fodder

Municipal Trash Incinerators in Upstate NY (Google Maps)

These incinerators are sorted by their size, with the largest ones up top, and smallest ones below. These numbers are converted from the yearly numbers of the DEC, to average tons per day, as calculated in standard format for landfills (21-day months).

Incinerators normally are rated by 31-day months, as they typically burn trash year round, unlike landfills which are closed on Sundays and all Major Holidays, and also work only half days on Saturdays. For the sake of comparison, 31-day incinerator tonnages where converted to 21-day landfill tonnages. Tonnages can vary per day, as incinerators are not rated on the tonnage of waste they may accept, but how many BTUs of energy are produced by burning the waste. Incinerators burning larger volumes highly combustable wastes, such as tires or roofing material, must reduce their tonnage to comply with air quality permits.

Incinerated waste produces bottom (unburnable stuff) and fly ash (toxic by-products of combustion captured in various smoke stack filters), which must be disposed at a landfill, so for example, the 1,266 tons per day incinerator in Ondononga County still produces an average of 316 tons per day of ash that is currently sent to the Seneca Falls Landfill off of NY 414.

Also, it should be noted the minimal electricity protection of these facilities. The largest incinerator in Upstate NY, produces only 67 MW of electricity, compared to even modest new power plants such as the new 635 MW Besicorp Natural Gas Plant in Rennselear or the 750 MW Bethlehem Steam Station Natural Gas Plant in Glenmont. All of the incinerators in Upstate NY, produce far less electricity (124 MW) then this one power plant.

Niagara Falls.


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MSW Processed: 3,869 tpd – Ash Generated: 906 tpd – Reduction in Tonnage: 24% – Average Electricity Sold: 24 MW/hr + steam

Westchester County.


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MSW Processed: 2,778 tpd – Ash Generated: 665 tpd – Reduction in Tonnage: 24% – Average Electricity Sold: 67 MW/hr

Onondaga County.


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MSW Processed: 1,266 tpd – Ash Generated: 316 tpd – Reduction in Tonnage: 25% – Average Electricity Sold: 23 MW/hr

Hudson Falls.


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MSW Processed: 688 tpd – Ash Generated: 215 tpd – Reduction in Tonnage: 31% – Average Electricity Sold: 10 MW/hr

Dutchess County.


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MSW Processed: 599 tpd – Ash Generated: 177 tpd – Reduction in Tonnage: 30% – Average Electricity Sold: 5 MW/hr

Oswego County.


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MSW Processed: 290 tpd – Ash Generated: 87 tpd – Reduction in Tonnage: 36% – Average Electricity Sold: 0.6 MW/hr + stream

Kayaking Hitchens Pond & Lows Lake, Aug 13

The Bog River Flow, also known as Lows Lake is a spectacular wilderness/primitive area located in South-East Saint Lawerence County. It consists of two dams, Lows Upper and Lows Lower, that create to massive man-made lakes. It is home to over 100 paddle in campsites along with some amazing views and wildlife.

Here is a downloadable map.

 

Above Lower Lows Dam. Paddling up the “flooded” Bog River, in the lower portion of Bog River flow, right above the Lower Lows Dam. If this area was not flooded by dams, it would be rapids, unaccessible by canoe or kayak.

Above Lower Lows Dam

Chimpmunk Swims. This was taken about a mile above the Lower Lows Dam.

Chimpmunk Swims

Bog River Flow Narrows. The Lower portion of the Bog River, is pretty narrow in part, due to the rocky terrain that it covers. You can easily bottom out a canoe or kayak in these parts, and other parts appear quite deep. There are a couple of paddle-in campsites along here.

 Bog River Flow Narrows

Bog River Open Up A Little Bit. The first mile or so of the Bog River Flow is mostly flooded stream. But as you get closer to Hitchens Pond, it starts to widen a bit.

Bog River Open Up A Little Bit

Entering Hitchens Pond. Just past here, is a hairpin turn, as the flooded River, winds a bit, and becomes a much larger lake, in the form of a series of bays and marshes.

Entering Hitchens Pond

Hitchens Pond. Here things open up quite bit.

