Temperate Forests


Victoria's forest Environment

Outcome 1: students should be able to describe the geographic characteristics of Victorian forest environments and the natural processes that develop them.
Outcome 2: students should be able to analyse and explain the changes in Victorian forest environments due to natural processes and human activity.

Topic Plan (12 lessons = 4 weeks)

  • Lesson 1: Introduction
  • Lesson 2: The natural systems of forests
  • Lesson 3: Geographic characteristics of Victorian forest environments
  • Lesson 4: Dynamics in Victorian forests
  • Lesson 5-6: Characteristics of Victorian forests
  • Lesson 7: Changes to Victorian forest environments
  • Lesson 8: Future of Victorian forest environments
  • Fieldwork: (4 Lessons) Case study: River Red Gum forests of the Murray River

Assessment:
Classwork tasks (HW tasks on SIMON)
Fieldwork participation, data recording, application of theory, explanation.


Lesson 1: Introduction:

  • New Keynote
  • Copy Outcome 1 & 2 (discuss)
  • Identify Issues (concept map)
  • Notes based on text: biological diversity, definition of a forest, spatial change over time in the distribution of the world's forests, % of victoria covered by forest, definition of a plantation.
  • Copy Fig 4.1 (Simon resources)
  • Activities.


Lesson 2: The natural systems of forests

  • Copy Fig 4.5 (Simon resources)
  • What are the three major cycles and why are they critical to life on Earth?
  • Carbon cycle:
    • Copy Fig 4.6 (Simon resources).
    • Identify 4 ways that carbon can be changed in the carbon cycle and what can happen to it next.
    • What role do bushfires and the burning of fossil fuels play in the carbon cycle?
  • Nitrogen cycle:
    • Copy fig 4.7 (Simon resources)
    • What % of the atmosphere is composed of Nitrogen?
    • What are three ways that Nitrogen from the atmosphere can be converted to a form that can be used by plants?

  • Water cycle:
    • Copy fig 4.8 (Simon resources)
    • Describe 3 ways that water is important to the biosphere.
    • Explain why stable forests are important in the catchments of major cities like Melbourne.
  • Activities.



Lesson 3: Geographic characteristics of Victorian forest environments. p60-63


Task: How Geographic Characteristics of an area affect forest type.
  • Draw a table with 3 columns and 8 rows.
  • In column 1, identify what factors influence the structure of a forest and where it is located.
  • In column 2, describe how some trees adapt to these factors.
  • In column 3, explain how two or more factors can combine to form uniquely challenging environments for trees.

Task: Interpreting graphical and spatial information (maps).
Copy Fig 4:11 (Climate effect on forest type) and
Copy Fig 4:12 (Victorian climate zones based on temperature and humidity) into your notes.

In 50 words explain the relationships shown in each.



Natural Systems - Forest Distribution



world-map-ecoregions.png



Read p 56
  1. What is the definition of a forest? Compare your definition with the rest of the class. Improve your definition.
  2. Look at the diagram at the top of page 56. Notice that types of forest occur in bands when you look on a global scale.
  3. These bands are called degrees of latitude. Using an atlas, or resources on the internet calculate the degrees of latitude that each type of forest occurs between.
  4. Why do forests occur in bands of latitude?

Tropical Rainforest (moist tropical)

occurs on or near the equator.
Tropical Rainforest is moist all year round. Rain falls throughout the year.
There is no rainy season along the equator because days are the same length all year through.


rainforest.jpeg
Australian Rainforest
rainforeststructure.jpeg
Rainforest Structure
australian_rainforest.jpeg
Buttressed Roots on rainforest trees



The equator runs through the following countries:
· Africa: _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _
· South America: _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _
· Asia: _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _

Further away from the equator… grow
Tropical Dry Forests,
they have a rainy season. The rainy season in Australia is in the southern summer.
In Darwin the rainy season is from _ _ _ _ _ _ _ till _ _ _ _ _ _ _. This is also when the cyclones arrive.
The strongest cyclone ever to hit Australia was _ _ _ _ _ _ _ _ _ in _ _ _ _ _ _ _ _ at _ _ _ _ _ _.



drytropicalaustralia.jpeg
Termite mounds Australia
drytropicalforestindia.jpeg
India
boabforest.jpeg
Boab Forest in Africa


