Indian Artifacts
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Indian Artifacts |
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Paleo Weapons Exotic Replicas made with authentic stone artifacts.
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The Discovery A waning screech catapults me out of a daydream. Overhead, a circling hawk parts the sky with a twist of its red tail and I’m back on the bare cornfield where I’ve been walking for hours. There’s a subtle sense of reverence for being on the very ground my distant ancestors once walked. Through the lace of human genetics stretching far back into dark Africa, we are all related, I thought. Sweet moldy scent of fresh earth pulls me back once again to the damp soil. How much have I missed? I vow to railroad my attention to the ground looking for clues, a single glint of reflected light - even for a brief instant – of how life was for the people who, lost to time, lived on this land. Long before recorded history, Paleo Indians inhabited the upper Spoon River valley in Illinois.[1 Footnote: How the river got its name] These stone age people left behind stone axes, adzes, and dart tips or "arrowheads". Among these pre-Columbian Indian artifacts sprouting in the springtime cornfields along the Spoon River are various other stones with no apparent useful function. Locally called “field stones” these rocks are a nuisance; wearing on the farmer’s implements and tripped over by us arrowhead hunters.
In some fields by the lazy river are ancient campsite mounds laying a few feet above flood plane. It’s around these Indian mounds we find Indian artifacts - arrowheads, tools and flint chips. My cousin Dan found a large, beautiful, and complete stone axe head when we were teenagers – we often cultivated the fields on tractors in early summer. My father had a collection of several arrowhead points he picked up over the years: Sometimes when working a field, a shiny flint point would catch his eye and he would stop the tractor to pick it up. I was in my late forties when Dad died. It was then I became interested in Indian artifacts and so set out to find them: I walk the likely places in 10-foot swaths until I cover the whole area. This simple technique made my collection grow quite rapidly. My wife Delores and I sometimes hunt in other fields – the farmers don’t mind if you pick them up, as long as you ask permission first, don’t drive into the field or step on his crops.
My favorite place while growing up on our small dairy farm was a hilltop overlooking the rich Spoon River bottomland. The hill was cow pasture for as long as Mom could remember but she had the top of it plowed for cropland about 10 years ago. It too had a campsite mound, but was concealed under grass all these years, so wasn't hunted-out like the rest of our fields by visitors in the past. It was ripe for the picking. It’s March of 2002, the beginning of my fifth year as a relic hunter and I was alone this time, anxious to find the top-half of a beautiful multicolored, dove-tailed spear point. I found the bottom-half on the hill the previous spring, so that’s where I headed. It’s there I would come upon a pair of stones that changed my view of the North American Indian forever.
Cracked Nut? Sun-drenched dewdrops spangle the spring morning grass along the edge of the field. The hawk is circling over the misty river bottom now, looking for some unfortunate field mouse foraging in last fall’s leaf litter. I turn my attention back to walking the ground. This hobby had become a walking meditation of sorts. What’s this? A couple of old red rocks. By now, I am quite conservative with bending over. But if I don’t check them out, I’ll wonder what they were for the rest of the day and will have to back-track to find them again. I pick up one of the dirt-caked stones. It has no remarkable features other than sparkling red in the morning sun. I make a mental note of their location and carefully slip both heavy stones into my pack containing a crude projectile-point found nearby on the previous pass.
Later, back at home I wash the red stones with water and a dedicated toothbrush. I study the pieces more intently. Huh. They're heavy for their size. They appear to be crystalline metaquartzite of a deep red color and peppered with black hematite inclusions. The normally clear quartzite is colored bright red by hematite (iron oxide). At first, I thought them to be a millstone and base, but the top piece will not sit flush with the bottom. Next the nutcracker theory was invoked, explaining the fissures in the base and old "hinge fractures" (cracks running parallel to the surface) under the top piece. (This area still supports many hickory and walnut trees.)
Then one evening about a week later, while casually observing the nutcracker set, the hair raised on the back of my neck. I saw her: A kneeling woman holding up an infant (#74 Mother & Child). The baby’s head is against her left shoulder. With trembling hands I reaffirmed this conclusion by re-examining the base. The bottom stone appears to have been chipped to divide her knees and its left side was cleaved – across the natural layers of stone – to make both thighs the same thickness. This was a deliberate attempt by someone long ago to make a stone figurine! I re-assemble the stones and study every detail. Anxiously I reach out to pick up the top stone but stop short, gently nudging it. It rocks left-to-right for several cycles like a dampening spring as if rocking the baby to sleep. This action does not misplace the top stone in the least. To stone age man this would have been quite a novelty.
