The second stop on the way home from my college visit was in Richmond!

The Richmond Kmart appears to be a former Grants (and thus reminded me of the Erie Kmart that I visited last summer). It is very noticeably bigger than Anderson; it is also very nice; it has a Kmart Express gas station and it has a former Kmart Cafe (that still has the counter/displays, the full menu board and even the register! Looks like a more recent KCafe closure from what I've seen; if anybody else here has any more information I would like to know more about it!). This store appears to be doing fairly well for one of the last remaining stores in/near the Miami Valley.

Of course, I had to check out the Kmart Express after my main store rounds were complete, so I headed over there and looked around. This is the second Kmart Express I've seen, but the first one I have actually visited, as the other one (at the now nonexistent Brooklyn Super Kmart) had already closed. I didn't buy anything at this KExpress though, as I had spent my money in the main store. Hopefully next time I can buy some coffee or donuts from Kmart Express while going to/from Anderson (if I plan another college visit to Anderson U, which is likely)!

Hopefully the Richmond Kmart will still be able to remain "normal" for a good time longer...I like this store! :D

Kmart #7246 - 3150 National Road West - Richmond, Indiana

Pepacton Cemetery. Cannonsville Reservoir reinterments. Board of Water Supply force placing memorials and concrete markers at graves, and resurfacing the cemetery by placing topsoil, seed and fertilizer. Camera located approximately 75' west of Section 92, looking easterly. Photo shows an area extending across the middle third of the picture on which mulch, in the form of loose hay, has been placed on the upper and lower slopes of the cemetery, also covering the Sections 92 to 105 which were disturbed by natural forces during the winter and spring. The cemetery roadway, seen in the upper left, was nonexistent at the start of the project; it was aligned and graded to conform to existing conditions. That section of the roadway at the extreme left of the picture is the start of a sharp curve on a steep slope and contains considerable run-of-bank gravel fill. At the upper left are seen the memorials of Section 62 and 66 inclusive, while in the center of the picture, at the south shoulder of the cemetery road, are seen concrete highway posts, triangular in shape, about 6' in length and embedded approximately 2.5' in the ground. The protruding 3.5' of these posts were painted, before embedding, with two coats of a good quality of outside white concrete paint, on which have been stenciled with black paint the name of the cemetery from which the bodies therein were disinterred. July 22, 1965. (Digital Image ID: CRP112)

Something I Do *NOT* Need

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FGR theme o' the day: Ads for Nonexistent Products

And to give THIS one a run for her money.

This photo was taken on 20 March 2017, but I also saw and photographed these rather strange animals every day that we were staying at the Asa Wright Nature Centre on the island of Trinidad. They like to hang around the Asa Wright building, finding food, and then they seem to disappear into the forest for most of the day. Many of my photos of them came out blurry for some reason, but this one worked OK.

"Agoutis have five front and three hind toes; the first toe is very small. The tail is very short or nonexistent and hairless. Agoutis may grow to be up to 60 cm (24 in) in length and 4 kg (8.8 lb) in weight. Most species are brown on their backs and whitish or buff on their bellies; the fur may have a glossy appearance and then glimmers in an orange colour. Reports differ as to whether they are diurnal or nocturnal animals.... They can live for as long as 20 years, a remarkably long time for a rodent

In the wild, they are shy animals and flee from humans, while in captivity they may become trusting. In Trinidad, they are renowned for being very fast runners, able to keep hunting dogs occupied with chasing them for hours." From Wikipedia.

en.wikipedia.org/wiki/Common_agouti

This adventure was only the second holiday of any kind, anywhere, that I have had in something like 30 or 35 years! The other holiday was a wonderful, one-week trip with my dear friends from England, Linda and Tony, when we went down south to Yellowstone National Park and the Grand Tetons in September 2012. I have had maybe half a dozen weekends away, including to Waterton National Park, which have helped keep me going.

Six birding/photographer friends and I decided that we would take this exciting trip together (from 12-21 March 2017), spending the first two or three days on the island of Tobago and then the rest of the time at the Asa Wright Nature Centre on the nearby, much larger island of Trinidad. We decided to take a complete package, so everything was included - accommodation at both places, all our food, and the various walks and day trips that we could choose from. Two of my friends, Anne B. and Brenda, saw to all the planning of flights and accommodations, which was so very much appreciated by the rest of us. I could never have done all this myself! We were so lucky with our flights, as we were just in time to get Black Friday prices, which were 50% off!

What a time we had, seeing so many beautiful and interesting things - and, of course, everything was a lifer for me. Some of these friends had visited Costa Rica before, so were familiar with some of the birds. There was a lot more to see on Trinidad, so we were glad that we chose Tobago to visit first and then spend a longer time at Asa Wright. It was wonderful to be right by the sea, though, at the Blue Waters Inn on the island of Tobago. Just gorgeous.

The Asa Wright Nature Centre, on Trinidad, is such an amazing place! We stayed in cabins up or down hill from the main building. Really, one doesn't need to travel away from the Centre for birding, as so many different species visit the Hummingbird feeders that are right by the huge, open veranda, and the trees of the rain forest high up the mountainous road. The drive up and down this narrow, twisting, pot-holed road was an adventure in itself! Never would I ever do this drive myself - we had a guide who drove us everywhere in a minibus. I had read many accounts of this road, lol! There was enough room for two vehicles to pass each other, and the honking of horns was almost continuous - either to warn any vehicle that might be coming fast around the next bend or as a sign that drivers knew each other. The drive along this road, from the coast to Asa Wright, took just over an hour each way.

I still miss the great food that was provided every single day at Asa Wright and even the Rum Punch that appeared each evening. I never drink at all, so I wasn't sure if I would even try the Punch - glad I did, though, as it was delicious and refreshing. Breakfast, lunch and dinner were all served buffet-style, with a great variety of dishes from which to choose. To me, pure luxury. So very, very grateful to have been invited to be part of this amazing adventure.

This is a video that I came across on YouTube, taken by Rigdon Currie and Trish Johnson, at many of the same places we visited on Trinidad and Tobago. Not my video, but it made me feel like I was right there still. Posting the link here again, so that I won't lose it.

youtu.be/BBifhf99f_M

I also came across the following 27-minute YouTube video of the flora and fauna of Trinidad, filmed by John Patrick Smith in February 2015.

youtu.be/6HHBm9MIxnk

I found Burt in my toolbox not to long ago.

He is a symbol of a car that no longer exists. A car that was important to a few people- me being one of them.

The 1994 Crown Victoria police car that once served as Burt's home was just one of 15 new patrol cars awaiting assignment that summer. It was unceremoniously named 8025 and for me became a special car right from the beginning.

On Saturday nights back then I drove a bus for a city sponsored group. In July of 1994 I had begun to date a woman who, on occasion, would accompany me on my weekly rides. The bus I drove didn't have air conditioning and by the end of those July nights we were pretty well soaked. After parking the bus one night she asked me, “What's with all of those brand new cars over there?” pointing at the 15 new patrol cars. I knew where we kept the keys so I picked one, jumped in, started it and cranked up the “AC”. The cool air was nice but the company was even nicer. Needless to say that car became special and I had made a mental note as to which one it was.

A few weeks later the cars were numbered and permanently assigned. One of the female officer's, who I had become friends with, came in and asked me which one was 8025?

“Oh, you got the make-out car!”

She looked at me with a combination of horror and amusement (I think) and I told her the story.