Hitchens Pond

Lows Ledge. Here is Lows Ledge reflecting into Hitchins Pond. It’s much larger in person then it appears in this picture, unless you have a very big computer monitor.

Lows Ledge

Railroad Bridge. About two miles into Bog River Flow, you cross under a relatively low railroad bridge. It’s actually about 5 or 6 feet above the flow, and doesn’t feel at all cramped in a canoe or kayak.

Railroad Bridge

Under the Railroad Bridge. This shouldn’t be too bad to clear.

Under the Railroad Bridge

Trees Along Hitchens Pond. This picture can’t even reflect the beauty of this portion of Bog River Flow.

Trees Along Hitchens Pond

Break Time. Drinking all that beer, meant I had to find a place along the Flow to get out, stretch, and take a piss. Things being so boggy and soft in parts, meant there wasn’t a lot of open area to take a break.

Spokey Nights at Camp

Lows Ledge. I’m now about halfway between Lows Lower Dam and Lows Upper Dam, as the ledge reflects beautifully into the lake. It’s a very spiritual thing for sure, paddling along through this lake.

Lows Ledge

Clouds Rolling Out. To the south, it looked still quite cloudy. But there was something quiet spiritual about the area, and quiet vast. Something also spoke to me as being Saint Lawrence County, and as vast as one would expect the biggest county in the state to be.

Clouds Rolling Out

The Channel. The lake turns once again, with beautiful marsh lands along the edge of the lake.

The Channel

Marshy. Portions of Hitchens Pond are quite marshy, and can be tough going, especially if one gets out of the channel.

Marshy

Trees. These trees line the last big turn at Hitchens Pond, where you finally get into the main bay, as you head towards the Upper Lows Dam.

Trees Along Hitchens Pond

Marshland. Along Hitchens Pond as we get closer to Lows Upper Dam.

Marshland

Lows Ledge. Now we are almost up to the portage for Lows Upper Dam. Quite purty I must say.

Lows Ledge

Kayakers Pull Out. You have to pull your boat out of the water, and carry it over the Lows Lake Upper Dam, about a 10 feet elevation, and maybe a 50 foot portage.

2020 US Census Urban Areas in New York State

Bog River Area Pull Off. A lot of people pull out here, for lunch. Or they can be fools, and not use the channel to bottom of the dam, and carry their canoes, an additional 1/4 mile for no real purpose, to get it over the Lows Upper Dam. Not like I would be that stupid, now right? Of course, I just covered my camera with beer, so I shouldn’t be opening my mouth.

These days won\'t last long

Lows Upper Dam. This is the last picture I got for the day, because I dropped the camera in a pool of beer in kayak, and things go wet. Eventually the camera dried out and started to work fine, but for now, we have to go pictureless. From here, the bottom portion of Lows Lake proper, above the Upper Lows dam, is much like the bottom part of Hitchens Pond, narrow, deep channel, that widens up.

Debar Pond

Above Upper Lows Dam. This is the channel above the Upper Lows Dam, which technically is Lows Lake now. About a mile up from here, the lake gets shallow, and you must portage up into the more open Lows Lake main section. Yes, the camera lens has beer in it, that now has to dry out before I can take any more pictures. Nothing until tomorrow. It’s my Friday the 13th luck and stupidity of leaving the camera in the kayak, not in it’s protective case, as I pull out, and spilled beer soaks everything.

Above Upper Lows Dam

Goodnow Mountain

Goodnow Mountain 🗻 🚶‍♀️

A couple of weeks ago I hiked up Goodnow Mountain, on a beautiful clear afternoon, that by the time I reached the mountain it started to cloud up and the humidity started to increase. I had previously in the morning attempted to hike up Giant Mountain in the High Peaks, and wanted to do something easier for the afternoon.

Goodnow Mountain is located at the SUNY ESF (Environmental Science-Forestry) College, just south of the Adirondack High Peaks on NY 28, just to the west of Newcomb. It’s a bit of a drive from the Adirondack Northway from the east or even a little ways from Long Lake to the west, but well worth it for the views.

 Trailhead Sign

About a quarter mile up the trail you pass an interesting tree grown over a rock. This is not as uncommon as you might think in the Adirondacks where the soils are poor and the ground is rocky, and trees seek to put down more roots to pick up nuetrants.

