Jayville, New York

Last updated
Jayville Centuri
Hamlet
USA New York location map.svg
Red pog.svg
Jayville Centuri
Location within the state of New York on the East side of the river
Coordinates: 44°9′15″N75°11′20″W / 44.15417°N 75.18889°W / 44.15417; -75.18889 Coordinates: 44°9′15″N75°11′20″W / 44.15417°N 75.18889°W / 44.15417; -75.18889
Country United States
State New York
County St. Lawrence
Elevation
1,121 ft (341 m)
Population
 (2000)
  Total0
Time zone UTC-5 (Eastern (EST))
  Summer (DST) UTC-4 (EDT)
Area code(s) 315

Jayville was a hamlet located in the southwest part of St. Lawrence County, New York, in the United States. The hamlet started as a mining community in 1850 on what eventually became the Carthage and Adirondack Railroad. [1] Its existence was short lived as its non-favorable mineral composition and difficult ore availability was abandoned in favor of neighboring Benson Mines, located 14 miles (23 km) down the railroad to the east. [2] After mining stopped in the community, other industries such as saw mills kept the population busy. Ultimately, these business were short lived. A further attempt to reopen the mines in 1914 failed and an eventual fire ended the existence of the hamlet of Jayville. [3] Today remnants of the hamlet can be found off the now abandoned railroad station located on New York State owned land [4] southeast of Harrisville on Jayville Road.

Contents

History

1850-1880: According to old reports, the Jayville property was opened for iron ore in 1854 by Z.H. Benton. Little ore was removed at that time. In 1886, upon completion of the Carthage and Adirondack Railroad to Jayville, the property was leased from Beton by the Bryon D. Benson interest. Operation by the Bensons, under the name of the Magnetic Iron Ore Co, continued to 1888, in which year the property was abandoned in favor of the deposit at Little River (now Benson Mines) [5]

1880s: One of the most significant events if Jayville history was in 1884 when New York State commissioned the building of the Carthage and Adirondack railroad to run from Carthage to Jayville. This railroad was completed in 1887. Later in 1889 the railroad was continued to Benson Mines. [6]

Mining thrived in the 1880s. Prior to 1889, the Megnetic Iron Ore Company had expended a large amount of money in building a railroad to the mines at Jayville, NY, developing them and securing the property at little river, before it was finally discovered that ore of good quality, in its natural state, could not be taken from the mines in paying quantities. It was therefore decided by the company that the only thing to be done, to save the investment in these properties, was to establish a large concentrating plant at Little River – now Benson Mines – and to extend the railroad to that point. [7]

1890s: During the 1890s sawmills were opened in the hamlet of Jayville. Sawmills ultimately replaced the mining activity in Jayville. In 1892, costly litigation over mineral rights and railroad tariffs that traveled through private land owned by Proctor (Proctor vs Benson) ultimately stopped mining in the hamlet. [8] Throughout the 1890s and through the early 1900s, Jayville remained in existence surviving on Railroad traffic and saw mill industries.

1900s: In 1914, the mines were attempted to be reopened; however this attempt was short lived and activity in the hamlet slowly wound down to its eventual demise in history. [9] Mr. Howard Hughes bought the mines property and sunk a lot of money pumping the water out of the old pits. He operated at a loss for about 3 years and then closed them. The mother load of ore hiding under Twin Ponds was the goal, but water kept seeping in and filled them as fast as they could be pumped out.