She was one of my favorite officers- driving my favorite car, so there were perks. 8025 for years was unquestionably the best maintained vehicle in the city. It didn't wait in line for anything. If there was a road call or she was going out of town and the car needed looking after, I was there.

One day in April of 1998 a flatbed tow truck came into the motorpool with 8025 riding up top. I walked over to it wondering what was wrong (and why I didn't get the call) when I realized that the drivers side of the car was almost nonexistent. 8025 took such a “T-bone” hit on the left front door that the drivers seat couldn't be seen.

My heart sank- where was she and how bad was she hurt.

All I could find out was another police car hit hers during a chase and she was taken to the hospital.

It's customary to remove personal items from a wreck and secure them until the officer can reclaim their stuff. I was in the process of crawling through her car when I noticed a car pull up. Her husband is also a cop and, just out of the hospital, the two of them had come by for a look at the damage. . Relieved to see her, I walked over and said: “Don't worry “Crash”, I can fix it!”

She was out for two months with a broken pelvis and came back to work on light duty. .

8025...was a total loss- or so everyone thought.

I made a deal with Cliff that if I could drive it to the body shop for an estimate, he would fix it.

A few days later, I fired up 8025 and ignored cliff's screams as I drove out of the motorpool. I had to straddle the center console and operate the brake and gas with my left foot (the door was where the drivers seat was supposed to be) but I made it. When I came back and gave him the estimate he laughed and said “Ya know if it was anyone else's car it would be so gone...OK, Lets fix it.”

A few weeks later 8025 came back to the motorpool good as new.

I kept it safe until she got off of light duty. I was so happy to give her that car back. She drove it for many years after that. Ultimately, she was assigned a newer car and 8025 went for auction. I remember saying to the winner that last day, “You are getting one special car.” I doubt he realized how special it truly was.

And Burt...

Burt I found under the seat the day I brought it to the body shop. It was her sons toy. One of those mementos that are kept as a reminder of the people who are important in your life.

I put Burt back in my toolbox...where he is safe.

Click here for this years 365 collection.

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.

NWA 2737

Martian Chassignite

Morocco

Found: 2000

TKW: 611 g / OBJ: Micro

NORTHWEST AFRICA 2737

‘Diderot’

Martian Chassignite

Dunite

Nine rock fragments constituting a single 611 g stone were found in the Moroccan Sahara by meteorite hunters under the organization of Bruno Fectay and Carine Bidaut. These black fragments were not recognized as meteoritic until several years later, at which time a sample was submitted for analysis. The importance of this meteorite was soon evident, and multiple analyses were conducted through a collaboration of research groups in France and elsewhere:

Laboratoire des Sciences de la Terre, (Centre National de la Recherche Scientifique—Unité Mixte de Recherche [CNRS–UMR]), École Normale Supérieure de Lyon: P. Beck, Ph. Gillet, B. Van de Moortele, B. Reynard

Université de Bretagne Occidentale, Institut Universitaire Européen de la Mer: J-A. Barrat, J. Cotten

Institut français de recherche pour l'exploitation de la mer (IFREMER), Centre de Brest (Centre national de la recherche scientifique—Unité mixte de recherche [CNRS-UMR]): M. Bohn

Planetary and Space Science Research Institute, Open University, United Kingdom: I.A. Franchi, R.C. Greenwood

Johnson Space Center, Houston, Texas

University of Tokyo, Japan

With the assigned name of NWA 2737, this olivine–chromite cumulate was classified as a dunite that exhibits many mineralogical, chemical, and petrographical similarities to the first known martian chassignite that fell in Chassigny, France in 1815. A third chassignite designated NWA 8694 (photo courtesy of L. Labenne) has been classified at the Museum National d'Histoire Naturelle, Paris, France (Hewins et al., 2014, 2015). Northwest Africa 2737 is composed of 89.6 vol% shock-blackened, cumulus forsteritic olivine, 3.1 vol% chromite, 1.6 vol% sanidine, 1.0 vol% pyroxene (augite, pigeonite, and orthopyroxene), and 0.2 vol% phosphate. Carbonates are present in both chassignites, with at least some of them showing evidence for a martian origin—shock fractures post-date the carbonate formation (Beck et al., 2006). Both chassignites have similar REE patterns, elements that are carried mostly in their apatite component. A martian origin is attested by the abundance ratio of Fe/Mn in olivine, the bulk Na/Al ratios, and by the O-isotopic ratios.

Northwest Africa 2737 is one of the least terrestrially altered martian finds as shown by its trace element composition (e.g., low Ba and Sr contents) and noble gas signatures. However, in contrast to Chassigny and the nakhlites, NWA 2737 contains trapped noble gases more similar to those in shergottites, as evidenced by the lack of martian mantle Xe, the lack of fission-derived Xe from plutonium, and the enrichment of martian atmospheric Xe (Marty et al., 2006).

While feldspars in Chassigny are mostly composed of plagioclase, with lesser amounts of labradorite and sanidine, the feldspars in NWA 2737 only occur as K-rich sanidine or Na-rich analbite. These differences could have been caused by a relatively low Al concentration in the parental melt, resulting in the delayed nucleation of plagioclase with a consequent buildup of Na in the melt (Beck et al., 2006; Papike et al., 2009). The olivine and chromite grains in both chassignites contain melt inclusions with a unique mineralogy, including the occurrence of hydrous kaersutitic (Ti-rich) amphibole, while those in NWA 2737 also include an alkali feldspar-rich glass. Six distinct melt inclusion species were described in NWA 2737 by He et al. (2010,2013) based on the diverse mineral assemblages, including olivine, orthopyroxene, augite, pigeonite, kaersutite, chlorapatite and fluorapatite, biotite, chromite, pyrrhotite, and feldspathic glass; these minerals occur in melt inclusions that span a wide range of sizes (~5–300 µm). It is thought that some melt inclusions might contain trapped parental magma at various stages of fractionation.

It was determined experimentally that the parental magma of the chassignites may have resembled a terrestrial, silica-saturated hawaiite magma with a higher than terrestrial Mg# and an aluminum content of ~12 wt% (Filiberto, 2008). It was ascertained that the chassignites likely crystallized after ~30% crystallization of mafic phases was attained.

In an effort to estimate the original magma composition of the cumulate chassignites, He et al. (2013) examined the ubiquitous, sub-mm-sized, trapped magmatic inclusions in olivine grains. In consideration of the water diffusion coefficient between amphibole and melt, as well as the extent of melt crystallization that occurred prior to amphibole formation (~45%) and other pertinent assumptions, the water content of the primary melt of NWA 2737 was calculated to be ~0.48–0.67 wt%; the water content of the primary melt of the Chassigny meteorite was previously calculated by McCubbin et al. (2010) to be 0.43–0.84 wt%. Utilizing the MELTS program with the known parameters, the research team determined that NWA 2737 was formed under pressure of ~6.8 kbar. Their deduced parental composition for NWA 2737 based on Ca:Al ratios and Mg# is quite similar to that of the martian basalt Humphrey, measured in situ by the MER rover Spirit in Gusev Crater. A broad range of Al contents has been found in martian parental source rocks—Al is relatively high in basaltic surface rocks and the chassignites, while it is thought to have been sequestered at depth in garnet in the nakhlites and most shergottites; this has implications for the magma ocean scenario of Mars' petrogenetic history.

