Sunday, January 15, 2012
Truck Driver Divorce -- The 1926 Version.
Here's a radically traditional 1926 version of a song by Frank Zappa that he and his band played quite a bit in their early 1980s tours. At the time, he allegedly described it as "a country song on PCP" that would cause the "death of country music." It did not surface in a recorded version until the 1984 double album, Them or Us.
Truck Driver Divorce -- 1926 Version.
In the late 1970s Zappa couldn't resist poking fun at country music, probably due to the ascendance of televangelists like Jerry Falwell and his waterboy, Ronald Reagan, who piously extolled the genre's celebration of enduring family values ... like ... umm ... cheating on your wife and being a useless drunk.
But Truck Driver Divorce is not a country song. It's really a mid 1920s Al Jolson kind of song ... on PCP. But then again, Al Jolson is like Al Jolson on PCP, so go figure.
And despite some enthusiasts' claims that this song is just Zappa's live band doing a loose, free improvisation behind a similarly free vocal improv, it is built on a standard 1920s-type descending I-IV blues progression using two major chords and their dominant seventh and minor, ie. I-I7-IV-IVm. In each second section, the I-IV resolves to the V. This is a scheme heard in countless ragtime and blues songs of the pre-1930s era and practically begs the singer to do the melody like Al Jolson, which is what Frank does, creating the appropriate level of cloying, obviously fake sentimentality the lyrical subject requires.
In the key of G, the basic chords are:
D7 (intro chord).
G -- G7 -- C -- Cm
G -- G7 -- C -- Cm -- A7 -- D7
While the vocal melody starts on the G, you need the D flatted seventh to set up the flavor of the song's tonality. This type of intro is a standard ragtime device, probably to get people in the room to notice the band is going to start playing a song. Blind Lemon Jefferson uses this kind of an intro in his 1926 song "Beggin' Back."
Note that all the seventh chords are not the major seventh but the dominant, ie. flatted seventh. So in G7, the seventh note is F natural, not F sharp, ie. G-B-D-F, which is what gives the progression a ragtimey feel.
Because this is supposed to be a country song, the G position on bass does not let you alternate down to a low D as the fifth which you really need to get that honky-tonk feel. Instead of detuning the low E bass string to D, I alternated the low G with the open D string. In the back end (4 bars) of each second section the bass really needs to walk through the chords on straight eighth notes instead of the rocking chair squeak kind of quarter notes at the front.
The final verse is different:
Cm - G - D7
Truck Driver divorce, it's very sad.
A7
Bust Your Ass
Cm
To deliver some string beans
A7
To deliver some string beans
D7
To Utah
G
Tonight.
Despite that Zappa's original live recording sort of sounds like a free improv, the composition is tightly structured and Zappa's vocal melody follows the I-IV progression closely, even though he and the bass player perversely flatten or double flatten a bunch of the notes. According to those who zealously research this arcane stuff, the instrumental back end of the recorded version is a spliced-in live performance of the song Zoot Allures from 1981 in New York City:
So anyways, if you have an acoustic guitar and can play open first position chords, you can play the 'real' arrangement of Truck Driver Divorce and exorcise your secret desire to be Al Jolson or Bessie Smith doing a really stupid country song about driving a truckload of string beans to Utah.
About the string beans. Zappa must have written these lyrics at the same time he wrote "No Not Know" from Ship Arriving Too Late To Save A Drowning Witch, since both songs contain a lot of the same phrases, like "transcontinental hobby horse" and "oh the wife ... oh the waitress ... oh the drive all night long," etc. And, of course, string beans to Utah, which apparently has some weird connection to Donny and Marie Osmond.
What I like about Truck Driver Divorce, aside from its sheer and unrelenting idiocy, is that the melody and chord progression are rooted in the 1900-1910s ragtime changes which by the 1920s became 'citified' by singers like Al Jolson, to the point where it's almost impossible to sing this song without subconsciously wanting to say, "Oh Mammy .... all the way home from Alabammie .... she used to cook me eggs and hammy ... Oh Mammy."
But the biggest challenge in recording the 1926 version of Truck Driver Divorce is that you can't sing the song straight because it's too flat-out stupid and songs in 1926 were never sung 'straight.' This is pre-method acting time. And I also didn't want to imitate Zappa's arrangement, since then what's the effing point?