1940s: In 1941 the Jones & Laughlin Steel Corp made geologic, dip-needle and Hotchkiss superdip surveys of the area on a scale of 1:600 and drilled eight inclined holes whole total length was 2,366 feet. Most of the diamond-drill holes were 200 to 250 feet deep, but several were 350 to 450 deep. As a result of this exploration, the company concluded that the property was of little interest as a potential producer of lump ore. [10]

Railroad

Railroad Companies

Rail Station

Jayville Station in 2005 JayvilleStation.jpg
Jayville Station in 2005

Location

A railroad station existed at Jayville. The Jayville stop on the railroad was labeled as 4E. [12] Its exact location was plotted by the USGS in 1913. That location is: 44°9′15″N 75°11′20″W. [13]

Workers

As was customary for the times a telegrapher was stationed at Jayville. The position of telegrapher was a union job, organized in New York State under the Order of Railroad Telegraphers. In 1913 it was noted that Brother Seamen was the telegrapher for the hamlet. [14]

Train Schedule

As published by the Rand-McNally in 1902, there were three trains that ran through Jayville. (437,487,451) The train schedule was published by the New York Central & Hudson Railroad and posted under the Carthage and Adirondack Branch. [15]

1902 Jayville Train Schedule.png

Mining

Early Mining/Furnaces

The earliest mentions of Ore being removed from Jayville date all the way back to 1833. At that time a blast furnace was built by the Fuller brothers at Fullervulle, southwest of Edwards. It operated on ores from Little York mine, bog ores from Edwards, and magnetic ores from Jaayville and Clifton. This furnace was closed in 1882. [16]

The next know uses of Jayville Magnetite was in 1855. IN 1846 the Alpine Host-blast Charcoal furnace was built. This furnace was owned by Z.H. Benton of Oxbow. Its location was southwest of Antwerp on the outlet of Boney Lake. 1,218 tonnes of iron out of red hematite ore from Kearney or Indian Lake mine, mixed with black magnetite from the Jayville bed was used at the furnace. [17]

Also around this time speculation of an abundance of magnetic iron ore was starting to build at Jayville. At the time in the 1850s over 100 tons were taken from the Jayville Mines. [18]

One of the most significant figures in increasing mine activity at Jayville was Z.H. Benton. It was said that the Carthage & Adirondack Railway owes its existence to Colonel Benton as he was unceasing in their errors to establish a link to the Jayville mines. [19]

Mineral Composition

The ore quality that was taken from Jayville was said to be of the utmost quality. Some very rich specimens of magnetic ore from the Jayville mine were shown in the Main Building at the May 5th, 1877 Iron Ores of the United States Philadelphia Exhibition. [20]

Four specimens represent the Jayville Mine; taken June 22, 1881: [21]

  1. Magnetite, pyroxene (40857)
  2. Magnetite, pyrite (40872)
  3. Magnetite (40855)
  4. Magnetite, (40860)

The mine has yielded several tens of thousands of tons of magnetite ore; associated with the magnetite ore are supergene hematite, vonsenite, Fluorite in dar mica skarn, pyroxeneamphibole skarn and quartz-bearing amphibole skarn. Parts of the amphibole skarn and the iron ore are rish in Fluorite; this type of skarn is as much as a few feet thick and ranges from 20 to 60 percent fluorite. If the iron deposit is mined again, Fluorite and vonsenite should be considered as coproducts. [22]

New Mining Techniques

Because of the magnetic properties of the ore in Jayville, new technologies were used, most notably the Magnetic Separation of Iron Ore. In 1895 the Ball-Norton electro-magnetic separator was used in a number of plants built and experiments made for magnetic separation, notably those at Benson Mines in St. Lawrence county, New York; at the Jayville mine and at the Mineville in Essex county. [23]

