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The F-101 Voodoo was originally built as an escort fighter for USAF strategic bombers. Unfortunately for the Voodoo, the jet bombers coming on the line for the USAF--the B-47, B-52, and B-58--didn't require escorts. The F-101 was a good aircraft without a mission. The USAF began building the F-101A as a low-level strike fighter, because if there was one thing the Voodoo had, it was high speed at all altitudes. This led the USAF to consider: would the F-101 make a good tactical reconnaissance aircraft?
In response, McDonnell rebuilt two of the YF-101A prototypes as RF-101A testbeds. This replaced the fighter nose with a more "chisel" design that contained six cameras instead of radar and cannon. The RF-101A turned out to be a superb reconnaissance aircraft, and entered production on a limited basis. Further variants were developed from later Voodoo versions, namely the purpose-built RF-101C, which entered service in 1958.
The RF-101 gave the USAF its first supersonic reconnaissance aircraft, and largely replaced the RF-84F Thunderflash and RT-33A Shooting Star. Pilots liked its speed and responsiveness; it was capable of genuine aerobatics in the hands of a good pilot. RF-101s would first be used by the Republic of China Air Force (Taiwan), either flown by ROCAF or CIA pilots, over the Chinese mainland; the USAF's first combat usage would be the Cuban Missile Crisis of 1962. The RF-101's dash speed was such that it was tough to intercept, though not impossible.
This was found to be true over Vietnam as well, where the RF-101 was the backbone of USAF tactical reconnaissance until the later years of the war. The Voodoo's speed at altitude made it impervious to flak, and even the MiG-21 could not keep up with it. However, the RF-101s often had to get down low to "get the pictures," and that meant that barrage flak could bring down Voodoos. SAMs were also a threat at higher altitudes. After losses began to mount, the RF-101s were camouflaged, which helped some, but also slightly lowered their top speed. 39 RF-101s were lost over Vietnam.
With the age of the aircraft beginning to tell, the Voodoo was gradually relegated to second-line units, replaced by the RF-4C Phantom II. Some soldiered on in Air National Guard units, but all the RF-101s were gone by 1979. A handful remain in museums.
56-0214 joined the USAF in 1958, and was assigned to the 66th Tactical Reconnaissance Wing at Laon, France; the 66th later moved to RAF Upper Heyford, UK in 1966 when France withdrew from NATO. It returned stateside in 1969 to serve with the 363rd TRW at Shaw AFB, South Carolina, but was only with the 363rd a short time before going to the Air National Guard, first with the 189th TRG (Arkansas ANG) at Little Rock AFB, and then with the 186th TRG (Mississippi ANG) at Key Field. It was retired in 1979 and was donated to the Pima Air and Space Museum in 1982.
56-0214 is looking a bit worn: the Southeast Asia camouflage has faded, and her tail numbers are nonexistent. Most of the aircraft around it have been recently restored, so 56-0214 probably won't have much longer to wait.
Astute followers of my page may notice that the career history for 56-0214 is virtually identical to the other RF-101C I photographed in 2019--56-0229, on display at the Museum of Aviation at Robins AFB, Georgia.
left this sucker pretty unedited.
decided to snap some quick pics after dinner.
Thoughts
1. For Today's new cd Portraits is awesome.
2. Mexican food doesn't settle well but taste good.
3. Science channel is awesome.
4. I want Lightroom 2.
5. Jami Wilson is a zipperhead.
6. Alien Bees needs to release Cyber Commander already.
7. I'm interested to see what the new beauty dish looks like.
8. iPhone 3.0 firmware needs to be released NOW.
9. I need to wash/vacuum my car.
10. Zio's spicy chicken alfredo sounds good right now.
I managed to smash my index finger in a door today.
So the skin/flesh above the nail is nonexistent for now.
Thanks to Jami i have a cool spiderman band aid on it. haha
Strobist Info
A sculpture of a swan that I made from LEGO bricks. This is actually a combination of two different species of swans. I grabbed various characteristics from the two of them, making a probably nonexistent species. It took maybe 40 hours to design and build.
The head and feet are recycled parts from my old bird old bird, made a 1.5 years before this one. The old one fell off of a shelf, and I didn't want to repair it, so I made a better version.
The wings of this sculpture ended up being too heavy to sustain their own weight (although they are pretty durable), but the cross support holds them firmly in place.
Doubtful Sound is a very large and naturally imposing fjord (despite its name) in Fiordland, in the far south west of New Zealand. It is located in the same region as the smaller but more famous and accessible Milford Sound.
Doubtful Sound was named 'Doubtful Harbour' in 1770 by Captain Cook, who did not enter the inlet as he was uncertain whether it was navigable under sail. It was later renamed Doubtful Sound by whalers and sealers.
A Spanish scientific expedition commanded by Alessandro Malaspina visited Doubtful Sound in February 1793 to conduct experiments measuring the force of gravity using a pendulum, a part of the effort to establish a new metric system. The officers of the expedition, which included Felipe Bauzá y Cañas, a cartographer, also made the first chart of the entrance and lower parts of the Sound, naming features of it. Today these form a unique cluster of the only Spanish names on the map of New Zealand: Febrero Point, Bauza Island and the Nee Islets, Pendulo Reach and Malaspina Reach.
There are three distinct arms to the sound, which is the site of several large waterfalls, notably Helena Falls at Deep Cove, and the Browne Falls which have a fall of over 600 metres. The steep hills are known for their hundreds of waterfalls during the rainy season.
Access to the sound is either by sea, or by the Wilmot Pass road from the Manapouri Power Station. Most areas of the sound itself are only accessible by sea however, as the road network in this area of New Zealand is sparse or nonexistent, as is the human population.
Charles John Lyttelton, 10th Viscount Cobham, Governor-General of New Zealand (1957-1962) wrote about this part of Fiordland:
"There are just a few areas left in the world where no human has ever set foot. That one of them should be in a country so civilized and so advanced as New Zealand may seem incredible, unless one has visited the south-west corner of the South Island. Jagged razor backed mountains rear their heads into the sky. More than 200 days of rain a year ensure not a tree branch is left bare and brown, moss and epiphytes drape every nook. The forest is intensely green. This is big country... one day peaceful, a study in green and blue, the next melancholy and misty, with low cloud veiling the tops... an awesome place, with its granite precipices, its hanging valleys, its earthquake faults and its thundering cascades."
Doubtful Sound is unusual in that it contains two distinct layers of water that scarcely mix. The top few meters is fresh water, fed from the high inflows from the surrounding mountains, and stained brown with tannins from the forest. Below this is a layer of cold, heavy, saline water from the sea. The dark tannins in the fresh water layer makes it difficult for light to penetrate. Thus, many deep-sea species will grow in the comparatively shallow depths of the Sound.
This fiord is home to one of the southernmost population of bottlenose dolphins. The Doubtful Sound bottlenoses have formed a very insular sub-group of only about 70 individuals, with none having been observed to leave or enter the Sound during a multi-year monitoring regime. Their social grouping is thus extremely close, which is also partly attributed to the difficult and unusual features of their habitat, which is much colder than for other bottlenose groups and is also overlaid by the freshwater layer.
Other wildlife to be found in Doubtful Sound includes fur seals and penguins (Fiordland crested and blue), or even rare large whales (Southern Right Whale, Humpback Whale, Minke Whale, Sperm Whale and some Giant Beaked Whales. Orca, the Killer Whales and Long-Finned Pilot Whales can be found also. The waters of Doubtful Sound are also home to an abundance of sea creatures, including many species of fish, starfish, sea anemones and corals. It is perhaps best known for its black coral trees which occur in unusually shallow water for what is normally a deep water species.
The catchment basin of Doubtful Sound is generally steep terrain that is heavily forested except for locations where surface rock exposures are extensive. Nothofagus trees are dominant in many locations. In the understory there are a wide variety of shrubs and ferns.
I just got the hankering to do some night shooting. I set up in my backyard and shot this 22 minute exposure at ISO 200. Even though the exposure is 22 minutes, the noise is nonexistent.
Doubtful Sound is a very large and naturally imposing fjord (despite its name) in Fiordland, in the far south west of New Zealand. It is located in the same region as the smaller but more famous and accessible Milford Sound.
Doubtful Sound was named 'Doubtful Harbour' in 1770 by Captain Cook, who did not enter the inlet as he was uncertain whether it was navigable under sail. It was later renamed Doubtful Sound by whalers and sealers.
A Spanish scientific expedition commanded by Alessandro Malaspina visited Doubtful Sound in February 1793 to conduct experiments measuring the force of gravity using a pendulum, a part of the effort to establish a new metric system. The officers of the expedition, which included Felipe Bauzá y Cañas, a cartographer, also made the first chart of the entrance and lower parts of the Sound, naming features of it. Today these form a unique cluster of the only Spanish names on the map of New Zealand: Febrero Point, Bauza Island and the Nee Islets, Pendulo Reach and Malaspina Reach.
There are three distinct arms to the sound, which is the site of several large waterfalls, notably Helena Falls at Deep Cove, and the Browne Falls which have a fall of over 600 metres. The steep hills are known for their hundreds of waterfalls during the rainy season.
Access to the sound is either by sea, or by the Wilmot Pass road from the Manapouri Power Station. Most areas of the sound itself are only accessible by sea however, as the road network in this area of New Zealand is sparse or nonexistent, as is the human population.
Charles John Lyttelton, 10th Viscount Cobham, Governor-General of New Zealand (1957-1962) wrote about this part of Fiordland:
"There are just a few areas left in the world where no human has ever set foot. That one of them should be in a country so civilized and so advanced as New Zealand may seem incredible, unless one has visited the south-west corner of the South Island. Jagged razor backed mountains rear their heads into the sky. More than 200 days of rain a year ensure not a tree branch is left bare and brown, moss and epiphytes drape every nook. The forest is intensely green. This is big country... one day peaceful, a study in green and blue, the next melancholy and misty, with low cloud veiling the tops... an awesome place, with its granite precipices, its hanging valleys, its earthquake faults and its thundering cascades."
Doubtful Sound is unusual in that it contains two distinct layers of water that scarcely mix. The top few meters is fresh water, fed from the high inflows from the surrounding mountains, and stained brown with tannins from the forest. Below this is a layer of cold, heavy, saline water from the sea. The dark tannins in the fresh water layer makes it difficult for light to penetrate. Thus, many deep-sea species will grow in the comparatively shallow depths of the Sound.
This fiord is home to one of the southernmost population of bottlenose dolphins. The Doubtful Sound bottlenoses have formed a very insular sub-group of only about 70 individuals, with none having been observed to leave or enter the Sound during a multi-year monitoring regime. Their social grouping is thus extremely close, which is also partly attributed to the difficult and unusual features of their habitat, which is much colder than for other bottlenose groups and is also overlaid by the freshwater layer.
Other wildlife to be found in Doubtful Sound includes fur seals and penguins (Fiordland crested and blue), or even rare large whales (Southern Right Whale, Humpback Whale, Minke Whale, Sperm Whale and some Giant Beaked Whales. Orca, the Killer Whales and Long-Finned Pilot Whales can be found also. The waters of Doubtful Sound are also home to an abundance of sea creatures, including many species of fish, starfish, sea anemones and corals. It is perhaps best known for its black coral trees which occur in unusually shallow water for what is normally a deep water species.
The catchment basin of Doubtful Sound is generally steep terrain that is heavily forested except for locations where surface rock exposures are extensive. Nothofagus trees are dominant in many locations. In the understory there are a wide variety of shrubs and ferns.
www.factcheck.org/2022/09/scicheck-qa-on-omicron-updated-...
Q&A on Omicron-Updated COVID-19 Boosters
Earlier this month, the U.S. began administering the first COVID-19 booster vaccines that have been updated to better match the latest circulating coronavirus strains.
Many scientists expect the revised boosters will be more effective than their predecessors, but whether that’s the case and to what degree remains unknown.
The new vaccines, from mRNA vaccine makers Pfizer/BioNTech and Moderna, are bivalent, meaning that along with the original version of the coronavirus, or SARS-CoV-2, they also specifically target the BA.4 and BA.5 omicron subvariants. At the end of August, the Centers for Disease Control and Prevention estimated that together the two subvariants accounted for more than 90% of new COVID-19 cases in the U.S.
The Food and Drug Administration authorized the retooled boosters on Aug. 31, and the CDC signed off on the shots the following day, after the agency’s vaccine advisory committee voted 13 to 1 to recommend both boosters.
The authorizations mark a shift in American COVID-19 vaccination policy. In what’s being called a “fall booster ‘reset,’” people will no longer count the number of vaccine doses they’ve received. Instead, the guidelines are simple: If you’ve had your primary series (one dose of J&J or two doses Pfizer/BioNTech, Moderna or Novavax) and it’s been at least two months since your last dose, then you’re eligible for one omicron-updated booster.
We’ll explain how the new vaccines are different and what experts are saying about them.
How are the updated shots different from the original ones?
The revised boosters are essentially identical to the original ones, except for a tweak to some of the mRNA included in the shots.
For both Pfizer/BioNTech and Moderna, half of the mRNA in the vaccine includes the instructions used in the earlier vaccines for cells to make the spike protein of the original coronavirus strain. The other half includes the instructions for making the spike protein of the BA.4 and BA.5 strains, which is the same in the two subvariants. The spike proteins trigger a protective immune response in the body.
The dual components are why the boosters are referred to as “bivalent.” For the same reason, you may hear the original vaccines being called “monovalent.”
As before, the new Pfizer/BioNTech booster contains a total of 30 micrograms of mRNA, matching the dosage of the primary series shots, while the revamped Moderna booster contains a total of 50 micrograms, or half of the dosage of the primary series.
Who is eligible to get an updated booster?
People 12 years of age and older are eligible to receive Pfizer/BioNTech’s updated booster and adults 18 years or older are eligible to receive Moderna’s updated booster, two or more months after a previous COVID-19 vaccination.
It doesn’t matter if you’ve never been boosted or if you’ve received multiple boosters already — everyone who meets the age requirements and has had their primary vaccinations can get the updated booster as long as they are two months or more out from their last COVID-19 dose. (If you’re still not sure if you’re eligible, you can take an online quiz from the CDC to find out.)
The updated boosters are only authorized as booster shots, so they can’t be given to people as primary vaccinations. For the specified populations, the updated boosters are also replacing the earlier versions of the boosters, which are no longer authorized. As a result, all booster doses will be the bivalent ones — except for kids 5 to 11 years old, who are currently only eligible to receive Pfizer/BioNTech’s original booster dose for their age group.
What evidence supports the use of these omicron-updated boosters?
To authorize the updated boosters, the FDA borrowed its approach for influenza vaccines, which each year are modified to match the flu strains that are expected to circulate that season. Because the changes are only tweaks — and because it would be impractical if not impossible to test the vaccines in people prior to the flu season — flu vaccines are approved without doing clinical studies each year.
The omicron-updated boosters are similar in that they have not yet been evaluated in people, although there is other supporting evidence to suggest that they will work. For one, there is clinical data on a slightly different omicron-specific bivalent booster that targets the BA.1 subvariant that was dominant earlier this year.
Moderna tested this booster in about 600 adults who had received two primary doses and one original booster, and at least three months later were given a second original booster or a BA.1 bivalent booster. In blood tests, there was a stronger antibody response a month out in those who had received the BA.1 booster against both BA.1, BA.4/5 and the original virus, as well as against a variety of other variants.
The Pfizer/BioNTech BA.1 bivalent booster was tested in a similar way, in about 600 people over the age of 55, with a median of about six months in between the booster doses. At one month, the antibody responses to BA.1 were better in those who had received the BA.1 booster than the original, and the antibody responses to the original virus were similar in the two groups.
Although similar studies are being done in people for the BA.4/5 bivalent booster now, those results aren’t in yet. However, experiments from both companies show that mice previously vaccinated and then boosted with the bivalent BA.4/5 vaccines have higher BA.5 neutralizing antibody responses than those boosted with the original vaccine.
immune responses.
Still, some experts have been wary of moving forward with a new COVID-19 booster without human data on these specific vaccines. Dr. Pablo Sanchez, a professor of pediatrics at the Ohio State University and a member of the CDC’s vaccine advisory committee, ultimately voted against recommending the new boosters because of that concern.
“I voted no because I really feel that we need the human data,” he said during the meeting. “There’s a lot of vaccine hesitancy already. We need the human data.” Nonetheless, Sanchez said that, given his age, he was “almost sure” that he would take it.
The rest of the committee, though, felt comfortable enough, given the precedent with flu, to recommend the boosters.
Numerous other countries have opted to go with updated BA.1 bivalent vaccines, which do have clinical data (although the European Medicines Agency, which recommended BA.1-adapted boosters in early September, also recommended the BA.4/5 boosters on Sept. 12). The FDA, however, decided that the best strategy would be to target BA.4/5, since BA.1 is already no longer circulating.
The agency could have waited for the clinical data on BA.4/5, but thought that doing so would sacrifice too many lives. Estimates from the COVID-19 Scenario Modeling Hub suggest that delaying the booster campaign by a month would result in 137,000 more hospitalizations and 9,700 more deaths.
“We have to be a step ahead, or at least we have to try,” FDA chief Dr. Robert Califf explained in a press conference following the authorization of the new boosters. “Because if we waited for all the proof to come in, the wave will have already passed us by and the damage will have been done.”
E. John Wherry, an immunologist at the University of Pennsylvania, said the difference between BA.1- versus BA.4/5-targeted boosters was likely to be small, but given the choice, he would also opt for BA.5.
“This will not be the last version of the vaccine that we see,” he said. “Going with what’s here currently makes a lot of sense to me.”
As for when the human data on the bivalent BA.4/5 booster will be available, Dr. Peter Marks, the head of vaccines at the FDA, said on Aug. 31 that it would probably be at least until the end of September or October, “because of the time it takes to actually dose and then do the assays.”
How effective are the new boosters?
Scientists don’t know how well the redesigned shots will work. In theory, the omicron-updated boosters should be better than the original boosters in protecting against disease because they will more specifically target the coronavirus strains currently circulating — and some data suggest that will be the case.
It’s also possible the updated boosters will prevent more infections, although that protection will be short-lived.
But as the World Health Organization has said, “The full public health benefit of variant-updated vaccines and their value proposition over current vaccines can only be quantified once vaccine effectiveness data have been obtained.”
The real question is not whether the booster will increase protection — they will, scientists told us — but whether and to what degree the updated booster will be better than the original boosters.
Wherry said he thought the new boosters would be better, but the difference would likely be modest.
“I think it’s important to not give the false sense of hope that this new bivalent vaccine is going to be a magic bullet that stops all omicron viruses,” he said. “We should be expecting that they keep the most vulnerable people out of the hospital, but we should not be expecting them to completely protect from, say, mild disease.”
Dr. Paul A. Offit, a vaccine expert and pediatrician at the Children’s Hospital of Philadelphia, is not convinced that the updated boosters will be an improvement.
“I think they’re all going to be of value, I don’t think they’re necessarily going to be of any greater value than just boosting with the ancestral strain,” he said. “What worries me in all this is … that it’s sort of being oversold, being overpromised,” Offit added. “I just fear that people might be disappointed.”
How safe are the new boosters?
The exact formulation found in the new boosters has not yet been tested in people, but the revised vaccines are very similar to the original vaccines that have now been given hundreds of millions of times in the U.S. alone and have been shown to only very rarely result in serious side effects.
In addition, both companies tested the slightly different BA.1 omicron-specific bivalent booster in people, and found no new safety concerns. Vaccine recipients reported experiencing the same expected and temporary side effects as the original shots, including pain, redness and swelling at the injection site; fatigue; headache; muscle pain; and fever.
Given the similarity in design and manufacturing process as the original vaccines, the FDA felt very confident authorizing the boosters. Other experts also told us there is no reason to think that the revamped boosters will pose any new safety hazards. Offit, for example, said it was “extremely unlikely” that the new boosters would be any different in terms of safety.
Notably, Sanchez, the sole dissenter on the CDC’s advisory committee, explained after his “no” vote that while he felt there needed to be clinical data to be able to recommend the boosters, he was not that worried about safety.
“I am comfortable that the vaccine will likely be safe like the others,” he said, adding that he would almost certainly get the new booster himself.
Like the original vaccines, scientists do expect the updated shots will carry a small increased risk of myocarditis and pericarditis, or inflammation of the heart muscle and its surrounding tissue, particularly in young males. Most people who are affected by the rare side effect and are treated, the CDC says, feel better quickly.
Another issue being monitored by scientists is whether boosting could hurt a person’s ability to respond to a future variant, as we have written. But Wherry, who has been following this topic, said there is no indication that is a current risk. “From the data that exists, I see no concern about that whatsoever,” he said. Some animal studies suggest that giving an omicron-only vaccine as a first vaccine dose in animals could be detrimental, he added, but that’s not what is being given to people.
What do experts say about who should get the updated shots, and when?
