Slide Image Left << Flying into the Bridge (BRV).
For Shades of Volcanoes, Seismic Faults, Arsenic, Cobalt, Gold, Jade, Mercury, Molybdenum, Radium, Silver, Titanium, Tungsten and Uranium. Hyperlinks your own social media are at the bottom of each post. To View VIDEOS >> SOUND ON >> FULL SCREEN click the YouTube Icon first, expand from there. To get back here, close it.
SOUND ON >> TO WATCH FULL SCREEN start the video and click on the YouTube Icon at the bottom and expand there. Later When you close that window you will be brought back here.
Extreme Winter Camping at (-60F/-51C)
alone with my 4 year old son in our hot tent. The extreme cold tests
all of our gear and makes everything difficult. But we had a great
time and made some amazing food. Check out our camping and adventure
playlist https://youtube.com/playlist?list=PL5...
Out tent is the Arctic Oven Igloo. Sleeping bags are the Feathered
Friends Snowy Owl GoPro Hero 10 Food: Raclette Cheese, Reindeer mango
Curry, Rice Pudding, Bacon and Eggs Outdoor Boys on FACEBOOK
https://www.facebook.com/TeamOutdoorBoys
Outdoor Boys on INSTAGRAM @outdoorboyschannel
BUY OUTDOOR BOYS T-SHIRTS http://shop.spreadshirt.com/catsandcarp/
Cool way to remove a stump from the inside out. Stump burning. How long does it take?
507,328 viewsMay 23, 2021I had a very large stump that I needed removed for cheep. I tried burning it from the outside but after a full day, I found it was going to take way too long and too much tending to keep it burning. I decided to try something new and let it burn from the inside.
How long will it take to burn?
I grew up in small towns and in the North where the rule is share and share alike. So, I'm a Creative Commons type of guy. Copy and paste ANY OF MY MATERIAL anywhere you want. Hyperlinks to your own Social Media are at the bottom of each post. <a ef="http://creativecommons.org/licenses/by/4.0/" rel="license"><img alt="Creative Commons License" src="https://i.creativecommons.org/l/by/4.0/88x31.png" style="border-width: 0;" / /></a><br />This work is licensed under my <a href="http://creativecommons.org/licenses/by/4.0/" rel="license">Creative Commons Attribution 4.0 International License. </a></a></span></span></span></p></a>
Around 5:30-7:15am. If it is a clear day I can see forever. I
took this photograph just after the sun had come up over the
mountains in the east, around the Coquihalla / Chilliwack / Hope area
as the sun's rays struck the bottoms of the clouds overhead, but
before the sun cleared Mount Seymour and the local mountains. I never
photo-shop anything, ever. Just get up in the morning.
8,015
views Oct 15, 2022 Working underground in my new secret gold mine! I
am collecting a sample of ~1000 lbs of ore from a quartz vein that is
rich in gold to run through the jaw crusher, hammer mill, and shaker
table to recover the gold and other precious metals. Stay tuned for
part two soon! For more info please email or call: Email:
info@MBMMLLC.com Phone: 360-595-4445 Website: http://www.mbmmllc.com/
Facebook: https://www.facebook.com/MBMMLLC
Instagram: https://www.instagram.com/mbmmllc/
Twitter: https://twitter.com/MBMMLLC00:00
Introduction 00:48
Exploring The Gold Mine 05:28
Mining Gold By Hand 05:55
Gold Specimens In Quartz 07:53
Mining Gold 10:39
Mucking The Gold Ore To The Truck 11:23
Drilling On The Gold Vein 19:06
Outro and Links
The Mount Meager massif produced the largest volcanic eruption in Canada in the last 10,000 years. About 2,400 years ago, an explosive eruption formed a volcanic crater on its northeastern flank and sent avalanches of hot ash, rock fragments and volcanic gases down the northern flank of the volcano. Evidence for more recent volcanic activity has been documented at the volcano, such as hot springs and earthquakes. The Mount Meager massif has also been the source of several large landslides in the past, including a massive debris flow in 2010 that swept down Meager Creek and the Lillooet River.
