text:
Typical 1-AD cycle?
Typical 1-AD cycle?
What would be a typical 1-AD cycle for mass only? Also if you guys could suggest what name brands for each 1-AD due to your experiences that would be great. If possible could you use some format like this: Weeks 1-2 1-AD xxxmg(or tabs) etc. Appreciate all the help guys....almost ready to start buying for my cycle.
Why 1-ad? The dose needed for solid gains is relatively high due to the need to convert. A 1-test/4AD transdermal at 50/50 will put some good solid mass on ya.
-Saving random peoples' nuts, one pair at at time... PCT info:
-Are you really ready for a cycle? Read this link and be honest:
*I am not a medical expert, my opinions are not professional, and I strongly suggest doing research of your own.*
Have you thought about a 1-test/4-ad transdermal. 1-ad is ok for a first cycle, but you should stack 4-ad with it to combat the sides. But for reasons of economics I personally would choose the 1-test/4-ad transdermal any day over 1-ad. More bang for your buck.Originally Posted by Souphtc
Well what would be the typical stack for a 1-Test/4-AD cycle? I'm not sure about transdermals as I had some prescription Test gel prescribed to me that I never used. I pulled it out one day and thought hmmm...(it wasn't expired). I tried it for training and found it did nothing for me. Maybe the dosages weren't high enough but after that I just never like the whole trans route. I'm still open for ideas and suggestions though. I think I asked this already about 2 weeks ago but I'm trying to bulk and looking for around 10-20lbs. I know that shooting a little high but I havent done a PH cycle in like 2 years so I know my gains would be pretty good. I'm even open to M1T but I'm concerned about the sides. Thanks again for the help guys.Originally Posted by Jimmy_4
1-Test can still be pretty tough for a first cycle. It is in fact an anabolic steroid. But if uve done some PH cycles before go with a 1-test/4-ad combo.
As for 1-AD id say go:
week1: 3 caps a day
week2: 4 caps a day
week3: 6 caps a day
Then take 3 weeks off, still workout ect. 6-OXO PCT will be fine for 1-AD.
M1T Will put some SERIOUSE mass on ya boday
It is a POTENT ANABOLIC STEROID. Only legal for a short time for small loopholes.
Back pumps(Lots of potassium/arginine to stop)
Raised BP(Hawthorne Berry)
Stress to liver(Milk Thistle/R-ALA/Vit C)
Lowered appetite
Lethargy(Stack with 4-ad)
Now let me tell u my personal experiences: I used 10mg ed for week 1, and 15mg ed for week 2. I gained 15 pounds of fairly lean mass. I was very happy, bench jumped like crazy along with other lifts. Went from 225x8 - 260x8. I was lucky, got no sides except lowered appetite. I stopped my cycle short one week due to a bit of discomfort around my liver area. Or so I thought, im going to the doctor tomorrow, but I have a feeling its something else, like my appendix, because its not near my liver rlly. Anyway i cant say, but I have heard some abd stories about liver values shooting through the roof on m1t. So if u do a cycle and experience a little pain, be safe, and just cut ur cycle short.
With M1T get some hawthorne berry (6 bucks) to keep blood pressure low. Get Milk Thistle for Liver support. Get some R-ALA and/or Vitamin C(Lots of orange juice) for liver as well. PCT, u need Nolva.
A 3 week gradual cycle:
Week1: 5mg
Week2: 10mg
Week3: 15-20mg
Popular 2on2off cycles:
Week1: 5-10mg
Week2: 15-20mg
Pct 2 weeks, Nolva 40/20
Week5: 10mg
Week6: 15-20mg
Pct 2 more weeks, Nolva, 40/20
So anyway, if u want anymore info, just ask man, and goodluck. Lots of protein water vitamins ect. And run any liver protectants u have full fledged during pct times.
I agree transdermals are a pain but they are much better than a non-methlyated oral cycle. Your best bet for setting up a good transdermal is the "Build your own transdermal" at powernutrition.net. I suggest 5 grams of 1-test and 5 grams of 4-ad just as MB suggested. That will definately put some bulk on you provided your diet is in order without overwhelming you with sides.Originally Posted by Souphtc
BTW, I don't agree with 6oxo being OK for ANY cycle. Get nolva, its much cheaper and proven to work. You need it in case of gyno during a cycle anyway, so have some for PCT as well...IMO.
With a transdermal, go 6 weeks. If you do choose the 1-ad oral route, run that 4 weeks.
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text:
Riverton poised to receive $256K in Consensus Funds; $2.3 million to be distributed around county
(Riverton, Wyo.) – Riverton Mayor Ron Warpness told the city council last week that the city has been approved for $256,500 in county consensus funds for two projects.
The funds, formerly known as Payment In Lieu of Taxes, or PILT, come to the county from the State of Wyoming.
In total, the county will disperse $2.3 million in consensus funds in the next fiscal year.
Riverton's share is going for the city's water treatment plant to replace several high service pumps which are at the end of their useful life. The grant of $131.500 will complete funding on the $513,000 project. The city will also be receiving $125,000 for expansion and work on the Big Bend Ditch. That project's total cost is $250,000. The ditch needs to be expanded as a result of the current installation of a new storm sewer network on South Federal Boulevard that will empty into the ditch. Both grants are matched with city funds.
Other consensus fund grants include:
Town of Shoshoni: $175,000 to replace sewer lines.
Town of Pavillion: $46,177 for Cedar Street Paving
Town of Dubois: $100,000 for various water projects
Town of Dubois: $75,000 for Airport Right-of-Way rebuild
City of Lander: $375,000 for Dillon Subdivision street rehabilitation
Fremont County Fire Protection District: $500,000 for the Hudson Fire Hall replacement project
Fremont County Library: $573,000 Riverton Branch Library roof replacement and drainage project
Fremont County Transportation Department: $266,000 for Mortimore Lane project

subset: commoncrawl


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All bonds have a face value amount and a maturity date. You can think of a the maturity date as the end of a life for a bond. At the maturity date, the holder of a bond is paid the face value of the bond by the issuer. Lets say you buy at bond at … [Read more...]
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Junk Bonds – How to Analyze, Compare, and Buy High Yield Bonds
Junk bonds are bonds whose credit rating is lower than Baa3 for Moody's or BBB- for Standard & Poor's and Fitch Ratings. This means that they have a higher risk of default than investment grade bonds, and therefore offer a higher yield as well. … [Read more...]
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While the definition of interest remains the same no matter how that interest is paid, in order to suite the needs of both the entity issuing a bond, and the buyer of that bond, different bonds pay out their interest payments in different … [Read more...]
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Bonds issued by a corporation with a maturity of greater than one year are called corporate bonds. Below is a video summary on what you need to know before investing in corporate bonds. You can find the longer text version below the video. Embed … [Read more...]
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Bond Duration is a measurement of how long it takes for the price of a bond to be matched by the money it generates. Here is a video overview, and you can find the longer text version below. [vimeo]https://vimeo.com/50864826[/vimeo] Measured in … [Read more...]
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text:
Life is quite different here in 1876 and the roles children play in a family are significantly changed. Before 1870 when the Education Act was passed, boys at the age of 12 worked nine or ten hours a day including having their meals at work, leaving very little time to play. Younger children spent time in school, worked at chores or at jobs for low paying wages. Whenever they had free time which included an occasional evening and holidays would play outdoors with hoops, balls, marbles, skipping rope or spinning tops.
The poorer the family, the less that can be afforded in the way of toys. What is bought is purchased at penny bazaars, market stalls, fairs or from peddlers. These peddlers are often referred to as "chapmen" derived from the word "cheap" and they sell small books called "chapbooks" as well as poorly made wooden dolls and cheap tin soldiers. Other toys one might find in these poor households includes home-made kits, carts and dolls. Only at Christmas time will some of these children receive better toys from the Clergy or the local gentry.
A popular toyshop, the Toy Warehouse, became known as "Noah's Ark" because it was one of the main toys sold there. William Hamley, the shop's owner, took great pride in selling the very best toys that he could, the range of which included tin soldiers, rag dolls, doll houses, marbles, hoops, games, wooden puzzles, wooden hobby horses and later sporting equipment.
Other popular toyshops include C. N. Mackie's Magical Depot, W. H. Cremer, Morrell's of Burlington Arcade and J. S. Theobald & Co.
Popular toys also include toy pistols, drums and trumpets, the baby rattle, kites, tops, and building bricks. Books also were available with titles such as "Easy Words", "Easy Spelling", "The Child's Own Alphabet", "Droll Moral Tales" and "A Hundred Short Tales for Children."
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face mask?
- (noun) mask that provides a protective covering for the face in such sports as baseball or football or hockey
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President Mbeki of South Africa was subjected to a blistering attack from G-8 leaders for his abject failure to act in the role of mediator regarding the situation in Zimbabwe where his close friendship with President Mugabe has made him blind to the violence that has ripped apart the nation. In heated exchanges by President Bush, Chancellor Merkel of Germany and Prime Minister Stephen Harper of Canada, the South African leader was told he failed to do his job as mediator and unless things changed for the better, G-8 nations will institute economic sanctions against his close friend, Mugabe.
In Zimbabwe, Justice Minister Patrick Chinamasa told the press representatives of the Movement for Democratic Change had agreed to talks under the supervision of President Mbeki. "We have received communication that they are ready for a resumption of inter-party talks." However, Morgan Tsvangirai, head of MDC has made clear there will be no talks until violence ends against members of his group.