Further away from the equator again the
Temperate Broadleaf forests
begin… Temperate broadleaf forests occur where there are 4 distinct seasons.


tempbroadleaf.jpeg
Europe & N. America
riverredgum.jpeg
River Red Gum Australia
mountainash.jpeg
Mountain Ash Australia
snowgum.jpeg
Snowgum Australia


Australian__ Broadleaf Forest include these species…
  • _ _ _ _ _ _ _ _
  • _ _ _ _ _ _ _ _
  • _ _ _ _ _ _ _ _
  • _ _ _ _ _ _ _ _


African Broadleaf Forest include these species…
  • _ _ _ _ _ _ _ _
  • _ _ _ _ _ _ _ _
  • _ _ _ _ _ _ _ _
  • _ _ _ _ _ _ _ _


South American Broadleaf Forest include these species…
  • _ _ _ _ _ _ _ _
  • _ _ _ _ _ _ _ _
  • _ _ _ _ _ _ _ _
  • _ _ _ _ _ _ _ _


European and American Broadleaf Forest include these species…
  • _ _ _ _ _ _ _ _
  • _ _ _ _ _ _ _ _
  • _ _ _ _ _ _ _ _
  • _ _ _ _ _ _ _ _




As you get nearer to the planet’s poles leafy forests are replaced by
Needle-leaf forests
(Trees that grow in Needle-leaf forests are called C_ ).
These are called the forests are known as the BOREAL forests.
They grow where leafy trees cannot grow because of the extremely low temperatures and short growing seasons.


borealforest.jpeg
borealforest2.jpeg
borealforest3.jpeg
Aurora Borealis


Find out why Auroras occur.



Where no trees can grow in the far North the land is called
Tundra.
Permafrost refers to soil that is permanently frozen.
In the Tundra the permafrost is only 8 cm under the surface of the ground – even in summer.


tundra1.jpeg

tundraalaska.jpeg
Alaskan Tundra
tundragrassland.jpeg
Tundra grassland
permafrost.jpeg
Permafrost




Natural Systems - Forest Structure
Forests have a distinct structure. They have a canopy (overstory), and understory, and ground-cover.
The over-story is usually made up of the crowns of trees, but can also include vines that have climbed up towards the light, as well as epiphytic ferns and orchids. The density of the over-story depends on climate and the amount of nutrients and moisture available in the soil.

rainforeststructure.jpeg

Using a graphics program make a copy the diagram of the layers of a wet schlerophyll and dry schlerophyll forest (as above)
Include labels in your diagram.

In a labelled diagram show the structure of...
  • rainforest
  • temperate forest
  • open forest
  • taiga
  • grasslands
  • tundra

Include relevant and limiting factors (such as rainfall, soil depth and type, permafrost, height, percentage cover).


Submit your work to your teacher for grading (accuracy, detail, completeness)



Natural Systems - Variation in Forest Type within Climatic Zones


Forests can look significantly different within the same climatic (latitude based) zones, depending on variations in climate factors based on landform, prevailing winds and land-use.

Australia
Temperate Broadleaf Forests and Rainfall.

1. Define and find a dominant species of tree and a large animal species from a…
  • Wet Sclerophyll forest – fire?
  • Dry Sclerophyll forest –

2. Find a picture for each kind of tree. Find out the conditions it grows in, the characteristics of its wood and what it is used for.

3. Using the diagram you made earlier, identify the structural and environmental differences between wet schlerophyll and dry schlerophyll forests.
  • In terms of the height of their canopy / overstory…
  • In terms of the space between trees in the forest…
  • In terms of their understory…

4. Find the current distribution of wet schlerophyll and dry schlerophyll forests in Australia.


5. What are the geographic factors which limit their distribution?

Submit your work to your teacher for grading (accuracy, detail, completeness)



  • What did you know
  • What do you know now
  • What would you like to know?

Why is it important?






Wikipedia: Bushfires
CSIRO: Bushfires Overview - Towards an understanding


Forest Dynamics

University of Michigan Teacher Resource Site

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MICHIGAN FORESTS FOREVER TEACHERS GUIDE

FOREST ECOLOGY BASICS
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1TreeSign.jpg (14729 bytes)

A forest is a collection of biological organisms and non-biological factors. From an ecological perspective, the definition of a forest includes all these things, from the trees to the bacteria, and the soil type to the microclimates. See the "Tree Basics" page for more about the definition of a forest. Forest management systems are rooted in forest ecology (pun intended!).
There are three groups of concepts with forest ecology, or the ecology of just about any natural system. Each of the three groups of concepts interact with each other to variable degrees, at variable times, and in variable ways.

