MOHAWK - Discovering the Valley of the Crystals Copyright 2002Chapter Four
Life Begins Anew
After the ice age the Mohawk Valley was barren. There were no grasses, no shrubs and no trees. Even when glaciers receded, most of the valley was flooded. In the mountains (and atop the highest hills), life began anew as lichens grew on solid rock. These pioneer plants died, rotted in crevices and depressions, and mosses took root. Decayed moss provided the soil for grass, small plants, shrubs and a few trees. (Thousands of years of rotting leaves and trees created the soil that eventually supported a mountain forest.)
In the lower valley, as temperatures increased and glacial lakes and rivers receded, glacial deposits of ground-up rock of every texture and composition encouraged plant growth at a much faster rate. This area became dominated by a great variety of grasses, plants and small trees, providing an abundant food supply for the many large mammals that followed the glacier as it retreated north. Now extinct animals like the woolly mammoth, mastodon, ground sloth, moose-elk and giant beaver moved into this area. Bear, bison, musk ox, moose, deer, caribou, elk and many other animal species also followed the ever-growing food supply.![]()
Although remains of these early inhabitants were not found in abundance in the Mohawk Valley, they were found in peat bogs and other sites throughout New York State. Some nearby discoveries were: mastodon, mammoth and giant beaver near Oneida Lake, and elk just south of the Herkimer County line in Otsego County.
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Mastodon and giant round-tailed beaver
moved into the Mohawk Valley
when life began anew.
The Cohoes Mastodon
The most famous prehistoric animal discovery in the Mohawk Valley was the Cohoes Mastodon.According to a Professor Hall's report:
"In the month of September, 1866 the workmen engaged in excavations for the foundation of a new mill to be erected by Harmony Mill Company, of Cohoes, N.Y., discovered the lower jaw of a mastodon with a single foot bone, resting upon a projection of rock between two depressions or concave walls of small pot-holes, in the margin of what afterward proved to be a larger pot-hole.
"Several thousand of loads of muck and peaty soil with trunks and branches of decayed trees had been removed previous to coming to the level where the jaw was found. . . .
"The discovery of the jaw with a single bone in such a position led to the inference that other parts of the skeleton would be found at the bottom of the pot-hole, could it be reached, and the progress of the excavation was watched with great interest. After considerable delay, the excavation was resumed and the peaty earth was removed from the eastern and central part of the pot-hole, which later proved to be the deepest portion. In the bottom of this cavity, lying upon a bed of clay, broken slate, gravel and water-worn pebbles, and covered with river ooze and vegetable soil, lay the principal parts of the mastodon skeleton. . . the head, with tusks unbroken and undisturbed, was directed to the eastward. . . ."The Mohawk - Codman Hislop 1948
The mastodon's skeleton was displayed in the offices of the Harmony Mills Company and exhibited at the Troy County Fair before the State of New York purchased it for $2,000. In 1867 the almost complete skeleton was assembled and displayed at the "State Cabinet of Natural History" in Albany.
How Do You Hide a Mastodon?When I learned that the skeleton of the Cohoes Mastodon was assembled and displayed at the "State Cabinet of Natural History" in Albany in 1867, I wondered why it wasn't on display at the New York State Museum. I had visited the museum a couple of times in recent years and never saw it. A month or so ago, Gert and I visited the museum and again I looked for the huge skeleton, but it wasn't in any of the exhibit rooms. On the second day of our visit, I stopped at the information desk at the main entrance to pick up some brochures. When I turned around I was astonished to discover the Cohoes Mastodon "under glass" standing between the entranceways. As is often the case, it was hiding right before my eyes.
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If you have never been to the New York State Museum, by all means do so. It is worth a visit just to see the Adirondack and Native Peoples of New York exhibits. The museum is open daily from 9:30 a.m. to 5 p.m. and it's easy to find at the Empire State Plaza in downtown Albany, right across from the State Capitol.From Thruway Exit 24, take I-90 toward Albany and exit onto I-787 South. Take I-787 to the Empire State Plaza exit. From Exit 23, take I-787 north to the Empire State Plaza exit. Visitors parking is available underground under the Plaza, however due to increased security since 9/11/02, photo identification is required. There is also above ground parking near the museum.