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Beniamino Schiavon Is Dead; Known as Mr. Nino of the Drake
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November 19, 1968
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Yellowstone hotspot
The Yellowstone hotspot, also referred to as the Snake River Plain-Yellowstone hotspot, is a volcanic hotspot responsible for large scale volcanism in Oregon, Nevada, Idaho, and Wyoming (in the United States) created as the North American tectonic plate moved across the Yellowstone hotspot. It formed the eastern Snake River Plain through a succession of caldera forming eruptions. The resulting calderas include the Island Park Caldera, the Henry's Fork Caldera, and the Bruneau-Jarbidge caldera. The hotspot currently lies under the Yellowstone Caldera.[1] The hotspot's most recent caldera forming supereruption, known as the Lava Creek eruption, took place 640,000 years ago and created the Lava Creek Tuff, and the most recent Yellowstone Caldera. The Yellowstone hotspot is one of a few volcanic hotspots underlying the North American tectonic plate; others include the Anahim and Raton hotspots.
Snake River Plain[edit]
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The eastern Snake River Plain is a topographic depression that cuts across Basin and Range Mountain structures, more or less parallel to North American plate motion. Beneath more recent basalts are rhyolite lavas and ignimbrites that erupted as the lithosphere passed over the hotspot. Younger volcanoes that erupted after passing over the hotspot covered the plain with young basalt lava flows in places, including Craters of the Moon National Monument.
The central Snake River plain is similar to the eastern plain, but differs by having thick sections of interbedded lacustrine (lake) and fluvial (stream) sediments, including the Hagerman Fossil Beds.
Nevada–Oregon calderas[edit]
Although the McDermitt volcanic field on the Nevada–Oregon border is frequently shown as the site of the initial impingement of the Yellowstone Hotspot, new geochronology and mapping demonstrates that the area affected by this mid-Miocene volcanism is significantly larger than previously appreciated.[2] Three silicic calderas have been newly identified in northwest Nevada, west of the McDermitt volcanic field as well as the Virgin Valley Caldera.[3] These calderas, along with the Virgin Valley Caldera and McDermitt Caldera, are interpreted to have formed during a short interval 16.5–15.5 million years ago, in the waning stage of the Steens flood basalt volcanism.[4] The northwest Nevada calderas have diameters ranging from 15–26 km and deposited high temperature rhyolite ignimbrites over approximately 5000 km2.
The Bruneau-Jarbidge caldera erupted between ten and twelve million years ago, spreading a thick blanket of ash in the Bruneau-Jarbidge event and forming a wide caldera. Animals were suffocated and burned in pyroclastic flows within a hundred miles of the event, and died of slow suffocation and starvation much farther away, notably at Ashfall Fossil Beds, located 1000 miles downwind in northeastern Nebraska, where a foot of ash was deposited. There, two hundred fossilized rhinoceros and many other animals were preserved in two meters of volcanic ash. By its characteristic chemical fingerprint and the distinctive size and shape of its crystals and glass shards, the volcano stands out among dozens of prominent ashfall horizons laid down in the Cretaceous, Paleogene, and Neogene periods of central North America. The event responsible for this fall of volcanic ash was identified as Bruneau-Jarbidge. Prevailing westerlies deposited distal ashfall over a vast area of the Great Plains.
Volcanic fields[edit]
Twin Falls and Picabo volcanic fields[edit]
The Twin Falls and Picabo volcanic fields were active about 10 million years ago. The Picabo Caldera was notable for producing the Arbon Valley Tuff 10.2 million years ago.
Heise volcanic field[edit]
The Heise volcanic field of eastern Idaho produced explosive caldera-forming eruptions which began 6.6 million years ago and lasted for more than 2 million years, sequentially producing four large-volume rhyolitic eruptions. The first three caldera-forming rhyolites — Blacktail Tuff, Walcott Tuff and Conant Creek Tuff — totaled at least 2250 km3 of erupted magma. The final, extremely voluminous, caldera-forming eruption — the Kilgore Tuff — which erupted 1800 km3 of ash, occurred 4.5 million years ago.[5][6][7][8][9]
Yellowstone Plateau[edit]
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The Yellowstone Plateau volcanic field is composed of four adjacent calderas. West Thumb Lake is itself formed by a smaller caldera[10] which erupted 174,000 years ago.[11] The Henry's Fork Caldera in Idaho was formed in an eruption of more than 280 km3 1.3 million years ago, and is the source of the Mesa Falls Tuff.[12] The Henry's Fork Caldera is nested inside of the Island Park Caldera and the calderas share a rim on the western side. The earlier Island Park Caldera is much larger and more oval and extends well into Yellowstone Park. Although much smaller than the Island Park Caldera, the Henry's Fork Caldera is still sizeable at 18 miles (29 km) long and 23 miles (37 km) wide and its curved rim is plainly visible from many locations in the Island Park area.
Of the many calderas formed by the Yellowstone Hotspot, including the later Yellowstone Caldera, the Henry's Fork Caldera is the only one that is currently clearly visible. The Henrys Fork of the Snake River flows through the Henry's Fork Caldera and drops out at Upper and Lower Mesa Falls. The caldera is bounded by the Ashton Hill on the south, Big Bend Ridge and Bishop Mountain on the west, by Thurburn Ridge on the North and by Black Mountain and the Madison Plateau on the east. The Henry's Fork caldera is in an area called Island Park. Harriman State Park is situated in the caldera.
The Island Park Caldera is older and much larger than the Henry's Fork Caldera with approximate dimensions of 58 miles (93 km) by 40 miles (64 km). It is the source of the Huckleberry Ridge Tuff that is found from southern California to the Mississippi River near St. Louis. This supereruption occurred 2.1 million years BP and produced 2500 km3 of ash. The Island Park Caldera is sometimes referred to as the First Phase Yellowstone Caldera or the Huckleberry Ridge Caldera. The youngest of the hotspot calderas, the Yellowstone Caldera, formed 640,000 years ago and is about 34 miles (55 km) by 45 miles (72 km) wide. Non-explosive eruptions of lava and less-violent explosive eruptions have occurred in and near the Yellowstone Caldera since the last super eruption. The most recent lava flow occurred about 70,000 years ago, while the largest violent eruption excavated the West Thumb of Lake Yellowstone around 150,000 years ago. Smaller steam explosions occur as well – an explosion 13,800 years ago left a 5 kilometer diameter crater at Mary Bay on the edge of Yellowstone Lake.
Both the Heise and Yellowstone volcanic fields produced a series of caldera-forming eruptions characterised by magmas with so-called "normal" oxygen isotope signatures (with heavy oxygen-18 isotopes) and a series of predominantly post-caldera magmas with so-called "light" oxygen isotope signatures (characterised as low in heavy oxygen-18 isotopes). The final stage of volcanism at Heise was marked by "light" magma eruptions. If Heise is any indication, this could mean that the Yellowstone Caldera has entered its final stage, but the volcano might still exit with a climactic fourth caldera event analogous to the fourth and final caldera-forming eruption of Heise (the Kilgore Tuff) – which was also made up of so-called "light" magmas. The appearance of "light" magmas would seem to indicate that the uppermost portion of the continental crust has largely been consumed by the earlier caldera forming events, exhausting the melting potential of the crust above the mantle plume. In this case Yellowstone could be expiring. It could be another 1–2 million years (as the North American Plate moves across the Yellowstone hotspot) before a new supervolcano is born to the northeast, and the Yellowstone Plateau volcanic field joins the ranks of its deceased ancestors in the Snake River Plain. (References to be added: Kathryn Watts (Nov 2007) GeoTimes "Yellowstone and Heise: Supervolcanoes that Lighten Up": Kathryn E. Watts, Ilya N. Bindeman and Axel K. Schmitt (2011) Petrology, Vol. 52, No. 5, "Large-volume Rhyolite Genesis in Caldera Complexes of the Snake River Plain: Insights from the Kilgore Tuff of the Heise Volcanic Field, Idaho, with Comparison to Yellowstone and Bruneau-Jarbidge Rhyolites" pp. 857–890).
Eruptive history[edit]
- Wapi Lava field and King's Bowl blowout, northeast of Rupert, Idaho; 2.270 ka ±0.15. (2,270 years ago)[14]
- Hell's Half Acre lava field, west to southwest of Idaho Falls; 3.250 ka ±0.15. (3,250 years ago)[15]
- Shoshone lava field, North of Twin Falls, Idaho; 8.400 ka ±0.3.[16]
- Craters of the Moon National Monument and Preserve; Great Rift of Idaho; the lava field was formed during eight eruptive episodes between about 15 and 2 ka.[17]
- Kings Bowl and Wapi lava fields formed about 2.250 ka.[18]
- Yellowstone Caldera; between 70 and 150 ka; 1,000 cubic kilometers (239.9 cu mi) intracaldera rhyolitic lava flows.[12]
- Yellowstone Caldera (size: 45 x 85 km); 640 ka; VEI 8; more than 1,000 cubic kilometers (240 cu mi) of Lava Creek Tuff.[12]
- Henry's Fork Caldera (size: 16 km wide); 1.3 Ma; VEI 7; 280 cubic kilometers (67.2 cu mi) of Mesa Falls Tuff.[12]
- Island Park Caldera (size: 100 x 50 km); 2.1 Ma; VEI 8; 2,450 cubic kilometers (588 cu mi) of Huckleberry Ridge Tuff.[12][19]
- Heise volcanic field, Idaho:
- Kilgore Caldera (size: 80 x 60 km); VEI 8; 1,800 cubic kilometers (432 cu mi) of Kilgore Tuff; 4.45 Ma ±0.05.[5][19]
- 4.49 Ma tuff of Heise[20]
- 5.37 Ma tuff of Elkhorn Springs[19]
- 5.51 Ma ±0.13 (Conant Creek Tuff)[5] (but Anders (2009): 5.94 Ma)[20]
- 5.6 Ma; 500 cubic kilometers (120 cu mi) of Blue Creek Tuff.[19]
- 5.81 Ma tuff of Wolverine Creek[20]
- 6.27 Ma ±0.04 (Walcott Tuff).[5]
- 6.57 Ma tuff of Edie School[20]
- Blacktail Caldera (size: 100 x 60 km); 6.62 Ma ±0.03; 1,500 cubic kilometers (360 cu mi) of Blacktail Tuff.[5][19]
- 7.48 Ma tuff of America Falls[20]
- 8.75 Ma tuff of Lost River Sinks[20]
- 9.17 Ma tuff of Kyle Canyon[20]
- 9.34 Ma tuff of Little Chokecherry Canyon[20]
- Twin Falls volcanic field, Twin Falls County, Idaho; 8.6 to 10 Ma.[20]
- Picabo volcanic field, Picabo, Idaho; 10.09 Ma (Arbon Valley Tuff A) and 10.21 Ma ±0.03 (Arbon Valley Tuff B).[5][20]
- Bruneau-Jarbidge volcanic field, Bruneau River/ Jarbidge River, Idaho; 10.0 to 12.5 Ma; Ashfall Fossil Beds eruption.[20]
- Owyhee-Humboldt volcanic field, Owyhee County, Idaho, Nevada, and Oregon; around 12.8 to 13.9 Ma.[20]
- McDermitt volcanic field, Orevada rift, McDermitt, Nevada/ Oregon (five overlapping and nested calderas; satellitic to these are two additional calderas), 20,000 km2 (7,700 sq mi):[21]
- Trout Creek Mountains, East of the Pueblo Mountains, Whitehorse Caldera (size: 15 km wide), Oregon; 15 Ma; 40 cubic kilometers (10 cu mi) of Whitehorse Creek Tuff.[19][22]
- Jordan Meadow Caldera, (size: 10–15 km wide); 15.6 Ma; 350 cubic kilometers (84 cu mi) Longridge Tuff member 2–3.[19][20][22][23]
- Longridge Caldera, (size: 33 km wide); 15.6 Ma; 400 cubic kilometers (96 cu mi) Longridge Tuff member 5.[19][20][22][23]
- Calavera Caldera, (size: 17 km wide); 15.7 Ma; 300 cubic kilometers (72 cu mi) of Double H Tuff.[19][20][22][23]
- Trout Creek Mountains, Pueblo Caldera (size: 20 x 10 km), Oregon; 15.8 Ma; 40 cubic kilometers (10 cu mi) of Trout Creek Mountains Tuff.[19][22][24]
- Hoppin Peaks Caldera, 16 Ma; Hoppin Peaks Tuff.[24]
- Washburn Caldera, (size: 30 x 25 km wide), Oregon; 16.548 Ma; 250 cubic kilometers (60 cu mi) of Oregon Canyon Tuff.[19][22][23]
- Yellowstone hotspot (?), Lake Owyhee volcanic field; 15.0 to 15.5 Ma.[25]
- Yellowstone hotspot (?), Northwest Nevada volcanic field, Virgin Valley, High Rock, Hog Ranch, and unnamed calderas; West of the Pine Forest Range, Nevada; 15.5 to 16.5 Ma; Tuffs: Idaho Canyon, Ashdown, Summit Lake, and Soldier Meadow.[3][26][27][28][29]
- Columbia River Basalt Province: Yellowstone hotspot sets off a huge pulse of volcanic activity, the first eruptions were near the Oregon-Idaho-Washington border. Columbia River and Steens flood basalts, Pueblo, and Malheur Gorge-region, Pueblo Mountains, Steens Mountain, Washington, Oregon, and Idaho, USA; most vigorous eruptions were from 14 to 17 Ma; 180,000 cubic kilometers (43,184 cu mi) of lava.[19][30][31][32][33][34][35][36]
- Crescent volcanics, Olympic Peninsula/ southern Vancouver Island, 50–60 Ma.[42]
- Siletz River Volcanics, Oregon Coast Range, a sequence of basaltic pillow lavas.
- Carmacks Group, Yukon, 63,000 square kilometers (24,324 sq mi), 70 Ma.[43][44][45]
- Harney Basin (Devine Canyon Tuff), McDermitt volcanic field, Owyhee-Humboldt volcanic field, Lake Owyhee volcanic field (or Jordan Valley volcanic field, Lake Owyhee), Jordan Craters, Santa Rosa – Calico volcanic field, Hawkes Valley – Lone Mountain volcanic field, Northwest Nevada volcanic field, Juniper Mountain caldera complex, and Silver City – Delamar caldera complex (Silver City, Idaho) are nested in one area. Geologic landmarks of the area: Steens Mountain, Northern Nevada Rift, Midas Trough, Santa Rosa Mountains, Bull Run – Tuscarora Mountains, Owyhee Mountains, Oregon-Idaho Graben, and western Snake River Plain.[37]