There is broad agreement that older people and those at higher risk of developing severe COVID-19 should get the new boosters. But experts differ on whether young, healthy people should get another dose.
“I don’t think that a healthy young person who has already received three doses frankly needs another dose, because I think they are protected against serious illness,” Offit said. “After about six months after their last dose, they’re not going to be as protected against mild illness, but that’s true of all infections like this one, meaning short incubation period, mucosal infections.”
Offit still recommends that people over 75 years old, those with significant underlying health problems and those who are immunocompromised seek out the shots. Those are the groups, he said, that have benefited from the previous boosters.
But others think it’s reasonable to give the shots more widely, and that younger people should at least consider them.
“Most young, healthy people are protected from severe disease even after three doses and that protection is pretty durable,” Wherry said. The updated booster, he said, is primarily meant to protect the most vulnerable and to perhaps offer a little bit better protection from mild or moderate disease.
“If you’re over 65, everyone should get boosted,” he said. “If you have comorbidities or are immunosuppressed, absolutely get boosted.”
For younger people, Wherry said boosters are still a good idea, but there can be more individual choice — and that people shouldn’t think that the booster will make them impervious to infection.
“I would encourage people to think about their own behavior and when the right timing for the boost would be,” he said. “If you last got a dose of vaccine or were last infected three months ago and you’re a middle-aged, otherwise healthy individual, you may consider waiting a month or two and time your next dose closer to the holidays or closer to when there’s going to be more indoor activities so that peak level of antibodies coincides with when you’re going to be attending family gatherings or be inside more.”
Although two months is the minimum amount of time to wait since the last COVID-19 dose before getting the updated booster, many experts, including Offit and Wherry, suggest that people wait longer than that since last being vaccinated or being infected with SARS-CoV-2.
“The science really says for a young, healthy individual, you’re going to get the best boosting if you wait four to six months,” Wherry explained. “That allows for your memory B cells and memory T cells to mature a little bit, antibody levels to come down from their sort of max peak level after infection or vaccination.”
But for people who are older or have health problems, Wherry suggested consulting a doctor, because those individuals might need to get their doses sooner.
Is this the start of a shift to an annual COVID-19 vaccine?
Maybe. The Biden administration has presented this fall’s booster as the first of a once-a-year shot for COVID-19, similar to an annual seasonal flu vaccine. But while that could be a reasonable approach, it’s too early to truly know.
Some federal health officials have said as much, noting that new variants might disrupt those plans and that older or high-risk people might need more than one vaccine a year. Some experts, including Offit, are critical of the administration for getting ahead of itself on this question. Offit told us it was reasonable to target high-risk groups, but that young, healthy people may not need an annual boost.
Others are more comfortable with the concept. Wherry, for instance, said that given data that protection against severe disease begins to wane a little around nine months, the one-year time frame makes sense as “a benchmark for the average person” — and also is practical.
“A bit of aligning to traditional health care is an important part of this because it’s actually going to help with vaccine compliance, keeping up with what’s new,” he said, adding that there would remain flexibility for higher-risk people, who likely already interact more with the health care system, to get additional doses if needed.
Where can I get an updated booster?
You can find where the new boosters are available in your area by visiting Vaccines.gov. As with other COVID-19 vaccines, the reformulated boosters will be available at pharmacies, community health centers, and some clinics and doctor’s offices. But a lack of funding means they are less likely than the earlier shots to be available in various public health outreach efforts.
In some places, the boosters may be difficult to find at first. Certain locales have reported shortages of the Moderna vaccine in particular in the first weeks of the rollout, in part due to the delayed release of 10 million doses from a packaging plant in Indiana.
Again, the only booster available to people 12 years and older will be the updated one, so even if it’s not advertised as being new or bivalent, that’s what you will receive.
Are the shots still free?
Yes. The U.S. government has purchased more than 170 million doses of the updated boosters, and at this time, all COVID-19 vaccinations remain available to the public free of charge, regardless of immigration or insurance status.
The administration, however, has warned that without additional funding, it expects it will need to transition COVID-19 vaccine costs “to the commercial market” as early as January. When that occurs, the vaccines will likely be covered for most people with health insurance, similar to flu and other vaccines. People without insurance, however, would need to pay out of pocket.
Can I get my updated booster along with my flu shot?
Yes. Health officials are suggesting this pairing be offered to you this fall, since they know that getting both in one go is more convenient and increases the likelihood that you’ll get both vaccinations.
After one nearly nonexistent and one mild flu season — likely thanks to COVID-19 mitigation measures — some experts are concerned this flu season might be worse than normal. The relative lack of flu for two years running likely means there is less immunity in the population and more people will be susceptible. Clues from the Southern Hemisphere, which often presage flu severity in the North, have been mixed. Australia has had a bad flu season in terms of the number of cases, raising concerns — but other countries have not had particularly active seasons.
Regardless of how severe the flu season turns out to be, vaccination is still recommended. Several studies, along with surveillance data, indicate that getting a COVID-19 shot at the same time as a flu shot is safe and doesn’t reduce your immune response to either virus. The temporary, expected side effects of vaccination are usually on par with or only slightly worse in people getting both shots compared with those just getting a COVID-19 dose.
For some individuals, getting the shots together may make sense, but for others, the timing might not be ideal. The CDC recommends getting the flu shot in September or October, but many experts recommend October or later because vaccine protection against flu wanes and may not last the entire season if given too early. Still, getting the flu vaccine a bit early is better than not getting it at all.
If you opt for dual vaccination, you should get the two shots in different arms or in the same arm with the injections at least an inch apart.
This year, for the first time, the CDC is preferentially recommending that people over 65 years of age get a high dose or adjuvanted flu vaccine instead of a standard flu vaccine, given evidence that those shots may work better for this group.
When will kids be able to get updated shots?
Teens 12 and older are eligible for Pfizer/BioNTech’s omicron-updated booster, but the wait is likely to be at least a few more weeks for younger kids.
On Sept. 21, the head of vaccines at the FDA said that the agency was “only a matter of weeks away” from authorizing updated boosters for kids 5 to 11 years old and “a few months away” for children under 5. The day before, the CDC released a planning document saying it expected Pfizer/BioNTech’s booster for 5- through 11-year-olds and Moderna’s booster for 6- to 17-year-olds in “early to mid-October.”
Pfizer and BioNTech had previously said that they expect to submit their EUA application for updated boosters for children 5 through 11 years of age in early October and that they were pursuing an application for the youngest children down to 6 months.
As with the new boosters for those 12 and up, there may not be clinical data in children for the specific vaccine prior to authorization.
At the CDC’s advisory committee meeting, a Moderna representative said that the company would be completing its EUA submission for its original booster vaccine in kids 6 through 17 by mid-September. The company, she said, is currently conducting a study of primary series BA.1 bivalent vaccines and original and BA.1 bivalent boosters in children 6 months to 5 years old, which is expected to be finished by the end of 2022. She added that Moderna was “exploring” ways of testing BA.4/5 bivalent vaccines in children for use as primary vaccinations and boosters.
A slightly early Independence Day (Fourth of July) fireworks show over Lake Monona in the heart of the Wisconsin capital.
* Fireworks pictures in a sense are double exposures, at least multiple exposures.
* My ISO was set at 100. Nothing higher is needed or even desirable.
* White balance set to auto because in raw capture it does not matter.
* The technique used (and it's an old one) was to hold the shutter open for 10, 20, or 30 seconds at a time.
* The aperture is adjusted in the opposite direction to keep the exposure uniform. In this case I found that 10 seconds at f/8 worked well. 30 seconds at f/16 captured more bursts, but if the action was very heavy then too many bursts made for a busy, messy picture. I had to keep changing the settings.
* The camera was in full manual mode (otherwise it would change the exposure and focus).
* Because the display was 2 miles away the camera only needed to be focused at infinity.
* Solidly mounted on a sturdy tripod and tripped with an electronic cable release to insure there is no camera movement.
* Vibration reduction turned off (otherwise the VR would "hunt" for nonexistent movement and smear the shot). I nearly forgot this but I made a couple of test exposures early on and realized immediately that they were smeared due to the VR.
* I also turned off the Long Exposure Noise Reduction when I realized that it was doubling the time for the picture to load, and I knew I could minimize any noise in Lightroom. As it turned out little noise reduction was necessary beyond the standard.
* I worked in live view and kept the auto review on for two seconds for each shot to insure that I was getting what I thought I was getting. It’s enormously reassuring!
* With the shutter open for longer periods, more individual bursts are recorded on each frame. You have to shoot a lot of frames and hope to luck out. There is no way to plan it. You open the shutter, the stuff goes up, at the end of the time the shutter closes and you've got what you've got. I think I made about 75 exposures to get 19 that were good. The rest were trashed.
* Despite some 75 extended exposures, live view, and constant instant reviews, the battery at the end of 45 minutes of fireworks still had 60% charge. Turning off the noise reduction undoubtedly helped, plus made the shoot more efficient; no waiting.
Spaceship Earth, the iconic and symbolic structure of Epcot, opened with the park in Future World in 1982. The 18-story, 180-foot tall geosphere, whose design was conceived by Wallace Floyd Design Group and completed by Simpson Gumpertz & Heger Inc., is derived from the Class 2 geodesic polyhedron.
Each face of the polyhedron is divided into three isosceles triangles to form each point—with, in theory, 11,520 triangles forming 3,840 points (some are nonexistent due to supports and doors). The 15,520,000 pound sphere, with a circumference of 518.1 feet and a diameter of 165 feet, is raised 18-feet off the ground by three pylons sunk more than 120-feet into the ground.
Inside the sphere, guests take a 15-minute dark Omnimover ride in a "time machine" to learn how advancements in communication have helped create the future. Narrators have included Lawrence Dobkin, Walter Cronkite, Jeremy Irons and now Dame Judi Dench.
Constructed in 1928, the Waukegan Hotel is a 12-story highrise on the corner of Sheridan and Washington. It rivaled the Karcher, just down the street, as Waukegan's grandest hotel, and both share a very similar history.
The building earned a shady reputation at the start of downtown Waukegan's decline in the 1960s; preventing restoration efforts that were already in-talks back then from ever happening. Towards the end of its original life, the Waukegan had been converted to a nursing home before closing in 1980, and left abandoned for nearly 15 years. By the time a successful renovation finally took place in 1995, it had become infested with pigeons -- a Tribune article claims that over 20,000 lbs. of pigeon shit was removed from the building.
Resurrected originally as the Chateau Apartments - senior housing - the building later became low-income housing known as the Harborview Apartments; and from the sounds of it, everything spiraled downhill fast. It has universally-poor reviews on ApartmentRatings.com, listing complaints ranging from nonexistent management to unsanitary conditions and shady tenants left and right. Fortunately, new management picked the building up only a couple of years ago and renovated it into luxury condos. The building is now known as the 102 Washington Apartments.
The building has seen only a couple of major changes to its architecture over the years; the biggest being an extension grafted to the west facade. What it houses I am unsure of, but I am under the impression of stairs and/or elevators seeing-as, like the Karcher, the exterior fire escape was removed. The balconies are also a fairly-recent addition.
Doubtful Sound is a very large and naturally imposing fjord (despite its name) in Fiordland, in the far south west of New Zealand. It is located in the same region as the smaller but more famous and accessible Milford Sound.
Doubtful Sound was named 'Doubtful Harbour' in 1770 by Captain Cook, who did not enter the inlet as he was uncertain whether it was navigable under sail. It was later renamed Doubtful Sound by whalers and sealers.
A Spanish scientific expedition commanded by Alessandro Malaspina visited Doubtful Sound in February 1793 to conduct experiments measuring the force of gravity using a pendulum, a part of the effort to establish a new metric system. The officers of the expedition, which included Felipe Bauzá y Cañas, a cartographer, also made the first chart of the entrance and lower parts of the Sound, naming features of it. Today these form a unique cluster of the only Spanish names on the map of New Zealand: Febrero Point, Bauza Island and the Nee Islets, Pendulo Reach and Malaspina Reach.
There are three distinct arms to the sound, which is the site of several large waterfalls, notably Helena Falls at Deep Cove, and the Browne Falls which have a fall of over 600 metres. The steep hills are known for their hundreds of waterfalls during the rainy season.
Access to the sound is either by sea, or by the Wilmot Pass road from the Manapouri Power Station. Most areas of the sound itself are only accessible by sea however, as the road network in this area of New Zealand is sparse or nonexistent, as is the human population.
Charles John Lyttelton, 10th Viscount Cobham, Governor-General of New Zealand (1957-1962) wrote about this part of Fiordland:
"There are just a few areas left in the world where no human has ever set foot. That one of them should be in a country so civilized and so advanced as New Zealand may seem incredible, unless one has visited the south-west corner of the South Island. Jagged razor backed mountains rear their heads into the sky. More than 200 days of rain a year ensure not a tree branch is left bare and brown, moss and epiphytes drape every nook. The forest is intensely green. This is big country... one day peaceful, a study in green and blue, the next melancholy and misty, with low cloud veiling the tops... an awesome place, with its granite precipices, its hanging valleys, its earthquake faults and its thundering cascades."
Doubtful Sound is unusual in that it contains two distinct layers of water that scarcely mix. The top few meters is fresh water, fed from the high inflows from the surrounding mountains, and stained brown with tannins from the forest. Below this is a layer of cold, heavy, saline water from the sea. The dark tannins in the fresh water layer makes it difficult for light to penetrate. Thus, many deep-sea species will grow in the comparatively shallow depths of the Sound.
This fiord is home to one of the southernmost population of bottlenose dolphins. The Doubtful Sound bottlenoses have formed a very insular sub-group of only about 70 individuals, with none having been observed to leave or enter the Sound during a multi-year monitoring regime. Their social grouping is thus extremely close, which is also partly attributed to the difficult and unusual features of their habitat, which is much colder than for other bottlenose groups and is also overlaid by the freshwater layer.
Other wildlife to be found in Doubtful Sound includes fur seals and penguins (Fiordland crested and blue), or even rare large whales (Southern Right Whale, Humpback Whale, Minke Whale, Sperm Whale and some Giant Beaked Whales. Orca, the Killer Whales and Long-Finned Pilot Whales can be found also. The waters of Doubtful Sound are also home to an abundance of sea creatures, including many species of fish, starfish, sea anemones and corals. It is perhaps best known for its black coral trees which occur in unusually shallow water for what is normally a deep water species.
The catchment basin of Doubtful Sound is generally steep terrain that is heavily forested except for locations where surface rock exposures are extensive. Nothofagus trees are dominant in many locations. In the understory there are a wide variety of shrubs and ferns.
This is another Bold-Spotted Griburius, or Griburius rileyi, that I found in the garden this morning just after first light!
Being a newly described species to science means that the stats and facts I love to share are nonexistent. I will say, I believe this one to be a female, solely due to her larger size and darker coloration from the ones I usually spot! That's a trend thats relatively common among case-bearing beetles in the Cryptocephalinae subfamily, so it would track.
Speaking of her coloration, check it out! There's been no color correction applied to this photo, outside of whatever happens in my camera as I shoot the raw shot. There's a distinct darkening from sunflower to slightly short of saffron, and it's seriously stunning to see in person! The patterning on these beetles also reminds me of the jack-o-lanterns you see kids carve around Halloween, only to kick around early November.
If I find any of y'all kicking this beetle, though, there'll be some issues!
This shot was captured at 1:1 using my Vivitar (Komine) 90mm f2.8 Macro. This photo is uncropped. This rare and relatively recent resident is around 5mm long!
Doubtful Sound is a very large and naturally imposing fjord (despite its name) in Fiordland, in the far south west of New Zealand. It is located in the same region as the smaller but more famous and accessible Milford Sound.
Doubtful Sound was named 'Doubtful Harbour' in 1770 by Captain Cook, who did not enter the inlet as he was uncertain whether it was navigable under sail. It was later renamed Doubtful Sound by whalers and sealers.
A Spanish scientific expedition commanded by Alessandro Malaspina visited Doubtful Sound in February 1793 to conduct experiments measuring the force of gravity using a pendulum, a part of the effort to establish a new metric system. The officers of the expedition, which included Felipe Bauzá y Cañas, a cartographer, also made the first chart of the entrance and lower parts of the Sound, naming features of it. Today these form a unique cluster of the only Spanish names on the map of New Zealand: Febrero Point, Bauza Island and the Nee Islets, Pendulo Reach and Malaspina Reach.
There are three distinct arms to the sound, which is the site of several large waterfalls, notably Helena Falls at Deep Cove, and the Browne Falls which have a fall of over 600 metres. The steep hills are known for their hundreds of waterfalls during the rainy season.
Access to the sound is either by sea, or by the Wilmot Pass road from the Manapouri Power Station. Most areas of the sound itself are only accessible by sea however, as the road network in this area of New Zealand is sparse or nonexistent, as is the human population.
Charles John Lyttelton, 10th Viscount Cobham, Governor-General of New Zealand (1957-1962) wrote about this part of Fiordland:
"There are just a few areas left in the world where no human has ever set foot. That one of them should be in a country so civilized and so advanced as New Zealand may seem incredible, unless one has visited the south-west corner of the South Island. Jagged razor backed mountains rear their heads into the sky. More than 200 days of rain a year ensure not a tree branch is left bare and brown, moss and epiphytes drape every nook. The forest is intensely green. This is big country... one day peaceful, a study in green and blue, the next melancholy and misty, with low cloud veiling the tops... an awesome place, with its granite precipices, its hanging valleys, its earthquake faults and its thundering cascades."
Doubtful Sound is unusual in that it contains two distinct layers of water that scarcely mix. The top few meters is fresh water, fed from the high inflows from the surrounding mountains, and stained brown with tannins from the forest. Below this is a layer of cold, heavy, saline water from the sea. The dark tannins in the fresh water layer makes it difficult for light to penetrate. Thus, many deep-sea species will grow in the comparatively shallow depths of the Sound.
This fiord is home to one of the southernmost population of bottlenose dolphins. The Doubtful Sound bottlenoses have formed a very insular sub-group of only about 70 individuals, with none having been observed to leave or enter the Sound during a multi-year monitoring regime. Their social grouping is thus extremely close, which is also partly attributed to the difficult and unusual features of their habitat, which is much colder than for other bottlenose groups and is also overlaid by the freshwater layer.
Other wildlife to be found in Doubtful Sound includes fur seals and penguins (Fiordland crested and blue), or even rare large whales (Southern Right Whale, Humpback Whale, Minke Whale, Sperm Whale and some Giant Beaked Whales. Orca, the Killer Whales and Long-Finned Pilot Whales can be found also. The waters of Doubtful Sound are also home to an abundance of sea creatures, including many species of fish, starfish, sea anemones and corals. It is perhaps best known for its black coral trees which occur in unusually shallow water for what is normally a deep water species.
The catchment basin of Doubtful Sound is generally steep terrain that is heavily forested except for locations where surface rock exposures are extensive. Nothofagus trees are dominant in many locations. In the understory there are a wide variety of shrubs and ferns.
A modern computer hovers between the obsolescent and the nonexistent
Sidney Brenner
I found this broken down truck buried in the show near the entrance to
Joshin-Etsu Kogen National Park, Nagano Prefecture, Japan.
Why it Works: The diagonal border of the snow on the truck divides the frame in two. Then there’s the rust signifying the battle between things manmade and nature. Reference number: JA_110219_1252
Spaceship Earth, the iconic and symbolic structure of Epcot, opened with the park in Future World in 1982. The 18-story, 180-foot tall geosphere, whose design was conceived by Wallace Floyd Design Group and completed by Simpson Gumpertz & Heger Inc., is derived from the Class 2 geodesic polyhedron.
Each face of the polyhedron is divided into three isosceles triangles to form each point—with, in theory, 11,520 triangles forming 3,840 points (some are nonexistent due to supports and doors). The 15,520,000 pound sphere, with a circumference of 518.1 feet and a diameter of 165 feet, is raised 18-feet off the ground by three pylons sunk more than 120-feet into the ground.
Inside the sphere, guests take a 15-minute dark Omnimover ride in a "time machine" to learn how advancements in communication have helped create the future. Narrators have included Lawrence Dobkin, Walter Cronkite, Jeremy Irons and now Dame Judi Dench.
Oedipoda careulescens is a medium-sized grasshopper, between 15 and 21 mm for males and between 22 to 28 mm for females. The body coloration varies greatly depending on the substrate on which the animals have developed: reddish brown, gray, yellowish, or even completely dark or bright. The forewings are crossed most often by two or three pale bands, but the most striking characteristic, very visible when the insect flies away, is the bright coloration of the hind wings, a beautiful turquoise highlighted with a black marginal stripe. Furthermore, the posterior femora have a notch on their upper surface. At rest, confusion is possible with other Oedipoda species such as O. germanica.