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ArrowCircle.jpg (4021 bytes)


Ideas on this page:

Diversity
Populations
Communities
Forest Layering
Crown Cover
Edge Effect
Fragmentation
Parcelization
Snags
Microenvironment
Visual Quality
Aesthetics
Food Chains
Nutrient Cycles
Organic Matter
Trophic Levels
Weathering
Hydrologic Cycle
Temperature
Humidity
Succession
Disturbance


Composition
Composition has to do with species, taxonomy, and biological diversity. The number of species and how they relate to each other according to taxonomic classes is a reasonably straight-forward concept. Biological diversity, on the other hand, is a bit more slippery to wrap our minds around. At first, diversity sounds like a simple species count and relative abundance of each species. This is certainly a component of the diversity question. It's also the easiest to identify and study. However, the diversity of species is only one level of several.

Species: the main category of taxonomic classification into which genera are subdivided, comprising a group of similar interbreeding individuals sharing a common morphology, physiology, and reproductive process. Note 1, there is generally a sterility barrier between species, or at least reduced fertility in interspecific hybrids. Note 2, the species is the basic unit of taxonomy on which the binomial system has been established; the lower taxonomic hierarchy is species, subspecies, variety, and forma.

At the most fundamental level of diversity, there is genetic diversity. How many genes and pieces of genetic information are present in a forest? The chlorophyll gene, for example, is common throughout most of the plant kingdom (although there are several variants). Many other attributes or genetic characteristics are also quite common in a forest system. Vertebrates have far more genetic commonality than genetic difference. The loss of a species may not represent a loss of genetic diversity, only the loss of particular combination of genetic material. The raw material will probably remain in the biota. If you remove the word "the" from the English language, it would make our speech awkward, but it would not eliminate all words with the letters "t", "h", and "e".
Species diversity is the next level of diversity. These are the combinations of genes that we are most accustomed to dealing with in the life sciences and from legal perspectives (e.g. endangered species laws). Yet, the definition of the word species escapes a single, concise, universally-accepted agreement. Species abundance addresses the issue of how common a particular species is, often in the context of particular region or ecosystem. There might be 100 species in a suite of characters. However, 90% of the biomass might consist of only 3 species. There may be a few species that are very uncommon, or have low abundance. It is usually the species with low abundance that we are concerned about from the perspective of potential species loss. It is usually the abundant species that we derive the most of economic base from. See the tree species diversity page for more information about Michigan forests.
A collection of individuals of a given species make up a population. The size, frequency, and distributions of populations are important elements of diversity. A Canada lynx might be listed as endangered in Michigan, but across its range it is a common animal. Sometimes populations on the edge of species range will display unique set of genes. Northern populations of animals tend to have larger size and shorter appendages. Flowering times of a tree species varies with climate conditions. The conservation of distinct populations may be important in some cases.
With a given ecosystem, populations interact with other. There are identifiable associations of species. These species associations are called communities. Community diversity is more difficult to measure in the landscape because there are usually a large number of components. To make identification possible, key species are used to describe a community, such as "northern hardwoods", which is defined by such tree species as sugar maple, beech, and basswood. However, northern hardwood associations in the western Upper Peninsula lose the beech component. Community descriptions have an inherent degree of variability across a large geographical region. This is another element of "diversity".
Lastly, there is something called "ecosystem diversity". A collection of communities and the association physical factors make up an ecosystem. Ecosystem diversity is commonly described in terms of biomes, eco-regions, and similar large-scale terms. However, ecosystems can also be quite small. The various communities within a rotting log are distinct from the surrounding forest. That rotting log, or all the rotting logs in a forest, can be considered an ecosystem.
While the above levels of diversity suggest a strong hierarchy, the classifications are less distinct in the natural world. A considerable amount of flexibility and "confusion" exists. Diversity is complex set of concepts, despite our understandable tendency to reduce it to a species level.