- Other manifestations of the Yellowstone hotspot: Rexburg Volcanic Field (4.3 Ma), West of Rexburg, Idaho; Henry's Lake Volcanism (1.3 Ma), Henry's Lake; Blackfoot Volcanic Field (3 Ma), Northwest of Soda Springs, Idaho; Gem Valley Volcanic Field (600 to 50 ka), near Grace, Idaho.[46]
- The initial volcanism is part of the Basin and Range Province and the Oregon-Idaho graben (15.0 to 15.5 Ma).
See also[edit]
- ^ Yellowstone Caldera, Wyoming, USGS
- ^ Brueseke, M.E.; Hart, W.K.; M.T. Heizler (2008). "Chemical and physical diversity of mid-Miocene silicic volcanism in northern Nevada". Bulletin of Volcanology. 70 (3): 343–360. Bibcode:2008BVol...70..343B. doi:10.1007/s00445-007-0142-5.
- ^ a b Matthew A. Coble & Gail A. Mahood (2008). New geologic evidence for additional 16.5–15.5 Ma silicic calderas in northwest Nevada related to initial impingement of the Yellowstone hot spot (PDF). Earth and Environmental Science 3. Collapse Calderas Workshop, IOP Conf. Series. doi:10.1088/1755-1307/3/1/012002. Retrieved 2010-03-23.
- ^ Brueseke, M.E., Heizler, M.T., Hart, W.K., Mertzman S.A. (15 March 2007). "Distribution and geochronology of Oregon Plateau (U.S.A.) flood basalt volcanism: The Steens Basalt revisited". Journal of Volcanology and Geothermal Research. 161 (3): 187–214. Bibcode:2007JVGR..161..187B. doi:10.1016/j.jvolgeores.2006.12.004.
- ^ a b c d e f Lisa A. Morgan & William C. McIntosh (March 2005). "Timing and development of the Heise volcanic field, Snake River Plain, Idaho, western USA". Geological Society of America Bulletin. 117 (3–4): 288–306. Bibcode:2005GSAB..117..288M. doi:10.1130/B25519.1.
- ^ Robert J. Fleck; Ted G. Theodore; Andrei Sarna-Wojcicki & Charles E. Meyer (1998). Richard M. Tosdal, eds. "Chapter 12, Age and possible source of air-fall tuffs of the Miocene Carlin Formation, Northern Nevada" (PDF). Contributions to the Gold Metallogeny of Northern Nevada, Open-File Report 98-338. U.S. Geological Survey. Retrieved 2010-03-26
- ^ Christiansen, R.L. (2001). "The Quaternary and Pliocene Yellowstone Plateau volcanic field of Wyoming, Idaho and Montana". U.S. Geol. Surv. Prof. Paper. 729: 146.
- ^ Lanphere, M.A.; Champion, D.E.; Christiansen, R.L.; Izett, G.A.; Obradovich, J.D. (2002). "Revised ages for tuffs of the Yellowstone Plateau volcanic field: Assignment of the Huckleberry Ridge Tuff to a new geomagnetic polarity event". Geol. Soc. Am. Bull. 114 (5): 559–568. Bibcode:2002GSAB..114..559L. doi:10.1130/0016-7606(2002)114<0559:RAFTOT>2.0.CO;2.
- ^ Pierce, K.L. & Morgan, L.A. (1992). Link, P.K., Kuntz, M.A., and Platt, L.B., eds. "The track of the Yellowstone hot spot: Volcanism, faulting, and uplift". Regional Geology of Eastern Idaho and Western Wyoming. Geological Society of America. Memoir 179: 1–52
- ^ West Thumb Lake is not to be confused with West Thumb Geyser Basin. The caldera created West Thumb Lake, and the underlying Yellowstone hotspot keeps West Thumb Geyser Basin active. See Fig. 22. See also File:Yellowstone Caldera map2.JPG.
- ^ Please refer to File:Yellowstone Caldera map2.JPG.
- ^ a b c d e "Yellowstone". Global Volcanism Program. Smithsonian Institution. Retrieved 2008-12-31.
- ^ "Yellowstone National Park Earthquake listings". Retrieved 2013-04-20.
- ^ http://imnh.isu.edu/digitalatlas/geo/greatrft/greatrft.htm
- ^ "Hell's Half Acre". Global Volcanism Program. Smithsonian Institution. Retrieved 2008-08-21.
- ^ "Shoshone Lava Field". Global Volcanism Program. Smithsonian Institution. Retrieved 2010-03-27.
- ^ "Craters of the Moon". Global Volcanism Program. Smithsonian Institution. Retrieved 2010-03-27.
- ^ "Wapi Lava Field". Global Volcanism Program. Smithsonian Institution. Retrieved 2010-03-27.
- ^ a b c d e f g h i j k l "Supplementary Table to P.L. Ward, Thin Solid Films (2009) Major volcanic eruptions and provinces" (PDF). Teton Tectonics. Retrieved 2010-03-16.
- ^ a b c d e f g h i j k l m n o "Mark H. Anders, associate professor: Yellowstone hotspot track". Columbia University, Lamont-Doherty Earth Observatory (LDEO). Retrieved 2010-03-16.
- ^ Rytuba, James J; McKee, Edwin H. "Peralkaline Ash Flow Tuffs and Calderas of the McDermitt Volcanic Field, Southeast Oregon and North Central Nevada" (abstract). Retrieved 2013-10-09.
The McDermitt volcanic field covers an area of 20,000 km2 in southeastern Oregon and northwestern Nevada and consists of seven large-volume ash flow sheets that vented from 16.1 to 15 Ma ago
- ^ a b c d e f Lipman, P.W. (Sep 30, 1984). "The Roots of Ash Flow Calderas in Western North America: Windows Into the Tops of Granitic Batholiths". Journal of Geophysical Research. 89 (B10): 8801–8841. Bibcode:1984JGR....89.8801L. doi:10.1029/JB089iB10p08801.
- ^ a b c d Steve Ludington; Dennis P. Cox; Kenneth W. Leonard & Barry C. Moring (1996). Donald A. Singer, eds. "Chapter 5, Cenozoic Volcanic Geology in Nevada". An Analysis of Nevada's Metal-Bearing Mineral Resources. Nevada Bureau of Mines and Geology, University of Nevada
- ^ a b Rytuba, J.J.; McKee, E.H. (1984). "Peralkaline ash flow tuffs and calderas of the McDermitt Volcanic Field, southwest Oregon and north central Nevada". Journal of Geophysical Research. 89 (B10): 8616–8628. Bibcode:1984JGR....89.8616R. doi:10.1029/JB089iB10p08616. Retrieved 2010-03-23.
- ^ Rytuba, James J.; John, David A.; McKee, Edwin H. (May 3–5, 2004). "Volcanism Associated with Eruption of the Steens Basalt and Inception of the Yellowstone Hotspot". Rocky Mountain (56th Annual) and Cordilleran (100th Annual) Joint Meeting. Paper No. 44-2. Retrieved 2010-03-26.
- ^ Noble, D.C. (1988). "Cenozoic volcanic rocks of the northwestern Great Basin: an overview". Spring Field Trip Guidebook, Special Publication No. 7. Geological Society of Nevada: 31–42
- ^ Castor, S.B. & Henry, C.D. (2000). "Geology, geochemistry, and origin of volcanic rock-hosted uranium deposits in northwest Nevada and southeastern Oregon, USA". Ore Geology Review. 16: 1–40. doi:10.1016/S0169-1368(99)00021-9.
- ^ Korringa, Marjorie K. (December 1973). "Linear vent area of the Soldier Meadow Tuff, an ash-flow sheet in northwestern Nevada". Geological Society of America Bulletin. 84 (12): 3849–3866. Bibcode:1973GSAB...84.3849K. doi:10.1130/0016-7606(1973)84<3849:LVAOTS>2.0.CO;2.
- ^ Matthew E. Brueseke & William K. Hart (2008). "Geology and Petrology of the Mid-Miocene Santa Rosa-Calico Volcanic Field, Northern Nevada" (PDF). Nevada Bureau of Mines and Geology. Bulletin 113: 44.
- ^ Carson, Robert J.; Pogue, Kevin R. (1996). Flood Basalts and Glacier Floods:Roadside Geology of Parts of Walla Walla, Franklin, and Columbia Counties, Washington. Washington State Department of Natural Resources (Washington Division of Geology and Earth Resources Information Circular 90). ISBN none.
- ^ Reidel, Stephen P. (January 2005). "A Lava Flow without a Source: The Cohasset Flow and Its Compositional Members". The Journal of Geology. 113: 1–21. Bibcode:2005JG....113....1R. doi:10.1086/425966.
- ^ Brueseke, M.E., Heizler, M.T., Hart, W.K., and S.A. Mertzman (15 March 2007). "Distribution and geochronology of Oregon Plateau (U.S.A.) flood basalt volcanism: The Steens Basalt revisited". Journal of Volcanology and Geothermal Research. 161 (3): 187–214. Bibcode:2007JVGR..161..187B. doi:10.1016/j.jvolgeores.2006.12.004.
- ^ SummitPost.org, Southeast Oregon Basin and Range
- ^ USGS, Andesitic and basaltic rocks on Steens Mountain
- ^ GeoScienceWorld, Genesis of flood basalts and Basin and Range volcanic rocks from Steens Mountain to the Malheur River Gorge, Oregon
- ^ "Oregon: A Geologic History. 8. Columbia River Basalt: the Yellowstone hot spot arrives in a flood of fire". Oregon Department of Geology and Mineral Industries. Retrieved 2010-03-26.
- ^ a b c "High Lava Plains Project, Geophysical & Geological Investigation, Understanding the Causes of Continental Intraplate Tectonomagmatism: A Case Study in the Pacific Northwest". Department of Terrestrial Magnetism, Carnegie Institution of Washington. Retrieved 2010-03-26.
- ^ Tolan, T.L., Reidel, S.P., Beeson, M.H., Anderson, J.L., Fecht, K.R. and Swanson, D.A. (1989). Reidel, S.P. and Hooper, P.R., eds. "Revisions to the estimates of the areal extent and volume of the Columbia River Basalt Group". Volcanism and tectonism in the Columbia River flood basalt province. Geol. Soc. Amer. Spec. Paper. 239: 1–20
- ^ Camp, V.E. & Ross, M.E. (2004). "Mantle dynamics and genesis of mafic magmatism in the intermontane Pacific Northwest". Journal of Geophysical Research. 109 (B08204): B08204. Bibcode:2004JGRB..10908204C. doi:10.1029/2003JB002838.
- ^ Carlson, R.W. & Hart, W.K. (1987). "Crustal Genesis on the Oregon Plateau". Journal of Geophysical Research. 92 (B7): 6191–6206. Bibcode:1987JGR....92.6191C. doi:10.1029/JB092iB07p06191.
- ^ Hart, W.K. & Carlson, R.W. (1985). "Distribution and geochronology of Steens Mountain-type basalts from the northwestern Great Basin". Isochron/West. 43: 5–10.
- ^ Murphy, J. Brendan; Andrew J. Hynes; Stephen T. Johnston; J. Duncan Keppie (2003). "Reconstructing the ancestral Yellowstone plume from accreted" (PDF). Tectonophysics. 365: 185– 194. Bibcode:2003Tectp.365..185M. doi:10.1016/S0040-1951(03)00022-2. Retrieved 13 June 2010.
- ^ Johnston, Stephen T.; P. Jane Wynne; Don Francis; Craig J. R. Hart; Randolph J. Enkin; David C. Engebretson (November 1996). "Yellowstone in Yukon: The Late Cretaceous Carmacks Group" (PDF). Geology. 24 (11): 997–1000. Bibcode:1996Geo....24..997J. doi:10.1130/0091-7613(1996)024<0997:YIYTLC>2.3.CO;2. Retrieved 10 June 2010.
- ^ McCausland, P. J. A.; D. T. A. Symons; C. J. R. Hart (2005). "Rethinking "Yellowstone in Yukon" and Baja British Columbia: Paleomagnetism of the Late Cretaceous Swede Dome stock, northern Canadian Cordillera". Journal Geophysical Research. 110 (B12107): 13. Bibcode:2005JGRB..11012107M. doi:10.1029/2005JB003742.
- ^ "O Ma large mafic magmatic events". www.largeigneousprovinces.org. Retrieved 2010-06-10.
- ^ "Snake River Plain-Yellowstone Hot Spot Migration" (PDF). Idaho Geological Survey. Retrieved 2010-03-26.
Map references[edit]
- "Mark H. Anders, associate professor: Yellowstone hotspot track". Columbia University, Lamont-Doherty Earth Observatory (LDEO). Retrieved 2010-03-16.
- "Map of Nevada" (PDF). Nevada Bureau of Mines and Geology, University of Nevada (NBMG). Retrieved 2010-03-25.
- "Shaded relief map of the northwestern United States" (PDF). Nevada Bureau of Mines and Geology, University of Nevada (NBMG). Retrieved 2010-03-26.
Further reading[edit]
- Smith, Robert B.; Jordan, Michael; Steinberger, Bernhard; Puskas, Christine M.; Farrell, Jamie; Waite, Gregory P.; Husen, Stephan; Chang, Wu-Lung; O'Connell, Richard (20 November 2009). "Geodynamics of the Yellowstone hotspot and mantle plume: Seismic and GPS imaging, kinematics and mantle flow" (PDF). Journal of Volcanology and Geothermal Research. 188 (1–3): 26–56. doi:10.1016/j.jvolgeores.2009.08.020.
- DeNosaquo, Katrina R.; Smith, Robert B.; Lowry, Anthony R. (20 November 2009). "Density and lithospheric strength models of the Yellowstone-Snake River Plain volcanic system from gravity and heat flow data". Journal of Volcanology and Geothermal Research. 188 (1–3): 108–127. doi:10.1016/j.jvolgeores.2009.08.006.
- Farrell, Jamie; Husen, Stephan; Smith, Robert B. (20 November 2009). "Earthquake swarm and b-value characterization of the Yellowstone volcano-tectonic system". Journal of Volcanology and Geothermal Research. 188 (1–3): 260–276. doi:10.1016/j.jvolgeores.2009.08.008.
- Perkins, Michael E.; Nash, Barbara P. (March 2002). "Explosive silicic volcanism of the Yellowstone hotspot: the ash fall tuff record". The Geological Society of America Bulletin. 114 (3): 367–381. Bibcode:2002GSAB..114..367P. doi:10.1130/0016-7606(2002)114<0367:ESVOTY>2.0.CO;2.
- Puskas, C.M.; Smith, R.B.; Meertens, C.M.; Chang, W.L. (2007). "Crustal deformation of the Yellowstone-Snake River Plain volcanic system: campaign and continuous GPS observations, 1987–2004". Journal of Geophysical Research. 112 (B03401): B03401. Bibcode:2007JGRB..11203401P. doi:10.1029/2006JB004325.
- Huang, Hsin-Hua; Lin, Fan-Chi; Schmandt, Brandon; Farrell, Jamie; Smith, Robert B.; Tsai, Victor C. (15 May 2015). "The Yellowstone magmatic system from the mantle plume to the upper crust". Science. 348 (6236): 773–776. doi:10.1126/science.aaa5648. PMID 25908659.
External links[edit]
- Yellowstone hotspot interactive
- National Park Service interactive map showing trace of the hotspot over time
- The Yellowstone magmatic system from the mantle plume to the upper crust (46,000 km3 magma reservoir below chamber)
- Yellowstone hotspot
- Hotspots of North America
- Volcanism of the Rocky Mountains
- Volcanism of Idaho
- Volcanism of Montana
- Volcanism of Nevada
- Volcanism of Oregon
- Volcanism of Washington (state)
- Volcanism of Wyoming
- Volcanism of Yukon
- Landforms of Yellowstone National Park
- Cretaceous volcanism
- Paleocene volcanism
- Eocene volcanism
- Miocene volcanism
- Pliocene volcanism
- Pleistocene volcanism
- Holocene volcanism
- Paleogene Idaho
- Paleogene Montana
- Paleogene geology of Oregon
- Paleogene geology of Washington (state)
- Paleogene geology of Wyoming
- Neogene Idaho
- Neogene Montana
- Neogene geology of Nevada
- Neogene geology of Oregon
- Neogene geology of Wyoming
- Paleocene North America
- Eocene North America
- Pleistocene North America
- Holocene North America
- Cretaceous United States
- Miocene United States
- Pliocene United States
- Pleistocene United States
- Quaternary Idaho
- Quaternary Nevada
- Quaternary Wyoming
- Quaternary United States