Mine Layout

In Jayville, the ore occurrences presents a phase quite dissimilar from that of Benson Mines and more like the magnetite deposits on the east side of the Adirondacks. There are innumerable shoots, lenses and irregular bunches in which the magnetite is found showing sharp boundaries in contact with the wall rock. The latter is for the most part a hornblende-biotite gneiss of sedimentary appearance. The horizon of the ore lie close to the contact of the gneiss with a red pegmatitic hornblende granite. Outcrops of the granite occur to the north and east within short distances where they break through and cut off the gneiss area in such a way that their intrusive character is plainly evidenced. In some of the openings the granite can be seen in immediate contact with the ore. The openings are on the northeastern and northwestern slopes of a low ridge of gneiss that rises just west of the railroad. The pits nearest the station are Hart no 1 and no2 of which the first is said to be 300 feet deep following a shoot 20 feet wide and 10 feet thick. Hart no2 is much shallower. At the northeastern end of the ridge where it curves to the west are the pits called New York no 1 and no 2, both of inconsiderable depth. Benson no1 farther to the west is reported by Smock to have depth of 250 feet on the incline; of its two levels the upper is about 25 feet long and the lower driven at a point 60 feet from the bottom of the slope runs off in a southerly direction for 160 feet and then north 60 feet. The pit supplied most of the shipping ore. Between Benson no 1 and no 2 an adit has been excavated into the hill on a lead which in the interior develops into a lens some 60 or 70 feet long and 20 feet wide. The Fuller and Essler pits are located at the extreme west, the former being opened on a pod of ore 50 feet wide, dipping 45 degrees west.

Jayville Mineral Composition by Mine Shaft Jayville Mine Shaft Production.png
Jayville Mineral Composition by Mine Shaft

The distribution of the ore in disconnected bodies which pitch and strike in all directions has probably resulted from the intrusion of granite. The bodies occupy approximately the same horizon and have the aspect of an originally continuous band which has been disrupted and faulted. The intrusion has exercised also a metamorphic influence upon the deposits shown by the abundance of garnet and hornblende that often replace the magnetite almost completely. Well-developed titanite crystals of unusual size are found in the contact zone. The analysis taken below from Putnams report, gives the composition of the Jayville ore. It was made from a sample of 500 tons mined in 1880 and shipped to the furnace at Alpine. [24]

Jayville Quarry Materials Jayville Quarry Materials.png
Jayville Quarry Materials

More information on the mine layout and shaft coordinates can be found in the Geological Survey professional paper, Volumes 376-377

Most Recent Prospecting

When Lump ore was at a premium, just before WWII, the Jayville property seemed promising enough to warrant exploration. Accordingly, in 1941 the Jones & Laughlin Steel Corp made geologic, dip-needle and Hotchkiss superdip surveys of the area on a scale of 1:600 and drilled eight inclined holes whole total length was 2,366 feet. Most of the diamond-drill holes were 200 to 250 feet deep, but several were 350 to 450 deep. As a result of this exploration, the company concluded that the property was of little interest as a potential producer of lump ore. [25]

In the winter of 1947, USGS performed a study on the Jayville mines. The [USGS] found an unidentifiable metallic mineral in ore from two drill holes at the Jayville [magnetite] deposit. The striking optical properties of the unknown set it apart from other metallics that had been investigated mineragraphically. It was thought for a while that the unknown might be ilvaite. In the spring of 1950, the USGS investigated the unknown. [26]

Saw Mills

In the early 1890s, as mining was starting to be less fruitful as once anticipated, the timber on the land started to attract the attention of investors. Throughout the course of the hamlet's history, three separate investment groups operated sawmills in Jayville.

Post and Henderson Company

The partnership of Robert G Post and Washington J Henderson made its first venture into the Adirondacks in the early 1890s with a small sawmill in Jayville. Production in the mid-1890s was four million board feet of lumber yearly. However, once again, Jayville lost out to Benson Mines as in 1898 a much larger sawmill was built in the village of Benson Mines. In 1900 the two partners formed the post and Henderson Company. [27]

The day-to-day operation of the mill was run by W.J. Henderson. The superintendent at the Post & Henderson was John Peter Kirch. His yearly salary was $1,200. John Peter Kirch would later become famous for running away on his family for a younger woman, Mrs. Hattie Covey, who was then tarred and feathered for her actions. [28]

J. S. Demott

J.S. Demott, who was from Oswego, in 1894 operated a Steam powered saw mill in Jayville. [29]