Several differences between Chassigny and NWA 2737 have been identified by Mikouchi (2005): interstitial chromite has a larger grain size in NWA 2737, feldspar occurs as the sodic plagioclase albite in NWA 2737 rather than the calcic plagioclase anorthite, and all phases of NWA 2737 have a more magnesian composition than those in Chassigny, perhaps reflecting conditions of higher temperature and pressure during fractional crystallization from a less evolved parental melt as suggested by Nekvasil et al. (2005). Petrographic evidence indicates that NWA 2737 was the first cumulate to crystallize at the bottom of the pile, followed by Chassigny next in the sequence, while the order for NWA 8694 remains to be determined (McCubbin et al., 2013). In further studies, Mikouchi et al. (2016) found that significant ambiguities exist among the three known chassignites. For example, although each of the chassignites exhibit a similar cooling rate (0.003–0.1 °C/hr), olivine compositions between them show large variations: NWA 8694 is Fa46, Chassigny is Fa31, and NWA 2737 is Fa21; moreover, each chassignite exhibits a distinct shock history. Therefore, they suggest that each of the chassignites is more likely associated with a separate flow or lobe (possibly within a common extensive igneous unit) rather than a single sequential accumulation. See the Nakhla page for further details on the stratographic sequence for nakhlites and chassignites.

Lorand et al. (2012) studied the sulfide mineralogy and native metal assemblages in NWA 2737 and made comparisons to Chassigny. While the bulk sulfide abundance in NWA 2737 is low, troilite (and rare pentlandite) blebs up to tens of µm in size are ubiquitous at primary mineral grain contacts, and as even smaller blebs associated with chromite within melt inclusions. Although the sulfide pyrite is abundant in Chassigny, it was not identified in NWA 2737, and the Cu-sulfide chalcopyrite was virtually nonexistent; both sulfide phases were likely lost during an impact-heating event. Similarly, Fe–Os–Ir alloys that are observed in close association with troilite grains in NWA 2737 are considered to have exsolved from pyrrhotite during subsequent cooling from an impact-heating event. These differences that exist between these two chassignites can be attributed to impact-shock-related reduction processes involving high temperatures, leading to the devolatilization of S and the loss of magnetic properties.

While the overall shock effects in Chassigny are only moderate (S4), portions are present that must have experienced much higher shock pressures (45–55 GPa; S5–S6) consistent with the presence of planar deformation features and localized melting. By contrast, the olivine in NWA 2737 exhibits exceptional darkening which is thought to reflect the disordered lattice state of an incomplete transformation to olivine high pressure polymorphs, as well as the presence of nanophase FeNi-metal particles within the olivine (Reynard et al., 2006). These Fe nanoparticles are thought to have formed through subsolidus reduction of olivine during the high temperature phase (~1300°C) of a shock event corresponding to a minimum shock stage of S5. A partial cause of the darkening (brown color) in olivines as described by Treiman et al. (2006) derives from the conversion of Fe2+ to Fe3+ in an oxidizing environment, resulting from the shock heating loss of H+ that was previously dissolved in a hydrous magma. Only a low ppm abundance of Fe3+ would be required to cause the observed darkening. Continued investigations utilizing spectral reflectance techniques, including Mössbauer spectroscopy, indicate that the darkening is primarily the result of shock disseminated nanophase metallic iron particles (Pieters et al., 2007). Other deformed olivine grains in NWA 2737 have been recrystallized to a visually colorless phase. Takenouchi et al. (2015) suggested that the Fe nanoparticles were formed in association with high-pressure polymorphs such as wadsleyite during a high-pressure, high-temperature shock event. Ultimately, the wadsleyite was back-transformed to olivine during a period of high post-shock temperatures, and this olivine now appears brown due to the presence of the Fe nanoparticles. Subsequent studies were conducted by Takenouchi and Mikouchi (2016) of NWA 2737 and several shergottites that contain darkened olivine associated with shock-melt phases. They found higher Fe3+ ratios in both brown (or brownish) olivine compared to adjacent colorless olivine located within the same grain, attesting to the formation of Fe nanoparticles by olivine oxidation and reduction during transformation to high-pressure polymorphs such as ringwoodite and wadsleyite.

Cooling rate estimates for both Chassigny and NWA 2737 have been set at 28–30°C/year, consistent with a formation within a thick lava flow or a shallow dike or sill. The Sm–Nd data for both plot on a similar isochron—1.416 (±0.057) b.y. for NWA 2737, and 1.380 (±0.030) b.y. for Chassigny. Both of these chassignites, as well as the nakhlites, also have similar CRE ages of 10–11 m.y. based on 3He and 21Ne. Therefore, it may be argued that both of these chassignites, as well as the nakhlites, were ejected during a common impact event from the same igneous region on Mars. Based on Ar–Ar data, it was proposed by Bogard and Garrison (2008) that NWA 2737 may have experienced an intense impact event resulting in its burial ~1–20 m deep under a warm ejecta blanket, while a subsequent, less-intense impact event was responsible for its ejection from Mars 10–11 m.y. ago.

Differences have been noted in the gas retention ages of Chassigny and NWA 2737. After correction for terrestrial contamination, a more accurate determination of the K–Ar crystallization age for NWA 2737 was made, and this revised K–Ar age of 376 (±168) m.y. is significantly younger than that of Chassigny and the nakhlites, and more like that of shergottites (Marty et al., 2005; 2006). However, this discordant age has been attributed to the higher shock metamorphism experienced by NWA 2737

Barrow, Alaska, was practically nonexistent sixty years ago when my father was stationed at Point Barrow; but even then Browers Cafe was ancient. Originally built as a whaling station in the Nineteenth Century, it was a general store during my dad's time there.

These days, it's a very nice restaurant where I had a cheeseburger which was excellent verging on spectacular, and some Chinese dumplings which weren't quite so much.

Out back of the restaurant, on a long beach running down to the Arctic Ocean, are the skeletons of two whaling boats and one (partial) whale.

Flower Mound TX. (Photo rotated to horizontal for better viewing) Many weeks later we found our little friend in much better shape and with a longer tail, although as you can see the new tail is inferior with its coloring and distorted shape. Fortunately, we have many places for such critters to hide. I had to stand on my tip toe with my point and shoot and could not get very close because it kept running away. Note how parts of his body blends in with the screen. The Greater Roadrunners keep our toads, frogs and lizards almost nonexistent. I have noticed a change in coloring of these lizards over the years, as they are becoming paler and more yellowish. I found a sick one the other day that was really yellow, perhaps from liver problems. We do not use pesticide except for the fire ants that are taking over.

