


These quarries were "in the town of Bluehill, 3 miles east of Bluehill village, and north of Woods Point." The granite was reportedly a medium to light-gray color with a coarse texture.
Minerals in descending order of abundance: potash feldspar (microcline and orthoclase), smoky quartz, soda-lime feldspar (oligoclase), and black mica (biotite), with accessory magnetite.
About 350 feet east of the upper opening there was an area about 200 feet square which produced granite of a medium bluish-gray color with a fine texture referred to as the Chase monumental granite. It was only quarried occasionally for local monumental use.
Transport of the granite was by cable road 1,400 feet from the main quarry to the cutting shed and by locomotive track 650 feet more from the shed to the dock. At the time of the report, the quarries were no longer in operation.
Granite from the Chase Quarries was used in the following examples: the New York Stock Exchange, the Lying-in Hospital, the Manhattan Trust Building, and the Grand Union Hotel on Forty-second Street, New York; the General Thomas monument and the trimmings to the Bureau of Engraving and Printing, Washington; the League Island Dry Dock; and the post office at Harrisburg, Pennsylvania.
Structures in which this stone was used include: the Post Office in Harrisburg, Pennsylvania; the Grand Union Hotel in New York City; the Lying-in Hospital in New York City; the Manhattan Trust Building in New York City; the New York Stock Exchange in New York City; the Trimmings to the Bureau of Engraving and Printing in Washington, D. C.; the Drydock at League Island; the General Thomas Monument in Washington, D.C.; and other monuments.
This quarry was “in the town of Bluehill, 1 1/4 miles east of Bluehill village.” The operator was Jesse B. Park (Inc.), 1328 Broadway, New York. The granite from the quarry was reportedly a medium-gray with a slightly bluish color and a coarse to medium texture.
Minerals in descending order of abundance: potash feldspar (microcline and orthoclase), smoky quartz, soda-lime feldspar (oligoclase), and black mica (biotite), together with accessory zircon and magnetite.
The White Quarry was opened about 1855. In 1906 the quarry measured 300 by 350 feet and had a depth that ranged from 15 to 45 feet. Transport of the granite was by team one-third mile to the docks. At the time of the report, the quarry had been idle since 1913.
The waste granite was used for paving blocks. Granite from the White Quarry was used in the following examples: the Woman's Hospital in New York; the Mercantile Trust Co. and Caledonian Insurance Co. buildings in St. Louis, Missouri; the basement story of the District of Columbia Municipal Building; the First Day and Night Bank, the Delamar and Brokaw residences, in New York; the chemical laboratory of the Pratt Institute in Brooklyn, New York; the chemical laboratory of the Stevens Institute of Technology in Hoboken, New Jersey; and the fountain and large monolithic bowl in Deep River, Connecticut.
Excerpt from "Esther Wood: An Appreciation," by Hugh Curran.
"Quarries were a major local employer in the late 19th century. Esther's father was the manager of quarries in Blue Hill and Deer Isle. One of these was located near Friend's Corner and referred to as the Pittsburgh Quarry since so much of its stone went to Pittsburgh, Pa. I visited the site and saw the rubble and shards of granite that had been used to make docks for barges. A thin covering of grass lay over tens of acres of land that had once been mere slag and granite fragments. I could picture the meadows nearby covered with temporary cabins for granite workers, including immigrants from Italy and Ireland and Eastern Europe.
"As I stood there imagining the hammers and chisels chipping, the noise and yelling as the blocks were shaped to the required sizes, the small steam engines chuffing and swinging blocks of granite onto the barges, I could at the same time see in my mind's eye the work horses pulling wagons with their huge granite blocks slung underneath, slowly and carefully down the hill from the quarry above."
This quarry was "in the town of Bristol, one-fourth mile east of Round Pond village, and west of Muscongus Island." The operator was Peter Svensen & Co., Round Pond. Granite from the quarry was reportedly of very dark-gray and medium-gray colors with a fine texture. ("black granite") Transport of the granite was by cart about 300 feet from the lower quarry and 800 to 1,000 feet from the upper quarry to the wharf in Muscongus Bay.