After a lot of trial and error and messing around at 4 a.m. I started adding in all of the background noises, which consist of me pouring dirty bath water back and forth from a couple of plastic cat litter buckets and then kicking them over on the floor, shaking a bag of styrofoam packing peanuts, mumbling incoherently and imitating the voices of some weird people I know who talk like they have marbles in their mouth about shaving Brenda's crotch.
This fake audio verite approach is itself a direct rip-off of the Mothers' song "America Drinks and Goes Home" from Absolutely Free where Zappa creates a sound collage of a dive cocktail bar at closing time with Ray Collins saying 'last call for alcohol, drink it up folks' and offering them peanut butter and jelly and baloney sandwiches at their next gig while the patrons start throwing chairs and bottles at each other:
One problem with this recording approach is that it requires just the right mix of mayhem vs. music, which has a lot to do with mic placement and panning to enlarge the stereo spectrum so that you can still hear the song but the mayhem is right in your face. The production challenge is to take a completely studio recorded piece but make it sound like a single condenser mic at some weird PCP-laden hillbilly cabin in the woods.
The tail-out is me, Mark Kemezys, Jerry Trevino and Jeff Hursch doing some weird improv at 38-C Northern Ave with those 99 cent plastic slidey whistles.
Enjoy!
You can also do the song in C, which falls well on an open, first position guitar, and nicely on the bass, since you get to hit the C root on the 3rd fret, 2nd string and drop right to the G on the low E string. That progression is C-C7-F-Fm with D7 and G7 replacing A7 and D7 as the adds.
Actually, Lemon Jefferson was one of the only 1920s singers to 'drop' the theatrical pose and do a song straight, meaning sarcastically, in "Beggin' Back," where in the improvised verses he's goofing on the chorus of the song.
Tuesday, December 06, 2011
When kids used to go down to the Kennebec River to get Atlantic salmon for breakfast.
Citation: Boardman, Samuel L.: in Ninth Annual Report of the Secretary of the Maine Board of Agriculture. 1864. Augusta, Maine. Stevens & Sayward, Printers to the State. Subsequently published in the Maine Farmer, March 23, 1865.
At page 109:
"An aged woman, who formerly lived on the banks of the Kennebec in Vassalboro, and who, at that time, had a large family of children to support, once told me that, in spring and early summer, the fish from the river were a very essential aid to them -- that many times she has sent one of her boys down to the river early in the morning to catch a salmon for breakfast, with as much certainty that he would bring one home in season, as if she had sent him with the money to a city fish market, where she knew they were kept for sale."
How Maine's Sea-Run Fish were Dammed into Oblivion, 1864.
Citation: Boardman, Samuel L. 'Aquaeculture': in Ninth Annual Report of the Secretary of the Maine Board of Agriculture. 1864. Augusta, Maine. Stevens & Sayward, Printers to the State. Also pub. in Maine Farmer, March 23, 1865.
At p. 109-110:
"Everyone now knows that salmon, shad and alewives, and indeed all the other kinds of migratory fishes -- those that spend winters in the salt water, and come up out of the sea at certain periods, as if sent by a kind Providence, to spend the spring and summer in fresh water -- are now very scarce indeed, and in some streams totally extinct. Everyone knows, too, that many of the species of fishes which remain permanently in our fresh waters, have very much decreased in numbers, as well as in size and fatness. People say that this is a necessary consequence of the building of dams and mills, and filling the streams with obstructions of various kinds for the industrial pursuits of a civilized community. No doubt it is a consequence of these obstructions, but it not need be a necessary consequence. I hold that dams and mills might be constructed, and continued, and yet by a little concession on the part of dam and mill proprietors, and a more general diffusion of the knowledge of the natural history fishes, more intimate acquaintance with their peculiar habits, instincts, and wants of life, the mills might remain and the fish continue to perform their annual pilgrimage to and from their breeding haunts, if not in so great numbers as in former times, yet in such numbers as to afford a vast amount of provisions and even luxury to the communities which are now wholly deprived of them.