NWA 2737

Martian Chassignite

Morocco

Found: 2000

TKW: 611 g / OBJ: Micro

NORTHWEST AFRICA 2737

‘Diderot’

Martian Chassignite

Dunite

Nine rock fragments constituting a single 611 g stone were found in the Moroccan Sahara by meteorite hunters under the organization of Bruno Fectay and Carine Bidaut. These black fragments were not recognized as meteoritic until several years later, at which time a sample was submitted for analysis. The importance of this meteorite was soon evident, and multiple analyses were conducted through a collaboration of research groups in France and elsewhere:

Laboratoire des Sciences de la Terre, (Centre National de la Recherche Scientifique—Unité Mixte de Recherche [CNRS–UMR]), École Normale Supérieure de Lyon: P. Beck, Ph. Gillet, B. Van de Moortele, B. Reynard

Université de Bretagne Occidentale, Institut Universitaire Européen de la Mer: J-A. Barrat, J. Cotten

Institut français de recherche pour l'exploitation de la mer (IFREMER), Centre de Brest (Centre national de la recherche scientifique—Unité mixte de recherche [CNRS-UMR]): M. Bohn

Planetary and Space Science Research Institute, Open University, United Kingdom: I.A. Franchi, R.C. Greenwood

Johnson Space Center, Houston, Texas

University of Tokyo, Japan

With the assigned name of NWA 2737, this olivine–chromite cumulate was classified as a dunite that exhibits many mineralogical, chemical, and petrographical similarities to the first known martian chassignite that fell in Chassigny, France in 1815. A third chassignite designated NWA 8694 (photo courtesy of L. Labenne) has been classified at the Museum National d'Histoire Naturelle, Paris, France (Hewins et al., 2014, 2015). Northwest Africa 2737 is composed of 89.6 vol% shock-blackened, cumulus forsteritic olivine, 3.1 vol% chromite, 1.6 vol% sanidine, 1.0 vol% pyroxene (augite, pigeonite, and orthopyroxene), and 0.2 vol% phosphate. Carbonates are present in both chassignites, with at least some of them showing evidence for a martian origin—shock fractures post-date the carbonate formation (Beck et al., 2006). Both chassignites have similar REE patterns, elements that are carried mostly in their apatite component. A martian origin is attested by the abundance ratio of Fe/Mn in olivine, the bulk Na/Al ratios, and by the O-isotopic ratios.

Northwest Africa 2737 is one of the least terrestrially altered martian finds as shown by its trace element composition (e.g., low Ba and Sr contents) and noble gas signatures. However, in contrast to Chassigny and the nakhlites, NWA 2737 contains trapped noble gases more similar to those in shergottites, as evidenced by the lack of martian mantle Xe, the lack of fission-derived Xe from plutonium, and the enrichment of martian atmospheric Xe (Marty et al., 2006).

While feldspars in Chassigny are mostly composed of plagioclase, with lesser amounts of labradorite and sanidine, the feldspars in NWA 2737 only occur as K-rich sanidine or Na-rich analbite. These differences could have been caused by a relatively low Al concentration in the parental melt, resulting in the delayed nucleation of plagioclase with a consequent buildup of Na in the melt (Beck et al., 2006; Papike et al., 2009). The olivine and chromite grains in both chassignites contain melt inclusions with a unique mineralogy, including the occurrence of hydrous kaersutitic (Ti-rich) amphibole, while those in NWA 2737 also include an alkali feldspar-rich glass. Six distinct melt inclusion species were described in NWA 2737 by He et al. (2010,2013) based on the diverse mineral assemblages, including olivine, orthopyroxene, augite, pigeonite, kaersutite, chlorapatite and fluorapatite, biotite, chromite, pyrrhotite, and feldspathic glass; these minerals occur in melt inclusions that span a wide range of sizes (~5–300 µm). It is thought that some melt inclusions might contain trapped parental magma at various stages of fractionation.

It was determined experimentally that the parental magma of the chassignites may have resembled a terrestrial, silica-saturated hawaiite magma with a higher than terrestrial Mg# and an aluminum content of ~12 wt% (Filiberto, 2008). It was ascertained that the chassignites likely crystallized after ~30% crystallization of mafic phases was attained.

In an effort to estimate the original magma composition of the cumulate chassignites, He et al. (2013) examined the ubiquitous, sub-mm-sized, trapped magmatic inclusions in olivine grains. In consideration of the water diffusion coefficient between amphibole and melt, as well as the extent of melt crystallization that occurred prior to amphibole formation (~45%) and other pertinent assumptions, the water content of the primary melt of NWA 2737 was calculated to be ~0.48–0.67 wt%; the water content of the primary melt of the Chassigny meteorite was previously calculated by McCubbin et al. (2010) to be 0.43–0.84 wt%. Utilizing the MELTS program with the known parameters, the research team determined that NWA 2737 was formed under pressure of ~6.8 kbar. Their deduced parental composition for NWA 2737 based on Ca:Al ratios and Mg# is quite similar to that of the martian basalt Humphrey, measured in situ by the MER rover Spirit in Gusev Crater. A broad range of Al contents has been found in martian parental source rocks—Al is relatively high in basaltic surface rocks and the chassignites, while it is thought to have been sequestered at depth in garnet in the nakhlites and most shergottites; this has implications for the magma ocean scenario of Mars' petrogenetic history.

Several differences between Chassigny and NWA 2737 have been identified by Mikouchi (2005): interstitial chromite has a larger grain size in NWA 2737, feldspar occurs as the sodic plagioclase albite in NWA 2737 rather than the calcic plagioclase anorthite, and all phases of NWA 2737 have a more magnesian composition than those in Chassigny, perhaps reflecting conditions of higher temperature and pressure during fractional crystallization from a less evolved parental melt as suggested by Nekvasil et al. (2005). Petrographic evidence indicates that NWA 2737 was the first cumulate to crystallize at the bottom of the pile, followed by Chassigny next in the sequence, while the order for NWA 8694 remains to be determined (McCubbin et al., 2013). In further studies, Mikouchi et al. (2016) found that significant ambiguities exist among the three known chassignites. For example, although each of the chassignites exhibit a similar cooling rate (0.003–0.1 °C/hr), olivine compositions between them show large variations: NWA 8694 is Fa46, Chassigny is Fa31, and NWA 2737 is Fa21; moreover, each chassignite exhibits a distinct shock history. Therefore, they suggest that each of the chassignites is more likely associated with a separate flow or lobe (possibly within a common extensive igneous unit) rather than a single sequential accumulation. See the Nakhla page for further details on the stratographic sequence for nakhlites and chassignites.

Lorand et al. (2012) studied the sulfide mineralogy and native metal assemblages in NWA 2737 and made comparisons to Chassigny. While the bulk sulfide abundance in NWA 2737 is low, troilite (and rare pentlandite) blebs up to tens of µm in size are ubiquitous at primary mineral grain contacts, and as even smaller blebs associated with chromite within melt inclusions. Although the sulfide pyrite is abundant in Chassigny, it was not identified in NWA 2737, and the Cu-sulfide chalcopyrite was virtually nonexistent; both sulfide phases were likely lost during an impact-heating event. Similarly, Fe–Os–Ir alloys that are observed in close association with troilite grains in NWA 2737 are considered to have exsolved from pyrrhotite during subsequent cooling from an impact-heating event. These differences that exist between these two chassignites can be attributed to impact-shock-related reduction processes involving high temperatures, leading to the devolatilization of S and the loss of magnetic properties.

While the overall shock effects in Chassigny are only moderate (S4), portions are present that must have experienced much higher shock pressures (45–55 GPa; S5–S6) consistent with the presence of planar deformation features and localized melting. By contrast, the olivine in NWA 2737 exhibits exceptional darkening which is thought to reflect the disordered lattice state of an incomplete transformation to olivine high pressure polymorphs, as well as the presence of nanophase FeNi-metal particles within the olivine (Reynard et al., 2006). These Fe nanoparticles are thought to have formed through subsolidus reduction of olivine during the high temperature phase (~1300°C) of a shock event corresponding to a minimum shock stage of S5. A partial cause of the darkening (brown color) in olivines as described by Treiman et al. (2006) derives from the conversion of Fe2+ to Fe3+ in an oxidizing environment, resulting from the shock heating loss of H+ that was previously dissolved in a hydrous magma. Only a low ppm abundance of Fe3+ would be required to cause the observed darkening. Continued investigations utilizing spectral reflectance techniques, including Mössbauer spectroscopy, indicate that the darkening is primarily the result of shock disseminated nanophase metallic iron particles (Pieters et al., 2007). Other deformed olivine grains in NWA 2737 have been recrystallized to a visually colorless phase. Takenouchi et al. (2015) suggested that the Fe nanoparticles were formed in association with high-pressure polymorphs such as wadsleyite during a high-pressure, high-temperature shock event. Ultimately, the wadsleyite was back-transformed to olivine during a period of high post-shock temperatures, and this olivine now appears brown due to the presence of the Fe nanoparticles. Subsequent studies were conducted by Takenouchi and Mikouchi (2016) of NWA 2737 and several shergottites that contain darkened olivine associated with shock-melt phases. They found higher Fe3+ ratios in both brown (or brownish) olivine compared to adjacent colorless olivine located within the same grain, attesting to the formation of Fe nanoparticles by olivine oxidation and reduction during transformation to high-pressure polymorphs such as ringwoodite and wadsleyite.

