Bill Plotkin - Nature and Soul

“A genuine elder possesses a good deal of wildness, perhaps more than any adult, adolescent or child. Our human wildness is our spontaneity, our untamed vitality, our innocent presence, our resistance to oppression, and our rule-transcending vivacity and self-reliance that social convention can never contain. We are designed to grow deeper into that wildness as we mature, not to recede from it. When we live soulcentrically, immersed in a lifelong dance with the mysteries of nature and psyche, our wildness flourishes. A wild elderhood is not a cantankerous old age or a devil-may-care attitude, nor is it stubbornness or dreamy detachment. Rather, the wildness of elderhood is a spunky exuberance in unmediated, ecstatic communion with the great mysteries of life—the birds, fishes, tress, mammals, the stars and galaxies, and the dream of the Earth” ~Bill Plotkin

Monday, November 20, 2017

The Wildlife Story

Backyard feeding station with pups looking for dropped seed.

Lots of birds at my feeder this morning. Black-capped Chickadees, Blue Jays, Gray Jay, Northern Cardinal, Dark-eyed Juncos, Red-breasted Nuthatch, Mourning Dove and Hairy/Downy Woodpecker all converging on my little feeding station looking for sustenance. Of course the Juncos, ground feeders, had to compete with my dogs who love to eat the seed that has fallen from the feeders, but once my pups were back inside the Juncos had free reign once again. These are some of the birds found in my yard but there are clearly additional birds found within my ecoregion yet to be discovered.

In addition to birds, we also have wolves, bears, bobcats, fox, rabbits, skunk, deer and coyote in my ecoregion. Not to mention all of the fish, amphibians & reptiles, insects, etc… Listing all of these would be too time consuming so I am going to give some Michigan specific guide books which may be helpful:







Of course none of these animals would be here without the habitat plants provide. Based on research acquired through the book “A Field Guide to the Natural Communities of Michigan,” I believe according to the best of my ability that I live in what would be called Dry Northern Forest. A dry northern forest is found on a sandy glacial outwash plain and is made up of pine and hardwood trees. Some of the trees found in this community are red maple, paper birch, big toothed and trembling aspen, white pine and northern pin oak.

Obviously I am a long way from having knowledge regarding the plants and animals residing within my ecoregion. I am going to pick up some of the guidebooks listed here and start making discoveries about the natural beings I share space with, but what I find most interesting as I begin this research is how everything is tied together, interrelated and depending on one another.

References:


Sunday, November 19, 2017

The Indigenous People's Story




Rowing the dingy across the harbor to land, my two younger cousins in tow, I am excited to explore uninhabited Garden Island, one of many islands found in the Beaver Island archipelago off the coast of Michigan. It is July of ’74 and I am just barely 14 years old, sailing the waters of northern Michigan with my aunt and uncle. As I come ashore and disembark with my cousins, we soon find ourselves in thick woodlands, traversing overgrown footpaths. It is dim and dark under the cover of forest and I have decided of all things, to seek out the Native American cemetery, clearly identified on the map of the island my uncle had lent me. Maybe today I would have hesitated before making such a decision, understanding that cemeteries carry with them the energy and spirit of those who have passed. Wanting to make sure that it was respectful to visit such a place. But on this day, full of curiosity, I walk boldly into the clearing that holds the cemetery. Immediately I know I am in a special space as I can feel energy of the place hit me head on. Before me are about 20 spirit houses, little lodges built up off the ground, imbibing me with an ethereal feeling I have not been able to forget all these years later.

Over the years I have done a bit of research on the cemetery and discovered it was an Anishinaabe burial ground, more than likely from the Ottawa tribe. Upon talking to a member of the Ottawa tribe just recently, he confirmed to me that the Ottawa lived on Garden Island for many years. The tribes of the Great Lakes, the Ojibway, Algonquin, Ottawa, Potawatomi, Saulteaux, Nipissing and Mississauga, as well as some Oji-Cree and Metis communities, are known as the Anishinaabe. These tribes share cultural traditions and kinship ties but have their own identities and independent leadership. The Ottawa tribe, also known as the Odawa, have made their home in this part of Michigan since before the Europeans arrived. They had summer quarters in the northern part of the state and then traveled to the southern part of Michigan to overwinter. Because the lake offered the best form of travel, communities lived along the water rather than inland. The terms Grand Traverse Bay and Little Traverse Bay have roots in the Native American vernacular in that they referred to the size of the traverse needed to be made across the openings that formed bays as one was traveling by canoe along the lakeshore.