Curiously, from any angle the work reveals a variety of lingham profiles. This figurine may have been a female fertility (Venus) and/or male potency idol, or a wedding gift to a medicine man (shaman), chieftain, or warrior. The bottom stone has a bowl-like depression from much use. Having been used as a bone-and nut-cracker and left standing to be exposed to hundreds of years of weathering and then buried by time, the bottom stone has acquired a few ancient fissures from water standing and freezing in it's bowl-like depression. But this Indian artifact is beautiful when wet revealing a bright, translucent red stone peppered with occasional black streaks of magnetite crystals. Thousands of years ago when these stones were unsullied, fresh out of the river and dried, they probably looked much like they do today when wetted.
Totems of Stone Since the initial discovery of the Mother & Child nutcracker, my wife Delores and I have found other stones that assemble into even more plausible figurines. Some of these Indian artifacts were found together in the field as if the statuettes were left assembled while the elements buried them in the soil. However, about 70% of these Indian artifacts were found in a shallow washout on the hill, which by all apparent means, may have also been left standing assembled and covered by centuries, nay millennia of rain-washed soil and plant debris. These Indian artifacts are stacking stone figurines which consists of separate pieces because early man did not have a way to effectively carve stone. Carving quartz is a difficult and time consuming task, even today and virtually impossible in the stone age. Many of these stones would have been too dangerous to work without eye protection. It was much easier to stack or otherwise arrange stones to display a concept. Aside from hide-painting, these people had no other medium to express themselves. In Europe, cave painting had been practiced for about 40,000 years. Just a few thousand years ago the Ojibwas of Red Lake, Minnesota left ancient petroglyphs (mostly of giant Thunderbirds) carved or painted onto the soft limestone cliff faces. But there are no known caves or cliffs near our recovery site. So these people used their most abundant resource for artistic expression: riverstones.
Dozens of these pre-Columbian art figurines had been deliberately chipped on the undersides of some of their stones to stack together (a good example is #47 Catfish made of flint) and in one special case to define facial features (#70 Night Sky Maiden – a rare blue & white chalcedony geode, below). The former being the only flint art found so far that appears to have been extensively worked. One chalcedony figurine (#97 Fire Woman) of beautiful carnelian grade has a piece that, like flint tools made of the time, was completely chipped into a woman's head with hair tied into a bun and hollowed out underneath to seat on the torso. The chipped surfaces of all these figurine stones show long-term weathering, smooth edges, and patina, ruling out farm implements and historic man as being the sculptor. In other stones there are matching wear marks, even in deep recesses, revealing the way to stack some of these figurines. It is far from coincidence these “riverstones” - found on a hill with datable arrowheads - stack to produce expressive works of Ice-Age Indian art in recognizable forms: The odds of finding two or more natural stones together, of the same primal material, in clusters that make a statement in human terms, are otherwise astronomical. But how is it possible to find so many matching stones in one place? In most areas of the world only a massive flood or glacier can bring together such a diversity of odd stones from a geological deposit. So, in order to answer the question of where these stones came from we must first look at the geologic history of Illinois. Ice Age Remnants How do we know these stones to be from the Ice Age? Because of the immensity of past glaciers and their scraping effect upon the land, the geology of Illinois is unique. Moraines were scraped and piled ahead of the glacier's leading edge as it pushed southward. In this area, these ancient moraines, once seabed from various eons past, were left behind in receding bands as the glaciers retreated after the last Ice Age. After four glaciations, Illinois has been scraped to the bone with variations in bedrock from the Ordovician Period 500 million years ago to the Cretaceous Period 65 million years ago. It's like the whole state was scraped down as watershed towards the Mississippi River exposing a cross-section of the history of life on Earth. See map below and click to enlarge or go to site Bedrock Geologic Map of Illinois for a full-size view.
So the bedrock around here varies by county and in this particular region Stark, Fulton and Knox countries along the Spoon River, the deep bedrock is from the Pennsylvanian Period 300 mya. Below that is shale from the earlier Mississippian Period 335 mya. There is little exposed bedrock in Illinois, but in this region Pennsylvanian Period bedrock was exposed by the third major ice sheet of the Illinoisan ice age (between 250,000 to 135,000 years ago) when that ice sheet was 1 mile high and stretched across the landscape for as far as the eye could see. This whole region eventually filled with silt from that retreating glacier which is where we get most of our clay subsoil. The fourth and last retreating Wisconsinan ice sheet left our rich fertile topsoil. But this soil is much richer in history. The whole Spoon River region is also loaded with over 2,600 known archeological sites - some dating back to well over 12,000 years ago.