Cooling rate estimates for both Chassigny and NWA 2737 have been set at 28–30°C/year, consistent with a formation within a thick lava flow or a shallow dike or sill. The Sm–Nd data for both plot on a similar isochron—1.416 (±0.057) b.y. for NWA 2737, and 1.380 (±0.030) b.y. for Chassigny. Both of these chassignites, as well as the nakhlites, also have similar CRE ages of 10–11 m.y. based on 3He and 21Ne. Therefore, it may be argued that both of these chassignites, as well as the nakhlites, were ejected during a common impact event from the same igneous region on Mars. Based on Ar–Ar data, it was proposed by Bogard and Garrison (2008) that NWA 2737 may have experienced an intense impact event resulting in its burial ~1–20 m deep under a warm ejecta blanket, while a subsequent, less-intense impact event was responsible for its ejection from Mars 10–11 m.y. ago.

Differences have been noted in the gas retention ages of Chassigny and NWA 2737. After correction for terrestrial contamination, a more accurate determination of the K–Ar crystallization age for NWA 2737 was made, and this revised K–Ar age of 376 (±168) m.y. is significantly younger than that of Chassigny and the nakhlites, and more like that of shergottites (Marty et al., 2005; 2006). However, this discordant age has been attributed to the higher shock metamorphism experienced by NWA 2737

Actually it posted hours after I tried to post it so I was fast asleep. I live in the woods and the internet is almost nonexistent...

Arachnophobia - (ə-rāk'nə-fō'bē-ə, -nō-)

"Arachnophobia" is derived from the Greek "arachne" (spider) and "phobos" (fear). The Greek word was derived from the name "Arachne," a maiden in Greek mythology whom the goddess Athena turned into a spider after the girl, a skilled weaver, challenged Athena to a weaving contest. .

Ruigrijk | Python 31/03/2018 13h04

The contemporary way of communication in the Efteling. Designer Anton Pieck (19 April 1895 – 24 November 1987) who died more than 30 years ago never could imagine what this sign was about. Social media like Facebook, Messenger, Twitter, Instagram and Snapchat were nonexistent. Anton Pieck never wanted the Python in 'his' park as well, but the opening of Python transformed De Efteling from a playground with some fairytales to one of the most important themeparks in Europe and even in the world.

De Efteling

The Efteling is a fantasy-themed amusement park in Kaatsheuvel in the Netherlands. The attractions are based on elements from ancient myths and legends, fairy tales, fables, and folklore.

The park was opened in 1952. It has since evolved from a nature park with a playground and a Fairytale Forest into a full-sized theme park. It now caters to both children and adults with its cultural, romantic, and nostalgic themes, in addition to its wide array of amusement rides.

It is the largest theme park in the Netherlands and one of the oldest theme parks in the world. It is twice as large as the original Disneyland park in California and antedates it by three years. Annually, the park has nearly 5 million visitors. In 2016, it was the third most visited theme park in Europe, behind Disneyland Paris and Europa-Park. Over the years, it has received over 125 million visitors.

Location: Kaatsheuvel, North Brabant, Netherlands

Opened: 1952

Operating season: Year-round

Visitors per annum: 4.76 million in 2016

Area: 72 ha the park; 276 ha the resort

Rides: Total 35

Roller coasters 6

Water rides 4

[ Source and much more Info: Wikipedia - De Efteling [2017]

Oolick is a rambunctious little guy that never shuts up! He is the worst gossip in Hollywood. Racing around on those little wheels of his, he can spread news like a wildfire. The only trouble is that his memory is shot and his attention span is nonexistent. So, he gets all his stories mixed up. How did you think Tabloids get all their crazy stories?

Robot sculpture assembled from found objects by Brian Marshall - Wilmington, DE. Items included in my sculptures vary from vintage household kitchen items to recycled industrial scrap. Some of my favorite items to use are old oil cans, aluminum measuring spoons, electrical meters, retro blenders, anodized cups, and pencil sharpeners.

An nonexistent endless dream game without sense and rules.

Columbia Flyway Wildlife Show Association

35th Annual Show

Wildfowl, Wildlife, Fish & Artistic Creations Carving Competition and Art Festival aka Columbia Flyway Wildlife Show

Clatsop County Fairgrounds and Expo Center in Astoria, Oregon

September 21-22, 2024

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Speaking of snipe hunts:

A snipe hunt is a type of practical joke or fool's errand, in existence in North America as early as the 1840s, in which an unsuspecting newcomer is duped into trying to catch an elusive, nonexistent animal called a snipe. Although snipe are an actual family of birds, a snipe hunt is a quest for an imaginary creature whose description varies.

The target of the prank is led to an outdoor spot and given instructions for catching the snipe; these often include waiting in the dark and holding an empty bag or making noises to attract the creature. The others involved in the prank then leave the newcomer alone in the woods to discover the joke. As an American rite of passage, snipe hunting is often associated with summer camps and groups such as the Boy Scouts. In France, a similar joke is called "hunting the dahut".

In North America

Although snipe are a real family of birds, the snipe hunt is a practical joke, often associated with summer camps and other types of outdoor camping, in which the victim is tricked into engaging in a hunt for an imaginary creature.[1]

Snipe hunters are typically led to an outdoor spot at night and given a bag or pillowcase along with instructions that can include either waiting quietly or making odd noises to attract the creatures. The other group members leave, promising to chase the snipe toward the newcomer; instead, they return home or to camp, leaving the victim of the prank alone in the dark to discover that they have been duped and left "holding the bag".[2]

The snipe hunt is a kind of fool's errand or wild-goose chase, meaning a fruitless errand or expedition, attested as early as the 1840s in the United States.[3][4] It was the most common hazing ritual for boys in American summer camps during the early 20th century, and is a rite of passage[5] often associated with groups such as the Boy Scouts. In camp life and children's folklore, the snipe hunt provides an opportunity to make fun of newcomers while also accepting them into the group.[6][7]

Setting the stage for the prank is often done with imaginative descriptions of the snipe, similar to tall tales. For instance, the snipe is said to resemble a cross between a jackrabbit and a squirrel; a squirrel-like bird with one red and one green eye; a small, black, furry bird-like animal that only comes out during a full moon, and so on.[8] According to American Folklore: An Encyclopedia:

While the snipe hunt is known in virtually every part of the United States, the description of the prey varies: it may be described as a type of bird, a snake, or a small furry animal. In one version, the snipe is a type of deer with a distinctive call; the dupe is left kneeling and imitating the snipe call while holding the bag to catch it.[9]

In another variation, a bag supposedly containing a captured snipe is theatrically brought to the campsite after a group hunt; the snipe quickly "escapes" unseen when the bag is opened.[10]

Variations

A similar practical joke in France is known as "hunting the dahut".[11] While the description of the prey differs from the North American snipe hunt, the nature of the joke is the same.[8]

In Spain, a similar joke is called cazar gamusinos ('hunting gamusinos'). The gamusino [es] is an imaginary animal with no defined description.[12]

en.wikipedia.org/wiki/Snipe_hunt

For the first time in lo these many years, we didn't have to juggle my fall break with the kids' (nonexistent) fall break. So my husband and I hit the road and drove to New England for fall break. Yes, we did stop off on the way to visit the younger son (a freshman in college) - took him out to dinner and to a movie. After that, we drove to the family's summer place, a small house on an island on a lake in southern NH. An incredibly serene place to spend a few days, hiking and kayacking.