Mecca Lumber Company

In 1903 Nellis, Ames & Swift who ran an old and substantial lumber concern in Utica, NY purchased a timber tract of 7,000 acres around Jayville. The actual location of the Mill was Kalurah, NY. They immediately begin the erection of a large steam saw mill at a convenient point near the center of the purchase, building a railroad switch from the track of the Carthage and Adirondack Railroad at Jayville to the plant. The mill was said to have been built using modern construction equipment and large capacity and was operated wholly in the manufacture of hardwood lumber. This mill was touted to have been equipped band saws. [30]

The mill was built on a settlement known as Little Mill. The company renamed the settlement Kalurah, named after a Masonic Lodge in Binghamton. The sawmill was relatively small, producing about 30,000 board feet of logs daily. However, in 1907, the mill was the 7th largest producing mill in New York State. [31] The Mecca Lumber company produced a large quantity of railroad ties using the hardwood on the land. The Mecca Lumber Company ceased operation in 1910. On May 24, 1910, The New York Central Railroad company petitioned New York State to discontinued freight and ticketing service at the Kalurah station, thus ending the majority of mill functions. [32] The sawmill was operated by Alfred Kilbourne up until 1920 when the land was sold to the State of New York for $45,000. [33]

Education

KalurahSchool-Jayville.png

In 1887 school district No 10 was formed in Pitcairn for Jayville students by George A Lewis, School Commissioner. He wrote to NYS in a letter, "In August last, I issued an order forming school district No 10, in the town of Pitcairn, to meet the educational wants of the mining village known as Jayville." [34]

Later in the 1890s, this school was known as Jayville School No 1. During this time George W. Backus was a trustee of the Jayville school. Mr. Backus eventually married Miss Pina Mae Seelya who was a teacher at the local school. [35]

After the closing of the Jayville mines, the one-room school building was moved down the tracks to Kalurah, where it remained there until 1940.

Religion

In the early 1880s the St. Francis Solanus parish was formed in Harrisville, Ny by Rev. E. C. Laramee. Under Jeremiah Manning, Jayville was a mission. In 1907 Harrisville, Kalurah, Natural Bridge and Lewisburg formed a parish. The parish territory included the mission at Fine and Taleville, each of which had a church, and the stations at Jayville, Edwards and Fullerville. [36]

Hunting

Hunting was a way of life for local residents of Jayville. In 1902, NYS conducted a deer population study in the growing response for information on large animals of the Adirondack Region. In 1902 deer shipments were measured using carcase shipments with the aide of the American and National express Companies. During this time 30% more deer were secured by hunters in the area. A general rule was used that 4 deer were killed in the woods for every one that shipped out by rail. In 1902, a total of two deer carcases were shipped out of Jayville, while neighboring Harrisville shipped 35. Note that in Harrisville that year, a 253 lb deer was taken from the region. It was noted that the Adirondack deer, when properly protected, will develop a size and weight fully equal to or surpassing that of species in any other locality in North America. [37]

Jayville Tar and Feathering

Unfortunately, Jayville's most nationally acclaimed moment was the result of an lustrous affair that resulted in a public tar and feathering of a female resident, Mrs Hattie Covey. The story was so sensational that it was published in the New York Times on July 31, 1895.

As the story goes, Mrs Covey who was married jumped a train out of town with Saw Mill Superintendent John Kirch, who was married and had children. It was rumored that the two ran off to Ohio. After two months Hattie Covey returned to Carthage to visit her parents. Coincidence would have it that Mrs. Kirch was also on this train. Later that evening two men showed up at Hattie's mothers house and threatened to tar and feather Hattie Covey if she did not leave town immediately. That next morning, Mrs. Covey, her mother and brothers went to Pircairn to a judge to swear out a warrant for arrest of the two men who had threatened her the night before. The family then returned to Jayville that night. The Daily Journal of July 31, 1895 then explains what happened next:

When the train stopped at the station, the mother and daughter got off of the rear platform and walked to the front of the train, where they were suddenly surrounded by a crowd of men who seized the daughter and took her into the railroad freight house, where they stripped her. There was a crowd of women there, dressed in men's clothes and with blackened faces. The men held the women down on the floor, while the women applied the tar and feathers with a paint brush, completely covering her with the stuff, after which they left her. She was taken to her mother's house, where a physician was called. It was found that one arm and a number of ribs were broken. It is said to be doubtful if she lives.