Tree Grown Over Rock

At about 1/2 mile you reach the old woods road that at one time, decades ago, provide vehicular access to the tower for forest rangers. Part of the trail is flat, but then it keeps steeper and erosion is noticable on the old road bed, no longer passable by anything then ATV in an emergency.

Trail Follows Old Woods Road

Rougher Part of the Trail

Further up the mountain, the trail follows a series of boardwalks that keeps most of the trail out of the mud and the muck.

Boardwalk

Then you reach an old abandoned barn, a well, and some interesting old debris like what appears to be a tank from a hot water heater storage unit.

Old Barn on Goodnow

Old Well

Old Water Tank

You ascend a ledge, with some limited views to the south.

South East from Ledge

Then their is a thick planation of White Pines along the trail as you make one relatively short ascent to the firetower.

Thick White Pines

Eventually at the last possible moment, you break through the White Pines to see the Goodnow Firetower, and almost instantly want to start climbing it for the views, unless your suffering from heat exhaustion, then you might want to look for the relatively limited shaded but open sections on the mountain.

Goodnow Firetower

Open Window

SUNY ESF has restored to the Ranger’s cabin, and the porch is a farely popular place to sit, enjoy the view, beat the heat for a few moments.

SUNY ESF Ranger's Station

There are many interesting views from the firetower. Here are the High Peaks looking North, the Vanderwhacker Wild Forest to the east, Kempshall Mountain / Long Lake to the west, and Blue Mountain / Blue Ridge to the South.

High Peaks and Newcomb

Vanderwhacker Wild Forest

South from Tower

Here is a map of the hike.

The Catskill Wilderness Areas

Trees and Mountains

The text of today’s fodder is based on the Catskill Park State Lands Master Plan, as revised in 2008. Maps were rendered by myself, using Quantum GIS and DEC Lands and Forests data.

Big Indian Wilderness

(Formerly Big Indian – Beaverkill Range Wilderness Area)

This wilderness is located in the Towns of Hardenburgh, Denning and Shandaken in Ulster County. It lies generally west of Oliverea and the Frost Valley Road, south of Belleayre Ski Center, east of Seager and Hardenburgh and north of Willowemoc and Claryville. The area ranges in width from 1 to 5 miles, is about 19 miles long and contains approximately 33,500 acres of land. Elevations range from 1,500 feet in McKenley Hollow to 3,840 feet where the state boundary crosses Doubletop Mountain. The mountains in the northeastern portion of the area are quite rugged, while those to the south and west are more characteristic of high hills. Water from the area flows into three New York City water supply reservoirs and the Delaware River Basin. Nine mountains or ridges with elevations of over 3000 feet make up the area.

Peaks

Doubletop* 3,860′
Haynes 3,420′
Big Indian 3,700′
Spruce 3,380′
Fir 3,620′
Eagle 3,600′
Hemlock 3,240′
Balsam* 3,600′
Beaver Kill Range 3,377′

* Maximum elevations given are not necessarily located within the Wilderness Area.

The forest cover is predominantly hardwood mixtures in various associations. Spruce and fir, while present at some of the higher elevations, are less noticeable here than in other Catskill wilderness areas.

Interior facilities consisting of foot trails and lean-tos are generally considered adequate.

Area statistics:

Approximate Area 33,500 Acres
Roads (non conforming) 1.4 Miles
Foot Trails 29.4 Miles
Lean-tos 6
Designated Campsites 5
Parking Lots 5
Public Use (visitors/year) 4,500
Exterior Boundary Line 67 Miles
Minimum Elevation 1,500′
Maximum Elevation 3,840′

Non-conforming uses:

Motor vehicle use of Black Bear Road from the wilderness boundary to Fall Brook Lean-to.

A UMP for this area was completed in June of 1993.