There is much I need to learn about the Odawa people but one aspect of their lives I have been researching is how they were never removed from their homeland during Andrew Jackson’s Indian Removal Act of 1830 and the credit for this is owed to the Odawa themselves. Using strategies that involved making themselves meld in and become useful to the white folks they lived around - buying land, paying taxes, attending church and trading furs – encouraged the citizens of Michigan to ask that the Odawa be able to stay. There were tough years where it appeared the Removal Act would be enforced but each time something came up preventing the Odawa’s removal.


Just last year, I attended an Odawa Pow Wow up the street from me. It was a magical day filled with beautiful dress, dance and music. I was so happy to experience a part of their rich cultural heritage and am thankful they are here as a part of our community. But in reality, I am simply a visitor here on their reservation land. A large section of northwest Michigan is Odawa reservation land with a lawsuit pending that will allow them to gain jurisdiction over this land once again. Keeping my fingers crossed for them.

References:

Ottawa Adaptive Strategies to Indian Removal By James M. McClurken

History of the Ottawa and Chippewa Indians of Michigan:

Michigan State University, Native Americans in the Great Lakes Region:

Tribal History of Little Traverse Bay Bands of Odawa Indians:

Tuesday, November 14, 2017

The Weather and Climate Story

The weather and climate information for my ecoregion is collected by the National Weather Service out of Gaylord, Michigan. The area the Gaylord office covers roughly approximates the boundaries of my ecoregion so it is a good fit.

The climate in Michigan, especially the western side of the state where I live is greatly influenced by Lake Michigan. Because bodies of water tend to hold their energy longer than most substances, the lake serves as a warming influence as weather begins to cool in the fall and serves as a cooling influence as weather begins to warm in the spring. In the summer, these influences can result in lake breezes which blow across the cooler waters of the lake and bring cooler temperatures onto land. Temperatures along the water can be 10 degrees less than those found inland. These influences in the winter can result in lake effect snow which happens when cold air coming from the west travels eastward over the warm waters of the lake. The warm water evaporates and is then wrung out in the form of snow as cooler temperatures over land are met. These lake effect snowstorms typically happen during November through February while the lake remains unfrozen. Once the lake freezes over, there is no water available for these sort of storms to continue.

Generally summers in my ecoregion are sunny with moderate temperatures while winters are cold and snowy, a perfect mix in my mind as I don’t enjoy hot temperatures. I am reminded of a slogan we learned in grade school, “when you seek a pleasant peninsula, look about you.

National Weather Service:

WoodTV.com:

Teaching Great Lakes Science:

NOAA SciJinks:



The Seasons Story

We celebrate four seasons here in northern Michigan.

Fall runs from September 22 – December 21
Winter is from December 21 – March 20
Spring March 20 – June 21
Summer June 21 – September 22

Seasons are determined by when the equinoxes fall so even though we tend to think of snowfall only falling in the winter, it generally can be found throughout three seasons here in northern Michigan, anytime from the end of October through April, resulting in about 122 inches. Compare that to Lansing which averages 51 inches and Detroit which get about 42 inches of snow.

Winter equinox 2017 December 21 (shortest day of sunlight for the year)
Spring equinox March 20 (day and night are of equal length)
Summer equinox June 21 (longest day of sunlight for the year)
Autumn equinox September 22 (day and night are of equal length)

Fall, the season we are in, starts out pretty balmy with average highs in the 60’s which dip to highs only in the low 30’s by the time we get to December. These temperature dips correspond with the fading light as we move toward the winter equinox. We also see our first snow during this time.