Oedipoda caerulescens frequents dry areas with low and open vegetation: dunes, heathlands, grasslands on sand and sunlit limestone rocks. Many stations correspond to land recently used for human activities, such as coal spoil heaps, quarries and pits, the ballast of railway tracks, etc. It is exclusively a terrestrial insect, and its cryptic coloration often matches its substrate. The female lays her eggs in bare, dry soil. In this species, acoustic emissions are virtually nonexistent. The diet consists mainly of grasses.*
*Source: Wikipedia
This was my first time actually plane watching at Miami International Airport (MIA). I checked some spotter websites to find some good locations. They recommended The Holes as being an "official" site so we checked it out. I was pretty disappointed; there was a lot of construction going on and parking was nonexistent. My wife dropped me off. The area is totally exposed. Even though it was December it was pretty hot - no shade, no place to sit, no other people around. The holes are actually pretty small so it's hard to get a lens through the hole. Arrivals were almost impossible to shoot but you could see planes taxiing by for takeoff. After an hour I was cooking so we bagged it. We then went to the area close to the El Dorado furniture store. Much better. There were a bunch of spotters from around the world there. It was a great atmosphere. Nicely shaded, safe, close to some stores and a lot of good traffic to watch. I saw a bunch of planes from airlines I had not seen before, including some airlines I had not heard of. Some of the planes didn't show up on Flight Radar 24 so they were very pleasant surprises. All in all a very good day and I'd love to go back there!
I took these photos in December 2019.
Snakes are elongated, limbless, carnivorous reptiles of the suborder Serpentes Like all other squamates, snakes are ectothermic, amniote vertebrates covered in overlapping scales. Many species of snakes have skulls with several more joints than their lizard ancestors, enabling them to swallow prey much larger than their heads (cranial kinesis). To accommodate their narrow bodies, snakes' paired organs (such as kidneys) appear one in front of the other instead of side by side, and most have only one functional lung. Some species retain a pelvic girdle with a pair of vestigial claws on either side of the cloaca. Lizards have independently evolved elongate bodies without limbs or with greatly reduced limbs at least twenty-five times via convergent evolution, leading to many lineages of legless lizards. These resemble snakes, but several common groups of legless lizards have eyelids and external ears, which snakes lack, although this rule is not universal (see Amphisbaenia, Dibamidae, and Pygopodidae).
Living snakes are found on every continent except Antarctica, and on most smaller land masses; exceptions include some large islands, such as Ireland, Iceland, Greenland, the Hawaiian archipelago, and the islands of New Zealand, as well as many small islands of the Atlantic and central Pacific oceans. Additionally, sea snakes are widespread throughout the Indian and Pacific oceans. Around thirty families are currently recognized, comprising about 520 genera and about 3,900 species. They range in size from the tiny, 10.4 cm-long (4.1 in) Barbados threadsnake to the reticulated python of 6.95 meters (22.8 ft) in length. The fossil species Titanoboa cerrejonensis was 12.8 meters (42 ft) long. Snakes are thought to have evolved from either burrowing or aquatic lizards, perhaps during the Jurassic period, with the earliest known fossils dating to between 143 and 167 Ma ago. The diversity of modern snakes appeared during the Paleocene epoch (c. 66 to 56 Ma ago, after the Cretaceous–Paleogene extinction event). The oldest preserved descriptions of snakes can be found in the Brooklyn Papyrus.
Most species of snake are nonvenomous and those that have venom use it primarily to kill and subdue prey rather than for self-defense. Some possess venom that is potent enough to cause painful injury or death to humans. Nonvenomous snakes either swallow prey alive or kill by constriction.
Etymology
The English word snake comes from Old English snaca, itself from Proto-Germanic *snak-an- (cf. Germanic Schnake 'ring snake', Swedish snok 'grass snake'), from Proto-Indo-European root *(s)nēg-o- 'to crawl to creep', which also gave sneak as well as Sanskrit nāgá 'snake'. The word ousted adder, as adder went on to narrow in meaning, though in Old English næddre was the general word for snake. The other term, serpent, is from French, ultimately from Indo-European *serp- 'to creep', which also gave Ancient Greek ἕρπω (hérpō) 'I crawl' and Sanskrit sarpá ‘snake’.
The fossil record of snakes is relatively poor because snake skeletons are typically small and fragile making fossilization uncommon. Fossils readily identifiable as snakes (though often retaining hind limbs) first appear in the fossil record during the Cretaceous period. The earliest known true snake fossils (members of the crown group Serpentes) come from the marine simoliophiids, the oldest of which is the Late Cretaceous (Cenomanian age) Haasiophis terrasanctus from the West Bank, dated to between 112 and 94 million years old.
Based on comparative anatomy, there is consensus that snakes descended from lizards. Pythons and boas—primitive groups among modern snakes—have vestigial hind limbs: tiny, clawed digits known as anal spurs, which are used to grasp during mating The families Leptotyphlopidae and Typhlopidae also possess remnants of the pelvic girdle, appearing as horny projections when visible.
Front limbs are nonexistent in all known snakes. This is caused by the evolution of their Hox genes, controlling limb morphogenesis. The axial skeleton of the snakes' common ancestor, like most other tetrapods, had regional specializations consisting of cervical (neck), thoracic (chest), lumbar (lower back), sacral (pelvic), and caudal (tail) vertebrae. Early in snake evolution, the Hox gene expression in the axial skeleton responsible for the development of the thorax became dominant. As a result, the vertebrae anterior to the hindlimb buds (when present) all have the same thoracic-like identity (except from the atlas, axis, and 1–3 neck vertebrae). In other words, most of a snake's skeleton is an extremely extended thorax. Ribs are found exclusively on the thoracic vertebrae. Neck, lumbar and pelvic vertebrae are very reduced in number (only 2–10 lumbar and pelvic vertebrae are present), while only a short tail remains of the caudal vertebrae. However, the tail is still long enough to be of important use in many species, and is modified in some aquatic and tree-dwelling species.
Many modern snake groups originated during the Paleocene, alongside the adaptive radiation of mammals following the extinction of (non-avian) dinosaurs. The expansion of grasslands in North America also led to an explosive radiation among snakes. Previously, snakes were a minor component of the North American fauna, but during the Miocene, the number of species and their prevalence increased dramatically with the first appearances of vipers and elapids in North America and the significant diversification of Colubridae (including the origin of many modern genera such as Nerodia, Lampropeltis, Pituophis, and Pantherophis).
Fossils
There is fossil evidence to suggest that snakes may have evolved from burrowing lizards, during the Cretaceous Period. An early fossil snake relative, Najash rionegrina, was a two-legged burrowing animal with a sacrum, and was fully terrestrial. One extant analog of these putative ancestors is the earless monitor Lanthanotus of Borneo (though it also is semiaquatic). Subterranean species evolved bodies streamlined for burrowing, and eventually lost their limbs. According to this hypothesis, features such as the transparent, fused eyelids (brille) and loss of external ears evolved to cope with fossorial difficulties, such as scratched corneas and dirt in the ears. Some primitive snakes are known to have possessed hindlimbs, but their pelvic bones lacked a direct connection to the vertebrae. These include fossil species like Haasiophis, Pachyrhachis and Eupodophis, which are slightly older than Najash.
This hypothesis was strengthened in 2015 by the discovery of a 113-million-year-old fossil of a four-legged snake in Brazil that has been named Tetrapodophis amplectus. It has many snake-like features, is adapted for burrowing and its stomach indicates that it was preying on other animals. It is currently uncertain if Tetrapodophis is a snake or another species, in the squamate order, as a snake-like body has independently evolved at least 26 times. Tetrapodophis does not have distinctive snake features in its spine and skull. A study in 2021 places the animal in a group of extinct marine lizards from the Cretaceous period known as dolichosaurs and not directly related to snakes.
An alternative hypothesis, based on morphology, suggests the ancestors of snakes were related to mosasaurs—extinct aquatic reptiles from the Cretaceous—forming the clade Pythonomorpha. According to this hypothesis, the fused, transparent eyelids of snakes are thought to have evolved to combat marine conditions (corneal water loss through osmosis), and the external ears were lost through disuse in an aquatic environment. This ultimately led to an animal similar to today's sea snakes. In the Late Cretaceous, snakes recolonized land, and continued to diversify into today's snakes. Fossilized snake remains are known from early Late Cretaceous marine sediments, which is consistent with this hypothesis; particularly so, as they are older than the terrestrial Najash rionegrina. Similar skull structure, reduced or absent limbs, and other anatomical features found in both mosasaurs and snakes lead to a positive cladistical correlation, although some of these features are shared with varanids.
Genetic studies in recent years have indicated snakes are not as closely related to monitor lizards as was once believed—and therefore not to mosasaurs, the proposed ancestor in the aquatic scenario of their evolution. However, more evidence links mosasaurs to snakes than to varanids. Fragmented remains found from the Jurassic and Early Cretaceous indicate deeper fossil records for these groups, which may potentially refute either hypothesis.
Genetic basis of snake evolution
Main article: Limb development
Both fossils and phylogenetic studies demonstrate that snakes evolved from lizards, hence the question became which genetic changes led to limb loss in the snake ancestor. Limb loss is actually very common in extant reptiles and has happened dozens of times within skinks, anguids, and other lizards.
In 2016, two studies reported that limb loss in snakes is associated with DNA mutations in the Zone of Polarizing Activity Regulatory Sequence (ZRS), a regulatory region of the sonic hedgehog gene which is critically required for limb development. More advanced snakes have no remnants of limbs, but basal snakes such as pythons and boas do have traces of highly reduced, vestigial hind limbs. Python embryos even have fully developed hind limb buds, but their later development is stopped by the DNA mutations in the ZRS.
Distribution
There are about 3,900 species of snakes, ranging as far northward as the Arctic Circle in Scandinavia and southward through Australia. Snakes can be found on every continent except Antarctica, as well as in the sea, and as high as 16,000 feet (4,900 m) in the Himalayan Mountains of Asia. There are numerous islands from which snakes are absent, such as Ireland, Iceland, and New Zealand (although New Zealand's northern waters are infrequently visited by the yellow-bellied sea snake and the banded sea krait).
Taxonomy
All modern snakes are grouped within the suborder Serpentes in Linnean taxonomy, part of the order Squamata, though their precise placement within squamates remains controversial.
The two infraorders of Serpentes are Alethinophidia and Scolecophidia. This separation is based on morphological characteristics and mitochondrial DNA sequence similarity. Alethinophidia is sometimes split into Henophidia and Caenophidia, with the latter consisting of "colubroid" snakes (colubrids, vipers, elapids, hydrophiids, and atractaspids) and acrochordids, while the other alethinophidian families comprise Henophidia. While not extant today, the Madtsoiidae, a family of giant, primitive, python-like snakes, was around until 50,000 years ago in Australia, represented by genera such as Wonambi.
There are numerous debates in the systematics within the group. For instance, many sources classify Boidae and Pythonidae as one family, while some keep the Elapidae and Hydrophiidae (sea snakes) separate for practical reasons despite their extremely close relation.
Recent molecular studies support the monophyly of the clades of modern snakes, scolecophidians, typhlopids + anomalepidids, alethinophidians, core alethinophidians, uropeltids (Cylindrophis, Anomochilus, uropeltines), macrostomatans, booids, boids, pythonids and caenophidians.
Legless lizards
Main article: Legless lizard
While snakes are limbless reptiles, evolved from (and grouped with) lizards, there are many other species of lizards that have lost their limbs independently but which superficially look similar to snakes. These include the slowworm and glass snake.
Other serpentine tetrapods that are unrelated to snakes include caecilians (amphibians), amphisbaenians (near-lizard squamates), and the extinct aistopods (amphibians).
Biology
The now extinct Titanoboa cerrejonensis was 12.8 m (42 ft) in length. By comparison, the largest extant snakes are the reticulated python, measuring about 6.95 m (22.8 ft) long, and the green anaconda, which measures about 5.21 m (17.1 ft) long and is considered the heaviest snake on Earth at 97.5 kg (215 lb).
At the other end of the scale, the smallest extant snake is Leptotyphlops carlae, with a length of about 10.4 cm (4.1 in). Most snakes are fairly small animals, approximately 1 m (3.3 ft) in length.
Perception
Pit vipers, pythons, and some boas have infrared-sensitive receptors in deep grooves on the snout, allowing them to "see" the radiated heat of warm-blooded prey. In pit vipers, the grooves are located between the nostril and the eye in a large "pit" on each side of the head. Other infrared-sensitive snakes have multiple, smaller labial pits lining the upper lip, just below the nostrils.
A snake tracks its prey using smell, collecting airborne particles with its forked tongue, then passing them to the vomeronasal organ or Jacobson's organ in the mouth for examination. The fork in the tongue provides a sort of directional sense of smell and taste simultaneously. The snake's tongue is constantly in motion, sampling particles from the air, ground, and water, analyzing the chemicals found, and determining the presence of prey or predators in the local environment. In water-dwelling snakes, such as the anaconda, the tongue functions efficiently underwater.
The underside of a snake is very sensitive to vibration, allowing the snake to detect approaching animals by sensing faint vibrations in the ground. Despite the lack of outer ears, they are also able to detect airborne sounds.
Snake vision varies greatly between species. Some have keen eyesight and others are only able to distinguish light from dark, but the important trend is that a snake's visual perception is adequate enough to track movements. Generally, vision is best in tree-dwelling snakes and weakest in burrowing snakes. Some have binocular vision, where both eyes are capable of focusing on the same point, an example of this being the Asian vine snake. Most snakes focus by moving the lens back and forth in relation to the retina. Diurnal snakes have round pupils and many nocturnal snakes have slit pupils. Most species possess three visual pigments and are probably able to see two primary colors in daylight. The annulated sea snake and the genus Helicops appears to have regained much of their color vision as an adaption to the marine environment they live in. It has been concluded that the last common ancestors of all snakes had UV-sensitive vision, but most snakes that depend on their eyesight to hunt in daylight have evolved lenses that act like sunglasses for filtering out the UV-light, which probably also sharpens their vision by improving the contrast.
Skin
The skin of a snake is covered in scales. Contrary to the popular notion of snakes being slimy (because of possible confusion of snakes with worms), snakeskin has a smooth, dry texture. Most snakes use specialized belly scales to travel, allowing them to grip surfaces. The body scales may be smooth, keeled, or granular. The eyelids of a snake are transparent "spectacle" scales, also known as brille, which remain permanently closed.
The shedding of scales is called ecdysis (or in normal usage, molting or sloughing). Snakes shed the complete outer layer of skin in one piece. Snake scales are not discrete, but extensions of the epidermis—hence they are not shed separately but as a complete outer layer during each molt, akin to a sock being turned inside out.
Snakes have a wide diversity of skin coloration patterns which are often related to behavior, such as the tendency to have to flee from predators. Snakes that are at a high risk of predation tend to be plain, or have longitudinal stripes, providing few reference points to predators, thus allowing the snake to escape without being noticed. Plain snakes usually adopt active hunting strategies, as their pattern allows them to send little information to prey about motion. Blotched snakes usually use ambush-based strategies, likely because it helps them blend into an environment with irregularly shaped objects, like sticks or rocks. Spotted patterning can similarly help snakes to blend into their environment.
The shape and number of scales on the head, back, and belly are often characteristic and used for taxonomic purposes. Scales are named mainly according to their positions on the body. In "advanced" (Caenophidian) snakes, the broad belly scales and rows of dorsal scales correspond to the vertebrae, allowing these to be counted without the need for dissection.
Molting
Molting (or "ecdysis") serves a number of purposes. It allows old, worn skin to be replaced and it can remove parasites such as mites and ticks that live in the skin. It has also been observed in snakes that molting can be synced to mating cycles. Shedding skin can release pheromones and revitalize color and patterns of the skin to increase attraction of mates. Renewal of the skin by molting supposedly allows growth in some animals such as insects, but this has been disputed in the case of snakes.
Molting occurs periodically throughout the life of a snake. Before each molt, the snake stops eating and often hides or moves to a safe place. Just before shedding, the skin becomes dull and dry looking and the snake's eyes turn cloudy or blue-colored. The inner surface of the old skin liquefies, causing it to separate from the new skin beneath it. After a few days, the eyes become clear and the snake "crawls" out of its old skin, which splits close to the snake's mouth. The snake rubs its body against rough surfaces to aid in the shedding of its old skin. In many cases, the cast skin peels backward over the body from head to tail in one piece, like pulling a sock off inside-out, revealing a new, larger, brighter layer of skin which has formed underneath.
A young snake that is still growing may shed its skin up to four times a year, but an older snake may shed only once or twice a year. The discarded skin carries a perfect imprint of the scale pattern, so it is usually possible to identify the snake from the cast skin if it is reasonably intact. This periodic renewal has led to the snake being a symbol of healing and medicine, as pictured in the Rod of Asclepius.
Scale counts can sometimes be used to identify the sex of a snake when the species is not distinctly sexually dimorphic. A probe is fully inserted into the cloaca, marked at the point where it stops, then removed and measured against the subcaudal scales. The scalation count determines whether the snake is a male or female, as the hemipenes of a male will probe to a different depth (usually longer) than the cloaca of a female.
Skeleton
The skeletons of snakes are radically different from those of most other reptiles (as compared with the turtle here, for example), consisting almost entirely of an extended ribcage.
The skeleton of most snakes consists solely of the skull, hyoid, vertebral column, and ribs, though henophidian snakes retain vestiges of the pelvis and rear limbs.
The skull consists of a solid and complete neurocranium, to which many of the other bones are only loosely attached, particularly the highly mobile jaw bones, which facilitate manipulation and ingestion of large prey items. The left and right sides of the lower jaw are joined only by a flexible ligament at the anterior tips, allowing them to separate widely, and the posterior end of the lower jaw bones articulate with a quadrate bone, allowing further mobility. The mandible and quadrate bones can pick up ground-borne vibrations; because the sides of the lower jaw can move independently of one another, a snake resting its jaw on a surface has sensitive stereo auditory perception, used for detecting the position of prey. The jaw–quadrate–stapes pathway is capable of detecting vibrations on the angstrom scale, despite the absence of an outer ear and the lack of an impedance matching mechanism—provided by the ossicles in other vertebrates—for receiving vibrations from the air.
The hyoid is a small bone located posterior and ventral to the skull, in the 'neck' region, which serves as an attachment for the muscles of the snake's tongue, as it does in all other tetrapods.
The vertebral column consists of between 200 and 400 vertebrae, or sometimes more. The body vertebrae each have two ribs articulating with them. The tail vertebrae are comparatively few in number (often less than 20% of the total) and lack ribs. The vertebrae have projections that allow for strong muscle attachment, enabling locomotion without limbs.
Caudal autotomy (self-amputation of the tail), a feature found in some lizards, is absent in most snakes. In the rare cases where it does exist in snakes, caudal autotomy is intervertebral (meaning the separation of adjacent vertebrae), unlike that in lizards, which is intravertebral, i.e. the break happens along a predefined fracture plane present on a vertebra.
In some snakes, most notably boas and pythons, there are vestiges of the hindlimbs in the form of a pair of pelvic spurs. These small, claw-like protrusions on each side of the cloaca are the external portion of the vestigial hindlimb skeleton, which includes the remains of an ilium and femur.
Snakes are polyphyodonts with teeth that are continuously replaced
Snakes and other non-archosaur (crocodilians, dinosaurs + birds and allies) reptiles have a three-chambered heart that controls the circulatory system via the left and right atrium, and one ventricle. Internally, the ventricle is divided into three interconnected cavities: the cavum arteriosum, the cavum pulmonale, and the cavum venosum. The cavum venosum receives deoxygenated blood from the right atrium and the cavum arteriosum receives oxygenated blood from the left atrium. Located beneath the cavum venosum is the cavum pulmonale, which pumps blood to the pulmonary trunk.
The snake's heart is encased in a sac, called the pericardium, located at the bifurcation of the bronchi. The heart is able to move around, owing to the lack of a diaphragm; this adjustment protects the heart from potential damage when large ingested prey is passed through the esophagus. The spleen is attached to the gall bladder and pancreas and filters the blood. The thymus, located in fatty tissue above the heart, is responsible for the generation of immune cells in the blood. The cardiovascular system of snakes is unique for the presence of a renal portal system in which the blood from the snake's tail passes through the kidneys before returning to the heart.
The vestigial left lung is often small or sometimes even absent, as snakes' tubular bodies require all of their organs to be long and thin.[71] In the majority of species, only one lung is functional. This lung contains a vascularized anterior portion and a posterior portion that does not function in gas exchange. This 'saccular lung' is used for hydrostatic purposes to adjust buoyancy in some aquatic snakes and its function remains unknown in terrestrial species. Many organs that are paired, such as kidneys or reproductive organs, are staggered within the body, one located ahead of the other.
Snakes have no lymph nodes.
Venom
Cobras, vipers, and closely related species use venom to immobilize, injure, or kill their prey. The venom is modified saliva, delivered through fangs. The fangs of 'advanced' venomous snakes like viperids and elapids are hollow, allowing venom to be injected more effectively, and the fangs of rear-fanged snakes such as the boomslang simply have a groove on the posterior edge to channel venom into the wound. Snake venoms are often prey-specific, and their role in self-defense is secondary.