Hunter – West Kill Wilderness

(Formerly West Kill – North Dome Wilderness, Ox Clove Wild Forest, and a portion of the former Hunter Mountain Wild Forest)

The unit generally lies within the following boundaries: New York State Route 42 on the west, the Shandakan Wild Forest and NYS Route 28 to the south, and NYS Route 214 on the east. The northern extent of the unit is County Route 6, and continues along a line 100′ parallel to, and south or east of, the edge of Spruceton trailhead parking area and the centerline of the Spruceton Truck Trail, to the junction of the Colonel’s Chair Trail. A corridor, 100 feet either side of the center line of the Spruceton Truck Trail, from the Colonel’s Chair Trail to the summit of Hunter Mountain, culminating in a circle 175′ in radius from the center of the chimney on the observer’s cabin shall be within the Rusk Mountain Wild Forest.

The unit contains approximately 27,000 acres of land, and inside it’s boundaries are found the named mountain peaks of Balsam, Sherrill, North Dome, West Kill, Sheridan, Hunter and Southwest Hunter. Hunter Mountain is the second highest peak in the Catskills at 4,040 feet, and portions of it’s summit, along with a fairly extensive area on the summits of West Kill, North Dome and Sherrill Mountains are within the Catskill High Peaks Bird Conservation Area, and are of special significance in that they provide habitat for high elevation spruce-fir inhabitants such as Bicknell’s Thrush and the Blackpoll Warbler, among others.

There are currently two lean-to’s on the unit, the Diamond Notch lean-to located just off the Diamond Notch Trail, and the Devil’s Acre Lean-to off of the Devil’s Path Trail. Waters from this unit drain into Schoharie and Esopus Creeks and then into the Schoharie and Ashokan Reservoirs, which are in the New York City water supply system.

Area statistics:

Approximate Area 27,000 Acres
Foot Trails 18 Miles
Lean-to’s 2
Parking Lots 5
Minimum Elevation 920′ Maximum Elevation 4,040′

Indian Head Wilderness

(Formerly Plateau Mountain – Indian Head Mountain Wilderness Area)

This wilderness is located in the Town of Hunter, Greene County and the Towns of Saugerties and Woodstock, Ulster County. It lies generally west of the east boundary of the Catskill Park, south of Platte Clove, east of Devil’s Tombstone Campground and north of Lake Hill and Shady. The area ranges from 1 ½ miles to 3 ½ miles in width, is eight miles long and contains approximately 16,800 acres.

Elevations range from 900 to 3840 feet and the four major mountains in the area are visible against the skyline from all directions. Echo Lake, the only natural lake in a Catskill wilderness, is located in the east-central portion of the area. Water from this eastern section flows into the Kingston and Saugerties water supply reservoirs, while drainage from the central and western section flows into two New York City water supply reservoirs. Six named mountain peaks over 3,000 feet in elevation dominate the area.

Peaks

Plateau 3,840′
Indian Head 3,573′
Sugarloaf 3,800′
Olderbark 3,440′
Twin 3,640′
Plattekill 3,100′

The forest cover varies from extensive oak stands on the eastern most slopes to mature spruce-fir on top of Plateau Mountain. An excellent mature stand of northern hardwood and hemlock occupies the slopes south of the Saw Kill.

Echo Lake, unique to the Catskill wilderness, is very popular for undeveloped camping. A small number of scattered primitive tent sites with fire rings have been established and public camping is limited to their capacities.

Public access is provided by several foot trails entering the area, including the old road from Meads to Overlook Mountain.

Area statistics:

Approximate Area 16,800 Acres
Roads 6.6 Miles
Foot Trails 24.1 Miles
Cross-country Ski Trails 5.6
Lean-tos 3
Designated Campsites 10
Parking Lots 1
Public Use (visitors/year) 8,000
Length of Boundary 33 Miles
Minimum Elevation 900′
Maximum Elevation 3,840′

A UMP for this area was completed in October of 1992.

Slide Mountain Wilderness

(Formerly Slide Mountain – Panther Mountain Wilderness Area)

This wilderness is located in the towns of Shandaken, Denning and Olive in Ulster County. It lies generally south of NYS Route 28, west of West Shokan, north of the Peekamoose Road (County Route 42) and east of the Frost Valley Road (County Route 47). It surrounds the Woodland Valley Campground and abuts the Sundown Wild Forest to its south. This area ranges from 1 to 10 miles in width, is about 13 miles long, and contains approximately 47,500 acres of land. The wilderness boundary is 118 miles long.