Winter offers average highs in the upper 20’s to lower 30’s with lots of snowfall, averaging 124 inches a year. Average lows are not as bad as you’d think given our location above the 45th parallel, with temperatures ranging in the teens and 20’s. Generally this season has the most cloudy days of the year given the influence of Lake Michigan on the weather.

Spring is heralded by finding average temperatures moderating from those seen in the colder months with average temperatures moving from highs of 37 in March to 70 in June. As daylight increases, warmth increases.

Summer finds us with average highs in the 70’s, with very few uncomfortable days where air conditioning is required. Skies tend to have less clouds and more blue days than those found in the winter.

Climate Petoskey - Michigan

°C | °F

Jan
Feb
Mar
Apr
May
Jun
Average high in °F:
27
29
37
49
60
70
Average low in °F:
14
13
20
33
42
53
Av. precipitation in inch:
2.05
1.38
1.89
2.52
2.87
2.8
Days with precipitation:
-
-
-
-
-
-
Hours of sunshine:
-
-
-
-
-
-
Average snowfall in inch:
37
25
12
2
0
0


Jul
Aug
Sep
Oct
Nov
Dec
Average high in °F:
75
74
68
55
43
32
Average low in °F:
59
58
51
40
31
22
Av. precipitation in inch:
2.64
3.43
3.58
3.78
2.64
2.4
Days with precipitation:
-
-
-
-
-
-
Hours of sunshine:
-
-
-
-
-
-
Average snowfall in inch:
0
0
0
0
9
39

Petoskey weather averages

Annual high temperature:
51.6°F
Annual low temperature:
36.3°F
Average temperature:
43.95°F
Average annual precipitation - rainfall:
31.98 inch
Days per year with precipitation - rainfall:
-
Annual hours of sunshine:
-
Av. annual snowfall:
124 inch

References:

Current Results, weather and science facts:

US Climate Data:


The Geology Story


Geology story

As I walk along a path near my home, I can gaze up into the hills of the Boyne Highlands or Nub's Nob ski areas and enjoy the beauty of the varied terrain around me. What helps to better connect me to this land though, is to create a sense of place, to understand how these hills came to be. As a young girl studying Michigan history in school, we learned all about the great sheets of ice that covered our land which created its varied topography and lakes. We never got into the more in depth specifics regarding the mechanics of how the glaciers worked their magic and thus never came to understand words such as recessional moraines or outwash plains. Words which give better meaning to what I am looking at or walking upon as I take a stroll out my door.

As glaciers advanced over Michigan 10,000 to 12,000 years ago, they took the path of least resistance, widening river valleys to form today what is known as the Great Lakes. As these glaciers moved over the land, they operated as a conveyor belt, scooping up debris as they went along, not bulldozing the land as you would think, and then as they melted and began to retreat, hills and valleys were created through this melting as they dropped the debris they had picked up along the way.

As the ice sheets melted, their retreat was done in a stop and go fashion. When they stopped, the glacier dropped the material it was holding known as glacial till. This till as it was deposited, formed hills known as recessional moraines such as what you'd find at Boyne Highlands or Nub's Nob. The flatter areas in front of the moraines were known as outwash plains, where the melting water containing smaller particles of debris such as sand, moved away from the moraines. This is a very simplistic explanation of the process of glaciers and the story of how my local landscape was formed, but to me I find it interesting to begin to connect the dots of how things came to be. To begin to understand why the soil under my feet is comprised of sand or why some places are hilly while others are not. 

Now, as I walk along the path near my home, I no longer just see hills and valleys, but think instead of the huge glaciers that carved out the story of my landscape. There is much more to learn and so many questions to be unlocked regarding this story but that is what gets me out the door over and over again. 

References:

Outwash plains, Michigan State Geology

The Watershed Story

There are three watersheds in my ecoregion - Cheboygan, Lake Michigan and Boardman – Charlexoix. At this point in time, I am just going to focus on the Cheboygan watershed as my house lies within that one.