How old are these "pre-Colombian" Indian artifacts? To the northeast Illinois region lies a vast arc of moraines. See map below and click to enlarge. This arc outlines the fourth and last ice sheet, the Wisconsinan of that same ice age (between 75,000 and 13,000 years ago). At the height of the last Ice Age, the Wisconsinan ice sheet only extended down through, and just south of, the Chicago region along a line running south to southeast from Harvard through Rochelle, Princeton, Bloomington-Normal, Effingham, Decatur, and Paris Illinois.[2] However, this region ends just 25 miles east of the recovery site but right at the headwaters of the Spoon. When the final giant ice sheet retreated, even though the Spoon itself was not covered by this fourth and final ice sheet, the Spoon River valley again became a-washed clearing away any riverbed silt or debris accumulated over the previous eons. (The Wisconsinan also provided glaciologists glues on how glaciers transported and deposited material. In New York City, for example, before it was settled in the 1800s, large boulders peppered the landscape, brought down by the Wisconsinan. The last of those boulders can be seen in Central Park.)
Fortunately many of these stones have fossils and we can date to when they were formed. Nearly all these rocks come from a geologic strata of the Devonian mass extinction 354 million years ago. In the seas lived sponges, corals, ammonoids, trilobites, brachiopods, sharks and bony fishes. On the land, short primitive plants appeared along with the first trees only 3 feet high. The first wingless insects crawled from the seas to escape predation by the arachnids. Soon the arachnids followed. Shortly thereafter the first reptiles appeared on land to feed on the insects and the arachnids. There are still many unanswered questions about life on earth and the mass extinction in the Devonian Period[3]. But our core question here is, how did 354 million year old rock end up on the surface of 75,000 year old soil?
Where did these artifact stones come from? Beneath the end moraines of the Chicago-to-Paris arc lies bedrock from the Upper Devonian Period 354 mya with its fossil evidence of that mass extinction. See Bedrock Geologic Map of Illinois above. By the end of the last ice age, the end moraines forming this giant arc contain torn-up rock from this period. Some of these rocks may have been held captive by the Wisconsinan glacier for tens of thousands of years. When the giant Wisconsinan ice field thawed about 13,000 years ago, it dropped its load of stones and silt called "end moraines" which sometimes held back lakes of water. When these moraine "dams" break, the flood washes down rivers and streams. Torrents of melt water swept through the riverbeds throughout Illinois. The residual end moraines in the Chicago-to-Paris, IL arc are evidence that there were at least three major floods throughout the Illinois river system during the last big thaw. Scraped-up Devonian rock of various materials ranging from quartzite, metaquartzite and jasper to amethyst, along with younger Pennsylvanian slate, shale, and sandstone were washed down the headwaters of the Spoon River. The raging torrents ground and polished these stones as if in some giant rock tumbler. All Illinois tributaries of the Mississippi River were awash - the whole Illinois basin was flooded - the state probably looked like a giant lake or inland ocean. As the flood lessened, the waters slowed, clearing the riverbeds of silt and light debris like a giant sluice. The now smooth stones with similar specific gravities had settled into eddy pockets of the Spoon - especially near bends and meanders. After all the flooding was over, parts of the crystal-clear rivers must have been paved in beautiful cobblestones of endless shapes and colors.
Earth Sculpted by Ice Near the end of the Devonian Period some 354 million years ago - long before Earth's Ice Ages - Illinois, as well as much of the Midwestern United States, was at the bottom of a shallow sea teeming with life. The seabed in this region was iron-rich and oily with decayed sea life. (Much of the ancient plants that came later during the Pennsylvanian Period (300 mya) became coal in this region.) The resulting oily mud was buried by tectonic action and baked under immense heat and pressure in the earth’s crust. After the water had steamed away, a smooth, reddish-brown mass rich in silicates was left. Most of this material became microcrystalline jasper. Some of the silicates crystallized into cavities such as geodes but also within Devonian fossils, sometimes replicating the original animal in great crystalline detail. In the eyes of archaic man these stones must have seemed like they were alive - a gift from the mysterious river and Mother Earth’s poetic license. When did these stones become Indian Artifacts?