The terrain is rugged and steep with elevations ranging from 1,100 to 4,180 feet. All water draining from the area eventually reaches three New York City water supply reservoirs by way of the East and West Branches of the Neversink River, Rondout Creek and Esopus Creek. Twelve named mountain peaks with elevations over 3000 feet exist in the area. Of these, six may still be considered trail-less to the extent that they have no marked and maintained trails.

Peaks with Trails

Slide 4,180′
Peekamoose 3,843′
Cornell 3,860′
Wittenberg 3,780′
Table 3,847′
Panther 3,720′

Trail-less Peaks

Lone 3,721′
Rocky 3,508′
Friday 3,694′
Van Wyck 3,206′
Wildcat 3,340′
Balsam Cap 3,623′

The forest cover consists of nearly every possible mixture and association of hardwood and softwood trees native to the mountain region. While hardwoods predominate higher elevations are often covered with red spruce and balsam fir.

This area receives more public use than any other Catskill wilderness. Superb vistas are found on Slide, Wittenberg, Cornell, Giant Ledge and Panther Mountains. Access via foot trails is available from the north, south, east and west.

Area statistics:

Approximate Area 47,500 Acres
Foot Trails 35.3 Miles
Lean-tos 3
Parking Lots 10
Designated Campsites 29
Public Use (visitors/year) 23,000
Length of Boundary 118 Miles
Minimum Elevation 1,100′
Maximum Elevation 4,180′

A UMP for this area was completed in March of 1987 and revised in October of 1998.

Windham – Blackhead Range Wilderness

(Formerly Blackhead Range, and North Mountain Wild Forests, and portions of Windham High Peak, and Black Dome Valley Wild Forests)

The combination of these Wild Forest areas creates the Windham – Blackhead Range Wilderness Area, which lies within the Greene County towns of Cairo, Hunter, Jewett, Windham and Durham. The classification of these former Wild Forest areas was changed to Wilderness because their combined area comprises approximately 17,100 acres and contains rugged, high elevation land that clearly exhibits wilderness character. This newly classified area has seven named mountain peaks over 3,000 feet in elevation.

They are:

Peaks Black Dome 3,980′
Windham High Pk 3,520′
Blackhead 3,940′
Stoppel Point 3,420′
Thomas Cole 3,940′
Burnt Knob 3,180′
Acra Point 3,100′

The unit also contains six unnamed peaks over 3,000 feet, which range from 3,040 feet to 3,540 feet in elevation. Of the five highest peaks in the Catskills, three – Black Dome, Thomas Cole and Blackhead – are in this unit. This concentration of 13 peaks over 3,000 feet, within an area of approximately 28 square miles, with limited access, structures and improvements (30 miles of maintained foot trails and two lean-to’s) make the Windham – Blackhead Range Unit an area with excellent wilderness character.

A fairly extensive area of old growth forest can be found on this unit at the higher elevations, along the ridge stretching from an area west of Thomas Cole Mountain to Blackhead Mountain, and on Windham High Peak. The presence of this old growth forest, with its distinctive flora and fauna, add to the wilderness character of the unit. The unit also includes the headwaters of the Batavia Kill and, to the south over the Blackhead Range, the headwaters of the East Kill. Both of these rivers flow into Schoharie Creek, and are an integral part of the New York City Watershed system.

The western boundary of this unit shall be the east side of the Elm Ridge Trail, Black Dome Trail leaving it within the Elm Ridge Wild Forest, continuing north along the drainage to the Catskill Park boundary. The southern boundary of the unit shall be the Escarpment Trail approximately one half mile south of Stoppel Point to a point on the Escarpment Trail where it comes closest to the eastern Forest Preserve boundary. Both North Point and Stoppel Point will be within the Wilderness area. Lands to the south of the south edge of the Escarpment Trail in this area, will be in the Kaaterskill Wild Forest.

Because the Windham – Blackhead Range Wilderness surrounds the smaller Colgate Lake Wild Forest Unit, and because they are linked together by public use, the Unit Management Plans for the two units shall be contained in one document.

Area statistics:

Approximate Area 18,0000 Acres
Foot Trails 30 Miles
Lean-tos 2
Parking Lots 1
Minimum Elevation 980′
Maximum Elevation 3,980′

Why You Should Sleep Until Noon During Black Fly Season

Black flies — there really is only one solution to them: don’t be hanging out until they are gone for the night. That means waiting for darkness to come over the land. Then the party can get started.