text:
Henrico voters face long lines at precincts
By Tom Lappas, Citizen Editor 11/06/12
UPDATED: 2:30 P.M. – Voting in Henrico County – viewed as one of several key swing counties in the nation in today's presidential election – was brisk this morning and early afternoon, with longer than normal lines reported countywide and many voters waiting an hour or more to cast their ballots.
But despite the crowds, Henrico Registrar Mark Coakley told the Citizen that he doesn't expect voter turnout today to exceed the county's 79.8 percent turnout rate in the 2008 presidential election.
That year, morning rain kept turnout slightly lower early in the day. Today, voters had only cold temperatures to deal with as they went to the polls. The morning rush should reduce the length of lines at Henrico's 92 precincts this evening, Coakley said.
President Barack Obama and Republican challenger Mitt Romney identified Henrico early in this campaign as the key swing county in Virginia, the potential key state in the election. Obama won the county by nearly 19,000 votes four years ago, turning a historically red county blue. His victory here that year was due in large part to his 23,000-vote advantage over Republican John McCain in the Fairfield and Varina districts.
For Romney to paint Henrico red today, he'll likely need to cut into Obama's margins in those two districts and attract more voters in the traditionally Republican Three Chopt and Tuckahoe districts, where McCain won by slightly less than 9,000 votes in 2008.
If Romney's margins in those two district offset Obama's margins in Fairfield and Varina, then the county's vote could come down to the Brookland District – which McCain won four years ago by just 42 votes out of the 37,219 cast there.
This is the first presidential election since the county shifted the lines of its magisterial districts slightly in 2011, following the 2010 U.S. census.
Only minor voting issues had been reported in Henrico as of 1:45 p.m. today. Power flickered at two precincts in the Fairfield District this morning, but Dominion Power crews quickly restored it and no votes were lost, Coakley said.
The number of absentee voters in the county was lower this year than in 2008 by about 4,000, Coakley said. But, at about 16,000, "it's still high," he said.
Henrico voters today also are helping select a replacement for outgoing U.S. Senator Jim Webb in a race contesting former governors George Allen, a Republican, and Tim Kaine, a Democrat. Webb defeated Allen six years ago to claim the seat.
Voters in the western portion of Henrico also are choosing between Republican incumbent Eric Cantor and Democrat Wayne Powell in the race for the 7th District U.S. House of Representatives seat, while voters in the eastern part of the county are choosing between Democratic incumbent Bobby Scott and Republican challenger Dean Longo.
Crime Stoppers' Crime of the Week: May 22, 2017
This week, Crime Stoppers needs your help to find the suspects vandalizing Dominion Energy equipment in Varina.
On Feb. 6 and May 3, someone shot at equipment belonging to Dominion Energy. Both incidents occurred near Kingsland Road between the hours of midnight and 3 a.m. The equipment was damaged, causing a major inconvenience to customers who lost power and posing a safety hazard to people nearby. > Read more.
On Feb. 6 and May 3, someone shot at equipment belonging to Dominion Energy. Both incidents occurred near Kingsland Road between the hours of midnight and 3 a.m. The equipment was damaged, causing a major inconvenience to customers who lost power and posing a safety hazard to people nearby. > Read more.
A place to excel
By Tom Lappas, Citizen Editor General News
It's no surprise when a business deal begins to take shape during a golf outing.
Perhaps less common is the business deal that percolates during a youth football practice. But such was the case for Varina District Supervisor Tyrone Nelson.
During a visit to former Varina High School football star Michael Robinson's football camp, Nelson was discussing with Robinson his excitement for the new Varina Library, whose opening last June was at that time forthcoming.
> Read more.
Perhaps less common is the business deal that percolates during a youth football practice. But such was the case for Varina District Supervisor Tyrone Nelson.
During a visit to former Varina High School football star Michael Robinson's football camp, Nelson was discussing with Robinson his excitement for the new Varina Library, whose opening last June was at that time forthcoming.
> Read more.
Business in brief
Citizen Staff Reports 05/22/2017 BusinessBusiness in Brief
Long & Foster Real Estate recently named Amy Enoch as the new manager of its Tuckahoe office. Enoch brings more than 15 years of real estate expertise to her new position, and she most recently led Long & Foster's Village of Midlothian office. Enoch has served in both sales and management positions during her tenure at Long & Foster. Prior to her real estate career, Enoch worked in information technology and hospitality. She is a graduate of Radford University, where she earned a Bachelor of Science degree in economics, English and history. Enoch has also received the designation of Graduate, Realtor Institute (GRI) from the National Association of Realtors, and this showcases her expertise in the fundamentals of real estate. > Read more.
Henrico recognized as a 2017 'Playful City USA' community
Citizen Staff Reports 05/21/2017 Features
A national nonprofit organization, KaBOOM!, has selected Henrico County as a 2017 Playful City USA community. The organization encourages communities to bring fun and balanced activities to children every day.
Henrico's selection is joined by the city of Richmond, town of Ashland, as well as the counties of Charles City, Chesterfield, Goochland, Hanover, New Kent and Powhatan. All of the localities make up the first region completely recognized through Playful City USA. > Read more.
Gallagher Foundation serves more than 14,000 teens in first year
Citizen Staff Reports 05/21/2017 FeaturesNon-Profits
In its first year, The Cameron K. Gallagher Foundation reached 14,000 teens through its programs from Spring 2016 to date. The foundation is dedicated to spreading positivity and erasing stigmas by educating and creating awareness on depression, anxiety and stress among teens. CKG delivers programs at schools, community events and its West End office.
"Students are in need of the information in the workshops, whether they know it or not, and they aren't getting it anywhere else," said Beth Curry, Director of Health and Wellness at The Steward School. > Read more.
Gallagher Foundation serves more than 14,000 teens in first year
Illegal voting in Virginia? Yes. Massive? Doubtful.
Tuckahoe meeting May 24 to address opioid crisis
32 Wegman's Short Pump employees receive college tuition scholarships
Henrico's Top Teachers - 2017
- More News
Print Edition
May. 18, 2017Current edition | Archive
Center for the Arts at Henrico H.S. to present 2017 Visual Art Senior Show
Weekend Top 10
Weekend Top 10
Restaurant Watch
Weekend Top 10
- More Entertainment
Obituary – Harold Gary Beard
Obituary – Rose Marie F. Mathews
Obituaries – Doris Fern Cook
- More Obituaries
New Active RVA certification recipient to be announced May 17
Anthem LemonAid opens registration for July 14-16
READ Center to hold free tutor training
- More Community
How to grow an adult
Make 'em take the pledge: no more snuff boxes!
Thanksgiving, Part II
- More Opinions
RIR to host Smithfield PWBA Tour Championship
RIR bringing back red stripes to track walls
Austin Dillon headlines Track Takeover at RIR
- More Sports
|May 2017
Place an Ad | More Classifieds
CalendarThe 13th annual Gallmeyer Farms Strawberry Fields Festival will take place from 10 a.m. to 5 p.m. at The Berry Patch, 3622 Darbytown Ct. in Varina. The festival features fresh local strawberries (pick your own or pre-picked), live music, food and craft vendors, free hay rides, pony rides ($5) and more. Coolers, chairs and picnics welcome. Admission and parking are free. No pets. For details, visit http://www.gallmeyerfarms.com. Full text