Within a few days the attackers of Mrs Covey were arrested and a trial was held for the five known attackers. [38]

The story was so popular that it reached news papers as far away as Utah. [39]

Notable residents

Jayville Junction (play)

Title Jayville Junction: An Hour and a Half of Comedy in a Railroad Depot Denison's specialties Author Harry Lee Newton Publisher T.S. Denison, 1906 Length 38 pages

Related Research Articles

Ore Rock with valuable metals, minerals and elements

Ore is natural rock or sediment that contains one or more valuable minerals, typically containing metals, that can be mined, treated and sold at a profit. Ore is extracted from the earth through mining and treated or refined, often via smelting, to extract the valuable metals or minerals. The grade of ore refers to the concentration of the desired material it contains. The value of the metals or minerals a rock contains must be weighed against the cost of extraction to determine whether it is of sufficiently high grade to be worth mining, and is therefore considered an ore.

Limonite Hydrated iron oxide mineral

Limonite is an iron ore consisting of a mixture of hydrated iron(III) oxide-hydroxides in varying composition. The generic formula is frequently written as FeO(OH)·nH2O, although this is not entirely accurate as the ratio of oxide to hydroxide can vary quite widely. Limonite is one of the three principal iron ores, the others being hematite and magnetite, and has been mined for the production of iron since at least 2500 BP.

Lyon Mountain, New York Census-designated place & hamlet in New York, United States

Lyon Mountain is a hamlet and census-designated place located in the town of Dannemora in Clinton County, New York, United States. The population was 423 at the 2010 census.

Clifton, New York Town in New York, United States

Clifton is a town in St. Lawrence County, New York, United States. The population was 751 at the 2010 census. The town takes its name from a mining company.

Iron ore Ore rich in iron or the element Fe

Iron ores are rocks and minerals from which metallic iron can be economically extracted. The ores are usually rich in iron oxides and vary in color from dark grey, bright yellow, or deep purple to rusty red. The iron is usually found in the form of magnetite (Fe
3
O
4
, 72.4% Fe), hematite (Fe
2
O
3
, 69.9% Fe), goethite (FeO(OH), 62.9% Fe), limonite (FeO(OH)·n(H2O), 55% Fe) or siderite (FeCO3, 48.2% Fe).

Mesabi Range Mining district in northeastern Minnesota

The Mesabi Iron Range is a mining district in northeastern Minnesota following an elongate trend containing large deposits of iron ore. It is the largest of four major iron ranges in the region collectively known as the Iron Range of Minnesota. First described in 1866, it is the chief iron ore mining district in the United States. The district is located largely in Itasca and Saint Louis counties. It has been extensively worked since 1892, and has seen a transition from high-grade direct shipping ores through gravity concentrates to the current industry exclusively producing iron ore (taconite) pellets. Production has been dominantly controlled by vertically integrated steelmakers since 1901, and therefore is dictated largely by US ironmaking capacity and demand.

Taconite Variety of iron-bearing sedimentary rock

Taconite is a variety of iron formation, an iron-bearing sedimentary rock, in which the iron minerals are interlayered with quartz, chert, or carbonate. The name "taconyte" was coined by Horace Vaughn Winchell (1865–1923) – son of Newton Horace Winchell, the Minnesota State Geologist – during their pioneering investigations of the Precambrian Biwabik Iron Formation of northeastern Minnesota. He believed the sedimentary rock sequence hosting the iron-formation was correlative with the Taconic orogeny of New England, and referred to the unfamiliar and as-yet-unnamed iron-bearing rock as the 'taconic rock' or taconyte.

