Which was found first, Beanland Mine or Burwash Mine?
Beanland Mine
Beanland Mine
Beanland Mine, also known as Clenor Mine, is an abandoned surface and underground mine in Northeastern Ontario, Canada.
 It is located about 1 km west of Arsenic Lake and 4 km northwest of the town of Temagami in central Strathy Township.
 It is named after Sydney Beanland, who first claimed the mine site in the 1920s and was a director for the mine from 1937 to 1938.
Burwash Mine
The Burwash Mine was a small gold property discovered in the fall of 1934 by Johnny Baker and Hugh Muir at Yellowknife Bay, Northwest Territories.
 The town of Yellowknife did not exist yet at that point, but the discovery of gold at Burwash was the catalyst that brought more gold prospectors into the region in 1935 and 1936.
 A short shaft was sunk in 1935-1936 at Burwash, and in the summer of 1935 a 16-ton bulk sample of ore was shipped to Trail, British Columbia for processing, yielding 200 troy ounces (6 kg) of gold.
 The mine did not become a substantial producer and it is believed the gold vein was mined out.
Milne-Sherman Road
The Milne-Sherman Road is a concrete road in Northeastern Ontario, Canada, located about 2 km north of the town of Temagami.
 It has its connection with Highway 11 and is the main road that allows access to the abandoned Milne Townsite, as well as the abandoned Sherman Mine.
 Several gravel roads branch off the Milne-Sherman Road.
 One of these enters the main garbage dump of Temagami while another extends into a gravel pit and the Beanland Mine property. Crystal Mine
Crystal Mine is located near Juneau in the U.S. state of Alaska.
 The quartz ledge at the Crystal Mine was first discovered in 1895 by B. Heins.
 It was so named because of the large pyrite cubes which were found occurring in the surface outcrops of the ledge.
 Gold was extracted till 1905 from quartz using ten-stamp mill and from about 1,000 feet of underground workings yielded 1,210 ounces of gold.
 Intermittent production of gold is reported till 1925 but there are no records of the yield.
 The formation was determined as of 54 to 56 Ma age.
 The gold yielding resources available from the mine were assessed as 9,000 tons of material with yield of 0.21 ounce of gold per ton. Accentor-class minesweeper
In World War II, the United States Navy needed a vessel that could consistently locate mines in [foreign or domestic?]
 or littoral waters.
 Littoral waters are found between the shore line and waters 60 meters deep.
 The Accentor-class minesweeper (sometimes called the Accentor/Acme-class minesweeper) was developed for this task.
 This class of minesweeper was named after the Accentor bird, Prunella modularis.
 This bird is endemic to Europe, Asia, and North Africa which is the area that World War II occurred.
 The bird is a drab brown and gray color and is in the same family as warblers and thrushes.
 The Accentor-class mine sweeper was designed for the sweeping of mines in harbors, bays, and other littoral waters.
 The Accentor-class minesweeper had a wooden hull for three reasons.
 The first was that some of the mines that the Accentor-class minesweeper was trying to detect were detonated by a copper wire coming out of the top of the mine that is used to detect the magnetic field that is produced by the metal hulls of most ships; when the wire senses a magnetic field, it detonates the mine.
 Minesweepers use wooden hulls because wood is a non-magnetic material, unlike steel, and would not set off this type of mine.
 The second is that wooden hulls were lighter than metal hulls.
 This caused them to float higher in the water, which made them displace less water and have a smaller pressure wave, so pressure mines would not be set off by the movement of the ship.
 Lastly, due to the ship floating higher in the water, contact mines were not effective because they were often around 20 feet below the surface of the water, and the draft of this class of ship was between 8 feet 11 inches and 10 feet 8 inches.
 Typically, the Accentor-class minesweepers were armed with a pair of .50 caliber machine guns for protection.
 Rather than creating new minesweeping vessels, forty-five wooden-hulled fishing boats were converted into Accentor-class minesweepers.
 This saved the Navy both time and money.
 Since these converted fishing boats were not all the same, their specifications do vary a bit.
 The converted fishing boats had a displacement from 165 to 270 tons of water.