So what is this common stone we all call "jasper"? Jasper is a term which refers to a member of the chalcedony family of microcrystalline quartz which includes flint, agate and opal. Chalcedony (silicon dioxide - often with some iron and aluminum) itself is an opaque to translucent quartz, usually white with pale blue or gray tint and with a wax-like luster. Chalcedony has been considered a semi-precious stone since the 15th century (See Cloud Woman above) and it is considered a gemstone when it interferes with light such as opal and carnelian. Another member of the chalcedony family is flint a tough, glassy quartz which breaks and chips easily but keeps a sharp edge. Its color scales the rainbow and was the primary material of projectile points, knives and other tools.[4]
Chert is silica-rich and similar to flint but not as glassy – almost dull – and not as tough, but was also fashioned into tools. Agate forms in bands or rings in rock cavities with successive layers growing in parallel rings usually towards the center of some stones. We have found a beautiful red and yellow carnelian agate figurine - #15 Stars Eyes Baby. Quartz has the bizarre property of generating electrical sparks (piezo-electric) when impacted (like in a modern cigarette lighter), squeezed, or rubbed with another piece of quartz. In the dark, some translucent figurines will make bright sparks within the stones when the parts are rubbed together. Judging by what those figurines represent, it's certain early man knew of this strange property. These sparks however are not intense enough to start a fire without a volatile gas like that in butane lighters. Piezoelectric quartz is also the heart of modern electronics.
Microcrystalline quartz such as jasper however, usually comes in varying shades of yellow, brown, and red depending on the amount of iron present in its formation. Jasper, a chalcedony, becomes various gemstones the more it interferes with light. Jasper can also hold fossils such as crinoids. Their stem segments are commonly called "Indian beads" and were drilled in their centers and worn like jewelry by some later tribes of Native Americans. Other such jasper fossils would include small mollusks, sponges and other creatures often in crystalline form. Over millions of years in water saturated mud, some of the carbon and oils from those extinct sea creatures became displaced with silicates which precipitate to form quartz crystals within the fossil cavity. Jasper colored blue, gray or black is from the carbon of ancient sea life and, depending on the quality, is usually waxy smooth and classified as a chalcedony.
In one special case we found a few pieces of a rare chalcedony that can only be described as "decayed animal matter". Despite the grotesque description, it's made up of many colors in a beautiful swirl pattern with fossil remnants. A geologist told me that he had never seen such a chalcedony before so we took the liberty to name it. These "Necro" chalcedony pieces assemble into figurine #77 Great Grandfather's Bones below. (Recently we found another pair of stones made of a lesser grade of this material, 75. Father's Bones, below, but contains citrine crystals for a "third eye".) Figure #71 Harvest Woman is another new stone we named "Salsa" chalcedony. There are other new chalcedonies in our Ice-Age Indian art collection we have yet to name.
Sometimes a large fossil such as a crinoid’s head would form a steam pocket, allowing beautiful quartz crystals to grow within to become a geode or a collapsed jasper nodule. A few have beautifully colored crystals, tainted by various minerals. Many jasper geodes were torn out and some broken up by glacial action and and ended up as riverstone.
Sandstone is a sedimentary rock made predominantly of fine, round grains of quartz (sand). Gritstone is similar to sandstone but made of angular grains and was prized by early man for its sanding abilities. It sparkles quite brightly in sunlight. Quartzite is also a sedimentary sandstone with much larger grains of round to irregular shape. Many of our quartzite figurines are downright beautiful in bright sunlight. Metaquartzite is quartzite that had been heated by the Earth so that the grains are fused together (metamorphic) into a singular crystalline mass, often times with streaks, making the individual grains almost indistinguishable. Without a microscope it is sometimes difficult to distinguish the latter two from each other. Semiprecious gemstones are found in this area and archaic man surely appreciated them. Shiny items were extremely rare and highly prized. Stones of any kind were few and far between after the flooding subsided and plant life took over. Some semi-precious stones such as Carnelian (a fire-red and yellow chalcedony) and Amethyst (a clear quartz crystal colored violet-to-purple by tiny traces of iron) were even more rare. (It was a very popular gemstone in the 1920s.) Citrine is amethyst crystal that has been slowly cooked in the earths crust. It has a clear yellow to golden color and considered valuable to gemstone collectors. Pieces of beautiful petrified wood and dinosaur dung are also occasionally found in this area and we have several specimens of each.
Olivine, which is made primarily of peridot, is a beautiful semi-precious olive-green gemstone colored by iron and magnesium and has a sheen luster. Sometimes olivine can manifest abundantly in quartzite and metaquartzite (see #84 Thunderstorm Bird in "Thunderbirds"). Olivine can also be found in granite (see #90. Green Thunderbolt in "Thunderbirds") and in varying degrees in jasper. Other green rocks may include sedimentary shale and slate, which are usually colored by chlorite, such as #7. Medicine Man, below.