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PLT Charting Diversity
PLT The Fallen Log

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Structure
The structure, or "architectural" arrangement of a stand and forested region is important. Structure impacts wildlife habitat in a major way. It also influences light, water, and nutrients levels. These things, in turn, impact the trees and other vegetation. Structural components of a forest, or lack of a particular component, are not inherently "good" or "bad", or "natural" or "unnatural". Structure is an ecological feature of a forest that can be measured, and subsequently evaluated against a set of criteria. Seven elements of structure are discussed.
  • Vertical & Horizontal Arrangement
  • Heterogeneity and Forest Density
  • Edge Effects
  • Islands and Fragmentation
  • Dead Trees and Snags
  • Micro-Environments
  • Appearance
Vertical & Horizontal Arrangement

Vertical.jpg (67831 bytes)
Vertical.jpg (67831 bytes)


This is the physical arrangement of a forest; the different tree heights, "layers" of forest, and the continuity of branches from tree to tree. A forest with more structure generally has more habitat characteristics. A continuous forest offers transport routes for arboreal animals (animals that live in trees). "Crown cover" is the percent of the ground that has tree crown growing over it. A forest will have variable percentages of "holes" in the canopy. These "holes", or the amount of crown cover or crown closure, have important ecological ramifications.
Classical tropical humid rain forests probably have the most structure of any forest on Earth. Our north temperate forests are different. Not all forest types have a full complement of layering (understory, shrub, mid-size trees, main canopy trees, really tall trees). Jack pine stands, for instance, generally lack much vertical structure, especially with the kinds of soils they typically grow on. Northern hardwoods, if managed accordingly, will have a well-developed structure. Left unmanaged, they tend to lose structure close to the ground.
Heterogeneity and Forest Density
The level of "heterogeneity" refers to how similar or different the parts of a forest are to each other. Diversity is a big part of this, but so is structure and other forest descriptors. Heterogeneity might be evaluated within a single stand of trees, or be assessed across a large landscape, such as a national forest or the eastern Upper Peninsula.
"Density" has to do with how many trees are in an area and how large the trees are. A thousand trees per acre may, or may not, be a lot of trees depending upon their size. A thousand seedlings are generally more than recommended, but the density is still low. 250 large, saw-timber sized trees per acres would likely be a high density forest. Density is typically measured in units of square feet and is called "basal area" (link to the Forest Descriptor page in the Tree Basics section).
Edge Effects

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Edge.jpg (13827 bytes)

The design of a timber harvest can have significant on habitat quality. Within a given area, more or less "edge" can be created according to the management objectives of the forest stand.

"Edge" refers to the transition zone between two different vegetation types. Some "edge zones" are sharp or narrow, such as the transition between a lake and the shoreline vegetation. Other transitions are more gradual, such as the change in forest composition up a slope in the Keweenaw Peninsula. These edge zones usually have representative species from both vegetation types, so they tend to be more diverse than either of the constituent types. Edge zones may also have species not found in either constituent type. In terms of broad-brush diversity, forest edge is a good thing, especially if higher numbers of species were the only measure.
The downside of forest edge is the affect on species that prefer or require "deep woods" conditions. The introduction of edge to a "deep woods" type forest will stress those species that don't benefit from edge effects. The ovenbird is often cited as an example of an animal that can only be found in undisturbed, mature forests. This conclusion is arguable, as ovenbirds can often be heard in other forest types. What the ovenbird really needs is protection from ground predators, as they build their nests on the ground. Deep, dark forests tend to have fewer species and do not support high numbers of large predators.
Islands and Fragmentation

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Fragment.jpg (42967 bytes)

Forest fragmentation is the land use change from forest cover to a non-forest cover. This is represented in the above image starting from the upper left and moving clockwise.