Venom, like all salivary secretions, is a predigestant that initiates the breakdown of food into soluble compounds, facilitating proper digestion. Even nonvenomous snakebites (like any animal bite) cause tissue damage.
Certain birds, mammals, and other snakes (such as kingsnakes) that prey on venomous snakes have developed resistance and even immunity to certain venoms.Venomous snakes include three families of snakes, and do not constitute a formal taxonomic classification group.
The colloquial term "poisonous snake" is generally an incorrect label for snakes. A poison is inhaled or ingested, whereas venom produced by snakes is injected into its victim via fangs. There are, however, two exceptions: Rhabdophis sequesters toxins from the toads it eats, then secretes them from nuchal glands to ward off predators; and a small unusual population of garter snakes in the US state of Oregon retains enough toxins in their livers from ingested newts to be effectively poisonous to small local predators (such as crows and foxes).
Snake venoms are complex mixtures of proteins, and are stored in venom glands at the back of the head. In all venomous snakes, these glands open through ducts into grooved or hollow teeth in the upper jaw. The proteins can potentially be a mix of neurotoxins (which attack the nervous system), hemotoxins (which attack the circulatory system), cytotoxins (which attack the cells directly), bungarotoxins (related to neurotoxins, but also directly affect muscle tissue), and many other toxins that affect the body in different ways. Almost all snake venom contains hyaluronidase, an enzyme that ensures rapid diffusion of the venom.
Venomous snakes that use hemotoxins usually have fangs in the front of their mouths, making it easier for them to inject the venom into their victims. Some snakes that use neurotoxins (such as the mangrove snake) have fangs in the back of their mouths, with the fangs curled backwards. This makes it difficult both for the snake to use its venom and for scientists to milk them. Elapids, however, such as cobras and kraits are proteroglyphous—they possess hollow fangs that cannot be erected toward the front of their mouths, and cannot "stab" like a viper. They must actually bite the victim.
It has been suggested that all snakes may be venomous to a certain degree, with harmless snakes having weak venom and no fangs. According to this theory, most snakes that are labelled "nonvenomous" would be considered harmless because they either lack a venom delivery method or are incapable of delivering enough to endanger a human. The theory postulates that snakes may have evolved from a common lizard ancestor that was venomous, and also that venomous lizards like the gila monster, beaded lizard, monitor lizards, and the now-extinct mosasaurs, may have derived from this same common ancestor. They share this "venom clade" with various other saurian species.
Venomous snakes are classified in two taxonomic families:
Elapids – cobras including king cobras, kraits, mambas, Australian copperheads, sea snakes, and coral snakes.
Viperids – vipers, rattlesnakes, copperheads/cottonmouths, and bushmasters.
There is a third family containing the opistoglyphous (rear-fanged) snakes (as well as the majority of other snake species):
Colubrids – boomslangs, tree snakes, vine snakes, cat snakes, although not all colubrids are venomous.
Reproduction
Although a wide range of reproductive modes are used by snakes, all employ internal fertilization. This is accomplished by means of paired, forked hemipenes, which are stored, inverted, in the male's tail. The hemipenes are often grooved, hooked, or spined—designed to grip the walls of the female's cloaca. The clitoris of the female snake consists of two structures located between the cloaca and the scent glands.
Most species of snakes lay eggs which they abandon shortly after laying. However, a few species (such as the king cobra) construct nests and stay in the vicinity of the hatchlings after incubation. Most pythons coil around their egg-clutches and remain with them until they hatch. A female python will not leave the eggs, except to occasionally bask in the sun or drink water. She will even "shiver" to generate heat to incubate the eggs.
Some species of snake are ovoviviparous and retain the eggs within their bodies until they are almost ready to hatch. Several species of snake, such as the boa constrictor and green anaconda, are fully viviparous, nourishing their young through a placenta as well as a yolk sac; this is highly unusual among reptiles, and normally found in requiem sharks or placental mammals. Retention of eggs and live birth are most often associated with colder environments.
Sexual selection in snakes is demonstrated by the 3,000 species that each use different tactics in acquiring mates. Ritual combat between males for the females they want to mate with includes topping, a behavior exhibited by most viperids in which one male will twist around the vertically elevated fore body of its opponent and force it downward. It is common for neck-biting to occur while the snakes are entwined.
Facultative parthenogenesis
Parthenogenesis is a natural form of reproduction in which growth and development of embryos occur without fertilization. Agkistrodon contortrix (copperhead) and Agkistrodon piscivorus (cottonmouth) can reproduce by facultative parthenogenesis, meaning that they are capable of switching from a sexual mode of reproduction to an asexual mode. The most likely type of parthenogenesis to occur is automixis with terminal fusion, a process in which two terminal products from the same meiosis fuse to form a diploid zygote. This process leads to genome-wide homozygosity, expression of deleterious recessive alleles, and often to developmental abnormalities. Both captive-born and wild-born copperheads and cottonmouths appear to be capable of this form of parthenogenesis.
Reproduction in squamate reptiles is almost exclusively sexual. Males ordinarily have a ZZ pair of sex-determining chromosomes, and females a ZW pair. However, the Colombian Rainbow boa (Epicrates maurus) can also reproduce by facultative parthenogenesis, resulting in production of WW female progeny. The WW females are likely produced by terminal automixis.
Embryonic Development
Snake embryonic development initially follows similar steps as any vertebrate embryo. The snake embryo begins as a zygote, undergoes rapid cell division, forms a germinal disc, also called a blastodisc, then undergoes gastrulation, neurulation, and organogenesis. Cell division and proliferation continues until an early snake embryo develops and the typical body shape of a snake can be observed. Multiple features differentiate the embryologic development of snakes from other vertebrates, two significant factors being the elongation of the body and the lack of limb development.
The elongation in snake body is accompanied by a significant increase in vertebra count (mice have 60 vertebrae, whereas snakes may have over 300). This increase in vertebrae is due to an increase in somites during embryogenesis, leading to an increased number of vertebrae which develop. Somites are formed at the presomitic mesoderm due to a set of oscillatory genes that direct the somitogenesis clock. The snake somitogenesis clock operates at a frequency 4 times that of a mouse (after correction for developmental time), creating more somites, and therefore creating more vertebrae. This difference in clock speed is believed to be caused by differences in Lunatic fringe gene expression, a gene involved in the somitogenesis clock.
There is ample literature focusing on the limb development/lack of development in snake embryos and the gene expression associated with the different stages. In basal snakes, such as the python, embryos in early development exhibit a hind limb bud that develops with some cartilage and a cartilaginous pelvic element, however this degenerates before hatching. This presence of vestigial development suggests that some snakes are still undergoing hind limb reduction before they are eliminated. There is no evidence in basal snakes of forelimb rudiments and no examples of snake forelimb bud initiation in embryo, so little is known regarding the loss of this trait. Recent studies suggests that hind limb reduction could be due to mutations in enhancers for the SSH gene, however other studies suggested that mutations within the Hox Genes or their enhancers could contribute to snake limblessness. Since multiple studies have found evidence suggesting different genes played a role in the loss of limbs in snakes, it is likely that multiple gene mutations had an additive effect leading to limb loss in snakes.
Behavior
Snake coiled on a stick in Oklahoma. It was brumating in a large pile of wood chips, found by this landscaper after he bulldozed the pile in late autumn 2018.
In regions where winters are too cold for snakes to tolerate while remaining active, local species will enter a period of brumation. Unlike hibernation, in which the dormant mammals are actually asleep, brumating reptiles are awake but inactive. Individual snakes may brumate in burrows, under rock piles, or inside fallen trees, or large numbers of snakes may clump together in hibernacula.
Feeding and diet
All snakes are strictly carnivorous, preying on small animals including lizards, frogs, other snakes, small mammals, birds, eggs, fish, snails, worms, and insects. Snakes cannot bite or tear their food to pieces so must swallow their prey whole. The eating habits of a snake are largely influenced by body size; smaller snakes eat smaller prey. Juvenile pythons might start out feeding on lizards or mice and graduate to small deer or antelope as an adult, for example.
The snake's jaw is a complex structure. Contrary to the popular belief that snakes can dislocate their jaws, they have an extremely flexible lower jaw, the two halves of which are not rigidly attached, and numerous other joints in the skull, which allow the snake to open its mouth wide enough to swallow prey whole, even if it is larger in diameter than the snake itself. For example, the African egg-eating snake has flexible jaws adapted for eating eggs much larger than the diameter of its head. This snake has no teeth, but does have bony protrusions on the inside edge of its spine, which it uses to break the shell when eating eggs.
The majority of snakes eat a variety of prey animals, but there is some specialization in certain species. King cobras and the Australian bandy-bandy consume other snakes. Species of the family Pareidae have more teeth on the right side of their mouths than on the left, as they mostly prey on snails and the shells usually spiral clockwise.
Some snakes have a venomous bite, which they use to kill their prey before eating it. Other snakes kill their prey by constriction, while some swallow their prey when it is still alive.
After eating, snakes become dormant to allow the process of digestion to take place; this is an intense activity, especially after consumption of large prey. In species that feed only sporadically, the entire intestine enters a reduced state between meals to conserve energy. The digestive system is then 'up-regulated' to full capacity within 48 hours of prey consumption. Being ectothermic ("cold-blooded"), the surrounding temperature plays an important role in the digestion process. The ideal temperature for snakes to digest food is 30 °C (86 °F). There is a huge amount of metabolic energy involved in a snake's digestion, for example the surface body temperature of the South American rattlesnake (Crotalus durissus) increases by as much as 1.2 °C (2.2 °F) during the digestive process. If a snake is disturbed after having eaten recently, it will often regurgitate its prey to be able to escape the perceived threat. When undisturbed, the digestive process is highly efficient; the snake's digestive enzymes dissolve and absorb everything but the prey's hair (or feathers) and claws, which are excreted along with waste.
Hooding and spitting
Hooding (expansion of the neck area) is a visual deterrent, mostly seen in cobras (elapids), and is primarily controlled by rib muscles.[98] Hooding can be accompanied by spitting venom towards the threatening object,[99] and producing a specialized sound; hissing. Studies on captive cobras showed that 13 to 22% of the body length is raised during hooding.
Locomotion
The lack of limbs does not impede the movement of snakes. They have developed several different modes of locomotion to deal with particular environments. Unlike the gaits of limbed animals, which form a continuum, each mode of snake locomotion is discrete and distinct from the others; transitions between modes are abrupt.
Lateral undulation
Lateral undulation is the sole mode of aquatic locomotion, and the most common mode of terrestrial locomotion In this mode, the body of the snake alternately flexes to the left and right, resulting in a series of rearward-moving "waves". While this movement appears rapid, snakes have rarely been documented moving faster than two body-lengths per second, often much less. This mode of movement has the same net cost of transport (calories burned per meter moved) as running in lizards of the same mass.
Terrestrial lateral undulation is the most common mode of terrestrial locomotion for most snake species. In this mode, the posteriorly moving waves push against contact points in the environment, such as rocks, twigs, irregularities in the soil, etc. Each of these environmental objects, in turn, generates a reaction force directed forward and towards the midline of the snake, resulting in forward thrust while the lateral components cancel out. The speed of this movement depends upon the density of push-points in the environment, with a medium density of about 8[clarification needed] along the snake's length being ideal. The wave speed is precisely the same as the snake speed, and as a result, every point on the snake's body follows the path of the point ahead of it, allowing snakes to move through very dense vegetation and small openings.
When swimming, the waves become larger as they move down the snake's body, and the wave travels backwards faster than the snake moves forwards. Thrust is generated by pushing their body against the water, resulting in the observed slip. In spite of overall similarities, studies show that the pattern of muscle activation is different in aquatic versus terrestrial lateral undulation, which justifies calling them separate modes. All snakes can laterally undulate forward (with backward-moving waves), but only sea snakes have been observed reversing the motion (moving backwards with forward-moving waves).
Sidewinding
Most often employed by colubroid snakes (colubrids, elapids, and vipers) when the snake must move in an environment that lacks irregularities to push against (rendering lateral undulation impossible), such as a slick mud flat, or a sand dune, sidewinding is a modified form of lateral undulation in which all of the body segments oriented in one direction remain in contact with the ground, while the other segments are lifted up, resulting in a peculiar "rolling" motion. This mode of locomotion overcomes the slippery nature of sand or mud by pushing off with only static portions on the body, thereby minimizing slipping. The static nature of the contact points can be shown from the tracks of a sidewinding snake, which show each belly scale imprint, without any smearing. This mode of locomotion has very low caloric cost, less than 1⁄3 of the cost for a lizard to move the same distance. Contrary to popular belief, there is no evidence that sidewinding is associated with the sand being hot.
Concertina
When push-points are absent, but there is not enough space to use sidewinding because of lateral constraints, such as in tunnels, snakes rely on concertina locomotion. In this mode, the snake braces the posterior portion of its body against the tunnel wall while the front of the snake extends and straightens. The front portion then flexes and forms an anchor point, and the posterior is straightened and pulled forwards. This mode of locomotion is slow and very demanding, up to seven times the cost of laterally undulating over the same distance. This high cost is due to the repeated stops and starts of portions of the body as well as the necessity of using active muscular effort to brace against the tunnel walls.
Arboreal
The movement of snakes in arboreal habitats has only recently been studied. While on tree branches, snakes use several modes of locomotion depending on species and bark texture. In general, snakes will use a modified form of concertina locomotion on smooth branches, but will laterally undulate if contact points are available. Snakes move faster on small branches and when contact points are present, in contrast to limbed animals, which do better on large branches with little 'clutter'.
Gliding snakes (Chrysopelea) of Southeast Asia launch themselves from branch tips, spreading their ribs and laterally undulating as they glide between trees. These snakes can perform a controlled glide for hundreds of feet depending upon launch altitude and can even turn in midair.
Rectilinear
The slowest mode of snake locomotion is rectilinear locomotion, which is also the only one where the snake does not need to bend its body laterally, though it may do so when turning. In this mode, the belly scales are lifted and pulled forward before being placed down and the body pulled over them. Waves of movement and stasis pass posteriorly, resulting in a series of ripples in the skin. The ribs of the snake do not move in this mode of locomotion and this method is most often used by large pythons, boas, and vipers when stalking prey across open ground as the snake's movements are subtle and harder to detect by their prey in this manner.
Interactions with humans
Snakes do not ordinarily prey on humans. Unless startled or injured, most snakes prefer to avoid contact and will not attack humans. With the exception of large constrictors, nonvenomous snakes are not a threat to humans. The bite of a nonvenomous snake is usually harmless; their teeth are not adapted for tearing or inflicting a deep puncture wound, but rather grabbing and holding. Although the possibility of infection and tissue damage is present in the bite of a nonvenomous snake, venomous snakes present far greater hazard to humans. The World Health Organization (WHO) lists snakebite under the "other neglected conditions" category.
Documented deaths resulting from snake bites are uncommon. Nonfatal bites from venomous snakes may result in the need for amputation of a limb or part thereof. Of the roughly 725 species of venomous snakes worldwide, only 250 are able to kill a human with one bite. Australia averages only one fatal snake bite per year. In India, 250,000 snakebites are recorded in a single year, with as many as 50,000 recorded initial deaths. The WHO estimates that on the order of 100,000 people die each year as a result of snake bites, and around three times as many amputations and other permanent disabilities are caused by snakebites annually.
The treatment for a snakebite is as variable as the bite itself. The most common and effective method is through antivenom (or antivenin), a serum made from the venom of the snake. Some antivenom is species-specific (monovalent) while some is made for use with multiple species in mind (polyvalent). In the United States for example, all species of venomous snakes are pit vipers, with the exception of the coral snake. To produce antivenom, a mixture of the venoms of the different species of rattlesnakes, copperheads, and cottonmouths is injected into the body of a horse in ever-increasing dosages until the horse is immunized. Blood is then extracted from the immunized horse. The serum is separated and further purified and freeze-dried. It is reconstituted with sterile water and becomes antivenom. For this reason, people who are allergic to horses are more likely to have an allergic reaction to antivenom. Antivenom for the more dangerous species (such as mambas, taipans, and cobras) is made in a similar manner in South Africa, Australia , and India, although these antivenoms are species-specific.
Snake charmers
In some parts of the world, especially in India, snake charming is a roadside show performed by a charmer. In such a show, the snake charmer carries a basket containing a snake that he seemingly charms by playing tunes with his flutelike musical instrument, to which the snake responds. The snake is in fact responding to the movement of the flute, not the sound it makes, as snakes lack external ears (though they do have internal ears).
The Wildlife Protection Act of 1972 in India technically prohibits snake charming on the grounds of reducing animal cruelty. Other types of snake charmers use a snake and mongoose show, where the two animals have a mock fight; however, this is not very common, as the animals may be seriously injured or killed. Snake charming as a profession is dying out in India because of competition from modern forms of entertainment and environment laws proscribing the practice. Many Indians have never seen snake charming and it is becoming a folktale of the past.
Trapping
The Irulas tribe of Andhra Pradesh and Tamil Nadu in India have been hunter-gatherers in the hot, dry plains forests, and have practiced the art of snake catching for generations. They have a vast knowledge of snakes in the field. They generally catch the snakes with the help of a simple stick. Earlier, the Irulas caught thousands of snakes for the snake-skin industry. After the complete ban of the snake-skin industry in India and protection of all snakes under the Indian Wildlife (Protection) Act 1972, they formed the Irula Snake Catcher's Cooperative and switched to catching snakes for removal of venom, releasing them in the wild after four extractions. The venom so collected is used for producing life-saving antivenom, biomedical research and for other medicinal products. The Irulas are also known to eat some of the snakes they catch and are very useful in rat extermination in the villages.
Despite the existence of snake charmers, there have also been professional snake catchers or wranglers. Modern-day snake trapping involves a herpetologist using a long stick with a V-shaped end. Some television show hosts, like Bill Haast, Austin Stevens, Steve Irwin, and Jeff Corwin, prefer to catch them using bare hands.
Consumption
Although snakes are not commonly thought of as food, their consumption is acceptable in some cultures and may even be considered a delicacy. Snake soup is popular in Cantonese cuisine, consumed by locals in the autumn to warm their bodies. Western cultures document the consumption of snakes only under extreme circumstances of hunger, with the exception of cooked rattlesnake meat, which is commonly consumed in Texas and parts of the Midwestern United States.
In Asian countries such as China, Taiwan, Thailand, Indonesia, Vietnam, and Cambodia, drinking the blood of a snake—particularly the cobra—is believed to increase sexual virility. When possible, the blood is drained while the cobra is still alive, and it is usually mixed with some form of liquor to improve the taste.
The use of snakes in alcohol is accepted in some Asian countries. In such cases, one or more snakes are left to steep in a jar or container of liquor, as this is claimed to make the liquor stronger (as well as more expensive). One example of this is the Habu snake, which is sometimes placed in the Okinawan liqueur Habushu (ハブ酒), also known as "Habu Sake".
Snake wine (蛇酒) is an alcoholic beverage produced by infusing whole snakes in rice wine or grain alcohol. First recorded as being consumed in China during the Western Zhou dynasty, this drink is considered an important curative and is believed to reinvigorate a person according to traditional Chinese medicine
Pets
In the Western world, some snakes are kept as pets, especially docile species such as the ball python and corn snake. To meet the demand, a captive breeding industry has developed. Snakes bred in captivity are considered preferable to specimens caught in the wild and tend to make better pets. Compared with more traditional types of companion animal, snakes can be very low-maintenance pets; they require minimal space, as most common species do not exceed 5 feet (1.5 m) in length, and can be fed relatively infrequently—usually once every five to 14 days. Certain snakes have a lifespan of more than 40 years if given proper care.
Symbolism
In ancient Mesopotamia, Nirah, the messenger god of Ištaran, was represented as a serpent on kudurrus, or boundary stones. Representations of two intertwined serpents are common in Sumerian art and Neo-Sumerian artwork and still appear sporadically on cylinder seals and amulets until as late as the thirteenth century BC. The horned viper (Cerastes cerastes) appears in Kassite and Neo-Assyrian kudurrus and is invoked in Assyrian texts as a magical protective entity. A dragon-like creature with horns, the body and neck of a snake, the forelegs of a lion, and the hind-legs of a bird appears in Mesopotamian art from the Akkadian Period until the Hellenistic Period (323 BC–31 BC). This creature, known in Akkadian as the mušḫuššu, meaning "furious serpent", was used as a symbol for particular deities and also as a general protective emblem. It seems to have originally been the attendant of the Underworld god Ninazu, but later became the attendant to the Hurrian storm-god Tishpak, as well as, later, Ninazu's son Ningishzida, the Babylonian national god Marduk, the scribal god Nabu, and the Assyrian national god Ashur.