"I am also aware that this subject has been discussed over and over again -- that for years and years past, every session of our Legislature was thronged, and committees were worried and teased by mill owners on the one hand and fishermen on the other -- one demanding the privilege of building dams and mills without let or hindrance as to the fish, and the other pleading for some reserve, some fish-way, or some accommodation to the annual flow of the fish, which had been of such signal service to the support of the people on the banks and vicinity of the waters in question. I am also aware that our Legislators, actuated by a sincere desire to do justice to all parties, and to give equal rights to all, have, in most instance, made provisions in the several charters and private acts pertaining to mill owners, for the passage of fish at certain times and seasons, with a hope that, while it encouraged the establishment of mills and machinery, there would be also at the required times a safe and successful transit for the various species of fishes that required such passes as one of the indispensable requirements for the continuation of their existence. And we are all aware also that, either from ignorance of what habits of the fish demand, these ways have not always been properly constructed, or from selfishness in mill owners in not keeping them open at suitable times, these provisions in most cases failed, and the destruction of the fish is the inevitable result."
At p. 109-110:
"Everyone now knows that salmon, shad and alewives, and indeed all the other kinds of migratory fishes -- those that spend winters in the salt water, and come up out of the sea at certain periods, as if sent by a kind Providence, to spend the spring and summer in fresh water -- are now very scarce indeed, and in some streams totally extinct. Everyone knows, too, that many of the species of fishes which remain permanently in our fresh waters, have very much decreased in numbers, as well as in size and fatness. People say that this is a necessary consequence of the building of dams and mills, and filling the streams with obstructions of various kinds for the industrial pursuits of a civilized community. No doubt it is a consequence of these obstructions, but it not need be a necessary consequence. I hold that dams and mills might be constructed, and continued, and yet by a little concession on the part of dam and mill proprietors, and a more general diffusion of the knowledge of the natural history fishes, more intimate acquaintance with their peculiar habits, instincts, and wants of life, the mills might remain and the fish continue to perform their annual pilgrimage to and from their breeding haunts, if not in so great numbers as in former times, yet in such numbers as to afford a vast amount of provisions and even luxury to the communities which are now wholly deprived of them.
"I am also aware that this subject has been discussed over and over again -- that for years and years past, every session of our Legislature was thronged, and committees were worried and teased by mill owners on the one hand and fishermen on the other -- one demanding the privilege of building dams and mills without let or hindrance as to the fish, and the other pleading for some reserve, some fish-way, or some accommodation to the annual flow of the fish, which had been of such signal service to the support of the people on the banks and vicinity of the waters in question. I am also aware that our Legislators, actuated by a sincere desire to do justice to all parties, and to give equal rights to all, have, in most instance, made provisions in the several charters and private acts pertaining to mill owners, for the passage of fish at certain times and seasons, with a hope that, while it encouraged the establishment of mills and machinery, there would be also at the required times a safe and successful transit for the various species of fishes that required such passes as one of the indispensable requirements for the continuation of their existence. And we are all aware also that, either from ignorance of what habits of the fish demand, these ways have not always been properly constructed, or from selfishness in mill owners in not keeping them open at suitable times, these provisions in most cases failed, and the destruction of the fish is the inevitable result."
How Maine's Sea-Run Fish were Overfished to Oblivion
A few early to mid 1800s historic references I just came across illustrate how early and quickly the sea-run fish of Maine rivers were wiped out by over-fishing:
Citation: William Durkee Williamson. 1832. The History of the State of Maine. Vol. 1. Glazer, Masters & Co. Hallowell, Maine.
At p. 158, describing striped bass:
"The Bass is a large scale fish, variable in its size from 10 to 60 pounds. They are striped with black, have bright scales and horned backs, and are caught about the coasts. They ascend into the fresh water to cast their spawn, in May or June, being lean afterwards and fat in the autumn. In June 1807, there were taken at the mouth of the Kenduskeag, 7,000 of these fishes, which were of a large size -- a shoal, either pursued up the river by sharks, or ascended in prospect of their prey, or to cast their spawn."
Smelt at p. 160:
"They are caught in abundance, after March, in our rivers; 20 barrels of them have been taken at the mouth of the Kenduskeag at a sweep, and sometimes they are worth no more than half a dollar a bushel."
At footnote 3, same page: "On the 2d of May, 1794, at the mouth of the Kenduskeag (on the Penobscot) were taken at one draft 1,000 shad and 30 barrels of alewives."
----
Citation: Boardman, Samuel L. 'Aquaeculture': in Ninth Annual Report of the Secretary of the Maine Board of Agriculture. 1864. Augusta, Maine. Stevens & Sayward, Printers to the State. Also pub. in Maine Farmer, March 23, 1865.