The process of changing a large forested area into an area of forest patches is called "fragmentation". These forest patches are referred to as "islands." The fragmentation of forest has important ecological impacts. These impacts are not necessarily "good" or "bad" but they are definable, at least in part.
Forest fragmentation should not be confused with forest "parcelization". Parcelization is an ownership phenomenon that often, but not always, translates into forest fragmentation. Parcelization has direct economic impacts, as well as potentially direct ecological impacts.
Mathematical theories relating biological diversity and fragmentation were promulgated by a man named E.O. Wilson. These theories were developed to explain ecological trends and patterns found among the islands of the South Pacific. The theory is called "island biogeography". Both the original theory and its subsequent application to continental situations remain highly controversial.
Dead Trees and Snags
Dead trees, both on the ground and standing, provide habitat elements for many species, particularly cavity nesters. Dead wood also provided habitat for a number of insects which, in turn, are important parts of some food chains. A standing dead tree is called a "snag". Large snags and fallen trees have more value than small ones.
"Snag management" means producing more snags in a forest where snags are uncommon. From a strict timber perspective, snags are trees that could have been merchantable had timber been the only management goal and management implementation was perfect. As a legacy of our forest history, many of our forests remain in younger, more vigorous age classes. Snags become increasingly common as forests grow older. Forests of short-lived species already display an abundance of snags. The presence of snags in longer-lived forests can sometimes be accelerated through management. Snags in short-lived forests are usually retained during timber harvest.
Micro-Environments
Small areas within a forest environment that have markedly different characteristics are called "micro-environments". Examples might be rock outcrops, large rotting logs, pit-mound topography (tree tip-ups), springs and seeps, vernal (spring-time) ponds, or other features. These micro-environments sometimes harbor special sets of species, occasionally endangered or threatened species. Seeds of some tree species may depend on micro-climates / micro-environments to enhance their reproduction success. Manipulation of the forest canopy through management practices alters micro-environmental conditions such as light, temperature, and humidity.
Appearance
The "appearance" of a forest is not really an ecological factor, but it has great influence on how forests are managed or not managed. Forest management or lack of management can have significant ecological impact. The appearance of a forest strongly influences public opinion and public policy of the "goodness" or "badness" of a particular forest practice. An entire of compendium of "pseudo-science" has been developed to support what is essentially an argument against forest practices resulting in poor appearance. Generally, balanced ecological and biological information is not considered. This phenomenon is not unique to natural resources, of course.
"Visual quality" is the term often used as an objective in forest management. "Aesthetics" is a misnomer that is also quite common. An aesthetic involves the appreciation of something. Appreciation has deeper meaning than mere visual appearance. A well-done and properly applied clearcut can have high aesthetic value, but rather low visual quality.
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Function
The "function" part of an ecosystem involves "how" things happen. It's equivalent to "economics" in our human society, or the themes of geography that involve the movement of goods and interactions between humans and the environment. How ecosystem functions are played-out can be highly complex, but the functions themselves are fairly easy concepts to understand. These areas of forest ecology are probably the least understood, but the most resilient.
Energy Capture & Trophics
Nearly all life on Earth is solar-driven. Plants capture solar energy and store it as chemical energy (photosynthesis). Animals eat plants to obtain this stored energy, among other things. Some animals eat other animals, for the same reasons. These threads of energy transfer are called "food chains". Energy can be likened to the currency that measures an ecosystem economy. Life bucks the laws of entropy. In this sense . . . life is not "natural", but eventually all the energy is dispersed.

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Trophics.jpg (70546 bytes)


The "rule of 10 percent" says that only 10 percent of the energy in each transfer is actually captured. So, plants only capture about 10 percent of the solar energy available to them. Herbivores capture only 10 percent of the energy stored in plants. And, the same is true "on down the line" of the food chain. Energy transfers occur between "trophic levels".
Mineral & Nutrient Cycling
In addition to energy, a host of minerals and nutrients cycle through the biota. Understanding these cycles involves chemistry, biology, and physical geography. The most common elements are carbon, hydrogen, oxygen, phosphorus, potassium, nitrogen, sulfur, calcium, iron, and magnesium. A jingle to help remember these nine elements is "CHOPKNS CaFe Mg" or "see Hopkins Cafe, might good". There are another couple dozen or so elements needed, too.
How minerals and nutrients cycle through the biota varies considerably. Decomposers, soil type, water, and climate are determining factors. Cycles tend to be "open" in temperate zones, meaning nutrients are commonly lost to a system or a food web. A significant portion of available nutrients are found in "organic matter", or the layer of dead material on top of the soil surface. Tropical humid systems tend to be "closed" with very few nutrients slipping out of the system. Soils in these regions have very little organic matter.
The availability of a nutrient differs from the amount of a nutrient in the environment. For example, just because there is a lot of nitrogen in the atmosphere and the soil, doesn't mean it is in the form a plant can absorb. Nutrient availability varies with soil type, pH, and other factors. For more information about mineral & nutrient cycling, try the "cycles" page.
Weathering
New minerals and nutrients are added to an ecosystem as rocks and soils are chemically broken down by weather and biological factors. "Parent material" is the rock or mineral source(s) from which soils are derived. The productivity of a particular soil is highly dependent upon the parent material in the area. Parent material rich in key elements will produce soils that support higher levels of biomass. Weathering is the prime source of "new" minerals and nutrients in an ecosystem.
Water Movement