Anyone in the US can find their watershed by entering their zip code in the link below:


After clicking on the Cheboygan watershed, arrived at by the link above, I was taken to the link below which listed information specific to the watershed my house lies in.


This link lists water quality monitoring groups and where they are monitoring - as well as all the impairments to the different bodies of water in my area and what exactly is impairing them, such as PCB’s or mercury. It also lists stream flow for some of the rivers as well as local environmental organizations working to help with water quality which in my case is the Tipp of the Mitt Watershed Council.

First off, I am shocked to see all of the bodies of water which make up my watershed. Many lakes, rivers, and creeks. How is it possible to keep track of them all as well as their overall health? Some of the monitoring stations show contamination of Chlordane and DDT, both dangerous pesticides no longer used but which clearly still continue to persist both in the environment and in ourselves as well I am sure. Upon visiting The Global Healing Center websitewhich talks about Chlordane, I read that a diet rich in fruits and vegetables and one that avoids processed carbohydrates helps to rid your body of this pesticide. Oh my gosh, I pull on one thread to understand the watershed in my area, and I clearly wander into a whole other area, clearly pointing to the fact that everything is interrelated. What you do to one part of the web impacts another part of the web. There are many other things listed which are impacting the health of my watershed but I will have to investigate those impacts another day.


Ecoregions and Watersheds

Ecoregions and watersheds are methods to divide up a place using natural means rather than the human based divisions which use town or county boundaries. Of the six characteristics comprising sense of place – geology, weather, seasons, Indigenous story, water and wildlife, which ones are considered? Ecoregions consider the geology, water, weather, wildlife (just the plant aspect, not animals) of a place, whereas watershed only consider waterways and how water flows to divide up an area.

 Because an ecoregion considers the ecology of a place, you get a broad based view, seeing many natural elements coming together and relating to each other. For instance, I live in the ecoregion known as northern lakes and forests which has sandy soil. The combination of being in a northern area of the state and also having sandy soil would support those plants which can survive in both sand and cold climates such as Quaking Aspens, which in turn would support those animals who use aspens for survival.

Ecoregions look at the broader picture of a place whereas watersheds only consider how water drains in an area and is a less encompassing view for purposes of sense of place. It is important though to understand watersheds because whatever activity happens on a watershed – industry, golf course chemical use etc…ultimately impacts the quality of water flowing off that land and into the local waterways.

ECOREGIONS

If you are interested in determining your ecoregion, here is the EPA breakdown for the 120 ecoregions within the United States:

EPA Ecoregions

There are five ecoregions in Michigan as shown at the following link:


All of the information from this point through the descriptions of the ecoregions were taken from the above link.

The five Michigan ecoregions are:

level III ecoregions of Michigan


50. NORTHERN LAKES AND FORESTS - The Northern Lakes and Forests is a region of nutrient poor glacial soils, coniferous and northern hardwood forests, undulating till plains, morainal hills, broad lacustrine basins, and extensive sandy outwash plains. Soils in this ecoregion are thicker than in those to the north and generally lack the arability of soils in adjacent ecoregions to the south. The numerous lakes that dot the landscape are clearer and less productive than those in ecoregions to the south.

51. NORTH CENTRAL HARDWOOD FORESTS - The North Central Hardwood Forests is transitional between the predominantly forested Northern Lakes and Forests to the north and the agricultural ecoregions to the south. Land use/land cover in this ecoregion consists of a mosaic forests, wetlands and lakes.

55. EASTERN CORN BELT PLAINS - The Eastern Corn Belt Plains is primarily a rolling plain with local end moraines; it had more natural tree cover and has lighter colored soils than the Central Corn Belt Plains. The region has loamier and better drained soils than the Huron/Erie Lake Plain, and richer soils than the Erie/Ontario Hills and Lake Plain. Glacial deposits of Wisconsin age are extensive. They are not as dissected nor as leached as the pre-Wisconsin till which is restricted to the southern part of the region. Originally, beech forests were common on Wisconsin soils while beech forests and elm-ash swamp forests dominated the wetter pre-Wisconsin soils.