In Egyptian history, the snake occupies a primary role with the Nile cobra adorning the crown of the pharaoh in ancient times. It was worshipped as one of the gods and was also used for sinister purposes: murder of an adversary and ritual suicide (Cleopatra). The ouroboros was a well-known ancient Egyptian symbol of a serpent swallowing its own tail. The precursor to the ouroboros was the "Many-Faced", a serpent with five heads, who, according to the Amduat, the oldest surviving Book of the Afterlife, was said to coil around the corpse of the sun god Ra protectively. The earliest surviving depiction of a "true" ouroboros comes from the gilded shrines in the tomb of Tutankhamun. In the early centuries AD, the ouroboros was adopted as a symbol by Gnostic Christians and chapter 136 of the Pistis Sophia, an early Gnostic text, describes "a great dragon whose tail is in its mouth". In medieval alchemy, the ouroboros became a typical western dragon with wings, legs, and a tail.
In the Bible, King Nahash of Ammon, whose name means "Snake", is depicted very negatively, as a particularly cruel and despicable enemy of the ancient Hebrews.
The ancient Greeks used the Gorgoneion, a depiction of a hideous face with serpents for hair, as an apotropaic symbol to ward off evil. In a Greek myth described by Pseudo-Apollodorus in his Bibliotheca, Medusa was a Gorgon with serpents for hair whose gaze turned all those who looked at her to stone and was slain by the hero Perseus. In the Roman poet Ovid's Metamorphoses, Medusa is said to have once been a beautiful priestess of Athena, whom Athena turned into a serpent-haired monster after she was raped by the god Poseidon in Athena's temple. In another myth referenced by the Boeotian poet Hesiod and described in detail by Pseudo-Apollodorus, the hero Heracles is said to have slain the Lernaean Hydra, a multiple-headed serpent which dwelt in the swamps of Lerna.
The legendary account of the foundation of Thebes mentioned a monster snake guarding the spring from which the new settlement was to draw its water. In fighting and killing the snake, the companions of the founder Cadmus all perished – leading to the term "Cadmean victory" (i.e. a victory involving one's own ruin).
Three medical symbols involving snakes that are still used today are Bowl of Hygieia, symbolizing pharmacy, and the Caduceus and Rod of Asclepius, which are symbols denoting medicine in general.
One of the etymologies proposed for the common female first name Linda is that it might derive from Old German Lindi or Linda, meaning a serpent.
India is often called the land of snakes and is steeped in tradition regarding snakes. Snakes are worshipped as gods even today with many women pouring milk on snake pits (despite snakes' aversion for milk). The cobra is seen on the neck of Shiva and Vishnu is depicted often as sleeping on a seven-headed snake or within the coils of a serpent. There are also several temples in India solely for cobras sometimes called Nagraj (King of Snakes) and it is believed that snakes are symbols of fertility. There is a Hindu festival called Nag Panchami each year on which day snakes are venerated and prayed to. See also Nāga.
In India there is another mythology about snakes. Commonly known in Hindi as "Ichchhadhari" snakes. Such snakes can take the form of any living creature, but prefer human form. These mythical snakes possess a valuable gem called "Mani", which is more brilliant than diamond. There are many stories in India about greedy people trying to possess this gem and ending up getting killed.
The snake is one of the 12 celestial animals of Chinese zodiac, in the Chinese calendar.
Many ancient Peruvian cultures worshipped nature. They emphasized animals and often depicted snakes in their art.
Religion
Snakes are used in Hinduism as a part of ritual worship. In the annual Nag Panchami festival, participants worship either live cobras or images of Nāgas. Lord Shiva is depicted in most images with a snake coiled around his neck. Puranic literature includes various stories associated with snakes, for example Shesha is said to hold all the planets of the Universe on his hoods and to constantly sing the glories of Vishnu from all his mouths. Other notable snakes in Hinduism are Vasuki, Takshaka, Karkotaka, and Pingala. The term Nāga is used to refer to entities that take the form of large snakes in Hinduism and Buddhism.
Snakes have been widely revered in many cultures, such as in ancient Greece where the serpent was seen as a healer.[148] Asclepius carried a serpent wound around his wand, a symbol seen today on many ambulances. In Judaism, the snake of brass is also a symbol of healing, of one's life being saved from imminent death.
In religious terms, the snake and jaguar were arguably the most important animals in ancient Mesoamerica. "In states of ecstasy, lords dance a serpent dance; great descending snakes adorn and support buildings from Chichen Itza to Tenochtitlan, and the Nahuatl word coatl meaning serpent or twin, forms part of primary deities such as Mixcoatl, Quetzalcoatl, and Coatlicue." In the Maya and Aztec calendars, the fifth day of the week was known as Snake Day.
In some parts of Christianity, the redemptive work of Jesus Christ is compared to saving one's life through beholding the Nehushtan (serpent of brass). Snake handlers use snakes as an integral part of church worship, to demonstrate their faith in divine protection. However, more commonly in Christianity, the serpent has been depicted as a representative of evil and sly plotting, as seen in the description in Genesis of a snake tempting Eve in the Garden of Eden. Saint Patrick is purported to have expelled all snakes from Ireland while converting the country to Christianity in the 5th century, thus explaining the absence of snakes there.
In Christianity and Judaism, the snake makes its infamous appearance in the first book of the Bible when a serpent appears before Adam and Eve and tempts them with the forbidden fruit from the Tree of Knowledge. The snake returns in the Book of Exodus when Moses turns his staff into a snake as a sign of God's power, and later when he makes the Nehushtan, a bronze snake on a pole that when looked at cured the people of bites from the snakes that plagued them in the desert. The serpent makes its final appearance symbolizing Satan in the Book of Revelation: "And he laid hold on the dragon the old serpent, which is the devil and Satan, and bound him for a thousand years."
In Neo-Paganism and Wicca, the snake is seen as a symbol of wisdom and knowledge. Additionally, snakes are sometimes associated with Hecate, the Greek goddess of witchcraft.
Medicine
Several compounds from snake venoms are being researched as potential treatments or preventatives for pain, cancers, arthritis, stroke, heart disease, hemophilia, and hypertension, and to control bleeding (e.g. during surgery).
This was my first time actually plane watching at Miami International Airport (MIA). I checked some spotter websites to find some good locations. They recommended The Holes as being an "official" site so we checked it out. I was pretty disappointed; there was a lot of construction going on and parking was nonexistent. My wife dropped me off. The area is totally exposed. Even though it was December it was pretty hot - no shade, no place to sit, no other people around. The holes are actually pretty small so it's hard to get a lens through the hole. Arrivals were almost impossible to shoot but you could see planes taxiing by for takeoff. After an hour I was cooking so we bagged it. We then went to the area close to the El Dorado furniture store. Much better. There were a bunch of spotters from around the world there. It was a great atmosphere. Nicely shaded, safe, close to some stores and a lot of good traffic to watch. I saw a bunch of planes from airlines I had not seen before, including some airlines I had not heard of. Some of the planes didn't show up on Flight Radar 24 so they were very pleasant surprises. All in all a very good day and I'd love to go back there!
I took these photos in December 2019.
Pacific Western Airlines started off as Central British Columbia Airlines by two bush pilots in 1946 with a Beech 17 Staggerwing as its only equipment, and its sole purpose to fly forest fire patrol missions across the vast forests of British Columbia. Despite this, CBCA was founded at just the right time: after World War II, Canada was interested in tapping the barely-touched natural resources of Canada’s tundra, and CBCA was uniquely positioned to take advantage of the explosion of mining interests in northern British Columbia.
The little airline expanded rapidly to include a bewildering array of aircraft serving the remote mining camps and eventual towns that sprung up around them. By 1955, CBCA was profitable enough to buy out nine other airlines in the region, consolidating them into Pacific Western Airlines; Pacific Western again got lucky in 1959, when Canadian Pacific turned over most of its western Canadian routes to Pacific Western, as CP Air wanted to concentrate on its international routes.
Pacific Western was always looking for more ways to innovate. In 1963, it started a Douglas DC-4 shuttle between Calgary and Edmonton, Alberta: 30 years before low-cost operators like Easyjet started a similar program, Pacific Western was selling tickets onboard its own aircraft shortly before takeoff, with seats offered as first-come, first-served. It also was one of the first Canadian airlines to offer all-inclusive holiday charters to the Caribbean, Las Vegas, and the United Kingdom. Jets arrived with Boeing 707s in 1967, the same year Pacific Western became the first airline to adopt the Lockheed L-100 Hercules, the civilian version of the C-130; these supplied mining camps along the Arctic Sea, where runways were nonexistent. Even as brand-new Boeing 737s arrived, Pacific Western was still flying ancient Douglas DC-4s in the Northwest Territories. Besides its scheduled services, Pacific Western was flying worldwide ad hoc cargo charter services.
In 1974, with fuel prices rising and maintenance costs mounting for Pacific Western’s different aircraft, the province of Alberta assumed ownership of Pacific Western to ensure that the airline continued operations; it was that important to western Canada. Equipment was standardized on the Boeing 737, with its Northwest Territories cargo operations sold off. Four years later, the airline bought out Transair, giving it routes east of Alberta for the first time. By 1983, when Alberta privatized the airline again, Pacific Western was the largest airline in western Canada and one of the most profitable. It was doing so well that in 1987 it submitted an offer to buy its old rival, CP Air. When this was approved by the Canadian government, Pacific Western then bought out troubled carrier Wardair Canada, absorbing Canada’s third and second largest airlines in the space of two years. All three airlines were then merged into and renamed Canadian Airlines, retiring the Canadian Pacific, Wardair, and Pacific Western brands.
This 727 shows off Pacific Western's rather attractive livery, used throughout most of the airline's existence. The real CF-PWW did fly with Pacific Western, but it was either a 707 or 737. Note the cargo door on the forward fuselage: this is a mixed passenger/cargo Combi version.
Picture taken 1987 during my 5-month-trip around the world - digitally captured from paper print. Sorry for the bad quality.
I have uploaded a lot of my digitally captured photos, which I took since 2004. But the most interesting journeys I did between 1979 and 2004! Those photos are on slide.
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Bora Bora (French: Bora-Bora, Tahitian: Pora Pora) is a 30.55 km2 island group in the Leeward group in the western part of the Society Islands of French Polynesia, an overseas collectivity of France in the Pacific Ocean. The main island, located about 230 kilometres northwest of Papeete, is surrounded by a lagoon and a barrier reef. In the center of the island are the remnants of an extinct volcano rising to two peaks, Mount Pahia and Mount Otemanu, the highest point at 727 metres.
Bora Bora is a major international tourist destination, famous for its aqua-centric luxury resorts. The major settlement, Vaitape, is on the western side of the main island, opposite the main channel into the lagoon. Produce of the island is mostly limited to what can be obtained from the sea and the plentiful coconut trees, which were historically of economic importance for copra.
DEMOGRAPHICS
As of 2017, the Bora Bora group has a permanent population of 10,605.
NAME
In ancient times the island was called "Pora pora mai te pora", meaning "created by the gods" in the local Tahitian dialect. This was often abbreviated Pora Pora meaning simply "first born". Because of ambiguities in the phonemes of the Tahitian language, this could also be pronounced Bola Bola or Bora Bora. When explorer Jacob Roggeveen first landed on the island, he and his crew adopted the name Bora Bora which has stood ever since.
HISTORY
The island was inhabited by Polynesian settlers around the 4th century C.E.[citation needed] The first European sighting was made by Jakob Roggeveen in 1722.
James Cook sighted the island on 29 July 1769, using a Tahitian navigator, Tupaia. The London Missionary Society arrived in 1820 and founded a Protestant church in 1890. Bora Bora was an independent kingdom until 1888 when its last queen Teriimaevarua III was forced to abdicate by the French who annexed the island as a colony.
WORLD WAR II
In World War II the United States chose Bora Bora as a South Pacific military supply base, and an oil depot, airstrip, seaplane base, and defensive fortifications were constructed. Known as "Operation Bobcat", it maintained a supply force of nine ships, 20,000 tons of equipment and nearly 7,000 men.
At least eight 7"/44 caliber guns, operated by elements of the 13th Coast Artillery Regiment (later the 276th Coast Artillery Battalion), were set up at strategic points around the island to protect it against potential military attack. Eight of these guns remain in the area.
However, the island saw no combat as the American presence on Bora Bora went uncontested over the course of the war. The base was officially closed on 2 June 1946. The World War II airstrip was never able to accommodate large aircraft, but it nonetheless was French Polynesia's only international airport until Faa'a International Airport opened next to Papeete, Tahiti, in 1960.
ADMINISTRATION
The commune of Bora-Bora is made up of the island of Bora Bora proper with its surrounding islets emerging from the coral reef, 29.3 km2 in total. The surrounding islets include Motu Tapu, Motu Ahuna, Tevairoa, Motu Tane, Motu Mute, Motu Tufari, Motu Tehotu, Motu Pitiaau, Sofitel Motu, Motu Toopua, and Toopuaiti. The commune also includes the Tūpai atoll. (11 km2), located 20 kilometres north of Bora Bora. The atoll of Tūpai has no permanent population apart from about 50 workers in the coconut plantations.
The commune is an administrative subdivision of the Leeward Islands and consists of three associated communes: Anau, Faanui and Vaitape. The administrative centre of the commune is the settlement of Vaitape, on the island of Bora Bora proper. Gaston Tong Sang is the Mayor of the commune of Bora-Bora, serving since 1989.
TOURISM
The island's economy is driven almost solely by tourism. Several resorts have been built on motu (small islands, from Tahitian) surrounding the lagoon. Hotel Bora Bora opened in 1961, and nine years later built the first over-the-water bungalows on stilts over the lagoon. Today, over-water bungalows are a standard feature of most Bora Bora resorts. The quality of those bungalows ranges from comparably cheap, basic accommodations to very luxurious and expensive places to stay.
Most of the tourist destinations are aqua-centric; however it is possible to visit attractions on land such as WWII cannons. Air Tahiti has five or six flights daily to the Bora Bora Airport on Motu Mute from Tahiti (as well as from other islands). Public transport on the island is nonexistent so rental cars and bicycles are the recommended methods of transport. There are also small, two-seater buggies for hire in Vaitape. It is possible to rent a motorboat to explore the lagoon.
Snorkeling and scuba diving in and around the lagoon of Bora Bora are popular activities. Many species of sharks and rays inhabit the surrounding body of water. There are a few dive operators on the island offering manta ray dives and also shark-feeding dives. Sharks living in the island's lagoon are not considered to be dangerous to people.[citation needed]
In addition to the existing islands of Bora Bora, the new manmade motu of Motu Marfo has been added in the northeastern corner of the lagoon on the property of the St. Regis Resort.
WIKIPEDIA
This ship is my favorite out of my physical collection. Its just the rights size for play while still having enough detail for display and has an interior. Said interior is based of the cross section book for the force awakens. There is a single bed and nothing else. I wish that the bed could be moved over though, as it is taking up quite a bit a space.
Problems:
the rear door is invisible
the rear wings are not all the way at the end of the ship
there are no front wings
the cockpit is nonexistent
Minutes after leaving Wolfville, heading east towards Halifax on the Evangeline Trail, I spotted the skeleton of a completely demolished house. It sat dejectedly amongst its own innards which lay strewn about the yard. A quick U-turn in the middle of the empty Thursday afternoon highway brought me back to the rutted, overgrown road which led to the house. Without a fence, "no trespassing" sign, or person in sight I approached the house, carefully avoiding the minefield of bared, rusted nails jutting out of the shingles and boards about the yard. The house, beaten and broken, appeared to be giving itself up to the land, an offering readily accepted by the weeds and wildflowers that had already gently consumed a window frame or two as well as the foundations. Initially I enjoyed the starkness of the remaining stairs which lead up to the nonexistent second floor, yet upon a full circulation of the house I came across the bathroom. This remarkably preserved room was situated snugly under the stairs facing a vast stretch of land that was marked only by a perfectly red house in the distance. The raw, impersonal beauty of the house's skeleton was suddenly ripped away for me as I now saw the broken interior with its hauntingly personal touches. The bathroom, the last remaining sign of the house's original gentle nature, was now exposed since the wall had been ruthlessly torn down. The identifiable appliances so brutally smashed were startlingly provoking and the peeling pink paint seemed to be a subtle surrender. Most notably disheartening was the tiny heart-shaped wreath hanging from the wall. It had pink roses attached which happily matched the shower tiles and the pink paint. This heart, a final testament of the house's domestication, now open to the elements, was now a bared symbol of resignation.
Here he is demonstrating what's "normal" for human sexuality with extension cords. Given his choice in metaphors, I bet you money his sex life is nonexistent.
In fact that's what he was preaching. No sex before marriage, no masturbation for guys. After marriage only missionary sex, no blow jobs, no masturbation... etc.
I waited for him to get through to the gay side of the matters and preach how homosexuality is sin etc. The crowd listened on making comments every now and then. Now I am no activist but when he reached a stopping point, I raised my voice and I said:
"for one moment let's assume that all homosexuals in the world gave up homosexuality and we are done with homosexuality, so we're able to put that subject aside -- what else are you preaching exactly here? I mean do you have message for compassion, community, support, charity, feeding the poor, solving the hatred in the world, empowering the poor nations, increasing literacy... do you have any of these as action items? He had nothing to say. So I continued:
"Anyone can get up on a high ground and preach hatred, it comes naturally to most humans. If you say you're truly religious and that you have seen the light, you have to show me that you have risen above all that with your compassion and love for humanity whatever shape form or orientation they are. All you're doing here is making an ass of yourself showing us your intolerance and your inability to show compassion to others. Your said heaven as you describe it is the empty parking lot of the Mall of America, and you can keep it."
After stumbling for words, his operating system must have rebooted because Mr. Religious Hatret Bot was back in action within seconds of my statement. I let him speak a bit more until he came to a story from the bible where doing justice involved scorching out a relative's eyes.
At that point I bowed out. There is simply no hope.
Being a literal follower of any of the main religions with books is the equivalent of treating Alice in Wonderland as a literal book on historical events that actually took place. And please, dont even go there....
Carlos Fresquez
A Fairy Tale, 2007
Screen print / Serigraph / Silkscreen
Edition of 50 (Serie XIV / 14)
Visit the artist's page on our website to purchase this print. For more information about other artists in the series, visit serieproject.org/shop.
The print A Fairy Tale, represents Denver native Carlos Fresquez’s vision of the future, a place where borders of all kinds will be nonexistent and a time where world peace will prevail. The subjects in this print, The Jetson’s, or "Los Supersonicos" as they are called in Spanish, represent a future in which humans will get along with one another regardless of language or cultural identity.
Indeed, just as all cartoons are dubbed to fit the language in the country they are aired in, George Jetson speaks to the audience in Spanish while he his wife marvels at the perfection of their world in English. However, as the title reveals, this idealic vision of humanity will never come into fruition; like Los Supersonicos speaking to us from the future, this vision will remain a mere fantasy as there are too many factors that will prevent this world from taking shape.
Fresquez’s use of Aztec and Chicano-related imagery in the background make his print resemble an Aztec codex except that this one, with its cartoon imagery, is a modern day codex which takes notice of the past while keeping a keen focus of the future. A future which Fresquez hopes will most closely resemble the fantasy world Los Supersonicos reside in.
Fresquez earned his Bachelor of Arts from the Metropolitan State College in Denver and a Master of Fine Arts from the University of Colorado at Boulder. Currently, he teaches art at Metropolitan State College.
The kids were great - and I think they really understand the importance of the movement.
The children understand because it's their future that had been hocked by the greedy elite power structure between bankers, traders, agents, politicians and others who created the economic crisis then jumped out with millions of dollars in golden parachutes.
Check out this OccupyAugusta video by Jane Pietkivitch
She shot and edited video from the Occupy Augusta march on downtown on Saturday (10-15-11).
The OccupyAugusta movement is doing a fantastic job coordinating and the enthusiasm is no less that in New York
www.facebook.com/photo.php?v=302389719777944
OccupyAugusta did an impressive job on Sat., Oct. 15, 2011 as they marched on downtown Augusta protesting the evil greed that created the current economic crisis.
The bankers, Wall Street traders, insurance industry, politicians proved they cannot be trusted when left to their own devices when the Bush administration made oversight almost nonexistent.
And sure enough when the foxes were in charge of the hen-house it was a slaughter of American jobs, the evaporation of retirement funds, a flood of home foreclosures, sending the world economy into crisis.
See the photos at these links!
occupyaugusta.org/occupy/wp-content/lg-gallery/October%20...
occupyaugusta.org/occupy/gallery?file=October%2015%202011/
Occupy Augusta, GA: Occupy Wall Street Pages:
Occupy Augusta, GA on Facebook:
www.facebook.com/pages/OCCUPY-AUGUSTA/178325418914632
Occupy Augusta, GA on Twitter:
Occupy Augusta, GA on WordPress.org:
Occupy Augusta, GA on discussion page of WordPress.org (#OccupyAugusta ) in Solidarity with #OWS and #OccupyTogether:
occupyaugusta.org/discuss/index.php
Occupy Augusta, GA on MeetUp:
www.meetup.com/occupytogether/Augusta-GA/382952
Occupy Augusta, GA on Tumblr:
Occupy Wall Street Movement in other Georgia cities:
Inside a cloud. The views were nonexistent.