Mt Meager Massif (southside) Landslide Fly Over. A massif is a group of volcanic peaks. In this case - see MORE THOROUGH below the video on the north side Plinth Peak with is just above Downton Lake)
The
Mount
Meager massif
is a group of volcanic peaks in the Pacific
Ranges
of the Coast
Mountains
in southwestern British
Columbia,
Canada. Part of the Cascade
Volcanic Arc
of western North America, it is located 150 km (93 mi) north of
Vancouver
at the northern end of the Pemberton
Valley
and reaches a maximum elevation of 2,680 m (8,790 ft). The massif is
capped by several eroded volcanic edifices, including lava
domes,
volcanic
plugs
and overlapping piles of lava flows; these form at least six major
summits
including Mount Meager which is the second highest of the massif.
Six
main summits constitute the Mount Meager massif. The highest and
northernmost summit is Plinth
Peak
with an elevation of 2,680 m (8,790 ft).[1][25]
Mount Meager itself is 2,650 m (8,690 ft) in elevation.[25]Capricorn
Mountain
west of Mount Meager rises with an elevation of 2,570 m (8,430 ft).
Just west of Capricorn Mountain lies Mount
Job,
2,493 m (8,179 ft) in elevation.[1][25]Pylon
Peak
with an elevation of 2,481 m (8,140 ft) is south of Capricorn
Mountain and Mount Meager.[25]Devastator
Peak,
also known as The
Devastator,
has an elevation of 2,315 m (7,595 ft) and is the lowest and
southernmost summit of the massif.[1][25]
The
Garibaldi
Volcanic Belt
(GVB) has a long history of eruptions and poses a threat to the
surrounding region. Any volcanic
hazard
ranging from landslides
to eruptions could pose a significant risk to humans and wildlife.
Although the massif has not erupted for more than 2,000 years, it
could produce a major eruption; if this were to happen, relief
efforts would be quickly organized. Teams such as the Interagency
Volcanic Event Notification Plan
(IVENP) are prepared to notify people threatened by volcanic
eruptions in Canada.
The
Mount Meager massif produced the largest volcanic eruption in Canada
in the last 10,000 years. About 2,400 years ago, an explosive
eruption
formed a volcanic
crater
on its northeastern flank and sent avalanches of hot ash, rock
fragments and volcanic
gases
down the northern flank of the volcano. Evidence for more recent
volcanic activity has been documented at the volcano, such as hot
springs
and earthquakes.
The Mount Meager massif has also been the source of several large
landslides in the past, including a massive debris
flow
in 2010 that swept down Meager
Creek
and the Lillooet River.
Taking
off from pumice mine about 1 km north of campsite. Fly over of
campsite and the ridge we were evac'd from. Fly up the Meager valley
to Mt Meager and Capricorn Glacier. You can see the natural lake
created by the slide in a few shots. This is what created the
Pemberton evacuation warning. Fly back down valley towards Pemberton.
The expansion could increase the height of a dam holding back mining waste to 255 metres — taller than Vancouver's highest skyscraper — without requiring an environmental assessment
A B.C. mine that was fined $51,000 for unauthorized release of wastewater late last year is proposing to increase its tailings pond capacity by 70 per cent in a move that won’t automatically trigger an environmental assessment.
Kulshan is NOT a Flood Basalt eruptions; rather, at a glaciated Stratovolcano with active fumerols near the top. Flood
Basalt eruptions are the largest lava eruptions in the history of
this planet. In this video you will find out just enormous these
eruptions were exactly and what impact they had on Earth and its
inhabitants. I will include the sources in Part 2 Thanks for
watching. https://creativecommons.org/licenses/...
Our exploration of one of the upper portals of the Bralorne mine in
Bralorne BC. The Bralorne property is centred on a gold-quartz vein
system. The Bralorne mine, comprising the King, Empire (or Ida May)
and Crown workings, operated continuously from 1932 to 1971.