 They had speeds from 8.5 up to 14 knots and crews from as small as 15 up to 50. The 8G Band
The 8G Band is the house band for "Late Night with Seth Meyers".
 The band is led by "Saturday Night Live" alumnus Fred Armisen.
 He assembled the 8G Band, named for the studio where the show is taped, just two weeks before the test show.
 He texted friends Seth Jabour, Syd Butler and Eli Janney ("What are you guys doing this week?")
, then found first drummer Kimberly Thompson through an audition.
 Guitarist Marnie Stern later joined as well.
 After Thompson left the band, guest musicians frequently sit in often for an entire week.
 Some notable names to sit in on the drum kit include: Patrick Carney, Chad Smith, David Lovering, Kenny Aronoff, Jon Theodore, Nicko McBrain, Matt Sorum, Brad Wilk, Darren King, Danny Carey, Abe Cunningham, Dave Lombardo, Brann Dailor, Jimmy Chamberlin, Matt Cameron, and Abe Laboriel Jr. as well as other guest musicians.
 Additionally singer, guitarist: J Mascis, Bob Mould and others have also sat in with the band. Abellaite
Abellaite is a hydrous carbonate mineral discovered in the abandoned Eureka uranium mine in Catalonia, Spain, with the formula NaPb(CO)(OH).
 It is named in honor of Joan Abella i Creus, a Catalan gemmologist who has long studied minerals from the Eureka mine and first found abellaite in the mine.
 A team composed of Joan Viñals and Xavier Llovet from the University of Barcelona, Jordi Ibáñez-Insa and Josep Elvira from the Institute of Earth Sciences Jaume Almera, and Núria Oriols, from the National Museum of Art of Catalonia identified the mineral’s structure. History of anthracite coal mining in Pennsylvania
There are two types of coal found in Pennsylvania: anthracite (the “hard coal” found in Northeastern Pennsylvania below the Allegheny Ridge southwest to Harrisburg; also called “stone coal”, “rock coal” in the 1800s) and bituminous (“soft coal”, found west of the Allegheny Front escarpment).
 Anthracite coal is a natural mineral with a high carbon and energy content that gives off light and heat (produced energy) when burned, making it useful as a fuel.
 It was possibly first used in Pennsylvania as a fuel in 1769, but its real history begins with a documented discovery near Summit Hill and the founding of the Lehigh Coal Mine Company in 1792 to sporadically send expeditions to the wilderness atop Pisgah Ridge to mine the deposits, mostly with notable lack of great success, over the next 22 years.
 The owners of this company were absentee management—reliant on teams of workers sent under a foreman to fell timber to build so called 'Arks' (high-sided punts), then mine coal around nine miles (today's Summit Hill) from the right bank Lehigh (the Lehigh & Susquehanna Turnpike terminus at Mauch Chunk), then trek with mule loads to fill the boats for the trip down the rapid strewn Lehigh River,(Brenckman, p. 595-597) and then more than 60 mi to Philadelphia docks on the unimproved often log choked (Bartholomew, p. 4-5) Delaware River.
(Bartholomew, p. 4) Wheal Peevor
Wheal Peevor was a mine located on North Downs about 1.5 miles north-east of Redruth, Cornwall, England.
 The first mining sett was granted here in around 1701 on land owned by the St Aubyn family.
 It was originally mined at shallow depths for copper, but when the price for that metal slumped after 1788, the mine was able to change to mining tin ore, which was found deeper down.
 In the late 18th century Wheal Peevor had the advantage of being drained by the Great County Adit which was around 100 metres deep here.
 The mine covered only 12 acres (4.8 ha) but had rich tin lodes.
 In addition to tin and copper, pyrite was also mined here between 1872 and 1887. Andrew Corbett
Andrew John Corbett (born 20 February 1982) is an English former footballer.
 He was part of the Kidderminster Harriers youth system but found first team opportunities limited to seven appearances in the Football League, and moved to Solihull Borough.
 At Solihull he was a prolific striker and earned a move to Nuneaton Borough.
 After just a few months at Nuneaton, Burton Albion secured his signature for a small fee.
 Ironically Corbett joined the Brewers as a striker but has found more success at right back and right midfield, and won the club's Player of the Season award in 2005.