Gneiss (pronounced “nice”) is a hard metamorphic rock found primarily in mountain ranges. The mass of a growing mountain range and the Earth’s heat folds and tempers various minerals such as quartz and the softer feldspar like a steel blade worked by a blacksmith. It is forged into a material much harder than any one of the original components making rocks such as gneiss (see #72. Iron Maiden above) and hornblende (see hornblende mallet in "Shamans"). Gneiss is usually marked with striations or streaks like its cousin schist, a softer and finer grained stone. Hornblende is tougher and has a dark grainy appearance. Hematite is prized as an iron ore and a gemstone. It develops in many rock from granites to limestone. Sometimes it forms shiny crystals called spectacular hematite which describes the black, highly reflective crystals such as #89. Black Beaver. We are offering a beautiful hematite Thunderbird #81. Red Thunder. The River Owl may have prematurely started the Iron-Age by use of this mineral, not just for their Indian art, but as tough and dependable tools.
Patina & Surface Variations Stone patinas on figurines are the result of mineral deposits from soil. This process usually requires great lengths of time. But not all such depositions occur at the same rate for a given square yard of soil. Actually, differences in stone patina can be due to soil conditions that may vary by the inch. For example, a dead field mouse in a burrow may change the soil ph to alkali in a 12” circle for decades.
The amount of water that drains through a patch of soil can also vary by the inch and water balances soil ph but also increases iron oxidation. So some of these pre-Columbian Indian artifacts have parts with slightly different patinas even though they were buried a few inches apart. You will even notice variations in patina on a single stone. Some stones buried in a run-off may have no patina at all. Red-brown iron oxide (rust) stains (from bits of iron in the rich Illinois soil) on stone and flint Indian artifacts are “birthmark” signs of long-term burial.[5] These birthmarks, some as tiny specks, are also a sure sign that Indian artifacts such as arrowheads and tools are genuine.
Other Spoon River Indian artifact pieces are polished with a clear, almost sheen patina as if hand-rubbed smooth by the original owners. Some of these pre-Columbian Indian artifacts have this sheen patina on the head stones only, indicating they may have been carried or held like good luck charms by the owners. Like a photograph, a head stone might have been a reminder of a loved one. Or having the animals' spirit by the head gives the hunter the psychic edge. Fortunately for us, these figurines had their heads – left behind by the River Owl – for what would one day become the final autumn … Endnotes/Bibliography [1] The Spoon River is a meandering river in west-central Illinois, U.S. It rises at the confluence of the West Fork Spoon and East Fork Spoon rivers in Stark county and flows south and southwest to a point west of Lewistown, where it turns southeast, joining the Illinois River opposite Havana after a course of about 160 miles (260 km). It drains an area of some 1,850 square miles (4,800 square km). Spoon River was made famous by the poet Edgar Lee Masters, whose Spoon River Anthology (1915) details the frustrated ambitions of people who lived in the fictitious town of Spoon River—actually a compound of two towns, Petersburg and Lewistown. The river’s name is probably a translation of emiquon, an Illinois and Pottawatomie Indian word referring to the mussel shells they used as spoons. Dickson Mounds, a rich archaeological area, is near the confluence of the Spoon and Illinois. At the beginning of the 21st century, ecological restoration efforts were underway at the confluence. http://www.britannica.com/EBchecked/topic/560894/Spoon-River [2] www.geology.about.com [3] http://www.ucmp.berkeley.edu/devonian/devonian.html [4] Fuller, Sue. Rock & Minerals. New York, NY: DK Publishing, Inc., 2003. Also, National Audubon Society Field Guide to Rocks and Minerals, North American Edition. New York, NY: Alfred A. Knopf, Inc., 1979. Also, National Audubon Society Field Guide to Fossils, North American Edition. New York, NY: Alfred A. Knopf, Inc., 1982 [5] See Homo sapiens in the Americas www.radiocarbondating.com/origins/America.html Unfortunately, we can’t radiocarbon date stone, but its surface does age over extended periods of time and can be distinguished from its freshly broken surface and other interim breaks, the latter usually has smoother edges to varying degrees. PRE-COLUMBIAN Indian stone art ARTIFACTS figurine statue sale For more fine Stone-Age art, click below: |
This site was last updated 05/21/10