text:
Dragon Quest IX Gets Special Customer Service Hours
This is an important notice that you really should read.
Dragon Quest IX is just four days away from its Saturday release, and you know what that means! That's right! Extended hours for the Square Enix information center!
Sorry if you were expecting something more dramatic.
Square Enix posted notice today at its support page regarding extended hours in anticipation of DQIX's release. The support center, which is usually closed on Saturdays and Sundays, will run from 11:00 to 19:00 on both days this weekend.
This type of special treatment isn't reserved for DQIX only. Square Enix held special customer service hours for the Kingdom Hearts 358/2 Days release as well (yes, I wrote about it too). As it was then, the line is open to questions about any home video game.
The information center will presumably be more busy for DQIX than it was for Kingdom Hearts, especially since the latter will likely sell two to three million units over a couple of days. To ware the staffs' patience down, try speaking to them in English and, if they are unable to respond, suggest that they try out one of the DS's many fine English training programs.
If that doesn't work, complain about the whole single save file affair. I bet they aren't expecting any calls about that.


text:
EWWNP means Exploring Wild and Wonderful Number Patterns Created by Yourself! Investigate what happens if we create number patterns using some simple rules.
Find a great variety of ways of asking questions which make 8.
If you had any number of ordinary dice, what are the possible ways
of making their totals 6? What would the product of the dice be
each time?
If you are a teacher click here for a version of the problem suitable for classroom use, together with supporting materials. Otherwise, read on ...
On my calculator I divided one whole number by another whole number and got the answer $3.125$.
I know that both numbers were less than $50$, but can't remember what they were.
Can you work out what they were?
Once you've had a chance to think about it, click below to see how four different pupils began working on the task.
Here is Gemma and Flo's work:
Richard wrote the following:
He explained:
"I multiplied $3.125$ by $1$, then I tried multiplying $3.125$ by $2$, then I multiplied $3.125$ by $3$ ..."
Here is the start of Thomas' work:
Can you take each of these starting ideas and develop it into a solution?
Click here for a poster of this problem.