It's been more than 20 years since we've been able to spend autumn in New England. Even though we were about a week past the peak fall colors, they were still spectacular. The weather could have been better, but the dogs didn't care. They were just happy to get up with me at dawn (er, to get ME up) to enjoy "golden hour".

Good boy, Duncan - he was willing to sit still enough in dim early morning light to allow me to capture his portrait, This one was taken at 1/40s, but I had others that were as sharply in focus at 1/25s. I just liked his expression best in this one.

I was tagged by the lovely Terri, so here are my 16 things most people dont know about me:

1) Today I upgraded my fiddy (50mm f/1.8) for the brand spanking new 50mm f/1.4. The shop gave me a great trade in (what I paid for it 3 months ago, with all the R/$ price hikes). I happily handed it over, but as I left the shop a great sense of loss filled me. Like watching a friend leave at the airport. Even though it's 'just a lens' I had really become attached to it. Hope the 1.4 fills that hole...

2) I am passionate about making things myself. A very good friend of mine once asked me where all the craftsmen had gone. We live in the world of cheap and disposable, and to use your hands and heart to create something is one of the most special abilities we have. (I secretly think fmgbain's daughter is the finest creation I have ever seen)

3) I am a very messy person, and my desk has a large pile of (clean) clothes on it that desperately needs to be packed away.

4) I love cooking, but I hate having dirty hands in the kitchen, my all time worst is raw egg when battering food to fry.

5) Before starting my 365Days I used to have bad body image, and would literally run from cameras. Part of the reason I got my first camera (Canon A80) was to be behind it rather than infront of it (the main reason I bought it was an unforgettable trip to Namibia with Nic).

6) With my friend Nic, I have done a large amount of road tripping around South Africa. I am privelaged to live here and know the amazing people I do.

7) I am a chronic procrastinatior, and leave most things till the last minute - loads of evidence of photos taken at 2am in my photostream. (Like this one)

8) Often I look at my photos and have trouble believing I took them. This isn't boasting, its a testament to the great people here and the support and shared ideas. I only hope I have managed to inspire others.

9) On the 1st November 2008 my friend Tal emmigrated to London. I miss him deeply.

10) When I was growing up I was a very negative person. It's taken a lot of work to see the silver lining is always there.

11) I have issues with evangelical vegetarians, we were born to eat meat, thats why we have canines. That said, I love fruit, and I am very lucky to live in one of the top fruit producing countries of the world. I believe that people are disconnected from their food. Chicken does not grow on polystyrene and under plastic wrap. There is a respect that is missing that something died so we can live.

12) It takes a lot to get me down, and only a small handfull of people have the ability to really piss me off. I am only cranky when I have had no sleep or no food.

13) I am starting to detest Facebook, and i'm seriously considering removing my account.

14) I have a hard time saying "No", and I will do anything for anyone. Until they take advantage of me, then I get very upset.

15) In the last 3 years I have discovered my spirituality (with great help). I am appauled at the attrocities that are performed in the name of God, and the non-existent differences that religion promotes, that turns brothers on eachother. This is an observation and not a judgement - do what gets you to the spiritual level you seek.

16) I am not homophobic / sexist / racist at all, I believe that all people should be as happy as they want to be.

...

17) I love the people here, but thats no secret...

For FGR - Ads for nonexistent products

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.

__________________________________________

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

Landstafereel. Mudland island landscape, city on narrowest isthmus. 2009.

August 25, 2012

Twin Lakes, California

Part Two

Morale and spirits were high as the great journey was finally underway. As the caravan moved forward, it was inevitable that most would look back from time to time to see Independence as being the last glimpse of civilization. Their days, the wagon master explained, would have but two purposes: to move forward and to develop a strong routine that would provide personal and group stability and safety. The day would start early, often still dark. The women would start the fires to cook breakfast and prepare the noon day meal. The men would tend the livestock and make the wagons ready. After breakfast, the wagons would be packed and when everything and everyone was accounted for, the wagon train would arrange itself into single file and begin its move west. At noon, the company would stop for an hour or two. Afterwards, they would be on the move once more.

Aside from the driver, most of the pioneers were forced to walk along side, in front, or behind their wagons. One of the largest personal expenses for the trip was several pairs of good, sturdy shoes. Roads were virtually nonexistent. What was construed to be a road was little more than a uneven worn path full of ruts and stones. This made riding in the wagon far from comfortable. At about four or five in late afternoon, the party would come to a stop to set up camp. After the wagons had been positioned into a circle, the women would unload things necessary to prepare dinner. The men would look after feeding and bedding down the livestock and make needed repairs to the wagons. Cleaning up after the evening meal, everyone could relax, join others to talk about the day, sing familiar songs, dance, or tell stories. These pleasant evening activities did not last long into the night. Everyone was exhausted and sore. Morning came cruelly early. If there was room in the wagon to sleep, that was the most safe and comfortable option. If not, then sleeping under the wagon was a choice and offered some protection against unpredictable weather. Others slept under the vast canopy of stars. From necessity, some men were positioned about the ring of wagons as sentries as the night had known and unknown dangers.

Day after day, mundane activities, once novel and memorable, became as one. The travelers had entered a no man’s land. Independence, Missouri and “home” had become distant memories. Their destination was even more indistinct than previously envisioned. To keep some account of their journey, many of the wagon trains, before embarking, required each person who could read and write to keep a journal. Depending upon the skill of the writer, the day’s entry could be little more than an account of the weather. Others would write several paragraphs giving a clear image of their own and their companion travelers’ experiences and perceptions of significant or commonplace events.

Camera test. I bought a Certo Six medium format folding camera, and this is from the test roll I ran through it. It's a rangefinder, but the rangefinder patch is nonexistent, so I had to scale focus. That is being fixed now.

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.

On the Airport Express line at Kowloon Station to get to Chek Lap Kok Airport and fly to Seoul.

Kowloon Station offers remote check-in services for some airlines, though I did not take advantage of the services.

For these airlines, I need to board the front of the train for easy access to the check-in counters. It is notable that Asian airlines have official Chinese-script names, and non-Asian airlines have Chinese names that try to translate the proper names into Chinese equivalents as much as possible. For example, British Airways is showing up as 英國航空公司, or England Airline Company, as in written Chinese, the distinction between Britain and England is nonexistent.

At Chek Lap Kok Airport, I also noted (as seen on this board as well) that my favorite airline, United Airlines (聯合航空公司), and my most hated airline, Korean Air (大韓航空公司), share check-in counters.