The Round Pond Quarry was opened in 1885. There were two adjacent openings along a northwest-southeast line. The upper quarry (the northwestern) measured 100 feet square in 1905; the lower quarry measured 400 feet northwest-southwest by 100 feet across, "but with a central part 37 feet wide on each side-that is, 175 feet wide." The depth for these openings ranged from 10 to 65 feet. It was difficult to obtain many large blocks. The quarry was idle in 1916.
The granite from the quarry was used mainly for small monuments which were shipped to New York without the lettering. Waste was used to make paving blocks. The granite from the quarry was used in the following examples: the Die of the Maine monument at Andersonville, Georgia; the base and die of the General Sheridan monument in National Cemetery at Arlington, Virginia.
“The Crocker Slate Quarry crew, of Brownville, Me., has been working on winter time – eight hours per day. The Merrill quarry is partly shut down while winter tracks are being laid.”
“The Crocker Slate Quarry crew, of Brownville, Me., has been working on winter time – eight hours per day. The Merrill quarry is partly shut down while winter tracks are being laid.”
This article presents the history of the Brownville area slate quarries and workers. The photographs presented in this article include: Highland Quarry, Brownville; Group of quarry workmen at Crocker Quarry; Track lift at Crocker Slate Quarry, 1872; Adams H. Merrill, quarry owner; and Crew at Merrill Quarry waiting to be lowered into the pit.
Many of the early trained stone workers immigrated from near "Bethesda and Bangor in northern Wales." wher many of the workers had worked in the Penrhyn Quarry there. Another group of stone workers were Swedish, who came from New Sweden to work in the Brownville quarries.
One of the Brownville slate quarries mentioned in this article is located near Sparrow House, and the authors note that the Crocker Quarry is down the road from the Sparrow house. The Crocker Quarry was "one of the largest pits in the area." The quarry was operated by the Bangor and Pisctaquis Slate Company for about 20 years during the time it was actively quarried. The Crocker Quarry was abandoned in 1912. Today the quarry is not noticeable from the road as it is surrounded by birch and poplar trees.
The Merrill Slate Quarry was owned by Adams H. Merrill, and the story of Mr. Merril is presented in this article. The quarry was abandoned in 1914. The Merrill Quarry was reportedly at least 225 feet deep, although another person reported the depth to be closer to 300 feet deep. The Merrill Quarry is located across the river from the Crocker Quarry. Today the Merrill Quarry is not nearly as deep as rock and trash partially fill the old quarry hole. This article goes on to provide a "first hand lesson from Hugh Thomas on how a slate vein was 'farmed.'" Mr. Thomas used the Merrill Quarry to describe the slate quarrying process.
Another area slate quarry described in the article is the Highland Quarry, which is located east of the Crocker Quarry. The Highland Quarry produced large pieces of slate. Today this quarry is mostly filled with water ".to within several feet of the birches that curve out over the pit." Further west is the Barnard Slate Quarry. The authors indicate that the last attempt to start up this quarry occurred in 1952.
This quarry was located "in the town of Brunswick, 3 miles west of Brunswick village, on the south side of the Maine Central Railroad, on the Merriman farm." The granite from the quarry was reportedly a medium gray with a fine texture. When measured for the 1923 report, the opening measured about 75 by 50 feet and had a depth of 5 feet. Transport from the quarry was by team to the railroad nearby. At the time of the inspection, the quarry had not been in operation for many years. (Accessory mineral: Zircon.)
Granite from this quarry was used in the following examples: The chapel at Bowdoin College at Brunswick and the First Parish Church in Portland, Maine.
A. W. Libby has sold his marble and granite plant at Buckfield, Maine, to Horace Murch.
"Reportedly, the owners have been considering development of the Quarry as a tourist attraction. Otherwise, the quarry may occasionally be open to collectors on a fee basis.
"The quarry originally opened prior to 1900 to mine specimen tourmaline and beryl. Beginning in 1917, quartz crystals were mined for 10 years. Subsequently, from 1926 to 1931, feldspar was mined. In 1989, the reported largest morganite crystal in world was discovered in the quarry-it weighted 50 pds..."
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