Burden Iron Works United States historic place

The Burden Iron Works was an iron works and industrial complex on the Hudson River and Wynantskill Creek in Troy, New York. It once housed the Burden Water Wheel, the most powerful vertical water wheel in history. It is widely believed that George Washington Gale Ferris Jr., inventor of the Ferris wheel, had occasion to observe the wheel while a student at Rensselaer Polytechnic Institute. The iron works site was listed on the National Register of Historic Places as an archaeological site in 1977. The Burden Ironworks Office Building was previously listed in 1972.

Lehigh Crane Iron Company Defunct ronmaking firm in the Lehigh Valley, USA

The Lehigh Crane Iron Company was a major ironmaking firm in the Lehigh Valley from its founding in 1839 until its sale in 1899. It was founded under the patronage of Josiah White and Erskine Hazard, and financed by their Lehigh Coal & Navigation Company, which hoped to promote the then-novel technique of smelting iron ore with anthracite coal. This was an important cost and energy savings technique, since either an expensive charcoaling nor coke producing process and transport costs was totally eliminated so produced a great acceleration in the underpinnings of the American industrial revolution.

Ironsand A type of sand with heavy concentrations of iron

Ironsand, also known as iron-sand or iron sand, is a type of sand with heavy concentrations of iron. It is typically dark grey or blackish in colour.

Thomas Iron Company American iron manufacturing firm

The Thomas Iron Company was a major iron-making firm in the Lehigh Valley from its organization in 1854 until its decline and eventual dismantling in the early 20th century. The firm was named in honor of its founder, David Thomas, who had emigrated to the United States in 1839 to introduce hot blast iron making in the Lehigh Valley, and now embarked on an independent ironmaking venture.

Tahawus, New York

Tahawus was a village in the Town of Newcomb, Essex County, New York, United States. It is now a ghost town situated in the Adirondack Park. Tahawus is located in Essex County within the unpopulated northern area designated to the town of Newcomb. Tahawus was the site of major mining and iron smelting operations in the 19th century. Although standing as recently as 2005, the last mining facilities have since been demolished and removed.

The Catasauqua and Fogelsville Railroad was built in the 1850s to transport iron ore from local mines in Lehigh and later Berks County to furnaces along the Lehigh River in eastern Pennsylvania. Originally owned by two iron companies, the railroad later became part of the Reading system, and parts of it remain in operation today.

The Georges Creek Coal and Iron Company is a defunct coal mining, iron producer and railroad company that operated in Maryland from 1835 to 1863.

Cornwall Iron Furnace Historic district in Pennsylvania, United States

Cornwall Iron Furnace is a designated National Historic Landmark that is administered by the Pennsylvania Historical and Museum Commission in Cornwall, Lebanon County, Pennsylvania in the United States. The furnace was a leading Pennsylvania iron producer from 1742 until it was shut down in 1883. The furnaces, support buildings and surrounding community have been preserved as a historical site and museum, providing a glimpse into Lebanon County's industrial past. The site is the only intact charcoal-burning iron blast furnace in its original plantation in the western hemisphere. Established by Peter Grubb in 1742, Cornwall Furnace was operated during the Revolution by his sons Curtis and Peter Jr. who were major arms providers to George Washington. Robert Coleman acquired Cornwall Furnace after the Revolution and became Pennsylvania's first millionaire. Ownership of the furnace and its surroundings was transferred to the Commonwealth of Pennsylvania in 1932.

The Iron Mountain District, also known as the Iron Springs District, is a large, high-grade iron deposit in southwestern Utah, near Cedar City. It is currently in care and maintenance status by CML Metals Corporation, a division of Palladon Ventures and Luxor Capital. Previous owners include Geneva Steel and U.S. Steel.

The Buena Vista Mine is located 21 miles (34 km) south of Lovelock, Nevada. In the past, the area has been known as the Mineral Basin, though another name for the area has been the Buena Vista District. There are at least two other Buena Vista Mining Districts in Nevada, one is located near Unionville, Nevada, the other located in Esmeralda and Mineral counties near the California border. The nearby Buena Vista Hills are named for the mine. The district encompasses roughly 21 square miles (54 km2) of mineral and surface rights, and is one of the largest un-mined iron ore resources in the western United States.