Looking toward Perkins Peak, which I wanted to climb. Turned back here though, because of low visibility and annoying sideways snow.
We decided that hiking would be one of the methods for my wife and I to get healthier. Luckily there is a state park near us with some great trails. After working up to a five mile route we met a hiker who told us about the trails off the main trail, or ridge trails. They were a bit hard to find but once we got the hang of it locating the ridge trails was easy. They were more challenging and much more fun.
After reading many books on hiking the Appalachian Trail and Pacific Crest Trail, the last book I read was from a Michigander who hiked the AP Trail, tried it as a through-hike but life got in the way and he had to go home a few times. I knew this was beyond our interest but we really enjoy the day hikes. The wife won’t go for the backpacking just yet; I keep working on her though.
In looking to try something new, I came across information on the North Country Trail on the internet and read about the Hike 100 Challenge. We thought it was a good idea and made it our goal. We also decided to attend the 2016 Celebration in Fargo, ND.
We started in April at the Birch River Schoolhouse Loop in MI. We picked the hottest and most humid day in May to hike the NCT in Shawnee State Forest, OH. Met a nice local family who camped out on the trail because they got a late start the night before. Ohio pushed me to the limit physically with the weather, it was either up or down and the trail markings were nonexistent. After that we decided we were cool weather hikers.
So we took a break until mid-September when we went to the Celebration in Fargo. I was a bit worried we would not achieve the challenge since we were only about a third of the way in mileage. However, Fargo got us back on track, we really enjoyed the prairie hiking which is much different than that of MI. We made a vacation out of the trip and took our time coming home by way of the Upper Peninsula. But first we had to stop and walk across the Montreal River that borders Wisconsin and Michigan. You see, after hiking in MI, OH, ND, MN, it only seemed logical to hike in WI since we were already there. Then we could make a vacation out of going to the PA/NY border, that way we would have hiked in all the states of the NCT. Oh yes, we had decided to hike all seven states when we were at the Celebration in Fargo!
We camped and hiked in the Porcupine Mountains, the “Grand Canyon” of Michigan, and Hemingway country in the Upper Peninsula. We found the NCT crossing the highway near Lowell on our frequent drives to see the kids at the University of Michigan and got more mileage in that way. It is also a nice stop to get out of the car and stretch the legs. We then traveled to Bradford, PA and hiked the Allegheny National Forest in Pennsylvania and the Allegany State Park in New York. Oh, it’s not a typo, PA likes the “heny” and NY likes the “any”, I have the photos to prove it.
We took two days off then headed back to our now favorite place, Bitely MI. We camped and did our final twenty miles on the trail over three days. As a present we had just purchased backpacks for both of us at REI in Ann Arbor (shout out), they worked out great.
A shout out to the Outpost in Holland, MI where we purchase most of our stuff. Thanks to all the folks volunteering and working for the NCT, what a wonderful concept. It is a great way to get out and rejuvenate.
Greg & Cathy Brock, Members at Large
Capitol Reef National Park is an American national park in south-central Utah. The park is approximately 60 miles (97 km) long on its north–south axis and just 6 miles (9.7 km) wide on average. The park was established in 1971 to preserve 241,904 acres (377.98 sq mi; 97,895.08 ha; 978.95 km2) of desert landscape and is open all year, with May through September being the highest visitation months.
Partially in Wayne County, Utah, the area was originally named "Wayne Wonderland" in the 1920s by local boosters Ephraim P. Pectol and Joseph S. Hickman. Capitol Reef National Park was designated a national monument on August 2, 1937, by President Franklin D. Roosevelt to protect the area's colorful canyons, ridges, buttes, and monoliths; however, it was not until 1950 that the area officially opened to the public. Road access was improved in 1962 with the construction of State Route 24 through the Fremont River Canyon.
The majority of the nearly 100 mi (160 km) long up-thrust formation called the Waterpocket Fold—a rocky spine extending from Thousand Lake Mountain to Lake Powell—is preserved within the park. Capitol Reef is an especially rugged and spectacular segment of the Waterpocket Fold by the Fremont River. The park was named for its whitish Navajo Sandstone cliffs with dome formations—similar to the white domes often placed on capitol buildings—that run from the Fremont River to Pleasant Creek on the Waterpocket Fold. Locally, reef refers to any rocky barrier to land travel, just as ocean reefs are barriers to sea travel.
Capitol Reef encompasses the Waterpocket Fold, a warp in the earth's crust that is 65 million years old. It is the largest exposed monocline in North America. In this fold, newer and older layers of earth folded over each other in an S-shape. This warp, probably caused by the same colliding continental plates that created the Rocky Mountains, has weathered and eroded over millennia to expose layers of rock and fossils. The park is filled with brilliantly colored sandstone cliffs, gleaming white domes, and contrasting layers of stone and earth.
The area was named for a line of white domes and cliffs of Navajo Sandstone, each of which looks somewhat like the United States Capitol building, that run from the Fremont River to Pleasant Creek on the Waterpocket Fold.
The fold forms a north-to-south barrier that has barely been breached by roads. Early settlers referred to parallel impassable ridges as "reefs", from which the park gets the second half of its name. The first paved road was constructed through the area in 1962. State Route 24 cuts through the park traveling east and west between Canyonlands National Park and Bryce Canyon National Park, but few other paved roads invade the rugged landscape.
The park is filled with canyons, cliffs, towers, domes, and arches. The Fremont River has cut canyons through parts of the Waterpocket Fold, but most of the park is arid desert. A scenic drive shows park visitors some highlights, but it runs only a few miles from the main highway. Hundreds of miles of trails and unpaved roads lead into the equally scenic backcountry.
Fremont-culture Native Americans lived near the perennial Fremont River in the northern part of the Capitol Reef Waterpocket Fold around the year 1000. They irrigated crops of maize and squash and stored their grain in stone granaries (in part made from the numerous black basalt boulders that litter the area). In the 13th century, all of the Native American cultures in this area underwent sudden change, likely due to a long drought. The Fremont settlements and fields were abandoned.
Many years after the Fremont left, Paiutes moved into the area. These Numic-speaking people named the Fremont granaries moki huts and thought they were the homes of a race of tiny people or moki.
In 1872 Almon H. Thompson, a geographer attached to United States Army Major John Wesley Powell's expedition, crossed the Waterpocket Fold while exploring the area. Geologist Clarence Dutton later spent several summers studying the area's geology. None of these expeditions explored the Waterpocket Fold to any great extent.
Following the American Civil War, officials of the Church of Jesus Christ of Latter-day Saints in Salt Lake City sought to establish missions in the remotest niches of the Intermountain West. In 1866, a quasi-military expedition of Mormons in pursuit of natives penetrated the high valleys to the west. In the 1870s, settlers moved into these valleys, eventually establishing Loa, Fremont, Lyman, Bicknell, and Torrey.
Mormons settled the Fremont River valley in the 1880s and established Junction (later renamed Fruita), Caineville, and Aldridge. Fruita prospered, Caineville barely survived, and Aldridge died. In addition to farming, lime was extracted from local limestone, and uranium was extracted early in the 20th century. In 1904 the first claim to a uranium mine in the area was staked. The resulting Oyler Mine in Grand Wash produced uranium ore.
By 1920 no more than ten families at one time were sustained by the fertile flood plain of the Fremont River and the land changed ownership over the years. The area remained isolated. The community was later abandoned and later still some buildings were restored by the National Park Service. Kilns once used to produce lime are still in Sulphur Creek and near the campgrounds on Scenic Drive.
Local Ephraim Portman Pectol organized a "booster club" in Torrey in 1921. Pectol pressed a promotional campaign, furnishing stories to be sent to periodicals and newspapers. In his efforts, he was increasingly aided by his brother-in-law, Joseph S. Hickman, who was the Wayne County High School principal. In 1924, Hickman extended community involvement in the promotional effort by organizing a Wayne County-wide Wayne Wonderland Club. That same year, Hickman was elected to the Utah State Legislature.
In 1933, Pectol was elected to the presidency of the Associated Civics Club of Southern Utah, successor to the Wayne Wonderland Club. The club raised U.S. $150 (equivalent to $3,391 in 2022) to interest a Salt Lake City photographer in taking a series of promotional photographs. For several years, the photographer, J. E. Broaddus, traveled and lectured on "Wayne Wonderland".
In 1933, Pectol was elected to the legislature and almost immediately contacted President Franklin D. Roosevelt and asked for the creation of "Wayne Wonderland National Monument" out of the federal lands comprising the bulk of the Capitol Reef area. Federal agencies began a feasibility study and boundary assessment. Meanwhile, Pectol guided the government investigators on numerous trips and escorted an increasing number of visitors. The lectures of Broaddus were having an effect.
Roosevelt signed a proclamation creating Capitol Reef National Monument on August 2, 1937. In Proclamation 2246, President Roosevelt set aside 37,711 acres (15,261 ha) of the Capitol Reef area. This comprised an area extending about two miles (3 km) north of present State Route 24 and about 10 mi (16 km) south, just past Capitol Gorge. The Great Depression years were lean ones for the National Park Service (NPS), the new administering agency. Funds for the administration of Capitol Reef were nonexistent; it would be a long time before the first rangers would arrive.
Administration of the new monument was placed under the control of Zion National Park. A stone ranger cabin and the Sulphur Creek bridge were built and some road work was performed by the Civilian Conservation Corps and the Works Progress Administration. Historian and printer Charles Kelly came to know NPS officials at Zion well and volunteered to watchdog the park for the NPS. Kelly was officially appointed custodian-without-pay in 1943. He worked as a volunteer until 1950, when the NPS offered him a civil-service appointment as the first superintendent.
During the 1950s Kelly was deeply troubled by NPS management acceding to demands of the U.S. Atomic Energy Commission that Capitol Reef National Monument be opened to uranium prospecting. He felt that the decision had been a mistake and destructive of the long-term national interest. It turned out that there was not enough ore in the monument to be worth mining.
In 1958 Kelly got additional permanent help in protecting the monument and enforcing regulations; Park Ranger Grant Clark transferred from Zion. The year Clark arrived, fifty-six thousand visitors came to the park, and Charlie Kelly retired for the last time.
During the 1960s (under the program name Mission 66), NPS areas nationwide received new facilities to meet the demand of mushrooming park visitation. At Capitol Reef, a 53-site campground at Fruita, staff rental housing, and a new visitor center were built, the latter opening in 1966.
Visitation climbed dramatically after the paved, all-weather State Route 24 was built in 1962 through the Fremont River canyon near Fruita. State Route 24 replaced the narrow Capitol Gorge wagon road about 10 mi (16 km) to the south that frequently washed out. The old road has since been open only to foot traffic. In 1967, 146,598 persons visited the park. The staff was also growing.
During the 1960s, the NPS purchased private land parcels at Fruita and Pleasant Creek. Almost all private property passed into public ownership on a "willing buyer-willing seller" basis.
Preservationists convinced President Lyndon B. Johnson to set aside an enormous area of public lands in 1968, just before he left office. In Presidential Proclamation 3888 an additional 215,056 acres (87,030 ha) were placed under NPS control. By 1970, Capitol Reef National Monument comprised 254,251 acres (102,892 ha) and sprawled southeast from Thousand Lake Mountain almost to the Colorado River. The action was controversial locally, and NPS staffing at the monument was inadequate to properly manage the additional land.
The vast enlargement of the monument and diversification of the scenic resources soon raised another issue: whether Capitol Reef should be a national park, rather than a monument. Two bills were introduced into the United States Congress.
A House bill (H.R. 17152) introduced by Utah Congressman Laurence J. Burton called for a 180,000-acre (72,800 ha) national park and an adjunct 48,000-acre (19,400 ha) national recreation area where multiple use (including grazing) could continue indefinitely. In the United States Senate, meanwhile, Senate bill S. 531 had already passed on July 1, 1970, and provided for a 230,000-acre (93,100 ha) national park alone. The bill called for a 25-year phase-out of grazing.
In September 1970, United States Department of Interior officials told a house subcommittee session that they preferred about 254,000 acres (103,000 ha) be set aside as a national park. They also recommended that the grazing phase-out period be 10 years, rather than 25. They did not favor the adjunct recreation area.
It was not until late 1971 that Congressional action was completed. By then, the 92nd United States Congress was in session and S. 531 had languished. A new bill, S. 29, was introduced in the Senate by Senator Frank E. Moss of Utah and was essentially the same as the defunct S. 531 except that it called for an additional 10,834 acres (4,384 ha) of public lands for a Capitol Reef National Park. In the House, Utah Representative K. Gunn McKay (with Representative Lloyd) had introduced H.R. 9053 to replace the dead H.R. 17152. This time, the House bill dropped the concept of an adjunct Capitol Reef National Recreation Area and adopted the Senate concept of a 25-year limit on continued grazing. The Department of Interior was still recommending a national park of 254,368 acres (102,939 ha) and a 10-year limit for grazing phase-out.
S. 29 passed the Senate in June and was sent to the House, which dropped its own bill and passed the Senate version with an amendment. Because the Senate was not in agreement with the House amendment, differences were worked out in Conference Committee. The Conference Committee issued its report on November 30, 1971, and the bill passed both houses of Congress. The legislation—'An Act to Establish The Capitol Reef National Park in the State of Utah'—became Public Law 92-207 when it was signed by President Richard Nixon on December 18, 1971.
The area including the park was once the edge of a shallow sea that invaded the land in the Permian, creating the Cutler Formation. Only the sandstone of the youngest member of the Cutler Formation, the White Rim, is exposed in the park. The deepening sea left carbonate deposits, forming the limestone of the Kaibab Limestone, the same formation that rims the Grand Canyon to the southwest.
During the Triassic, streams deposited reddish-brown silt that later became the siltstone of the Moenkopi Formation. Uplift and erosion followed. Conglomerate, followed by logs, sand, mud, and wind-transported volcanic ash, then formed the uranium-containing Chinle Formation.
The members of the Glen Canyon Group were all laid down in the middle- to late-Triassic during a time of increasing aridity. They include:
Wingate Sandstone: sand dunes on the shore of an ancient sea
Kayenta Formation: thin-bedded layers of sand deposited by slow-moving streams in channels and across low plains
Navajo Sandstone: huge fossilized sand dunes from a massive Sahara-like desert.
The Golden Throne. Though Capitol Reef is famous for white domes of Navajo Sandstone, this dome's color is a result of a lingering section of yellow Carmel Formation carbonate, which has stained the underlying rock.
The San Rafael Group consists of four Jurassic-period formations, from oldest to youngest:
Carmel Formation: gypsum, sand, and limey silt laid down in what may have been a graben that was periodically flooded by sea water
Entrada Sandstone: sandstone from barrier islands/sand bars in a near-shore environment
Curtis Formation: made from conglomerate, sandstone, and shale
Summerville Formation: reddish-brown mud and white sand deposited in tidal flats.
Streams once again laid down mud and sand in their channels, on lakebeds, and in swampy plains, creating the Morrison Formation. Early in the Cretaceous, similar nonmarine sediments were laid down and became the Dakota Sandstone. Eventually, the Cretaceous Seaway covered the Dakota, depositing the Mancos Shale.
Only small remnants of the Mesaverde Group are found, capping a few mesas in the park's eastern section.
Near the end of the Cretaceous period, a mountain-building event called the Laramide orogeny started to compact and uplift the region, forming the Rocky Mountains and creating monoclines such as the Waterpocket Fold in the park. Ten to fifteen million years ago, the entire region was uplifted much further by the creation of the Colorado Plateau. This uplift was very even. Igneous activity in the form of volcanism and dike and sill intrusion also occurred during this time.
The drainage system in the area was rearranged and steepened, causing streams to downcut faster and sometimes change course. Wetter times during the ice ages of the Pleistocene increased the rate of erosion.
There are more than 840 species of plants that are found in the park and over 40 of those species are classified as rare and endemic.
The closest town to Capitol Reef is Torrey, about 11 mi (18 km) west of the visitor center on Highway 24, slightly west of its intersection with Highway 12. Its 2020 population is less than 300. Torrey has a few motels and restaurants and functions as a gateway town to Capitol Reef National Park. Highway 12, as well as a partially unpaved scenic backway named the Burr Trail, provide access from the west through the Grand Staircase–Escalante National Monument and the town of Boulder.
A variety of activities are available to tourists, both ranger-led and self-guided, including auto touring, hiking, backpacking, camping, bicycling (on paved and unpaved roads only; no trails), horseback riding, canyoneering, and rock climbing. The orchards planted by Mormon pioneers are maintained by the National Park Service. From early March to mid-October, various fruit—cherries, apricots, peaches, pears, or apples—can be harvested by visitors for a fee.
A hiking trail guide is available at the visitor center for both day hikes and backcountry hiking. Backcountry access requires a free permit.
Numerous trails are available for hiking and backpacking in the park, with fifteen in the Fruita District alone. The following trails are some of the most popular in the park:
Cassidy Arch Trail: a very steep, strenuous 3.5 mi (5.6 km) round trip that leads into the Grand Wash to an overlook of the Cassidy Arch.
Hickman Bridge Trail: a 2 mi (3.2 km) round trip leading to the natural bridge.
Frying Pan Trail: an 8.8 mi (14.2 km) round trip that passes the Cassidy Arch, Grand Wash, and Cohab Canyon.
Brimhall Natural Bridge: a popular, though strenuous, 4.5 mi (7.2 km) round trip with views of Brimhall Canyon, the Waterpocket Fold, and Brimhall Natural Bridge.
Halls Creek Narrows: 22 mi (35 km) long and considered strenuous, with many side canyons and creeks; typically hiked as a 2-3 day camping trip.
Visitors may explore several of the main areas of the park by private vehicle:
Scenic Drive: winds through the middle of the park, passing the major points of interest; the road is accessible from the visitor center to approximately 2 mi (3.2 km) into the Capitol Gorge.
Notom-Bullfrog Road: traverses the eastern side of the Waterpocket Fold, along 10 mi (16 km) of paved road, with the remainder unpaved.
Cathedral Road: an unpaved road through the northern areas of the park, that traverses Cathedral Valley, passing the Temples of the Sun and Moon.
The primary camping location is the Fruita campground, with 71 campsites (no water, electrical, or sewer hookups), and restrooms without bathing facilities. The campground also has group sites with picnic areas and restrooms. Two primitive free camping areas are also available.
Canyoneering is growing in popularity in the park. It is a recreational sport that takes one through slot canyons. It involves rappelling and may require swimming and other technical rope work. Day-pass permits are required for canyoneering in the park, and can be obtained for free from the visitor's center or through email. It's key to know that each route requires its own permit. If one is planning on canyoneering for multiple days, passes are required for each day. Overnight camping as part of the canyoneering trip is permitted, but one must request a free backcountry pass from the visitor center.
It is imperative to plan canyoneering trips around the weather. The Colorado Plateau is susceptible to flash flooding during prime rainy months. Because canyoneering takes place through slot canyons, getting caught in a flash flood could be lethal. Take care to consult reliable weather sources. The Weather Atlas shows charts with the monthly average rainfall in inches.
Another risk to be aware of during the summer months is extreme heat. Visitors can find weather warnings on the National Weather Service website. The heat levels are detailed by a color and numerical scale (0-4).
One of the most popular canyoneering routes in Capitol Reef National Park is Cassidy Arch Canyon. A paper by George Huddart, details the park's commitment to working with citizens to maintain the route as well as the vegetation and rocks. The canyon route is approximately 2.3 miles long (0.4 miles of technical work), consisting of 8 different rappels, and takes between 2.5 and 4.5 hours to complete. The first rappel is 140 ft and descends below the famous Cassidy Arch.
Utah is a landlocked state in the Mountain West subregion of the Western United States. It borders Colorado to its east, Wyoming to its northeast, Idaho to its north, Arizona to its south, and Nevada to its west. Utah also touches a corner of New Mexico in the southeast. Of the fifty U.S. states, Utah is the 13th-largest by area; with a population over three million, it is the 30th-most-populous and 11th-least-densely populated. Urban development is mostly concentrated in two areas: the Wasatch Front in the north-central part of the state, which is home to roughly two-thirds of the population and includes the capital city, Salt Lake City; and Washington County in the southwest, with more than 180,000 residents. Most of the western half of Utah lies in the Great Basin.
Utah has been inhabited for thousands of years by various indigenous groups such as the ancient Puebloans, Navajo, and Ute. The Spanish were the first Europeans to arrive in the mid-16th century, though the region's difficult geography and harsh climate made it a peripheral part of New Spain and later Mexico. Even while it was Mexican territory, many of Utah's earliest settlers were American, particularly Mormons fleeing marginalization and persecution from the United States via the Mormon Trail. Following the Mexican–American War in 1848, the region was annexed by the U.S., becoming part of the Utah Territory, which included what is now Colorado and Nevada. Disputes between the dominant Mormon community and the federal government delayed Utah's admission as a state; only after the outlawing of polygamy was it admitted in 1896 as the 45th.