Although not the case on this board, United Airlines is often written in Chinese as 美國聯合航空公司, adding "America" to the front, to better follow the Chinese airline naming convention of naming the airline's nationality first, and to distinguish it from unrelated China United Airlines, a domestic airline within China.

I am flying on Asiana Airlines (韓亞航空公司 - "Korea Asia Airlines") which is not listed on this board.

This "budget skull" model I got to study the anatomy of the head originally came with some metal hardware, metal hooks to hold the top of the cranium, and springs from the coronoid process of the mandible to the temple area, but I like it just fine without them. I'm concentrating more on the cranium now anyway.

There are things I like about this, and at the price I paid I can't say I regret the purchase, but on the other hand, its hard to understand why just because something is cheap it doesn't need to have detailed accuracy. I get the distinct impression that skull models are mostly priced to squeeze as much blood out of medical students as possible.

This cost me less than $30, including shipping. Though I had to wait almost a full month for it. Maybe my mistake was ordering so close to Halloween? From what I've seen the next step up in price is to a $60, miniature model from Freedom of Teach. Which company seems to be partnering with the Gnommon workshop to sell some of their excellent miniature anatomy models. More accurate life size skulls seem to start at about $120, and hover in the $120 - $265 range. In this range we also find some of the lowest priced complete plastic skeletons. I was seriously considering looking to buy one at some time hoping that I could get a better skull out of it as well as all the rest of the bones until I noticed a complete skeleton in a local art supply store, not for sale, but as an ornament apparently, which had the exact same "budget skull" you see above.

Skulls with separate skull bones, such as separate frontal, maxillary, and zygomatic bones, are available for over $500.

When you think of the materials of which such things are made, and the method of construction, molded plastic, of which half of our world seems to be constructed these days, its hard to see what could be so difficult about making an accurate skull that would justify the prices. It has to come down to a judgment of what the market will bear, I guess, and with medical students of some kind being the most likely to purchase such a thing, and artists far less likely to buy, or care about accuracy, well, I guess they make good ones in smaller batches, and take a lot more care gluing the pieces together and cleaning the seams. But even realizing all that, I have a hard time understanding why the artist priced model isn't even symmetrical from the right to the left side. Why, when the jaw is off, are the condyles in front of the foramen magnum so uneven that it is difficult to get it to sit flat on anything, why it lacks any squamousal suture on the side of the head, when the coronal and lambdoidal sutures are so clearly visible. These defects tend to decrease my confidence in other features which I notice are different from a majority of illustrations and photographs of the skull that I am studying, and have made note of all my life. Such as the relatively weak to nonexistent supra-temporal line, the weakly defined temporal fossa, a coronoid process of the mandible far shorter than the condylar process, when most pictures I've looked at recently show them coming to more nearly the same height. And the very square seeming eye sockets and cheek bones which are so flat from the front.

Can I really do no better than this without compromising my rent money?

Like it? Would send me some bitcoin as a tip?

1H76GsGpfkyg2PtwnsZnTYgED3NinWgsG6

Or QR code here: www.flickr.com/photos/sightrays/8672657341/

This completely hand-drawn map is named Regge. Seaside city on Wadden Sea like island. 2011.

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.

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.

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.

Westerwal. Border city on a river. 2009.

One of the buildings in the pretty much nonexistent "downtown Etobicoke"

As you see here, I have purchased set 7635 from Toys R Us. This is an excellent set and has no gist and feel what so ever of a CITY set, but has everything of a Town Set! All the bricks on the truck are pretty basic and Juniorization is nonexistent in this set. They also had 7631 - I'll probably buy it soon!

Spaceship Earth, the iconic and symbolic structure of Epcot, opened with the park in Future World in 1982. The 18-storym 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.

youtu.be/tTVWQ8dxPW0

Starring Richard Garland, Pamela Duncan, Russell Johnson, Leslie Bradley, Mel Welles, and Ed Nelson. Directed by Roger Corman.

ATTACK OF THE CRAB MONSTERS is one of a handful of B films that Roger Corman did for Allied Artists when he wasn't churning 'em out for Nicholson and Arkoff at AIP. It also happens to be one of his most beloved 50s monster efforts. Frequent collaborator Charles Griffith concocted the script and strays from the abundant humor present in LITTLE SHOP OF HORRORS and CREATURE FROM THE HAUNTED SEA, playing it straight this time (that is if you can accept a giant talking crab as serious). Griffith also appears in the film (he gets decapitated early on) and directed some underwater scenes.

A group of scientists find themselves marooned on a nuclear-affected atoll in the Pacific where they have come searching for members of a previous expedition. After doing some research, they learn that the other scientists were eaten by giant mutated land crabs, and that these creatures have also absorbed their minds. The menacing crustaceans begin to snack on this new set of guests, using telepathy (articulating with the voices of the person they just devoured) in order to summon their next victim.

Like all of the early Corman films, this was made on shoestring but was reportedly his highest grosser up until that time. It's a tight 60+ minute effort with very little time for chat, and the giant crabs don't look too bad at all in comparison with other 50s sleaze creatures. The film boasts a classic Corman stock ensemble: Richard Garland (PANIC IN YEAR ZERO) and Pamela Duncan (THE UNDEAD) are the heroic love interests, the vastly underrated Russell Johnson (still years away from "Gilligan's Island") is a life-saving technician, Mel Welles and Leslie Bradley are scientists with accents (you haven't lived until you've heard a giant crab speak with Welles' Mushnik persona, and Beach Dickerson and Ed Nelson are in there as well. Nelson also operated the crab and legend has it that Jack Nicholson did as well!

ATTACK OF THE CRAB MONSTERS has been released on DVD by Allied Artists Classics, a company whose legitimacy is still in question. Previously released on VHS, they utilize the same substandard transfer and it fairs no better on the digital format. The full frame black and white image is looks generations down in quality, with nonexistent black levels and video tape dropouts during the start of the show. The print source is in decent shape, but the overall appearance is dark and dingy. Sound quality is OK, if you can get past some hiss. This would be fine if this was an under-$10 budget release, but this baby retails for about $25! If you're willing to shell out the bucks, the quality is acceptable and this title is essential to any 50s monster movie buff's collection. Also included is the original trailer and a still gallery

A group of scientists travel to a remote island to study the effects of nuclear weapons tests, only to get stranded when their airplane explodes. The team soon discovers that the island has been taken over by crabs that have mutated into enormous, intelligent monsters. To add to their problems, the island is slowly sinking into the ocean. Will any of them manage to escape?

youtu.be/tTVWQ8dxPW0

Starring Richard Garland, Pamela Duncan, Russell Johnson, Leslie Bradley, Mel Welles, and Ed Nelson. Directed by Roger Corman.

ATTACK OF THE CRAB MONSTERS is one of a handful of B films that Roger Corman did for Allied Artists when he wasn't churning 'em out for Nicholson and Arkoff at AIP. It also happens to be one of his most beloved 50s monster efforts. Frequent collaborator Charles Griffith concocted the script and strays from the abundant humor present in LITTLE SHOP OF HORRORS and CREATURE FROM THE HAUNTED SEA, playing it straight this time (that is if you can accept a giant talking crab as serious). Griffith also appears in the film (he gets decapitated early on) and directed some underwater scenes.

A group of scientists find themselves marooned on a nuclear-affected atoll in the Pacific where they have come searching for members of a previous expedition. After doing some research, they learn that the other scientists were eaten by giant mutated land crabs, and that these creatures have also absorbed their minds. The menacing crustaceans begin to snack on this new set of guests, using telepathy (articulating with the voices of the person they just devoured) in order to summon their next victim.