At p. 117:
"Three years ago, in the month of May, in company with a friend, while passing by the lower lock of the Cumberland and Oxford Canal, in the city of Portland, our attention was drawn to the a crowd of men standing by the side of the lock, several of whom had long-handled nets, with which they were fishing, or rather dipping out fish from the water. On coming up, we saw that they were catching alewives in great numbers. It appeared that these fish, in their peregrinations along the coast, had been attracted by the fresh water of the canal, and instinctively entered it in order, as they supposed, to follow up to its source, (Sebago Lake,) but were brought to a standstill by the upper gate of the lock. The men engaged there then shut the lower gate, and commenced catching them. As soon as those of them that were confined in the lock were all caught, the men opened the lower gate again, and admitted a lot more of them, and thus a wholesale destruction of them went on. I supposed that some of them might possibly work their way up, when the several locks should be opened for the passage of boats, and thus Sebago made a breeding place for them, but on inquiry, am told that there are few or none seen there. Now it would be a very easy matter to stock that lake with young herrings (alewives) by proprietors of the canal forbidding any of them to be caught on certain days, and placing men along the route to let them go through the gates into the lake. Indeed, it seems that by renting the privilege of fishing for them on certain days, some considerable revenue might accrue to the company, while the production of the fish would again become a benefit to the section of country through with the canal passes. The same system might be adopted on many streams by having fish-ways or fish-locks, to aid their ascent, with much benefit to the country and no detriment to the mill interests."
_______
Citation: Twelfth Annual Report of the Maine Board of Agriculture, 1867. Stevens & Sayward, Printers to the State.
At page 90: "In Monmouth they [smelt] run into some very small rills that lead into Cochnewagon Pond, and are dipped out in considerable quantities. In May, 1867, after it was supposed they were all gone, a fresh run occurred, that yielded thirty barrels."
Citation: William Durkee Williamson. 1832. The History of the State of Maine. Vol. 1. Glazer, Masters & Co. Hallowell, Maine.
At p. 158, describing striped bass:
"The Bass is a large scale fish, variable in its size from 10 to 60 pounds. They are striped with black, have bright scales and horned backs, and are caught about the coasts. They ascend into the fresh water to cast their spawn, in May or June, being lean afterwards and fat in the autumn. In June 1807, there were taken at the mouth of the Kenduskeag, 7,000 of these fishes, which were of a large size -- a shoal, either pursued up the river by sharks, or ascended in prospect of their prey, or to cast their spawn."
Smelt at p. 160:
"They are caught in abundance, after March, in our rivers; 20 barrels of them have been taken at the mouth of the Kenduskeag at a sweep, and sometimes they are worth no more than half a dollar a bushel."
At footnote 3, same page: "On the 2d of May, 1794, at the mouth of the Kenduskeag (on the Penobscot) were taken at one draft 1,000 shad and 30 barrels of alewives."
----
Citation: Boardman, Samuel L. 'Aquaeculture': in Ninth Annual Report of the Secretary of the Maine Board of Agriculture. 1864. Augusta, Maine. Stevens & Sayward, Printers to the State. Also pub. in Maine Farmer, March 23, 1865.
At p. 117:
"Three years ago, in the month of May, in company with a friend, while passing by the lower lock of the Cumberland and Oxford Canal, in the city of Portland, our attention was drawn to the a crowd of men standing by the side of the lock, several of whom had long-handled nets, with which they were fishing, or rather dipping out fish from the water. On coming up, we saw that they were catching alewives in great numbers. It appeared that these fish, in their peregrinations along the coast, had been attracted by the fresh water of the canal, and instinctively entered it in order, as they supposed, to follow up to its source, (Sebago Lake,) but were brought to a standstill by the upper gate of the lock. The men engaged there then shut the lower gate, and commenced catching them. As soon as those of them that were confined in the lock were all caught, the men opened the lower gate again, and admitted a lot more of them, and thus a wholesale destruction of them went on. I supposed that some of them might possibly work their way up, when the several locks should be opened for the passage of boats, and thus Sebago made a breeding place for them, but on inquiry, am told that there are few or none seen there. Now it would be a very easy matter to stock that lake with young herrings (alewives) by proprietors of the canal forbidding any of them to be caught on certain days, and placing men along the route to let them go through the gates into the lake. Indeed, it seems that by renting the privilege of fishing for them on certain days, some considerable revenue might accrue to the company, while the production of the fish would again become a benefit to the section of country through with the canal passes. The same system might be adopted on many streams by having fish-ways or fish-locks, to aid their ascent, with much benefit to the country and no detriment to the mill interests."