Production during this period and from older operations totals 4.9
million tonnes of ore yielding 87.6 million grams of gold and 21.9
million grams of silver, for an average recovery of 16.1 grams per
tonne gold and 4.03 grams per tonne silver (MINFILE 092JNE001). The
property is a consolidation of 133 Crown-granted claims and
fractions, many of which were staked in 1897. The staking began after
the discovery of gold-bearing quartz veins on the north bank of the
lower course of Cadwallader Creek (Cairnes, 1937). Access to the area
at that time was 110 kilometres by difficult trail from the railway.
The original lode claims were explored individually or in small
groups (the Lorne and Pioneer groups of claims were staked in 1897)
and by 1898 almost all the veins that would be mined had been found.
Gold was first recovered by hand crushing and panning the oxidized
quartz from surface exposures. Adits were developed on the promising
leads and gold was won in quantity from the ore by improvising
primative mills. At Lorne two 12-foot arrastres were erected driven
by a 28-foot overshot water wheel to process in a few tons of ore per
day and in 1900 a 5-stamp mill was set up to increase production. On
selling the Pioneer property, Arthur Noel purchased the Lorne mine
from William Sloan and Dan Hurley. Prior to this the Lorne, King and
Woodchuck veins had been successfully worked by Mike Gaynor, Nat
Coghlan, William Young, John Williams and E.J. Taylor. In 1910 Lorne
Amalgamated Mines Company gained control of the King mine and the
adjacent key ground that included the Lorne, Golden King, Woodchuck,
Wood Duck, Telephone and Marquis Crown-granted claims. After some
shallow surface workings were completed the No.3 adit-crosscut was
driven 335 metres to intersect the King vein. Work on the property
was facilitated in 1915 when the Pacific Great Eastern Railway
reached Lillooet on the Fraser River. Supplies from the coast were
then routed 90 kilometres westward by road following the Bridge
River. By 1920 some 900 metres of underground drifts and crosscuts
had been developed and about 150 kilograms of gold produced, however,
increasing sulphide and arsenic content in the veins at depth made
gold recovery by amalgamation too low to pay in so remote an area. In
1928 Lorne Gold Mines Limited (Stobie, Furlong and Company) was
incorporated and acquired the Alhambra and Blackbird claims, the
Empire mine on the Ida May claim and the Coronation mine workings to
the southeast. Proceeds from the sale of stock were spent driving a
900-metre adit tunnel 800 feet (245 metres) below the surface
showings and by 1929 the principal veins in the King mine were
delineated but in 1930 underground development was suspended because
of financial difficulties. A new mining era began in 1931 when Lorne
sold 60% interest to Austin Taylor and Associates who then organized
Bralorne Mines Limited and took control of the property. A 100-ton
mill was installed employing blanket concentration and floatation,
thus commencing a 40-year period of continuous production (Photo 1).
In 1935 milling capacity was increased to 475 tons daily.
This is a video that I have
wanted to make for years, and I am so happy with the experience of
making it. I visited the old town location of Minto, in the central
interior of BC. There is nothing left structurally of the old town
because the entire location was flooded by the man made Carpenter
Lake, but that does not mean there isn't anything to see. My goal
while visiting Minto, was to put the drone in the air and see how
well I can map out the ruins and roads of the old town. This was more
difficult than I had hoped, but combining what I could see from the
air and what I could see from the ground, I was really able to start
building this map. While on location, I also wanted to do some metal
detecting and see if I could find some old relics. I put on a lot of
miles and dug a lot of holes, and it was worth every bit of the
effort. I got to see so many remnants from the residents that once
called this home, and I was able to dig up some really neat relics as
well. As beautiful as the town site is, I cant go without talking
about the drive to get there. I have done this drive five times now,
and it impresses me more every time I do it. I personally believe
that this is the most beautiful drive in British Columbia, and I am
so excited to share it with you all. Thank you so much for watching
and enjoying. If you would like to help support the channel, and help
make it possible to make more videos like this one, please consider supporting on Patreon: https://www.patreon.com/DestinationAd... [truncated;',
Dr. Glyn Williams-Jones, from Simon Fraser University, describes historical volcanic eruptions and explains the importance of studying Canadian volcanoes.