Getting Eaten Alive By Black Flies

Black flies aren’t out all night. So that’s the best time to up and own doing things. Like cooking dinner, drinking beer, and hanging out by the campfire. There is nothing wrong with staying up all night during black fly season, because the days really aren’t that wonderful, if you don’t like getting eaten alive.

Campfire

Granted, in the darkness, you are somewhat restricted in what you can do. But bring a flashlight, and hell, maybe a bunch of Christmas lights, party lights, and big bright 100-watt equivalent florescent lights, and pretend it’s day light. It’s also cooler, and generally much nicer in then in the day time.

Waking Up Deligted to See the Sun

During black fly season, the whole purpose of the day is to be sleeping, and recovering from the hang overs of the previous night.

Don’t Forget to Vote in School Board Elections

Many of us forget about School Board Elections.

They are in a strange time of year, the middle of May, as many of us are thinking more about our summer plans, rather then critical questions of local government spending. School board elections, as local elections, are poorly covered by the news, and often are uninteresting. You may no longer attend high school, and you may not have kids in school. Yet those are not good reasons for not voting.

School Board Elections, School Budget Vote, and Library Budget Vote are all important things to vote on for several reasons including:

  • Low turn out, local elections mean your vote can change results easily.
  • Your decision hits your pocketbook directly, especially if pay property taxes.
  • Only chance to directly comment on government spending — should we invest more in our public schools or further increase the crushing tax burden on working folk?

None of us have perfect information. Many years when I vote in school board elections, I don’t even know whose running for school board, and leave those ballots blank. If your concerned about government spending and waste, or think schools and the students being educated are getting cut too much, then either vote Yes or No. It’s that simple.

Don’t Forget to Vote!

Gasoline is Dangerous

I don’t know how many times I’ve told people that if you want to play with fire, never mess with gasoline. Diesel. Fine. Plastic. Whatever, just don’t burn yourself when you get melting and burning plastic on your skin. Blowing up aerosol cans. Fine, just make sure not to start a brush fire when you send partially burnt trash over your head. But gasoline — be aware!

What makes gasoline such a dangerous product is that it’s vapours are very explosive. Gasoline is relatively easy to vaporise as a fuel — you can vaporise it just by pouring it out of a container. And that vapour is very explosive. That’s why we use it as an engine fuel. It’s really easy to burn, and to burn cleanly under controlled conditions.

 Burnin\' Wood

Yet, you figure out the sheer amount of power that a gasoline engine gets out of minuscule amounts of gasoline, you can understand why it’s so readily explosive. The explosion can not only provide controlled propulsion, but it can also blow up and send objects in towards your face, and that can be quite painful, to say nothing about the burns from the flash of fire.

Few common things are as dangerous as gasoline. Diesel doesn’t vaporise under normal conditions. You have to heat up diesel and apply compression to it for an explosion to occur. It’s relatively safe to pour diesel on some trash to get it burning. Diesel will burn, and it will burn hot, once it’s caught from something else burning, but it won’t explode.

 Burnt

Gasoline in contrast does vaporise under normal conditions. It’s vapors will explode with an incredible amount of force. Pour gasoline on some trash, let it sit for a few seconds, toss a match at it from a half a dozen feet away, and boom. Hope you don’t have anything that will act as shrapnel coming towards you. And don’t do it in any kind of enclosed space that is likely to contain the explosion — as much fun as it is to watch.

If your ever working on anything that burns gasoline or similar fuel like Coleman fuel. Be very careful, if you care about your life, and don’t like visiting the Westchester Burn Unit.

  • Always check for fuel leaks with soap before lighting a white gas stove or other similar device
  • Don’t use gasoline to start fires, especially in enclosed spaces, or with anything you don’t want to hit you when it explodes.
  • Never pour gas in anything near flame or spark.

Camp Stove

These are all things we’ve learned as children. Yet the sheer fun of watching shit burn and explode, sometimes gets the best of us as adults. Just please remember, that gasoline goes boom and you don’t want to be in path of boom.