text:
Angels are around us everywhere, and there's no more welcomed angel than a guardian angel. Created in the spirit of compassion and genuine care, this beautiful angel can be personalized for a special person who deserves boundless love. Our angel of compassion and care is created by hand in stone resin, buffed, and then hand painted in a heavenly creme. Personalize this angel to create a truly special gift. Arrives in our serenely soft velvet bag.
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text:
Dishonored - Corvo's Folding Sword
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Cosplayer of things
Join Date: Dec 2006
Posts: 64
Originally Posted by
From the video, it looks like it would be EXTREMELY difficult to make it open exactly like the game.
Now, if you do want to have it so the blade sort of swings open like that, you will need to make the blade in a couple pieces, and offset the weight at the ends of each part. Hopefully that makes sense.
If you just wanted to have it spring open, that switchblade idea or butterfly knife (I think those are the names) like DarkCloud and Penlowe mentioned look pretty promising.
If you want more help, ask here or PM me, and I'll see what I can do.
Apparently it is a switch blade, the part that swings open making it look like a butterfly knife is just the mechanism that holds the blade parts.
This means that it would be a spring mechanism rather then a swing, or hinge *facepalm* which doesn't make life easy.
By your idea of the weights.... he blade is split into 2 sections so it fits in the handle,, If I make the bottom section act just like a switch blade,,, then weight the tip section, do you think the momentum of the bottom part moving out could potentially be enough to push the tip out?
Would you happen to know somewhere that sells metal sheets that i could try and make the blade from. Wood makes the blade too thick.
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text:
Carson City chooses new fire chief
CARSON CITY — Mark Crawfis has been a member of the Michigan National Guard for almost 30 years, a Carson City firefighter for 15 years and the assistant fire chief for 10 years.
It was only natural that he would be appointed the new fire chief.
Crawfis was announced as the new leader of the Carson City Fire Department at Tuesday night's Carson City Council meeting. Many of his firefighting colleagues attended the meeting to show their support.
Crawfis replaces Dan Kipp who recently stepped down as fire chief after a 13-year tenure. Kipp has relocated to Elm Hall and plans to focus on his new automotive manufacturing job in Mount Pleasant, as well as his family, including his fiancee Lisa, three children and one granddaughter.
Kipp, 46, became a firefighter 26 years ago when he was working at Carson City Hospital.
"A man I looked up to was (firefighter) Bill Fife," Kipp recalled. "He had a fire call come in and he saw me standing there and he said, 'What are you doing?' I said, 'Not much.' He said, 'Good, come along with me.' That was the first fire I went to."
Kipp went on to work under the supervision of Bob Brooks who was fire chief at that time before Kipp was named fire chief. He said he will miss "the camaraderie of family" with the fire department.
"We got some new fire trucks, a new air pack, we got our ISO rating lowered," Kipp recalled of his time with the fire department. "It wasn't just me, it was the department that made the accomplishments. It was a group effort as a family."
Crawfis, 51, was born and raised in Carson City, graduating from Carson City-Crystal High School in 1981. He is currently employed as an aircraft mechanic with the Michigan National Guard in Grand Ledge.
Crawfis recalls being inspired to join the Carson City Fire Department 15 years ago in part due to his great-uncle, who was on the Stanton Fire Department, and another uncle who was on the Crystal Township Fire Department.
"I was just looking for something else to do besides being in the Guard," he said. "I've stayed busy with it and I've enjoyed it ever since."
Crawfis said Kipp taught him a lot while they served together, including educating him about the city budget, different types of fire attacks, how to manage fire scenes and more. In return, Crawfis tried to pass on what he learned in the National Guard about aircraft incidents and hazardous materials.
Crawfis said a new assistant fire chief will be appointed in the near future, as well as a new captain to replace that position. In the meantime, Crawfis has some plans for the fire department.
"One of our major goals for the next five years is trying to get a new station that's big enough to handle all our equipment with some future growth," he said. "Right now we're very limited. There's not much room. We've been talking about it for four or five years and it seems like now the city is seeing our plight.
"I also want to get everybody back to the basics and reorganize our team into a family," he added. "We're down on numbers now. We need more people."
The Carson City Fire Department currently has about 14 volunteer firefighters. Anyone interested in becoming a firefighter can pick up an application at Carson City Hall or call Crawfis at (989) 763-6029.
"I wish Mark all the best of luck and bring them home alive," said Kipp of Carson City's new fire chief.