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WaterCycle.jpg (71046 bytes)

Image courtesy of the Michigan State University

Institute of Water Research/Center for Remote Sensing

The "hydrologic cycle" is commonly taught throughout Michigan at the upper elementary and middle school level. The amount of water on the Earth is a fairly finite quantity. Where it occurs and how it cycles has a tremendous impact on the biota in an area.
Essentially, water cycles through the atmosphere, living matter, and the soil. Movement can be "stalled" by a number of features, such as lakes, underground aquifers, glaciers, etc. As water moves downward through soils, it usually takes soluble nutrients with it. Water movement is the main reason for the "loss" of nutrients in an ecosystem.
Like nutrients, water availability to plants also varies. Coarse soils, those with relatively large particle size and pore size, tend to hold less water. They are drought-prone and most tree species don't grow well on these soil types. Finer soils, such as silts and clays, have very fine particles and hold more water. However, during dry periods, they may just as droughty as coarse (or sandy) soils because the drier these soils become, the tighter that water molecules "cling" to the soil particles. This cohesive property may be stronger than a root system's ability to pull the water molecules out of the soil.
For more information about the hydrologic cycle, try the "cycles" page.
Temperature & Humidity
Temperature and humidity play important roles in the transfer of materials throughout an ecosystem. They also have strong influences on "who grows where" and affect metabolic processes of both plants and animals.
Photosynthetic rates correlate to temperature. Higher temperatures increase rates, to a certain point, after which a plant can "burn out". Very arid environments cause plants to close their pores in order to conserve water. Less water inside the plants can slow photosynthesis to a crawl. Desert plants have special adaptations for dry conditions. So do many plants in our northern bogs and sandy outwash plains. And the temperature-humidity condition immediately above a forest canopy on a hot summer day can be every bit as hostile as that in a desert.
Successful germination of tree seeds and early seedling survival are quite sensitive to temperature and humidity conditions on the forest floor. For example, sugar maple seeds germinate in the spring, soon after snow melt, when the temperature is 34 degrees (F). If an early spring heat wave hits, germination for that year will be poor. On the other hand, yellow birch, a common associate of sugar maple, germinates best around 74 degrees. That's part of the reason why an unmanaged northern hardwood stand will often migrate towards a sugar maple monotype and a managed northern hardwood stand will encourage the regeneration of other northern hardwood tree species.
Succession and Disturbance

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Succession.jpg (85243 bytes)


As the living (biotic) and non-living (abiotic) components of an ecosystem react with each other over time, the composition, structure, and function of a forest will change. This process of change is called "succession" which is more fully explained on the succession web page. The classic concept of succession is the orderly and reasonably predictable path of vegetational change over time, from bare soil to mature forest. The early vegetation types (seres) are labeling as"pioneer" types. The final sere, if there is one, is called the "climax" type.
The progress of succession can be interrupted and set back by disturbances, usually the result of fire, wind, flood, or insect/disease epidemic, and nowadays by forest management. Disturbance might be on a grandiose scale, such a large wildfire, or a small scale, such as single large tree blown over in windstorm or killed by a lightning strike. Depending upon the severity of the disturbance, an earlier vegetational stage (or sere) will result, and succession will restart from that point.
Forest management is closely integrated with an understanding of forest successional pathways. Succession can be accelerated or slowed, depending upon the desired objectives for a particular stand and the natural capabilities of the site. Successional pathways vary according to many factors.

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PLT Nothing Succeeds Like Succession

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This website was developed and created by Michigan State University Extension for the teachers of the State of Michigan. The website is maintained by the Delta-Schoolcraft Independent School District in support of the Michigan Forests Forever CD-ROM from the Michigan Forest Resource Alliance.


Page Name: Environment/EcologyForest.htm

Please provide comments to Bill Cook: cookwi@msu.edu or 786-1575
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