People from Utah are known as Utahns. Slightly over half of all Utahns are Mormons, the vast majority of whom are members of the Church of Jesus Christ of Latter-day Saints (LDS Church), which has its world headquarters in Salt Lake City; Utah is the only state where a majority of the population belongs to a single church. A 2023 paper challenged this perception (claiming only 42% of Utahns are Mormons) however most statistics still show a majority of Utah residents belong to the LDS church; estimates from the LDS church suggests 60.68% of Utah's population belongs to the church whilst some sources put the number as high as 68%. The paper replied that membership count done by the LDS Church is too high for several reasons. The LDS Church greatly influences Utahn culture, politics, and daily life, though since the 1990s the state has become more religiously diverse as well as secular.
Utah has a highly diversified economy, with major sectors including transportation, education, information technology and research, government services, mining, multi-level marketing, and tourism. Utah has been one of the fastest growing states since 2000, with the 2020 U.S. census confirming the fastest population growth in the nation since 2010. St. George was the fastest-growing metropolitan area in the United States from 2000 to 2005. Utah ranks among the overall best states in metrics such as healthcare, governance, education, and infrastructure. It has the 12th-highest median average income and the least income inequality of any U.S. state. Over time and influenced by climate change, droughts in Utah have been increasing in frequency and severity, putting a further strain on Utah's water security and impacting the state's economy.
The History of Utah is an examination of the human history and social activity within the state of Utah located in the western United States.
Archaeological evidence dates the earliest habitation of humans in Utah to about 10,000 to 12,000 years ago. Paleolithic people lived near the Great Basin's swamps and marshes, which had an abundance of fish, birds, and small game animals. Big game, including bison, mammoths and ground sloths, also were attracted to these water sources. Over the centuries, the mega-fauna died, this population was replaced by the Desert Archaic people, who sheltered in caves near the Great Salt Lake. Relying more on gathering than the previous Utah residents, their diet was mainly composed of cattails and other salt tolerant plants such as pickleweed, burro weed and sedge. Red meat appears to have been more of a luxury, although these people used nets and the atlatl to hunt water fowl, ducks, small animals and antelope. Artifacts include nets woven with plant fibers and rabbit skin, woven sandals, gaming sticks, and animal figures made from split-twigs. About 3,500 years ago, lake levels rose and the population of Desert Archaic people appears to have dramatically decreased. The Great Basin may have been almost unoccupied for 1,000 years.
The Fremont culture, named from sites near the Fremont River in Utah, lived in what is now north and western Utah and parts of Nevada, Idaho and Colorado from approximately 600 to 1300 AD. These people lived in areas close to water sources that had been previously occupied by the Desert Archaic people, and may have had some relationship with them. However, their use of new technologies define them as a distinct people. Fremont technologies include:
use of the bow and arrow while hunting,
building pithouse shelters,
growing maize and probably beans and squash,
building above ground granaries of adobe or stone,
creating and decorating low-fired pottery ware,
producing art, including jewelry and rock art such as petroglyphs and pictographs.
The ancient Puebloan culture, also known as the Anasazi, occupied territory adjacent to the Fremont. The ancestral Puebloan culture centered on the present-day Four Corners area of the Southwest United States, including the San Juan River region of Utah. Archaeologists debate when this distinct culture emerged, but cultural development seems to date from about the common era, about 500 years before the Fremont appeared. It is generally accepted that the cultural peak of these people was around the 1200 CE. Ancient Puebloan culture is known for well constructed pithouses and more elaborate adobe and masonry dwellings. They were excellent craftsmen, producing turquoise jewelry and fine pottery. The Puebloan culture was based on agriculture, and the people created and cultivated fields of maize, beans, and squash and domesticated turkeys. They designed and produced elaborate field terracing and irrigation systems. They also built structures, some known as kivas, apparently designed solely for cultural and religious rituals.
These two later cultures were roughly contemporaneous, and appear to have established trading relationships. They also shared enough cultural traits that archaeologists believe the cultures may have common roots in the early American Southwest. However, each remained culturally distinct throughout most of their existence. These two well established cultures appear to have been severely impacted by climatic change and perhaps by the incursion of new people in about 1200 CE. Over the next two centuries, the Fremont and ancient Pueblo people may have moved into the American southwest, finding new homes and farmlands in the river drainages of Arizona, New Mexico and northern Mexico.
In about 1200, Shoshonean speaking peoples entered Utah territory from the west. They may have originated in southern California and moved into the desert environment due to population pressure along the coast. They were an upland people with a hunting and gathering lifestyle utilizing roots and seeds, including the pinyon nut. They were also skillful fishermen, created pottery and raised some crops. When they first arrived in Utah, they lived as small family groups with little tribal organization. Four main Shoshonean peoples inhabited Utah country. The Shoshone in the north and northeast, the Gosiutes in the northwest, the Utes in the central and eastern parts of the region and the Southern Paiutes in the southwest. Initially, there seems to have been very little conflict between these groups.
In the early 16th century, the San Juan River basin in Utah's southeast also saw a new people, the Díne or Navajo, part of a greater group of plains Athabaskan speakers moved into the Southwest from the Great Plains. In addition to the Navajo, this language group contained people that were later known as Apaches, including the Lipan, Jicarilla, and Mescalero Apaches.
Athabaskans were a hunting people who initially followed the bison, and were identified in 16th-century Spanish accounts as "dog nomads". The Athabaskans expanded their range throughout the 17th century, occupying areas the Pueblo peoples had abandoned during prior centuries. The Spanish first specifically mention the "Apachu de Nabajo" (Navaho) in the 1620s, referring to the people in the Chama valley region east of the San Juan River, and north west of Santa Fe. By the 1640s, the term Navaho was applied to these same people. Although the Navajo newcomers established a generally peaceful trading and cultural exchange with the some modern Pueblo peoples to the south, they experienced intermittent warfare with the Shoshonean peoples, particularly the Utes in eastern Utah and western Colorado.
At the time of European expansion, beginning with Spanish explorers traveling from Mexico, five distinct native peoples occupied territory within the Utah area: the Northern Shoshone, the Goshute, the Ute, the Paiute and the Navajo.
The Spanish explorer Francisco Vázquez de Coronado may have crossed into what is now southern Utah in 1540, when he was seeking the legendary Cíbola.
A group led by two Spanish Catholic priests—sometimes called the Domínguez–Escalante expedition—left Santa Fe in 1776, hoping to find a route to the California coast. The expedition traveled as far north as Utah Lake and encountered the native residents. All of what is now Utah was claimed by the Spanish Empire from the 1500s to 1821 as part of New Spain (later as the province Alta California); and subsequently claimed by Mexico from 1821 to 1848. However, Spain and Mexico had little permanent presence in, or control of, the region.
Fur trappers (also known as mountain men) including Jim Bridger, explored some regions of Utah in the early 19th century. The city of Provo was named for one such man, Étienne Provost, who visited the area in 1825. The city of Ogden, Utah is named for a brigade leader of the Hudson's Bay Company, Peter Skene Ogden who trapped in the Weber Valley. In 1846, a year before the arrival of members from the Church of Jesus Christ of latter-day Saints, the ill-fated Donner Party crossed through the Salt Lake valley late in the season, deciding not to stay the winter there but to continue forward to California, and beyond.
Members of the Church of Jesus Christ of Latter-day Saints, commonly known as Mormon pioneers, first came to the Salt Lake Valley on July 24, 1847. At the time, the U.S. had already captured the Mexican territories of Alta California and New Mexico in the Mexican–American War and planned to keep them, but those territories, including the future state of Utah, officially became United States territory upon the signing of the Treaty of Guadalupe Hidalgo, February 2, 1848. The treaty was ratified by the United States Senate on March 10, 1848.
Upon arrival in the Salt Lake Valley, the Mormon pioneers found no permanent settlement of Indians. Other areas along the Wasatch Range were occupied at the time of settlement by the Northwestern Shoshone and adjacent areas by other bands of Shoshone such as the Gosiute. The Northwestern Shoshone lived in the valleys on the eastern shore of Great Salt Lake and in adjacent mountain valleys. Some years after arriving in the Salt Lake Valley Mormons, who went on to colonize many other areas of what is now Utah, were petitioned by Indians for recompense for land taken. The response of Heber C. Kimball, first counselor to Brigham Young, was that the land belonged to "our Father in Heaven and we expect to plow and plant it." A 1945 Supreme Court decision found that the land had been treated by the United States as public domain; no aboriginal title by the Northwestern Shoshone had been recognized by the United States or extinguished by treaty with the United States.
Upon arriving in the Salt Lake Valley, the Mormons had to make a place to live. They created irrigation systems, laid out farms, built houses, churches, and schools. Access to water was crucially important. Almost immediately, Brigham Young set out to identify and claim additional community sites. While it was difficult to find large areas in the Great Basin where water sources were dependable and growing seasons long enough to raise vitally important subsistence crops, satellite communities began to be formed.
Shortly after the first company arrived in the Salt Lake Valley in 1847, the community of Bountiful was settled to the north. In 1848, settlers moved into lands purchased from trapper Miles Goodyear in present-day Ogden. In 1849, Tooele and Provo were founded. Also that year, at the invitation of Ute chief Wakara, settlers moved into the Sanpete Valley in central Utah to establish the community of Manti. Fillmore, Utah, intended to be the capital of the new territory, was established in 1851. In 1855, missionary efforts aimed at western native cultures led to outposts in Fort Lemhi, Idaho, Las Vegas, Nevada and Elk Mountain in east-central Utah.
The experiences of returning members of the Mormon Battalion were also important in establishing new communities. On their journey west, the Mormon soldiers had identified dependable rivers and fertile river valleys in Colorado, Arizona and southern California. In addition, as the men traveled to rejoin their families in the Salt Lake Valley, they moved through southern Nevada and the eastern segments of southern Utah. Jefferson Hunt, a senior Mormon officer of the Battalion, actively searched for settlement sites, minerals, and other resources. His report encouraged 1851 settlement efforts in Iron County, near present-day Cedar City. These southern explorations eventually led to Mormon settlements in St. George, Utah, Las Vegas and San Bernardino, California, as well as communities in southern Arizona.
Prior to establishment of the Oregon and California trails and Mormon settlement, Indians native to the Salt Lake Valley and adjacent areas lived by hunting buffalo and other game, but also gathered grass seed from the bountiful grass of the area as well as roots such as those of the Indian Camas. By the time of settlement, indeed before 1840, the buffalo were gone from the valley, but hunting by settlers and grazing of cattle severely impacted the Indians in the area, and as settlement expanded into nearby river valleys and oases, indigenous tribes experienced increasing difficulty in gathering sufficient food. Brigham Young's counsel was to feed the hungry tribes, and that was done, but it was often not enough. These tensions formed the background to the Bear River massacre committed by California Militia stationed in Salt Lake City during the Civil War. The site of the massacre is just inside Preston, Idaho, but was generally thought to be within Utah at the time.
Statehood was petitioned for in 1849-50 using the name Deseret. The proposed State of Deseret would have been quite large, encompassing all of what is now Utah, and portions of Colorado, Idaho, Nevada, Wyoming, Arizona, Oregon, New Mexico and California. The name of Deseret was favored by the LDS leader Brigham Young as a symbol of industry and was derived from a reference in the Book of Mormon. The petition was rejected by Congress and Utah did not become a state until 1896, following the Utah Constitutional Convention of 1895.
In 1850, the Utah Territory was created with the Compromise of 1850, and Fillmore (named after President Fillmore) was designated the capital. In 1856, Salt Lake City replaced Fillmore as the territorial capital.
The first group of pioneers brought African slaves with them, making Utah the only place in the western United States to have African slavery. Three slaves, Green Flake, Hark Lay, and Oscar Crosby, came west with this first group in 1847. The settlers also began to purchase Indian slaves in the well-established Indian slave trade, as well as enslaving Indian prisoners of war. In 1850, 26 slaves were counted in Salt Lake County. Slavery didn't become officially recognized until 1852, when the Act in Relation to Service and the Act for the relief of Indian Slaves and Prisoners were passed. Slavery was repealed on June 19, 1862, when Congress prohibited slavery in all US territories.
Disputes between the Mormon inhabitants and the federal government intensified after the Church of Jesus Christ of Latter-day Saints' practice of polygamy became known. The polygamous practices of the Mormons, which were made public in 1854, would be one of the major reasons Utah was denied statehood until almost 50 years after the Mormons had entered the area.
After news of their polygamous practices spread, the members of the LDS Church were quickly viewed by some as un-American and rebellious. In 1857, after news of a possible rebellion spread, President James Buchanan sent troops on the Utah expedition to quell the growing unrest and to replace Brigham Young as territorial governor with Alfred Cumming. The expedition was also known as the Utah War.
As fear of invasion grew, Mormon settlers had convinced some Paiute Indians to aid in a Mormon-led attack on 120 immigrants from Arkansas under the guise of Indian aggression. The murder of these settlers became known as the Mountain Meadows massacre. The Mormon leadership had adopted a defensive posture that led to a ban on the selling of grain to outsiders in preparation for an impending war. This chafed pioneers traveling through the region, who were unable to purchase badly needed supplies. A disagreement between some of the Arkansas pioneers and the Mormons in Cedar City led to the secret planning of the massacre by a few Mormon leaders in the area. Some scholars debate the involvement of Brigham Young. Only one man, John D. Lee, was ever convicted of the murders, and he was executed at the massacre site.
Express riders had brought the news 1,000 miles from the Missouri River settlements to Salt Lake City within about two weeks of the army's beginning to march west. Fearing the worst as 2,500 troops (roughly 1/3rd of the army then) led by General Albert Sidney Johnston started west, Brigham Young ordered all residents of Salt Lake City and neighboring communities to prepare their homes for burning and evacuate southward to Utah Valley and southern Utah. Young also sent out a few units of the Nauvoo Legion (numbering roughly 8,000–10,000), to delay the army's advance. The majority he sent into the mountains to prepare defenses or south to prepare for a scorched earth retreat. Although some army wagon supply trains were captured and burned and herds of army horses and cattle run off no serious fighting occurred. Starting late and short on supplies, the United States Army camped during the bitter winter of 1857–58 near a burned out Fort Bridger in Wyoming. Through the negotiations between emissary Thomas L. Kane, Young, Cumming and Johnston, control of Utah territory was peacefully transferred to Cumming, who entered an eerily vacant Salt Lake City in the spring of 1858. By agreement with Young, Johnston established the army at Fort Floyd 40 miles away from Salt Lake City, to the southwest.
Salt Lake City was the last link of the First Transcontinental Telegraph, between Carson City, Nevada and Omaha, Nebraska completed in October 1861. Brigham Young, who had helped expedite construction, was among the first to send a message, along with Abraham Lincoln and other officials. Soon after the telegraph line was completed, the Deseret Telegraph Company built the Deseret line connecting the settlements in the territory with Salt Lake City and, by extension, the rest of the United States.
Because of the American Civil War, federal troops were pulled out of Utah Territory (and their fort auctioned off), leaving the territorial government in federal hands without army backing until General Patrick E. Connor arrived with the 3rd Regiment of California Volunteers in 1862. While in Utah, Connor and his troops soon became discontent with this assignment wanting to head to Virginia where the "real" fighting and glory was occurring. Connor established Fort Douglas just three miles (5 km) east of Salt Lake City and encouraged his bored and often idle soldiers to go out and explore for mineral deposits to bring more non-Mormons into the state. Minerals were discovered in Tooele County, and some miners began to come to the territory. Conner also solved the Shoshone Indian problem in Cache Valley Utah by luring the Shoshone into a midwinter confrontation on January 29, 1863. The armed conflict quickly turned into a rout, discipline among the soldiers broke down, and the Battle of Bear River is today usually referred to by historians as the Bear River Massacre. Between 200 and 400 Shoshone men, women and children were killed, as were 27 soldiers, with over 50 more soldiers wounded or suffering from frostbite.
Beginning in 1865, Utah's Black Hawk War developed into the deadliest conflict in the territory's history. Chief Antonga Black Hawk died in 1870, but fights continued to break out until additional federal troops were sent in to suppress the Ghost Dance of 1872. The war is unique among Indian Wars because it was a three-way conflict, with mounted Timpanogos Utes led by Antonga Black Hawk fighting federal and Utah local militia.
On May 10, 1869, the First transcontinental railroad was completed at Promontory Summit, north of the Great Salt Lake. The railroad brought increasing numbers of people into the state, and several influential businessmen made fortunes in the territory.
Main article: Latter Day Saint polygamy in the late-19th century
During the 1870s and 1880s, federal laws were passed and federal marshals assigned to enforce the laws against polygamy. In the 1890 Manifesto, the LDS Church leadership dropped its approval of polygamy citing divine revelation. When Utah applied for statehood again in 1895, it was accepted. Statehood was officially granted on January 4, 1896.
The Mormon issue made the situation for women the topic of nationwide controversy. In 1870 the Utah Territory, controlled by Mormons, gave women the right to vote. However, in 1887, Congress disenfranchised Utah women with the Edmunds–Tucker Act. In 1867–96, eastern activists promoted women's suffrage in Utah as an experiment, and as a way to eliminate polygamy. They were Presbyterians and other Protestants convinced that Mormonism was a non-Christian cult that grossly mistreated women. The Mormons promoted woman suffrage to counter the negative image of downtrodden Mormon women. With the 1890 Manifesto clearing the way for statehood, in 1895 Utah adopted a constitution restoring the right of women's suffrage. Congress admitted Utah as a state with that constitution in 1896.
Though less numerous than other intermountain states at the time, several lynching murders for alleged misdeeds occurred in Utah territory at the hand of vigilantes. Those documented include the following, with their ethnicity or national origin noted in parentheses if it was provided in the source:
William Torrington in Carson City (then a part of Utah territory), 1859
Thomas Coleman (Black man) in Salt Lake City, 1866
3 unidentified men at Wahsatch, winter of 1868
A Black man in Uintah, 1869
Charles A. Benson in Logan, 1873
Ah Sing (Chinese man) in Corinne, 1874
Thomas Forrest in St. George, 1880
William Harvey (Black man) in Salt Lake City, 1883
John Murphy in Park City, 1883
George Segal (Japanese man) in Ogden, 1884
Joseph Fisher in Eureka, 1886
Robert Marshall (Black man) in Castle Gate, 1925
Other lynchings in Utah territory include multiple instances of mass murder of Native American children, women, and men by White settlers including the Battle Creek massacre (1849), Provo River Massacre (1850), Nephi massacre (1853), and Circleville Massacre (1866).
Beginning in the early 20th century, with the establishment of such national parks as Bryce Canyon National Park and Zion National Park, Utah began to become known for its natural beauty. Southern Utah became a popular filming spot for arid, rugged scenes, and such natural landmarks as Delicate Arch and "the Mittens" of Monument Valley are instantly recognizable to most national residents. During the 1950s, 1960s, and 1970s, with the construction of the Interstate highway system, accessibility to the southern scenic areas was made easier.
Beginning in 1939, with the establishment of Alta Ski Area, Utah has become world-renowned for its skiing. The dry, powdery snow of the Wasatch Range is considered some of the best skiing in the world. Salt Lake City won the bid for the 2002 Winter Olympics in 1995, and this has served as a great boost to the economy. The ski resorts have increased in popularity, and many of the Olympic venues scattered across the Wasatch Front continue to be used for sporting events. This also spurred the development of the light-rail system in the Salt Lake Valley, known as TRAX, and the re-construction of the freeway system around the city.
During the late 20th century, the state grew quickly. In the 1970s, growth was phenomenal in the suburbs. Sandy was one of the fastest-growing cities in the country at that time, and West Valley City is the state's 2nd most populous city. Today, many areas of Utah are seeing phenomenal growth. Northern Davis, southern and western Salt Lake, Summit, eastern Tooele, Utah, Wasatch, and Washington counties are all growing very quickly. Transportation and urbanization are major issues in politics as development consumes agricultural land and wilderness areas.
In 2012, the State of Utah passed the Utah Transfer of Public Lands Act in an attempt to gain control over a substantial portion of federal land in the state from the federal government, based on language in the Utah Enabling Act of 1894. The State does not intend to use force or assert control by limiting access in an attempt to control the disputed lands, but does intend to use a multi-step process of education, negotiation, legislation, and if necessary, litigation as part of its multi-year effort to gain state or private control over the lands after 2014.
Utah families, like most Americans everywhere, did their utmost to assist in the war effort. Tires, meat, butter, sugar, fats, oils, coffee, shoes, boots, gasoline, canned fruits, vegetables, and soups were rationed on a national basis. The school day was shortened and bus routes were reduced to limit the number of resources used stateside and increase what could be sent to soldiers.