56. SOUTHERN MICHIGAN/NORTHERN INDIANA DRIFT PLAINS - Bordered by Lake Michigan on the west, this ecoregion is less agricultural than those to the south, it is more well drained and contains more lakes than the flat agricultural lake plain to the east, and its soils are not as nutrient poor as the region to the north. The region is characterized by many lakes and marshes as well as an assortment of landforms, soil types, soil textures, and land uses. Broad till plains with thick and complex deposits of drift, paleobeach ridges, relict dunes, morainal hills, kames, drumlins, meltwater channels, and kettles occur.

57. HURON/ERIE LAKE PLAIN - The Huron/Erie Lake Plain is a broad, fertile, nearly flat plain punctuated by relic sand dunes, beach ridges, and end moraines. Originally, soil drainage was typically poorer than in the adjacent Eastern Corn Belt Plains, and elm-ash swamp and beech forests were dominant. Oak savanna was typically restricted to sandy, well-drained dunes and beach ridges.
I live the section listed as #50 on the map, northern lakes and hardwoods and will use this information to piece together information on the geology and wildlife of my area.

WATERSHEDS

In regard to watersheds for Michigan, the Department of Environmental Quality has put together a map for the hydrology of Michigan at this link:

An interesting thing about the watershed map is it only features the watersheds for the largest bodies of water in Michigan. Remember within those watersheds there are many other smaller watersheds moving the water toward the main river or lake featured on the watershed map. The Cheboygan watershed has many lakes and rivers, all with their own watersheds, moving the water ultimately toward the Cheboygan river. This link from the Tip of the Mitt Watershed Council talks all about the Cheboygan watershed:

It looks like my house is right on the border between the Lake Michigan and Cheboygan River watershed so I am going to have to search for a more detailed map which superimposes the Cheboygan watershed over a street map in order to determine which watershed I am in.

After a bit of searching, I found a Trout’s Unlimited map of the Cheboygan watershed which is really pretty cool because I was right, the watershed boundary literally crosses my road two houses down from me. So those on my side of the street are in the Cheboygan watershed and the folks down the road and across are in the Lake Michigan watershed. Really weird to think the rain falling on my property moves in a different direction than the water just down the road. Which really doesn’t make sense to me because the road in front of me moves downhill toward that watershed which makes me think the water falling on my property would move toward the Lake Michigan watershed. But then as I rethink what I am saying, I realize that yes, the road in front of my house goes downhill but then flattens out and the flat part is still in the Cheboygan watershed so it could essentially flow down the hill and then move back toward my watershed. Confusing to think about. So this talk of watersheds and how water moves gets me to thinking about the water which flows in the aquifers beneath the ground. Do they also flow in tandem with the watersheds? So would the water in my watershed flow toward the Cheboygan River and the water in the Lake Michigan aquifer flow toward Lake Michigan? Well before I research that question, let me add the link to the Cheboygan watershed boundary here:


After doing just a bit of research, I am pretty sure aquifers do move in conjunction with the watersheds. I based my information on these two sites from the US Geological Survey:


So now I have another question. If I am living on the boundary between two watersheds, does that mean the water flowing in the aquifers below my house are always flowing away from my house, one toward Lake Michigan and the other toward the Cheboygan River? If so, does that mean the water from my community well is pulling up mainly water that falls onto this area directly? Obviously I am going to have to pay the Watershed Council a visit to get that answer.

OK, so I certainly have a better understanding of the ecoregion and watershed I reside within and find it interesting that one set of questions leads to many others. I think that is the way it is with the natural world. Just about the time you figure one thing out, another layer presents itself to you to pull back. But for now I need to draw the line here and move on the do the work of looking at the six different areas that make up sense of place.

For the purposes of discovering my sense of place, I am going to be studying my ecoregion (which encompasses my watershed) rather than my watershed. I feel the area of my ecoregion is more representative of where I live. Because I live on the boundary between two watersheds, it would be weird to not consider factors that are just down the street from myself.