With Precipitation Map

Annual Precipitation Map

Frequency of Dry Years Map

Days With Dense Fog Map

- Winter
Winter Precipitation Map
Snowfall Map
January Sunshine Map
January Maximum Temperature Map
January Minimum Temperature Map
Extreme Minimum Temperature Map
- Spring
Spring Precipitation Map
Latest Date With Snow Map
April Sunshine Map
April Maximum Temperature Map
April Minimum Temperature Map
Last Killing Frost of Spring Map
- Summer
Summer Precipitation Map
Summer Frequency of Stagnation Map
July Sunshine Map
July Maximum Temperature Map
July Minimum Temperature Map
Extreme Maximum Temperature
- Autumn
Autumn Precipitation Map
Autumn Frequency of Stagnation Map
October Sunshine Map
October Maximum Temperature Map
October Minimum Temperature Map
First Killing Frost In Fall Map
- Seasonal Windflow Maps
Winter
Spring
Summer
Autumn

- Population
- Production
- Primary
- Agriculture
Wheat
- Barley
Grain
- Field Corn
Sweet Corn
- Oats
Grain
Hay
Alfalfa & mixtures
Field & Seed Peas
- Sugar Beats
Sugar
Irish Potatoes
Snap Beans
Apples
Pears
Peaches
Cherries
Grapes
Other
Irrigated and Non-Irrigated Farmland Map
Land In Farms By Percent of County Map

- Nature Reserves
Hunting
Established Natural Areas (105) Map

- Forest Industries
Generalized Commercial Forest Regions Map
Timber Harvest By County Map
Timber Mill Locations Map

- Mining
Average Value of Mineral Production By County Map
Industrial Minerals Map
Coal, Petroleum, and Geothermal Map
Ferrous Metals Map
Lead, Copper, Silver, and Gold Map
Gemstones and Semiprecious Stones Map
Lapidary Material Sites Map

- Fishing
Fish and Shellfish Landings Map (tons per year)

- Ranching
Cattle
Pigs
Sheep
Dairy Cows
Chickens
Goats
Other

- Secondary
Transportation Equipment
Lumber & Wood
Furniture & Fixtures
Food
Primary Metals
Fabricated Metals
Apparel
Chemicals & Potions
Stone, Clay & Glass
Instruments
Magic / (Electronics)
Other
Total Manufacturing Employment By County Map

- Tertiary
Wholesale
Retail
Professional
Personal
Basic Trading Areas and Business Centers Map

- Upper Class = 2500+ cl of best faire available per day.
- Physiological needs
Food
Shelter
Clothing
- Security needs
Home
Safety
Employment
- Social needs
Family
Community
Esteem
- Middle Class = >2500 cl choice of remaining faire per day.
- Physiological needs
Food
Shelter
Clothing
- Security needs
Home
Safety
Employment
- Social needs
Family
Community
Esteem
- Lower Class = 1500 cl off season min to 5000+ cl @ harvest / etc. (if 
available) faire per day.
- Physiological needs
Food
Shelter
Clothing
- Security needs
Home
Safety
Employment
- Social needs
Family
Community
Esteem
Population Pyramid
Population Density By County Map

- Power Structures
Military Chain of Command
- Political Structure
Counties
Royal Townships
Diplomacy
Legal Structure
Religious Hierarchy
Social Socieites
Guilds

- Timeline
History
- Events
Planed
Natural

- The Cottage
- Location
~Lat/Lon: 44.80N / 122.30W
+ Henline Topographic Map
- Views
+ Henline Mountain seen from Elkhorn Lake
+ Henline Mountain Summit seen from lookout point
- Floor Plan
The Conjurers' Crooked Cottage Map
- Room Descriptions
1
- Inventory
Furnature
Decor
Other
2
- Inventory
Furnature
Decor
Other
3
- Inventory
Furnature
Decor
Other
4
- Inventory
Furnature
Decor
Other
5
- Inventory
Furnature
Decor
Other
6
- Inventory
Furnature
Decor
Other
7
- Inventory
Furnature
Decor
Other
8
- Inventory
Furnature
Decor
Other

- Resources
- Discharge of Selected Rivers
Columbia At Mouth = 180 million acre-feet
Columbia At The Dalles = 134 million acre-feet
Snake At Mouth = 37 million acre-feet
Willamette At Mouth = 24 million acre-feet
Skagit At Mouth = 12 million acre-feet
Rogue At Mouth = 8 million acre-feet
Total Arable Land
Total Pasture
Total Timber Land
- Fish Population Trends
Freshwater Fish
Ocean Fish
- Game Animal Population Trends
Large Game Animals
Small Game Animals
- Mineral Reserves
Cement
Clay
Copper
Gem Stones
Gold
Lead
Lime
Peat
Pumice
Sand and Gravel
Silver
Stone
Zinc
Other 
=====
Post to the entire list by writing to tft@brainiac.com.
Unsubscribe by mailing to majordomo@brainiac.com with the message body
"unsubscribe tft"