_______
Citation: Twelfth Annual Report of the Maine Board of Agriculture, 1867. Stevens & Sayward, Printers to the State.
At page 90: "In Monmouth they [smelt] run into some very small rills that lead into Cochnewagon Pond, and are dipped out in considerable quantities. In May, 1867, after it was supposed they were all gone, a fresh run occurred, that yielded thirty barrels."
Thursday, July 07, 2011
Monday, July 04, 2011
Clay is Rusted Feldspar
My wife Lori asked me to explain to her pottery class in a fairly simple way what clay is, where it comes from, and how it got here. So here's an attempt at a non-technical explanation.
Clay is feldspar rusting. This is an analogy, but not that far from the actual process. We all know what happens if you buy a nice, shiny piece of cast iron from the hardware store and leave it outside in the sun and rain. It quickly rusts. If you leave it out long enough, it turns to almost all rust. So what is rust?
Rust is primarily the minerals limonite and goethite, created when iron combines with oxygen from the atmosphere and oxygen in water. We all know that iron things tend to rust faster when wet than when dry. Moisture hastens rusting.
Feldspar is not iron. Iron is one element, iron. Feldspar is a large family of minerals made from oxygen, silicon, aluminum, sodium, potassium and calcium. Feldspar does not form on the Earth's surface. It only forms miles beneath the Earth's surface, where solid rock is naturally in a semi-liquid, molasses-like state.
Feldspar is only released from its 'natural' home and to the Earth's surface either when it is forcibly ejected from a volcano as lava or when, after hundreds of millions of years, the 2-3 miles of solid rock above the feldspar is eroded away, leaving the feldspar nakedly exposed on the Earth's surface. This is usually in the form of granite, which is a rock made of feldspar and quartz and some mica.
To add another analogy, just like a piece of fine pottery on the edge of a shelf 'wants' to fall on the floor and smash, feldspar 'wants' to turn to clay when it is exposed to the Earth's surface. The agent for the pot on the shelf wanting to fall down and smash is gravity (in outer space, pottery does not break, it orbits). The agent for feldspar wanting to turn to clay is a bit more complex, but similar in design to iron rusting. In both, the agents are primarily air and water.
In the presence of air and water at the Earth's surface, the most natural and restive state for feldspar is to re-align its molecules into clay molecules. Clay is a mineral, just like quartz or feldspar. It has a very regular and ordered crystalline structure, like a diamond or a cube of salt. The three predominant clay minerals are kaolinite, illite and montmorillonite. With a scanning electron microscope you can get pictures of very nice, well formed, plate-like clay crystals growing right next to a crystal of feldspar.
Feldspar becomes clay by slowly bringing water into its crystal structure, like a sponge left in a puddle of water. This water becomes part of the very fabric of the feldspar; like how iron becomes part of your blood cells. The feldspar wants the water. It likes it. Which brings us back to rust.
What we call rust is the natural state of iron on the Earth's surface. Iron readily combines with oxygen to make rust. It wants to become rust. In fact, we have to do all kinds of crazy things to prevent iron from becoming rust. We coat it with oils, with paint (like Rust-Oleum) or galvanize it with zinc, all to keep the iron from contacting oxygen in the air and oxygen in water, sort of like teacher chaperones at a high school dance. Left to its own device, feldspar becomes clay because it wants to; that is its most stable and natural state on the Earth's surface. Like a thrown ball 'wants' to come back down, feldspar wants to become clay. Clay is rusted feldspar; and the actual chemical reactions are not that different.
In Maine, where I live, from 1880-1930 there was a flourishing industry where large feldspar deposits were quarried and mined for use as ceramic pottery glaze. This was feldspar that had not yet had time to weather into clay. It is still solid enough to make a house foundation. But if you crush into a fine enough powder, it works beautifully as a glaze ingredient. Most of the feldspar mined in Maine was shipped to pottery works in New Jersey as a basic glaze ingredient for everything from fine plateware to toilet bowls. It was an 'industrial mineral,' as the saying goes.