(Photo courtesy of NYS Museum)For more information give a click. http://www.nysm.nysed.gov/exhibits/
Man Hunts Giants To Extinction
Man moved into upstate New York around 9,000 years ago. These early inhabitants roamed the hills and valleys of central New York, hunting the animals that lived here. With flint and chert-tipped spears they are credited with hunting the largest mammals to extinction.
(After the ice age, wherever man migrated in the Northern Hemisphere, the largest "ice age" mammals ceased to exist. Man migrated across Europe much earlier than in North America, consequently these animals ceased to exist many years earlier in Europe than they did in North America.)
As the climate became more moderate and trees dominated the region, animals that fed on grass, such as bison, moved west. Others like the musk ox and caribou moved north. Many animals adjusted to the changing climate and dwindling food supplies, but in tree-dominated areas their numbers declined.Seasonal and High-Ground Settlements
The people who lived in this new habitat adjusted by establishing semi-permanent settlements near food supplies such as rivers, streams and lakes where fish and mussels were abundant most of the year or during spawning seasons, or where game was abundant during migration periods or as a result of habitat changes created by fires, floods, blowdowns and heavy snowfall.
Seasonal camps were established near the mouth of the river and the mouths of many of the tributaries, as well as near rapids and waterfalls where fish migration was slowed or halted. Hunting camps existed in areas where huge flocks of passenger pigeons roosted and where whitetail deer yarded in the winter.
Permanent settlements were established when area inhabitants developed gardens that included such foodstuffs as corn, beans and squash. When these plants failed to produce abundantly, gardens were moved to other locations near the village, allowing the previously planted land to rejuvenate. Villages near especially productive soil often remained in the same location for decades.
Some villages were built atop cliffs and
points of land jutting out into tributary valleys.
When soil fertility was depleted nearby and/or pests became abundant, the entire settlement moved to another location in the vast forest. At this new location, trees were girdled, burned at the base until the charcoaled-wood could be chopped away with stone tools. Seeds were planted around tree stumps in the rich soils of the forest floor and crops flourished.
Abandoned fields, reclaimed by the forest, soon provided the shrubs and small trees that attracted deer, turkey and other wildlife---and became productive hunting grounds. Burning large areas of forest during dry seasons created additional hunting grounds. As in the past, temporary hunting and fishing camps were occupied in areas where wildlife, fish and mussels were seasonally abundant.
When competition for the best croplands and hunting and fishing grounds caused increased tribal warfare, the larger settlements were established several miles from the river on high-ground, defendable positions. Quite often a point of land jutting out into a tributary valley provided a village site that was high-ground defensible from three directions. The fourth approach to the village was protected by a stockade of upright logs. See also Cayadutta Creek and Otsquago Creek
Other villages were established on relatively flat-topped hills and surrounded by stockades of two to three rows of upright logs. When the first Europeans came to this area in the early 1600s, they traveled up the Mohawk Valley, noting the Indian settlements along the way. They referred to these stockaded villages as "castles".
See also Indian CastlesWindows to the Past
In the Mohawk Valley there were more than a hundred seasonal and "permanent" villages. Many of these sites were discovered by amateur archaeologists or "collectors" in the 1800s and early 1900s. Most of them are well documented and located between Schenectady and East Canada Creek. For more information on these archaeological treasures, read Mohawk Valley Archaeology: The Sites - Dean R. Snow - 1995.
Although there are settlement sites west of East Canada Creek, they have not been surveyed or made public for various reasons. Except for the small Oneida Village near the mouth of Oriskany Creek, their locations remain "State Secrets" to prevent amateur archaeologists and collectors from destroying their historical integrity.