Originally published February 7, 2017.
The
Minto property is owned by Avino Mines and Resources Limited. The
property comprises eight Crown-granted mineral claims including Omega
and Omega 1-4, Alpha fraction, Jack fraction and Golden Girl;
reverted Crown-granted claims, Hillside Extension 1-2, Minto
fraction, Prince, Frank fraction, Hagmo, Ex fraction, and Om
fraction, Golden Queen, Helm fraction, and Juniper (located claim).
The original claims were staked about 1910 but little work was done
until the 1930s. The property was optioned to Consolidated Mining and
Smelting Company of Canada Limited (Cominco) by W. Davidson in 1930.
Work completed by this company in 1931 and 1932 included the initial
development of the River, Hagmo and Warren adits. The option was
relinquished in 1933 and property became the asset of the newly
formed Minto Gold Mines Limited. This company extended the previous
workings, the main adit and a winze from the lowest adit to three
deeper levels. A mill was installed in 1934 with a capacity of 50
tons per day; in 1935 this was increased and maintained at 125 tons
per day until the end of operations in 1937. In 1942 some broken ore
was extracted and a few pillars mined. Exploration below the adit
levels proved unsuccessful. Pioneer Gold Mines Limited obtained an
option from 1941 to 1942; in 1959 the claims were acquired by Ace
Mining Company Limited. Little additional work was done and the
property, now under the name of Minto Trading and Development
Company, became part of the estate of Marguerite W. Wiles. In 1975
Empire Metals Corporation Limited optioned the property and completed
geochemical and geophysical surveys. Avino Mines and Resources
Limited purchased the property in 1985 and, up to 1987, had completed
geological, geochemical and geophysical surveys which led to
trenching and diamond drilling, mostly north of the old mine
workings. Since this time the property has been dormant. The main
period of production from the Minto mine was from 1934 to 1940. A
total of 80.6 thousand tonnes of ore was mined yielding a total 0.5
million grams of gold, 1.6 million grams of silver, 9.7 million grams
of copper and 56.4 million grams of lead (MINFILE
092JNE075). . . . ARIS/www
Detailed Summary Report
Owner of a private cut and fill gold mine gives us a detailed tour, demonstrates tools, equipment, construction and the geology of his mine. Some of the clips are a little out of focus. Long video that explains many of the technicalities seen in old mines.
Mount Meager masiff produced the largest volcanic eruption in Canada in the last 10,000 years. About 2,400 years ago, an explosive eruption formed a volcanic crater on its northeastern flank and sent avalanches of hot ash, rock fragments and volcanic gases down the northern flank of the volcano. Evidence for more recent volcanic activity has been documented at the volcano, such as hot springs and earthquakes. The Mount Meager massif has also been the source of several large landslides in the past, including a massive debris flow in 2010 that swept down Meager Creek and the Lillooet River.
I have been a Wikipedia author and editor since 2003, so I'll use that stuff, but I have no compunction to continue that, as well. Oh, and meet my Big Brother.
My Big Brother when I lived in Minto. The grizzly bear (Ursus arctos horribilis), also known as
the North American brown bear or simply grizzly, is a population or
subspecies of the brown bear. If I ever catch Tyax bear baiting again (2003) there will be HELL to pay.
About 90%[2]of the world's earthquakes and about 81%[3]of the world's largest earthquakes occur along the Ring of Fire.[4][5]
All but three of the world's 25 largest volcanic eruptions of the last 11,700 years occurred at volcanoes in the Ring of Fire.[6]
The Ring of Fire is a direct result of plate tectonics: the movement and collisions of lithosphericplates,[7]especially subductionin the northern portion. The western portion is more complex, with a number of smaller tectonic plates in collision with the Pacific plate from the Mariana Islands, the Philippines, Bougainville, Tonga, and New Zealand.