Geneva Steel was built to increase the steel production for America during World War II. President Franklin D. Roosevelt had proposed opening a steel mill in Utah in 1936, but the idea was shelved after a couple of months. After the attack on Pearl Harbor, the United States entered the war and the steel plant was put into progress. In April 1944, Geneva shipped its first order, which consisted of over 600 tons of steel plate. Geneva Steel also brought thousands of job opportunities to Utah. The positions were hard to fill as many of Utah's men were overseas fighting. Women began working, filling 25 percent of the jobs.
As a result of Utah's and Geneva Steels contribution during the war, several Liberty Ships were named in honor of Utah including the USS Joseph Smith, USS Brigham Young, USS Provo, and the USS Peter Skene Ogden.
One of the sectors of the beachhead of Normandy Landings was codenamed Utah Beach, and the amphibious landings at the beach were undertaken by United States Army troops.
It is estimated that 1,450 soldiers from Utah were killed in the war.
Full Tour:
www.youtube.com/watch?v=vrH4AOjN23Y&t=28s
PDF Instructions: www.luxurybrickstore.com/
This is the ultimate home on wheels for your minifigure family. Not only are there two levels on this motorhome, but four separate slide outs that allow for maximum floor space possible. There’s even room for atvs, motorcycles, bicycles, and the family car in the enclosed stacker trailer to bring along as well. The original inspiration for this build was a prototype design I randomly came across on the internet. Double decker motorhomes with slide outs are pretty much nonexistent, but I figured why not put one together with Lego.
My C1's modified windshield frame.I hope it's help a little bit to imagine the nonexistent windshield.:)
The picture above attempts to show a few of the weapons and armaments used by the Spaniards in their conquest of Mexico. According to Bernard Grunberg, who set out to trace the origins of the Conquistadores, Cortes landed in Mexico with, “508 soldiers, including 32 crossbowmen and 13 escopeteros (musketeers, gunmen), and 109 seamen on 11 ships.” He would later be joined by more Spaniards from another expedition, but the number remains striking; how could a force of men this size capture a city of about 200,000? What is even more amazing is the Grunberg found that “real soldiers were very few, and officers nonexistent.” The Spanish forces were made up of seaman, carpenters, and laborers. Many historians point to the weapons of the Spaniards as one of the major advantages Cortes exploited in the conquest of Mexico.
The most obvious weapon in use here is the horse, which was unknown in central Mexico, at least as a weapon of devastating cavalry charges. The cavalry of Western Europe was used mainly to outflank an enemy already engaged with ground troops, usually light infantry. The cavalry would charge from the side or behind if possible, causing mass confusion, injury and death. With most of the Siege of Tenochtitlan taking place on Lake Texcoco and in the streets of the city itself, the mass cavalry charge would be more difficult to employ.
However, Bernaz del Castillo, one of Cortes’ own men, describes the effect that horseman did have during the battle. “When the people of the city saw that there were no horsemen with us they turned again on the Spaniards and drove them from the towers and courts… The Spaniards, unable to withstand the onset of the enemy, retreated in great danger and would have suffered great loss had it not pleased God that at that moment three horsemen should arrive… the horsemen killed some of them and we regained the courts and enclosure…. Five or six horsemen had now arrived… they killed over thirty of the enemy.” Even without the use of the mass charge tactics, the Spanish horsemen were able to kill roughly five or six enemy soldiers a piece. The psychological impact of seeing the horsemen inflict such losses is obvious.
Another weapon pictured is the light, but sharp sword used by the Spaniards. A descendant of the Roman gladius, the sword may account for many of the Spanish victories after bullets and powder, the traditionally viewed superior weaponry, had long run dry. As a further testament to its superiority, “the Aztecs quickly employed the precious few Castilian swords and lances the captured.”
The armor used by the Spaniards afforded them little protection against the bludgeoning weapons of the Aztecs. Most Spaniards were originally captured and killed later, but in the siege of Tenochtitlan, the clubs were able to kill a helmeted and armored Spaniard just as well. The main advantage arose in tactics.
Cortes had eighty crossbowmen and harquebusiers at his disposal during the battle. By placing his harquebusiers in formation behind armored swordsmen, and crossbowmen at the rear, Cortes was able to bring deadly fire down on the Aztecs any time they amassed into a large group. The strategy resulted in Aztec casualties growing horrifically high, as the Spaniards main enemy became exhaustion of both the swordsmen and the ammo supplies.
Bernard Grunberg, “The Origins of the Conquistadores of Mexico City,” The Hispanic American Historical Review 74 (1994): 259-283.
Victor Davis Hanson , Carnage and Culture (New York: Doubleday, 2001), 171-232
Bernal Diaz del Castillo, The Discovery and Conquest of Mexico, trans. A.P. Maudslay (New York: Farrar, Straus and Cudahy, 1956) 408.
The Creative Assembly Limited, SEGA of America Inc, Weapons of the Conquistadores, Digital Photograph, 2007, Sugar Hill, GA.
For more information about the Arquebus, please visit:
These pics are of an ABS version of my LDD sliding door mech. Some people told me it would work in hard lego and it does. my first test that wasnt published was without doors but this is conclusive. It works comepletely. The yellow plates in that spacer do make it a bit to high and interfere with the opening a little bit. This can be corrected by moving them to the far top and bottim.
1298FN21
©Romano
Bangle Making
West Bengal, India
A 7-year-old boy works putting glass ornaments onto bangles sold as far away as the US and EU. Working in cramped conditions and exposed to the constant heat of a small forge at his side, his life is one of constant misery. His chances of ever receiving an education are almost nonexistent due in large part to bureaucratic hurdles, poor access, an incompetently run education system and the lack of official commitment to make education - not work - a priority for children.
This was my first time actually plane watching at Miami International Airport (MIA). I checked some spotter websites to find some good locations. They recommended The Holes as being an "official" site so we checked it out. I was pretty disappointed; there was a lot of construction going on and parking was nonexistent. My wife dropped me off. The area is totally exposed. Even though it was December it was pretty hot - no shade, no place to sit, no other people around. The holes are actually pretty small so it's hard to get a lens through the hole. Arrivals were almost impossible to shoot but you could see planes taxiing by for takeoff. After an hour I was cooking so we bagged it. We then went to the area close to the El Dorado furniture store. Much better. There were a bunch of spotters from around the world there. It was a great atmosphere. Nicely shaded, safe, close to some stores and a lot of good traffic to watch. I saw a bunch of planes from airlines I had not seen before, including some airlines I had not heard of. Some of the planes didn't show up on Flight Radar 24 so they were very pleasant surprises. All in all a very good day and I'd love to go back there!
I took these photos in December 2019.
This was my first time actually plane watching at Miami International Airport (MIA). I checked some spotter websites to find some good locations. They recommended The Holes as being an "official" site so we checked it out. I was pretty disappointed; there was a lot of construction going on and parking was nonexistent. My wife dropped me off. The area is totally exposed. Even though it was December it was pretty hot - no shade, no place to sit, no other people around. The holes are actually pretty small so it's hard to get a lens through the hole. Arrivals were almost impossible to shoot but you could see planes taxiing by for takeoff. After an hour I was cooking so we bagged it. We then went to the area close to the El Dorado furniture store. Much better. There were a bunch of spotters from around the world there. It was a great atmosphere. Nicely shaded, safe, close to some stores and a lot of good traffic to watch. I saw a bunch of planes from airlines I had not seen before, including some airlines I had not heard of. Some of the planes didn't show up on Flight Radar 24 so they were very pleasant surprises. All in all a very good day and I'd love to go back there!
I took these photos in December 2019.
Occupy. Peacefully.
Chicago movement is beautiful and full of wonderful and amazing souls.
There is conversation going on. Plato and Socrates would be proud.
There are people from every generation, color, and probably country and financial class.
Gender does not matter, color of one's khakis or skin is nonexistent, education or background does not matter. In the end, everyone is worried about the capitalist disparity in our society. People are worried about their own standing in the caste-system of our generation.
This is where I stop.
It is sad that losing freedom, and countless lives were not the reason for an uprising...but losing financial status is what drove this social change.
Greed is still what drives our civilization toward the cliff.
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Google+ : gplus.to/saini
Facebook: www.facebook.com/paul.saini.photography
Blog: www.paulsaini.com/blog
Web: www.paulsaini.com
Former line between Riera Blanca junction and Barcelona Port Station, closed on June 21, 1985. The photo shows the entrance to the Barcelona Port station, with a branch to the left to CAMPSA facilities, nonexistent today. On the right, wide roads of RENFE. (Image scanned from an original paper).
Antigua línea entre la bifurcación Riera Blanca y la estación de Barcelona Port, clausurada el 21 de junio de 1985. En la foto vemos la entrada a la estación de Barcelona Port, con una derivación a la izquierda hacia las instalaciones de CAMPSA, hoy inexistente. A la derecha, las vías anchas de RENFE. (Foto escaneada de un original de papel).
I have a feeling other folks may want to debate this claim, unless they were to modify it as the birthplace of Chinese beer culture...
Qingdao is China’s premier “beer” city, as the country’s most famous brew – Tsingtao – was founded and continues to be brewed here. (For those who do come to the city, Tsingtao makes a decent dark beer – Yuan Jiang – that is quite hard to get outside of the city.) I guess the easiest comparison I can make would be to say that Qingdao is the same to beer culture here as St. Louis and Milwaukee are in the United States; a town famous for a mass-produced beer.
The Tsingtao brewery and museum (slightly underwhelming, according to my Lonely Planet guidebook) is located on Dengzhou Lu a bit north of Zhongshan Park. Dengzhou Lu is also famously known as Pijiu Jie (Beer Street). During the day, it’s easy to see the nightlife potential. At night, almost every establishment along this stretch of Dengzhou Lu (probably about a half kilometer to a one kilometer long) is a restaurant that opens up with the focus on drinking beer – almost always Tsingtao. (Curiously, in coming by here at night, the taxi took me past Hongjiu Jie – Red Wine Street. It looked quite a bit less subdued as wine culture here is, well, nonexistent. I didn’t have a chance to get back and look around there. Having drunk Chinese wine before…I don’t think I’m missing too much.)
I’ve lived in China for almost three years now; about two years in Shanghai and one year in Tianjin. Shandong province is the province that’s on the sea between the two cities. (From Shanghai to Tianjin by train is around 5 hours; by plane, 2 hours.) Qingdao, probably the most well-known city in Shandong, is a charming city, to say the least. In my opinion, it’s exceptionally photogenic – with very nice beaches, great architecture, good geography/topography, and terrific food.
Qingdao also happens to be known for the most famous of Chinese beers (Tsingtao), which is actually a company started by the Germans. (For what it’s worth, Chinese beers are quite watery and Tsingtao is somewhat like the Budweiser of Chinese beers. That being said, I’m happy to drink an ice cold Tsingtao on a hot summer day whereas I wouldn’t say the same thing about a Budweiser.
So what to make of Qingdao then? Before colonial powers swept in and started chopping up China piecemeal, Qingdao was basically a sleepy fishing village. During the Ming dynasty, a battery was built here. In 1898, the Germans seized control of Qingdao when two missionaries were killed. (Personally, it seems alarming to me that a country could lose a city because two foreigners happened to be killed – and China sure lost a lot that way during the 19th century. I guess that’s the downside to outmoded military technology; the Europeans and Americans basically plundered China…) At any rate, Qingdao was ceded to the Germans for 99 years, but that didn’t last long, thanks to World War I.
During the 15-20 years that the Germans did have control of the town, they managed to build a handful of churches (still standing) and missionaries, in addition to the aforementioned Qingdao brewery. Because of that, a lot of the European architecture has a heavy German influence and there are still a few random signs of German heritage around town.
From the Germans, Qingdao didn’t land directly with the Chinese. It spent 8 years under Japanese control (1914-1922) before being returned to the Kuomintang (aka General Chiang Kai-Shek’s clan). The Japanese took control once again in 1938 (as they swept through northeast China and across half the country) before losing it for the last time in 1945 at the end of World War II. Since then, it’s been in Chinese hands. (Brief history courtesy of Lonely Planet.)
Contemporary Qingdao certainly makes its way as a tourist destination – and it’s a fine one at that. The population (per my LP from 2011) lists it at 1.73 million. The city has a few areas that are quite appealing to tourists: the Old Town (the heart of the city) off the beach and just east of the railway station downtown, Badaguan (which means “eight passes”) is a hilly area with a lot of nice residential architecture to the east of the Old Town. Other than that, there are a lot of parks, a beer street, churches, and a 40 km. scenic walk (which, obviously, most people do not cover from end to end) along the shore which goes by all of the beaches in the area.
All in all, Qingdao is the type of town that, if you get the chance to visit, I think you would find yourself thinking it would be great to return again and again.
The last day of the season at Kings Island. Awesome time to go. The weather was cool, but wonderful. And the crowds were nonexistent. Definitely going again next year on the final day! We had a blast!
I love the opportunity to be backstage at my granddaughter's dance competitions, in spite of the almost nonexistent lighting and cramped (often just plain ugly) dressing rooms. This is from one of favorite routines done by her group choreographed to "All the Best People are Crazy (Mad Hatter)".
Barn is located in Mendon Ponds Park, at the intersection of Clover St and Pond Rd, Mendon, NY (near Rochester)... next to the Nature Center. MC Sheriff Mounted Division was started in 1938.
Mendon Ponds Park is owned and very poorly maintained by the County of Monroe, NY.
Unfortunately, this extraordinary property is rapidly deteriorating due to an egregious lack of care. Trails are not cleared of debris... signs are useless. Park maintenance is essentially nonexistent. They do have a marketing department. Seriously, the taxpayers are paying the salaries of a county parks marketing department.
Email Mendon Ponds Park complaints to: countyexecutive@monroecounty.gov
House of the Golden Well, sometimes called At the Red Chair, the house no. 175 in the Old Town of Prague on the corner of Seminary (no. 2) and Charles (no. 3), near Clementinum.
On the site today of Baroque building with Classicist elements became Romanesque building, whose walls are preserved vaulted cellar at the Seminary Street following the house čp.177 / I. The first written record of this house but it is up to the year 1354 when it cutler Vaclav Muldorfer bought from Nicholas Znojmo. The house was at the time and edited Gothic square around it was called cutlery commons (Latin Plateau cultellatorum). Also in the 15th century there were several cutlers and two Mecir. The house had already been a corner and stood against the church garden. Clement, which was about to southwest facade still nonexistent Klementinum. Its central location expressing house sign midst of the wheel.
In the early 17th century, the house was probably likely to radically rebuilt in the late Renaissance style (as evidenced by a few preserved Gothic elements). In the early 18th century, the house was connected (still recognizably) with the neighboring small Gothic house (in the 17th century, rebuilt in Baroque style) in the Seminary Street and after 1769, was rebuilt on the 3rd floor. In the 80s of the 20th century, the house was significantly modified from the original structure remained only part of the perimeter walls and interiors to the level of the first floor. In basements, ground floor and first floor are barrel vaults.
The facade is decorated with stucco reliefs Johann Ulrich Mayer from 1713. They are located in three levels. Amid under the associated window on the second floor, is in gilded medallion Palladium of Czech, ie. semifigures Stará Boleslav Virgin Mary with Jesus on the octagonal star-founded Circle. Above the star pair of angels bears the crown, under the star is on the sides of a pair of crowned Czech lion. Left stands St. Wenceslas, right there nesvatořečený John of Nepomuk. Around the windows on the first floor is dvojicemorových patrons (left St. Sebastian, right St. Roch) and the third floor of the Jesuit patrons (left about St. Ignatius and right St. Francis Xavier and Francis Borgia). Above the window on the third floor is a relief lying plague patron Saint Rosalia.
Today the building houses a hotel Aurus (www.aurushotel.cz).
cs.wikipedia.org/wiki/D%C5%AFm_U_Zlat%C3%A9_studn%C4%9B_(Karlova)
Siduri Beckman, Philly's first Youth Poet Laureate at her home
for Generocity.org
February 23, 2013
STROBIST:
D700 + 50mm f/1.8D + PWIII
Einstein 640 + MC2 + Photek Softlighter 60" camera left, 4' feathered down
SB600 + 1/2 CTO + PWIII behind Siduri mimicking some nonexistent sun on a dreary/drizzly Saturday morning.
Should definitely be viewed On Black
This is actually very true to how the sky looked that evening. How could you not fall in love with that fire on the horizon?
And the title does double duty... I am alive, I swear. I keep wanting to quote Mark Twain about how the rumors of my death have been greatly exaggerated... or possibly Zaphod Beeblebrox regarding that I might already be dead, I just haven't stopped moving yet. Some days, it's hard to tell which is a truer statement.
The house is coming along, slowly... so slowly... the manual (literally) labor is killing my hands and wrists, making it painful to edit photos and work much at a computer. It'll be worth it in the long run, but it does severely limit how much time I spend at a keyboard outside of what I have to do at work... so friends, please forgive me. I look, I marvel, I ooze a bit of jealousy, and I want you to know much I appreciate your continued support in spite of my semi-nonexistent nature.
::smiles, hugs and ruffled hair as appropriate::
My C1's modified windshield frame.I hope it's help a little bit to imagine the nonexistent windshield.:)
Human Enkeli (Pink hair)
Euri Enkeli (White hair)
I'm so excited!! Today my dream colored wig arrived. Leeke's Sakura was sure the perfect for Enkeli's human shape.
Hoy llegó la peluquita de Enkeli en mi soñado color sakura. De hecho ya había tirado la toalla con ese color... incluso ordené la peluca en misty rose, color que no me llenaba del todo.... hasta que unos días después en el mercado de DoA ... ahi estaba esperandome una peluca en este hermoso color!! [luego la alisaré]
y eso sólo significa una cosa....
www.flickr.com/photos/nonexistent/6053735371/in/photostream
They're the same doll!!! I put 2 pictures together here x3
2013-JUN-04; Mark Bauer had an op-ed article published in the Star Telegram: Stories about redemption are both memorable and educational. The authors of the Bible knew this long ago. King David had his top general Uriah killed so he could marry Uriah?s wife. Jacob stole his brother?s inheritance. The Apostle Peter publicly denied knowing Jesus three times to save his own life..
The Bible is more than 2,000 years old, and it has been painstakingly studied and debated for generations. The rabbis, monks, popes, copyists and typesetters had plenty of opportunities to clean up these narratives and remove these bothersome storylines..
But they didn?t clean it up, and we are fortunate to have the full narrative because King David went on to lead Israel into its Golden Era; Jacob and Esau reconciled; and Peter went on to shepherd the early Christian church..
Those are great stories. And what better learning method is there than to hear about good people or a great nation making bad choices then picking themselves up to go on to do great things?.
But Texas legislators? actions that essentially brought an end to the public school curriculum called CSCOPE make it look like they don?t want real history taught..
CSCOPE is an educational curriculum plan created by the non-profit Texas Education Service Center Curriculum Collaborative. CSCOPE was created in Texas by Texas educators for our Texas schools..
It is optional, and not all school districts use it. Seventy percent of Texas? 1,265 districts, plus some charter schools, have been using CSCOPE, though Crowley is the only large district in Tarrant County..
But many school systems, especially smaller districts (including Castleberry, Cleburne, Lake Worth and White Settlement, plus Weatherford), chose to use CSCOPE because it had good lesson plans that tracked the state?s standardized tests and curriculum standards..
It allowed our teachers to teach without worrying if they were also covering the mandated material..
But then politicians got involved. Some of them found out that CSCOPE covered real history, warts and all. Among the topics that drew complaints: the Boston Tea Party was a morally legitimate but illegal act..
Another example often mentioned by critics: Students were asked to design a flag for a socialist country. Apparently learning about socialist countries was too much..
What?s next? Many of our history textbooks also cover difficult topics about America, including slavery in North America, the My Lai massacre in Vietnam and the invasion of Iraq for nonexistent weapons of mass destruction..
James W. Loewen?s book Lies My Teacher Told Me details how our textbooks are dumbed down to avoid arguments of exactly this type. Publishers want to sell books ? not create the best history books possible and face the controversy that goes with it..
Loewen points out that few textbooks today will mention that Christopher Columbus initiated slavery in the Americas; our first six presidents owned slaves; and liberal President Woodrow Wilson sent troops into Russia, Mexico and the Caribbean without congressional authority..
In the classroom, do we hide our mistakes and hope the next generation doesn?t repeat them? Or do we teach our children that our leaders have not always done the right thing but we learn from our mistakes and are a better country for it?.
As a bill requiring the State Board of Education to give textbook-style review to curriculum plans developed by education service centers moved through the Legislature in May, the centers agreed to stop offering CSCOPE..
But how will districts pay for a replacement curriculum? When your legislator starts crowing about eliminating CSCOPE to preserve ?Texas values,? be sure to point out that we thought a Texas value was learning from our mistakes..
Mark Bauer of Colleyville has taught adult Sunday School for 20 years and has served as a substitute teacher for various North Texas school districts..
www.star-telegram.com/2013/06/03/4905939/texas-end-to-csc...