The only reason Maine does not have deposits of natural, 'primary' clay is because for the past million years Maine has been scoured by successive, mile high glaciers every 100,000 years or so, which like a steel plow on a snow-filled driveway, scraped away all the clay and softened rock right down to hard bedrock and dumped the residue in the Atlantic Ocean. In the U.S., you have to go south of the line of glaciers, ie. Kentucky or Tennessee, to find clay deposits still intact and near where they were first formed. What we in Maine call 'marine clay' is actually the finely ground-up residue from the glaciers' scraping and grinding that has partly altered into true clay minerals and is on its way to doing so, give another 10 million years. That said, it is still perfectly usable as a slip or a low-fire earthenware body. Be patient, Maine !!!
Clay is feldspar rusting. This is an analogy, but not that far from the actual process. We all know what happens if you buy a nice, shiny piece of cast iron from the hardware store and leave it outside in the sun and rain. It quickly rusts. If you leave it out long enough, it turns to almost all rust. So what is rust?
Rust is primarily the minerals limonite and goethite, created when iron combines with oxygen from the atmosphere and oxygen in water. We all know that iron things tend to rust faster when wet than when dry. Moisture hastens rusting.
Feldspar is not iron. Iron is one element, iron. Feldspar is a large family of minerals made from oxygen, silicon, aluminum, sodium, potassium and calcium. Feldspar does not form on the Earth's surface. It only forms miles beneath the Earth's surface, where solid rock is naturally in a semi-liquid, molasses-like state.
Feldspar is only released from its 'natural' home and to the Earth's surface either when it is forcibly ejected from a volcano as lava or when, after hundreds of millions of years, the 2-3 miles of solid rock above the feldspar is eroded away, leaving the feldspar nakedly exposed on the Earth's surface. This is usually in the form of granite, which is a rock made of feldspar and quartz and some mica.
To add another analogy, just like a piece of fine pottery on the edge of a shelf 'wants' to fall on the floor and smash, feldspar 'wants' to turn to clay when it is exposed to the Earth's surface. The agent for the pot on the shelf wanting to fall down and smash is gravity (in outer space, pottery does not break, it orbits). The agent for feldspar wanting to turn to clay is a bit more complex, but similar in design to iron rusting. In both, the agents are primarily air and water.
In the presence of air and water at the Earth's surface, the most natural and restive state for feldspar is to re-align its molecules into clay molecules. Clay is a mineral, just like quartz or feldspar. It has a very regular and ordered crystalline structure, like a diamond or a cube of salt. The three predominant clay minerals are kaolinite, illite and montmorillonite. With a scanning electron microscope you can get pictures of very nice, well formed, plate-like clay crystals growing right next to a crystal of feldspar.
Feldspar becomes clay by slowly bringing water into its crystal structure, like a sponge left in a puddle of water. This water becomes part of the very fabric of the feldspar; like how iron becomes part of your blood cells. The feldspar wants the water. It likes it. Which brings us back to rust.
What we call rust is the natural state of iron on the Earth's surface. Iron readily combines with oxygen to make rust. It wants to become rust. In fact, we have to do all kinds of crazy things to prevent iron from becoming rust. We coat it with oils, with paint (like Rust-Oleum) or galvanize it with zinc, all to keep the iron from contacting oxygen in the air and oxygen in water, sort of like teacher chaperones at a high school dance. Left to its own device, feldspar becomes clay because it wants to; that is its most stable and natural state on the Earth's surface. Like a thrown ball 'wants' to come back down, feldspar wants to become clay. Clay is rusted feldspar; and the actual chemical reactions are not that different.
In Maine, where I live, from 1880-1930 there was a flourishing industry where large feldspar deposits were quarried and mined for use as ceramic pottery glaze. This was feldspar that had not yet had time to weather into clay. It is still solid enough to make a house foundation. But if you crush into a fine enough powder, it works beautifully as a glaze ingredient. Most of the feldspar mined in Maine was shipped to pottery works in New Jersey as a basic glaze ingredient for everything from fine plateware to toilet bowls. It was an 'industrial mineral,' as the saying goes.
