The Schoharie Reservoir
Why Gilboa?
Under Construction
The Nature of a River
Headwaters: A river is fed by a network of tributaries that typically has steep drops in elevation making water move quickly downstream in relatively deep, narrow beds. Engineers have problems in this area because a heavy rain can stress the land while not providing a lot of water. In the three sketches of the Schoharie below, the headwaters would be to the right of the watershed.
Midreaches: As the river enters more level ground, it looks more like a river with larger amounts of water flowing at more moderate speeds in a broader, shallower channel. A good location for a midreach dam is in the left picture, marked with a red “X“
Mouth: The end of a river typically meanders in a flood plain. It has the greatest volume of water, slower speeds, and runs in a broad but shallow bed forming a delta. You rarely see man-made dams in a delta because the land form does not provide a natural bowl for the collection of water.
The locations for dams generally are in a river’s midreach. Engineers will find easier construction on the upstream side due to narrower, deeper channels; but one needing more water would go downstream for additional tributaries at the cost of possibly greater construction costs.
Spoiler Alert: In the case of Gilboa, they found Gilboa downstream from Prattsville (X in the middle picture), and built the dam where they could access additional water from the Bear Kill, Manor Kill, and Steenkill (right picture).
The Situation in 1914
- By the end of 1914, it was apparent that the Ashokan reservoir’s actual production plus Prattsville’s projected flows would not be enough water to run the Catskill Aqueduct at full capacity.
- The Schoharie creek flows west from the Hudson escarpment through Prattsville, and then turns to flow north into the Gilboa valley. The upstream boundary of the valley is marked by the 50-foot tall Devasego Falls.
- The valley itself has a south-north length of about 6 miles, with the village of Gilboa on the east shore perched on a 35-foot-high ledge. The village overlooks the Gilboa rapids at the north end of the valley.
- The valley basin is about 4.5 mi.²
- The Manorkill and Bear Kill waters both pass over tall waterfalls to get into the valley.
- The Steenkill waters join the Schoharie Creek over a long set of rapids just north of the projected dam
- A reservoir created by a dam located at the Gilboa falls has these benefits:
- The shape of the valley was a natural bowl with a depth of over 50 feet.
- The only constructed reservoir walls would be a narrow berm to the east, the dam itself, and a wider berm to the west to encircle Schoharie water.
- The Gilboa location would provide more water than one at Prattsville.
- The under-Hudson aqueduct could be run at full capacity in conjunction with Esopus water.
- The construction and maintenance costs of the relatively small Gilboa reservoir would be less than for a larger Prattsville one.
- Offsetting the above point, the Shandaken tunnel from Gilboa would be about 10% longer from Prattsville.
- Overall, the construction and maintenance costs (reservoir and tunnel) for Prattsville versus Gilboa were about equal.
GILBOA MUSEUM OPEN
12 TO 4 Saturday and Sundays
Memorial Day to Columbus Day.
MUSEUM TOURS-ON-CALL
(607) 588-6894 to set up a tour.
Map for the Gilboa Museum.
September, 2024
• Wednesday, 9/18 at 6: Bobby Curious
click here
After Bobby and refreshments, we will discuss the purchase of the museum property, plans for the addition under construction, and the near-total renovation of the 2024 exhibits. We will also cover next month’s annual meeting, changes to the by-laws, and status of our upcoming board elections.
• Thursday, 09/19, a lunchtime visit by the Mountaintop Seniors, with Museum resource people at each area display.
• Saturday, 9/21, 10 a.m.:
GILBOA NATURALIST PROGRAM
EASY ACCESS!
REGISTER TO ATTEND
(607) 437 7132
kristen.wyckoff@yahoo.com
A field trip to Cairo quarry. The oldest fossil forest in the world, hosted by Dr. Chuck Ver Straeton, Geologist from the NY State Museum.
We will also be shown geological outcroppings in the area.
MEET at Gilboa Museum to depart at 10:00 for Cairo
OR meet at the Cairo Highway Department garage, 755 Route 145, Cairo, NY at 10:40 am.
For information call Kristen Wyckoff at (607) 437 7132 or email her at kristen.wyckoff@yahoo.com
• Saturday, 9/28, 10 a.m. to 4 p.m. Amy Silberkleit print-making workshop
Click here
October, 2024
• Wednesday, 10/16, 6 p.m.:
Annual Meeting of Gilboa Historical Society & election of board members.
• Saturday, 10/19/ 1 p.m. Bob & Johanna Titus talk about the geologic basis of Catskill Mountains art
November, 2024
• Sunday, 11/17, 11 a.m.:
Holiday Boutique at Gilboa Museum.
• Wednesday, 11/20, 6 p.m.: General program TBA.
December, 2024
• Wednesday, 12/11, 6 p.m.:
Raffle and Bottle Auction and a pot luck dinner.
The Board of Gilboa Historical Society meets at 1:00 p.m. on the 4th Wednesday of each month.
Unlinked pages are under construction.√
GHS Facebook page
GilboaMuseum
Gilboa Museum Gift Shop
Gilboa Historical Society
GHS History (Founders, Early Supporters, First Decade, Expansion, Our 21stC)
GHS Activities
GHS Facilities
GHS — Who We Are
Publications and Podcasts
Gilboa Fossils and the Devonian ecology
Gilboa Fossils, a site of the Gilboa Historical Society.
Nicholas J. Juried History Center
Gilboa Village (under construction)
Gilboa Reservoir (under construction)
Communications between you and the Society is key to your enjoyment and our success.
You can type out your information on this form, save it to your desktop, and email it or print it out and send it to the Society (PO Box 52, Gilboa, NY 12076)
Our annual membership is based on an anniversary date established when we process your check. A renewal would simply add 12 months to the projected expiration date, while lapsed memberships are seen as new ones without penalty for the lapse.
Member benefits
- All GHS Newsletters and mailings.
- Gift shop discounts of 10% on all sales.
For donations, please use the QR code