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This is the first of many posts on this topic. Seriously, isn't personal finance at least as important important as teaching post-modern analysis of Wuthering Heights?
PS–I don't know what the last sentence means. English majors, please don't write me.
Anyway, check out a letter my friend Ian Ybarra wrote to Student Financial Services at MIT.
I graduated (with a student loan) from MIT in June, 2004. And like all students with those credentials, I sat in an "exit interview," which surely consisted of my receiving a folder of papers and watching a really bad instructional video about paying off student loans.
Recently, I revisited that folder of student loan documentation. In addition to the papers stating the principal, interest, and repayment terms of my loan, there was your business card (how I knew to contact you) and a paper with the headings "The Danger of Credit Cards, 10 Facts Students Need to Know." Below those headings were, as promised, 10 facts students need to know — 10 terribly scary facts students need to know about very basic matters of personal finance, like…
#1 "Debt problems can lead to depression, which affects study habits, academic performance and retention rates."
#2 "Unfortunately, in a few extreme cases, the stress associated with credit card debt has been a factor in student suicides."
#4 "Some studies suggest that those students with credit card balances in excess of $1000 drink more, smoke more, use more prescriptions for
depression and have lower grade point averages than those who don't carry credit card debt."
#6 "Colleges and universities are the one group that makes money out of the credit card industry without bearing any responsibility for educating the students about the possible pitfalls and the devastating effect bad credit can have on their financial future. In return for lucrative fees, many colleges allow the banks and credit card companies to hawk their cards right on campus."
(Read all 10 at
Great information. Definitely good to know…4 years earlier, don't you think?
Fortunately, I didn't leave school with credit card debt, my GPA was solid, I didn't kill myself, and I didn't develop substance abuse problems. But what about the kids who weren't so fortunate?
Why were they not given this information when they entered MIT rather than when they left? Why are MIT students not exposed to the basics of personal finance — like those covered by Ramit Sethi's seminars
http://seminars.iwillteachyoutoberich.com/ — as part of their "entrance interviews," rather than being notified of what could have happened to them over the past four years as part of their "exit interviews"?
For as intelligent as MIT students are, I meet far too many new MIT graduates who have crazy credit card debt or don't even have credit cards in their own names or wonder what kind of music comes on MITFCU's CDs…the list goes on.
This seems broken. I hope that the people in your office are working to fix it.
Ian Ybarra
If you have ideas for how to fix this at your school, please send an email or add a comment.
Also check out Ian Ybarra's blog, one of the best I read about discovering what you really want to do.
Do you know your actual earning potential?
Get started with the Earning Potential quiz. Get a custom report based on your unique strengths, and discover how to start making extra money — in as little as an hour.
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'Game of Thrones' pays tribute to dead characters
Rose Leslie, left, and Richard Madden participate in the "Game of Thrones" panel on Day 3 of 2013 Comic-Con International on Friday, July 19, 2103, in San Diego. (Photo by Jordan Strauss/Invision/AP)
SAN DIEGO (AP) — It's wasn't hard for "Game of Thrones" to say goodbye to several characters at Comic-Con.
The panel for the fantasy HBO series kicked off Friday with an "in memoriam" segment set to Boyz II Men's "It's So Hard to Say Goodbye to Yesterday."
The [auth] tribute was dedicated to the scads of characters who've bitten the dust on the show, ranging from Khal Drogo to Wine Merchant to Catelyn Stark, the character played by Michelle Fairley who died in the infamous "Red Wedding" installment.
"I knew how many years I signed for, so I knew what was coming," said Fairley at the pop-culture convention.
The vicious slayings of many Westeros residents in the third season surprised many viewers, especially the brutal "Red Wedding" episode.
"We'd been waiting for it for so long and dreading it, and having it turn out better than we expected because of these actors was one of the greatest moments of my life," series co-creator David Benioff said.
"Game of Thrones" cast members Fairley, Peter Dinklage, John Bradley, Kit Harrington, Rose Leslie, Richard Madden and Emilia Clarke joined "A Song of Fire and Ice" mastermind George R.R. Martin and series co-creators Benioff and D.B. Weiss.
Martin said he needed to get to work finishing the two upcoming novels, "The Winds of Winter" and "A Dream of Spring," because the show is catching up with source material.
The crowd inside Hall H in the San Diego Convention Center shrieked when Khal Drago actor Jason Momoa stomped on stage and planted a smooch on Clarke, who continues to play his love interest Daenerys Targaryen, the Mother of Dragons, on the show.
Momoa screamed into the microphone, "I'm not dead, George!"
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Fredericksburg Hotspur, one of the Premier Development League's newest entrants, held a "meet the team" event at a local restaurant on Thursday night in preparation for their home opener, a 2:00 pm match against the West Virginia Chaos at the University of Mary Washington on Sunday.
The gathering was well attended by fans, friends and families whose children are part of Hotspur's parent club, the Fredericksburg Area Soccer Association. But its most remarkable aspect – and the key to long-term success for Hotspur and its female counterpart, the Impact, who kick off in W-League later this month – was the fact that so much of the squad is actually quite familiar to this tightly-knit community.
"The majority of these players have some connection to central Virginia soccer in some way or another," said head coach Carl Gray, who is also FASA's technical director and a longtime Virginia ODP coach. "Many of them have come up in this program right here. And we wanted that connection. I got plenty – plenty – of emails from internationals who wanted to come and play, from people from many other states who wanted to come in for tryouts.
"But being that this was our first year, I wanted to have as much local connection as possible. We did bring in a few players from out of state on recommendations of some coaches that I know down in South Carolina, West Virginia, Pennsylvania. But for the most part, it's local talent."
FASA has grown spectacularly in recent years, blossoming from a small recreational league into one of the state's largest elite clubs, and the creation of PDL and W-League teams reflect another ambitious step forward. But the organization has retained a family atmosphere that gives club officials hope that their new ventures will be well-received, not to mention well-attended, this summer.
Hotspur even has two brothers on the roster, Nate and Nick Foglesong. Both play their college soccer at Old Dominion University, where their older Bobby starred before moving on to join the Richmond Kickers' USL PRO team, and both are ecstatic at the opportunity to represent their club and their hometown while also preparing for fall NCAA action.
"FASA was the first travel team I ever played for, my first club team. I was eight years old," explained Nick at Thursday's event. "I was stuck in Norfolk the last two summers, playing for those teams, just waiting for something to come up here. The second we heard FASA [had a PDL team], we both just instantly came running back here and couldn't wait to play for this club again."
Hotspur's entry into PDL also offers role models for younger FASA players, and a clear development path from Under-5 level all the way up to the doorstep of the professional game.
"Growing up playing soccer, I always wanted to watch older guys play," noted Nick Foglesong. "You learn from experience and all these kids growing up in Fredericksburg, now they have an even higher level – rather than just an older club, they have a PDL team. It's something for them to get excited for, because they can work their way through the club."
Gray has also sprinkled his roster with experienced performers like Doug Boateng, a 25-year-old Elon University product with pro ambitions, and defender Daryl Ferguson, a former Real Maryland standout who has also represented Barbados at the international level. Hotspur lost their season opener at Virginia Beach last weekend, but Gray was encouraged to see his team compete well despite missing several college players due to final exams and only having one full training session beforehand.
Fredericksburg have limited information about the Chaos, Sunday's opponents. But Gray and his charges are focused on entertaining and inspiring the home fans while making positive strides in their own development.
"I just want to improve every game," said Gray. "The real measure of our success for our first year, though we're going to look real hard at the win-loss column, obviously, and nobody's more competitive than I am, is I want a core of guys who are committed to this program and who are going to want to come back next year. The program can flourish from there. The most important thing is building that foundation, making sure that we're accepted in the community."


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4 Responses to "JESUS H. CHRIST vs. SWAG: THE TROOF ABOUT ASAP ROCKY"
Sleezy Trees Says:
June 28th, 2012 at 1:01 pm
that black guy has clear reptilian features.
my guess would be that he is masonic, but i'm no expert.
The Lion Says:
June 28th, 2012 at 2:39 pm
LOL @ believing in God, the devil, or that ASAP Rocky is a good rapper. It would probably be easier to convince me of God's existence than it would be to convince me that ASAP has talent.
tracy Says:
June 29th, 2012 at 2:15 pm
This guy has a valid point and knows what he is talking about.
dj frank white Says:
June 29th, 2012 at 3:40 pm
Damn never heard Texas Mike talk so much in my life


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To the Editors:
It is unfortunate that in his otherwise excellent article "Global Energy: The Latest Infatuation" (May–June), Vaclav Smil fails to mention a certain, safe, low-tech, low-cost and immediately available method for reducing energy consumption: a sharp reduction in the human population of the Earth. If every woman, world-wide, were to limit her reproductive effort to one successful pregnancy or fewer, the demand for energy would begin to decrease significantly within a few years.
Werner G. HeimColorado Springs, CO
Dr. Smil responds:
Only a catastrophe (a global megawar or an asteroid impact killing hundreds of millions) could bring a "sharp reduction" in human population that could lead to a significant decrease of energy demand "within a few years." The only effective noncatastrophic way to moderate human numbers is by lowering total fertility. But doing so is necessarily a gradual process that, even when forced by government intervention, takes decades and may still result in massive increases in energy use. China, through its compulsory one-child policy introduced in 1978, has nearly halved its total fertility rate from about 3.0 children per adult woman during the late 1970s to just 1.54 in 2010. But during the same time its total energy use increased about 5.5 times and its average per capita consumption quadrupled.
You can find this online at http://www.americanscientist.org/issues/num2/2011/4/energy-and-population/1
© 2016 Sigma Xi, The Scientific Research Society


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Founded in 1995, the IBHM was established to educate individuals about the history and culture of African Americans, with special emphasis on African Americans in Idaho.
Housed in the historic St. Paul Baptist Church building and located in Boise's Julia Davis Park - the museum presents exhibits and provides educational and community outreach programs including lectures, films, workshops, literacy programs and musical performances. The museum's purpose is to build bridges between cultures to explore issues that affect Americans of all cultures and ethnicities.
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Hi all,
During the dot Astronomy meeting in Oxford last week ( www.dotastronomy.com ), Jill Tarter encouraged us to have a look at the results produced by the new setiQuest Explorer app ( http://setiquest.org/wiki/index.php/SetiQuest_Explorer ).
Below is a brief summary of the analysis we carried out, which was based on data kindly uploaded by Francis Potter at: https://github.com/hathersagegroup/seti/tree/master/exported_data/20110404
1. Merging the data
The data uploaded by Francis consists of separate CSV (text) files containing:
a) targets.csv: places in the sky that have been observed for the app;
b) observations.csv: times when a given target was observed;
c) assignments.csv: times when a portion of an observation was shown to a user;
d) pattern_marks.csv: places where users have marked a signal.
The data is stored in separate tables to avoid data duplication (data from a single observation are assigned to multiple users, but the details of the observation are only stored once). The tables refer to eachother using unique keys: target_id, observation_id, assignment_id, user_id...
For the purpose of inspecting the results, we merged the tables using the "crossmatching" function in the excellent TopCat data analysis tool ( http://www.star.bris.ac.uk/~mbt/topcat/ ).
This resulted in a single merged table containing one row per "marked signal", with columns that contain all details on the assignment/observation/target (table uploaded here: http://www.arm.ac.uk/~gba/dotastro/seti/merged.fits ).
2. Visualizing the signal marks
Having obtained the merged table, we inspected the results using scatter plots and histograms in TopCat. For example, a visualization of the "signal marks" as a function of user_id and target_id looked like this:
The plot shows that most of the "marked signals" are clustered near 1500 Mhz, 4000 Mhz and 8500 Mhz. This is simply due to the fact that the beta-version of the setiQuest Explorer app uses a limited number of observations which were obtained in only a few ~6 Mhz-wide frequency bands. The clustering will naturally disappear when observations in more bands of the spectrum are added in the future.
When zooming in on a particular band (e.g. 1415-1425 Mhz), a more uniform frequency distribution becomes apparent:
Now, the interesting question is: are any of the "marked signals" found by multiple users at the same frequency? Or across multiple targets at the same frequency? (the latter being an indication of local interference)
3. Binning the "signal marks" by frequency
To answer the question, we checked how many of the marked signals occur within the same ~0.5 kHz region that is shown to the user in a single screen. We did this using a "quick & dirty" Python script uploaded here:
In brief, the Python script checks how many "signal marks" are contained within a moving 1 kHz window in the frequency spectrum. When marks are found in a given window, the script writes the corresponding user_id's and the 'signal categories' to a new CSV file.
We spent some time interpreting the output of the script. However, we found only few "signal marks" in the same frequency window. This may be explained from the fact that the number of times multiple users have looked at the same piece of data is still too small at this early stage. (Unfortunately, the exported data does not yet contain the necessary info to compute how many users have looked at the same frequency... Francis; do you think you can add the "inspected frequency window" to assignments.csv ? That would be very interesting!)
I look forward to a more extensive analysis when more data is available. Keep marking signals people! :-)
Geert Barentsen
(student at Armagh Observatory - UK)