The only reason Maine does not have deposits of natural, 'primary' clay is because for the past million years Maine has been scoured by successive, mile high glaciers every 100,000 years or so, which like a steel plow on a snow-filled driveway, scraped away all the clay and softened rock right down to hard bedrock and dumped the residue in the Atlantic Ocean. In the U.S., you have to go south of the line of glaciers, ie. Kentucky or Tennessee, to find clay deposits still intact and near where they were first formed. What we in Maine call 'marine clay' is actually the finely ground-up residue from the glaciers' scraping and grinding that has partly altered into true clay minerals and is on its way to doing so, give another 10 million years. That said, it is still perfectly usable as a slip or a low-fire earthenware body. Be patient, Maine !!!
Tuesday, June 21, 2011
Sunday, June 19, 2011
Fathers Day, Part I
Fathers Day
We live on stolen land
But what of it.
It was the Indians' land
So we told them to shove it.
Now they exist in our minds
Like little figurines
On the mantel or in
some magazine.
Some folks are surprised
when a fox is in their yard
Forgetting it was first
the foxes' yard.
Things you ignore
Don't go away.
Because you don't care
if they go or stay.
No country cheers
that it's number two.
The sky doesn't cry
because it's blue.
It can't have happened both ways
if we want it to.
A lie becomes true
if enough believe it.
A child stays pure
until you deceive it.
Then the kid starts asking why.
It's okay for you but
not for me to lie.
You'll learn son sometimes
It's what it takes
to get by.
Tuesday, May 24, 2011
The Great Goddards Ledge Rose Quartz Conspiracy Hoax

Philip Morrill et al. (1958) described Goddards Ledge near Rumford Center, Maine as a rose quartz locality, found while the pegmatite was worked for ceramic feldspar in the WWII era.
So in 1993 I tried to find it. It's a nasty traverse, pretty steep, up the side of a mountain, unmarked, no trails and 'intermittently' posted. But what the hell. Plus it's raining (keeps the black flies and mosquitoes down). Up and away we go.
Bonanza !!! I found an old feldspar working littered with giant shards of glass quartz way up the mountain, under lots of mud and leaves. This must be it. Light going fast in the rain. It's all rose quartz. Unbelievable! Nobody has been here for decades. It's all mine !!!
Get home at 10 p.m. totally soaked in mud, get up, go to work, next day take out all the 'finds' and cover the kitchen floor of the apartment with them. Yes !!! Sun comes out next day. All the 'rose quartz' is amazingly clear and devoid of any pink coloration.
My landlord, Yvon Doyon, comes by for the rent. The whole house and deck are covered with pieces of non-rosy quartz. We have to step around them as I write him the rent check. He gives me a quizzical look. It's a tenement. Lots of 'not-normal' people live here, and I get the feeling Yvon has officially put me in that category.
I've been hoodwinked. Shamboozled. Schlamottled. Diabolicized. It's all NON rose quartz !!! How could this be?
I think it was becuz I was a wee bit too 'eager,' or as Jim Mann would say, 'rock warped.'
Actually, a dozen or so of the pieces are true rose quartz. The rest are so faintly tinted it would have taken rose quartz tinted glasses to see it. And apparently I was wearing coke bottles of that stuff when I was at Goddards Ledge. Oops.
But it gets worse. Much worse. The next spring I brought my girlfriend to Goddards Ledge as the 'first stop' on a Memorial Day camping vacation; and we both climbed the 800 foot nasty incline up to the 'quarry.' But we didn't find it. I followed the wrong ravine. Since there are no trails, it's a bit complicated. And every mosquito and black fly in Oxford County had our number. So we ran back down the mountain to the car, totally sweaty, hungry, disgusted and bug-bitten.
Except I could not find the car keys. They were somewhere 'up there' on the mountain. I had put them in my backpack (for 'safe keeping') and forgot to zip the pocket shut. So they could be anywhere between us and the non-Goddards Ledge quarry. Under the leaves. In between two rocks. Anywhere. And it was getting dark. Smooth move, Doug.
So back up the mountain and about halfway up I saw a glint. The keys !!! Really? The keys !!!
They had fallen out of my pack when I was skidding up or down a glacial erratic. God must have had mercy on me that day.
So some of the rose quartz at Goddard's Ledge in Rumford is genuine, if you don't get too over enthusiastic. And when fashioned en cabochon it does display 6, 8 and 12-star asterism, as Phil Morrill said in 1958.
But keep an extra set of keys under the car wheel. Just in case.
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