The Benson Mine is an iron-ore mine located near Star Lake, a village in the southern St. Lawrence County, New York.

<i>The Iron Mine, Port Henry, New York</i> Painting by Homer Dodge Martin

The Iron Mine, Port Henry, New York is a painting by Homer Dodge Martin in the collection of the Smithsonian American Art Museum and measures 30 1/8 x 50 in..

Iron mining in the United States Overview of iron mining in the United States

Iron mining in the United States produced 48 million metric tons of iron ore in 2019. Iron ore was the third-highest-value metal mined in the United States, after gold and copper. Iron ore was mined from nine active mines and three reclamation operations in Michigan, Minnesota, and Utah. Most of the iron ore was mined in northern Minnesota's Mesabi Range. Net exports were 3.9 million tons. US iron ore made up 2.5 percent of the total mined worldwide in 2015. Employment as of 2014 was 5,750 in iron mines and iron ore treatment plants.

References

  1. The railroad commissioning can be found at
  2. Transactions of the American Institute of Mining Engineers, Volume 25
  3. New York State Museum bulletin, Issues 194-197
  4. Map of Jayville Location
  5. Geological Survey professional paper, Volumes 376-377 , pg. 135
  6. By New York (State) Board of Railroad Commissioners, New York (State). State Engineer and Surveyor , pg. 148
  7. Transactions of the American Institute of Mining Engineers, Volume 25 , pg. 547
  8. Pennsylvania state reports, Volume 149 , pg. 254
  9. Engineering and mining journal, Volume 97, Issues 1-13 , pg. 450
  10. Geological Survey professional paper, Volumes 376-377 , pg. 135
  11. New life in the North Country , 1997
  12. Guidebook, Volume 76, Part 2004
  13. Bulletin - United States Geological Survey, Issue 643
  14. Trans-communicator, Volume 20 , pg. 666
  15. Rand-McNally Official Railway Guide and Hand Book , pg 173
  16. Regional Geology of the St. Lawrence County Magnetite District Northwest Adirondacks, New York
  17. The iron manufacturer's guide to the furnaces, forges and rolling mills , Pg. 144
  18. A History of St. Lawrence and Franklin Counties, New York , pg. 431
  19. The growth of a century: as illustrated in the history of Jefferson county , pg 454
  20. Engineering and Mining Journal, Volume 23, Pg. 299
  21. Bulletin ..., Issue 42 , Pg. 142
  22. Geological Survey professional paper, Volume 933 , Pg 78
  23. Transactions of the Federated Institution of Mining Engineers, Volume 10
  24. Bulletin, Issues 423-424 , Pg 137
  25. Geological Survey professional paper, Volumes 376-377 , Pg 135
  26. Vasenite at the Jayville Magnetite Deposit, USG
  27. Logging Railroads of the Adirondacks , pg 212
  28. Wicked Northern New York , pg 68.
  29. THE BOSTON HISTORY COMPANY
  30. The Paper mill and wood pulp news, Volume 26 , pg. 6
  31. Documents of the Senate of the State of New York, Volume 23 , pg. 136
  32. Documents of the Assembly of New York State, Volume 4 , pg. 306
  33. Logging Railroads of the Adirondacks
  34. Annual report of the State Superintendent for the school year , Volume 34 , pg. 495
  35. Central Headlight Railroad News , pg. 1
  36. The Catholic Church in the United States of America: Undertaken to ..., Volume 3
  37. Forest and stream, Volume 60
  38. Wicked Northern New York , pg 71
  39. The Deseret Weekly, Volume 51 , pg 246
  40. The growth of a century: as illustrated in the history of Jefferson county ...
  41. Directory of iron and steel works of the United States and Canada, Volume 10
  42. Wicked Northern New York
  43. Manual for the use of the Legislature of the State of New York , 1903
  44. Central Headlight , November 1945