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I just purchased an SR*S exhaust pipe off ebay and it should arrive today.. would I need any extensive experience in installing the exhaust myself?
any help would be appreciated, I searched but I couldn't find a clear answer :x the place I could take it to charges $180 and it will take 3 hours? For some reason I don't think that price is at all worth it and/or I don't think it would take that long? please correct me if I'm wrong


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Has anyone ever tried to mold concrete around a fireplace? I have an idea in my head to cover my behemoth of fireplace in stained concrete. Any thoughts as to the pros and cons?
Has anyone ever tried to mold concrete around a fireplace? I have an idea in my head to cover my behemoth of fireplace in stained concrete. Any thoughts as to the pros and cons?
I haven't done it and suspect I never will, but I think it might be installed on metal lathe similar to stucco.
Another thing to do might be cover the brick with Arriscraft, a stone like product available different heights & lengths and 4" thick.
When you say "mold" concrete around the existing brick, I'm not sure if you really mean pouring concrete with a form or just plastering it.
Plastering it can be done and with a little work, you can put a float finish on it that comes out OK. If you're really talking about pouring concrete around it, yech! What a job! You're going to have to put up a form around the existing, that will be both strong and somewhat watertight. You should use a vibrator to make sure there are no voids in the concrete and you'll probably have to put in about 3-4" of concrete.
I'd also put in some reinforcing steel. Not a whole lot but some, maybe #3 rods, one foot on center, just to tie it all together. You might even get some welded wire reinforcing screen. Just use something.
Also, you'll want to make sure you tie it firmly to existing surfaces. The last thing you want is to see the whole front of the fireplace fall into your living room when it shrinks away from the existing surface.
Lastly, I'd give it some serious thought. Plastering it sure sounds like the way I'd go.
Good Luck.
I would suggest you talk to a good cement contractor about your idea. As was previously asked, are you going to stucco or really pour concrete? Neither idea is something you do on a whim, if you've never worked with concrete products before. Good Luck!
We are purchasing a home that has a traditional unpainted brick fireplace. We would like to add a modern touch by making it look like a smooth concrete finish. Another individual wrote you on this similar issue in February and you suggested using plaster. We are not wanting to stain the concrete or plaster but just would like it to look like concrete with a smooth gray finish. Would you still suggest plaster? If so, can it be spread over the brick with no preparation? And how thick would you suggest? Will it crack?
Proud to be suburban free.
Do you recomend Plaster? Or is there some other type of mortar or something that can be used and still get a fairly smooth surface?
Plaster is usually not as hard as concrete so you might find it chunks or crumbles if knocked into. I would say your best bet would be to fill in the mortar grooves flush with the brick face, and not try to cover the brick itself. Then find a paint you like and paint it so it looks like it's solid rather than brick.
Someone with more experience might have a different idea...I'm a newbie
Proud to be suburban free.


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Discussion in 'Great Skate Debate' started by Iceman, Oct 21, 2012.
Just a heads up that people have been posting their congratulations in the Matt Savoie Appreciation thread for the past few days as well: http://www.fsuniverse.net/forum/sho...ation-Thread&p=3714245&viewfull=1#post3714245
Congratulations to Matt and Brian. First Johnny, now Matt. Wonder how many other skaters will feel comfortable stepping out of the closet as they enjoy the right to marry, something others have taken for granted for far too long. (stepping off my soapbox)
Congratulations!!!! They are such an adorable couple. I wish Matt would do a few Disson shows.
Oddly, the other night, I ended up sitting next to the brother of someone who sang at Matt's wedding - and the event I was attending had NOTHING to do with figure skating. Truly a small world!
Congratulations to Matt! I'm so happy for him One of my all time favourite skaters!
What wonderful news to hear about Matt! His husband is very good looking too.
Congrats to the couple.
Congratulations to Matt and Brian!
Congrats to Matt and Brian!
How very cool! I wish them every happiness


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|Message view
|« Date » · « Thread »
|« Date » · « Thread »
|Albino B Neto <bin...@apache.org>
|Re: [PROPOSAL] "difficulty" field for Bugzilla
|Thu, 25 Oct 2012 11:32:04 GMT
Hi. On Wed, Oct 24, 2012 at 5:08 PM, Rob Weir <email@example.com> wrote: > As you have probably noticed, I'm engaged in a variety of initiatives > to grow the community, bring in more volunteers, etc. One additional > piece that I think would be useful is to add a new field to Bugzilla > to indicate the difficulty level of the bug. Of course, this will > often not be known. But in some cases, we do know, and where we do > know we can indicate this. > > What this allows us to do is then have search filters that return only > open easy bugs. These are ideal for new developer volunteers on the > project who are looking for items that match their lesser familiarity > with the code. It also allows a developer to step up to more > challenging bugs over time. > > A similar approach, which they called "easy hacks", was successfully > used by LibreOffice. > > If there are no objections, I'll add a new field to Bugzilla called > "cf_difficulty_level", and which a drop down UI with the following > choices: > > UNKNOWN (default) > TRIVIAL > EASY > MODERATE > HARD > WIZARD > > (I'm certainly open to variations on the names) > > I'd then rely on other developers to help "seed" the database with > some TRIVIAL and EASY bugs, so new volunteers will have something to > work with as they familiarize themselves with the project. > > I'll wait 72 hours, etc. > > Regards, > > -Rob +1 -- Albino
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Mike Gandy
|This article includes a list of references, related reading or external links, but its sources remain unclear because it lacks inline citations. (October 2014) (Learn how and when to remove this template message)
|No. 69
|Offensive tackle
|Personal information
|Date of birth:
|January 3, 1979
|Place of birth:
|Rockford, Illinois
|6 ft 4 in (1.93 m)
|316 lb (143 kg)
|Career information
|Notre Dame
|NFL Draft:
|2001 / Round: 3 / Pick: 68
|Career history
|Career NFL statistics
Michael Joseph Gandy (born January 3, 1979 in Rockford, Illinois) is a former American football offensive tackle. He was drafted by the Chicago Bears in the third round of the 2001 NFL Draft and later played for the Buffalo Bills and Arizona Cardinals. He played college football at the University of Notre Dame.
Professional career[edit]
Chicago Bears[edit]
He was drafted by the Chicago Bears in the third round of the 2001 NFL Draft and played with the team for four seasons.
Buffalo Bills[edit]
After the 2004 NFL season, Gandy signed with the Buffalo Bills, remaining with the team through the 2006 season.
Arizona Cardinals[edit]
On April 2, 2007, he signed with the Arizona Cardinals. After aggravating a pelvic/groin injury against the Titans in week 11 of the 2009 season that turned out to be season-ending, he was placed on injured reserve and released by the team after the season.
External links[edit]
- 1979 births
- Living people
- Garland High School alumni
- Sportspeople from Rockford, Illinois
- People from Dallas
- Players of American football from Illinois
- Players of American football from Texas
- American football offensive tackles
- American football offensive guards
- Notre Dame Fighting Irish football players
- Chicago Bears players
- Buffalo Bills players
- Arizona Cardinals players


text: DriverGear Fall Collection Has Something for Every VW Enthusiast Share Comments You may still be feeling the summer heat..but now's the time to prepare for cooler temperatures. The Volkswagen DriverGear Fall collection is here with hats, jackets and more. GTI enthusiasts should check out all the new items that have been added from the German collection. Shop now and be the envy of your friends with your new Fall DriverGear. Check it out at www.drivergear.vw.com.


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Flan napolitano receta
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topping 1/3 cup sugar 1 Tbsp water For the flan heavy cream - 1 1/2 cups whole milk
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in your homes and in your marriages. Receta en Español para Flan de Chocolate: AQUÍ Let us


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The Hypo Twins
On the band's MySpace page, The Hypo Twins eloquently describe their particular brand of rock as "disco party scum rock." If that gem of information doesn't inspire you to give their music a listen, I'm not sure what will. Not to mention that the band's description is not too far off the mark. The Scottsdale-based trio (lead singer Michael Loy, guitarist Jimi Johnson, and bassist Matt Brunsvold) are prototypical rock stars, in both image and music. Their songs are loud, fast, and heavy on guitars. What more could you ask for from a rock 'n' roll group? The group has built themselves a small but loyal fan base locally and nationally, thanks in large part to its loud, high-energy shows. The Hypo Twins have become something like regulars at the legendary L.A. music venue The Viper Room, where the band fits in quite nicely. The trio performs regularly in support of their four-track EP, It's Showtime, which was recently released on the independent label American Voodoo Records.
Wed., April 7, 2010
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