Like all of the early Corman films, this was made on shoestring but was reportedly his highest grosser up until that time. It's a tight 60+ minute effort with very little time for chat, and the giant crabs don't look too bad at all in comparison with other 50s sleaze creatures. The film boasts a classic Corman stock ensemble: Richard Garland (PANIC IN YEAR ZERO) and Pamela Duncan (THE UNDEAD) are the heroic love interests, the vastly underrated Russell Johnson (still years away from "Gilligan's Island") is a life-saving technician, Mel Welles and Leslie Bradley are scientists with accents (you haven't lived until you've heard a giant crab speak with Welles' Mushnik persona, and Beach Dickerson and Ed Nelson are in there as well. Nelson also operated the crab and legend has it that Jack Nicholson did as well!

ATTACK OF THE CRAB MONSTERS has been released on DVD by Allied Artists Classics, a company whose legitimacy is still in question. Previously released on VHS, they utilize the same substandard transfer and it fairs no better on the digital format. The full frame black and white image is looks generations down in quality, with nonexistent black levels and video tape dropouts during the start of the show. The print source is in decent shape, but the overall appearance is dark and dingy. Sound quality is OK, if you can get past some hiss. This would be fine if this was an under-$10 budget release, but this baby retails for about $25! If you're willing to shell out the bucks, the quality is acceptable and this title is essential to any 50s monster movie buff's collection. Also included is the original trailer and a still gallery

A group of scientists travel to a remote island to study the effects of nuclear weapons tests, only to get stranded when their airplane explodes. The team soon discovers that the island has been taken over by crabs that have mutated into enormous, intelligent monsters. To add to their problems, the island is slowly sinking into the ocean. Will any of them manage to escape?

With my 5 year old Nikon finally dying out on me and shooting film but being too lazy and forgetful to get it developed, I have been lacking in the photography department. Now I have been employed over the summer to wrangle young children and teach them the joy of art as well as a nanny for 4 different families. I wonder if I'll get anything done besides keeping my hands and clothes permanently stained. However, if I can't "do art", I'm glad I'm enabling 40+ kids to do so.

You can see my more frequent updates at pseudodivisions.tumblr.com

NY Times, Dec. 4 2011

Colin Huggins was there with his baby grand, the one he wheels into Washington Square Park for his al fresco concerts. So were Tic and Tac, a street-performing duo, who held court in the fountain — dry for the winter. And Joe Mangrum was pouring his elaborate sand paintings on the ground near the Washington Arch.

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Connect with @NYTMetro on Twitter for New York breaking news and headlines.

Enlarge This Image

Hiroko Masuike/The New York Times

Kareem Barnes of Tic and Tac collected donations on Sunday.

Enlarge This Image

Hiroko Masuike/The New York Times

Joe Mangrum showed his sand paintings on Sunday.

In other words, it was a typical Sunday afternoon in the Greenwich Village park, where generations of visitors have mingled with musicians, artists, activists, poets and buskers.

Yet this fall, that urban harmony has grown dissonant as the city’s parks department has slapped summonses on the four men and other performers who put out hats or buckets, for vending in an unauthorized location — specifically, within 50 feet of a monument.

The department’s rule, one of many put in place a year ago, was intended to control commerce in the busiest parks. Under the city’s definition, vending covers not only those peddling photographs and ankle bracelets, but also performers who solicit donations.

The rule attracted little notice at first. But the enforcement in Washington Square Park in the past two months has generated summonses ranging from $250 to $1,000. And it has started a debate about the rights of parkgoers seeking refuge from the bustle of the streets versus those looking for entertainment.

At a news conference in the park on Sunday organized by NYC Park Advocates, the artists waved fistfuls of pink summonses while their advocates, including civil rights lawyers, called on the city to stop what they called harassment of the performers.

“This is a heavy-handed solution to a nonexistent problem,” said Ronald L. Kuby, one of the lawyers.

The rule is especially problematic in Washington Square Park, performers say, because there are few locations across its 10 acres that are beyond 50 feet from a memorial or fountain — whether the bust of Alexander Lyman Holley, who introduced the Bessemer steel process to this country, or the statue of the Italian liberator Giuseppe Garibaldi.

Then there is the park’s international reputation as a gathering place for folk music pioneers and the Beats.

“Washington Square is the live-music park of New York City, and it would be close to impossible for any one of us to follow these regulations,” said Mr. Huggins, who has received nine summonses with fines totaling $2,250.

But Adrian Benepe, the parks commissioner, argues that there is ample room for performers away from the monuments. And, he added, a musician who is not putting out a tin cup is welcome to sit on the edge of the fountain or under a monument.

“It’s the whole issue of the ‘tragedy of the commons,’ ” he said. “If you allow all the performers and all the vendors to do whatever they want to do, pretty soon there’s no park left for people who want to use them for quiet enjoyment. This is a way of having some control and not 18 hours of carnival-like atmosphere.”

Gary Behrens, an amateur photographer visiting from New Jersey, applauded the city’s efforts to rein in the performers. “I’m O.K. with the guitar, but the loud instruments have taken over the park,” he said.

The lawyers and advocates, however, challenged the idea that street performers were selling a product as a vendor does. And threatening a lawsuit, they faulted the city for creating what they called “First Amendment zones” through the rules.

“Is this place zany?” asked Norman Siegel, the former director of the New York Civil Liberties Union. “You bet. Public parks are quintessential public forums. Zaniness is something we should cherish and protect.”

Park visitation has soared along with the rise of tourism in the last 15 years, and with it vendors and artists interested in a lucrative market.

Mr. Benepe insisted that the rules would not scare off future music legends.

“If Bob Dylan wanted to come play there tomorrow, he could,” he said, “although he might have to move away from the fountain.”

Oddly, the dispute coincided with the 50th anniversary of the so-called Folk Riot in Washington Square Park, when the parks commissioner tried to squelch Sunday folk performances. Hundreds of musicians gathered in protest, the police were called in and a melee ensued.

In April, Mayor Michael R. Bloomberg wrote a letter commemorating the Folk Riot, saying he applauded “the folk performers who changed music, our city and our world beginning half a century ago.”

© branko

www.a2b1.com

youtube channel: www.youtube.com/a2b1

NY Times, Dec. 4 2011

Colin Huggins was there with his baby grand, the one he wheels into Washington Square Park for his al fresco concerts. So were Tic and Tac, a street-performing duo, who held court in the fountain — dry for the winter. And Joe Mangrum was pouring his elaborate sand paintings on the ground near the Washington Arch.

Follow @NYTMetro

Connect with @NYTMetro on Twitter for New York breaking news and headlines.

Enlarge This Image

Hiroko Masuike/The New York Times

Kareem Barnes of Tic and Tac collected donations on Sunday.

Enlarge This Image

Hiroko Masuike/The New York Times

Joe Mangrum showed his sand paintings on Sunday.

In other words, it was a typical Sunday afternoon in the Greenwich Village park, where generations of visitors have mingled with musicians, artists, activists, poets and buskers.

Yet this fall, that urban harmony has grown dissonant as the city’s parks department has slapped summonses on the four men and other performers who put out hats or buckets, for vending in an unauthorized location — specifically, within 50 feet of a monument.

The department’s rule, one of many put in place a year ago, was intended to control commerce in the busiest parks. Under the city’s definition, vending covers not only those peddling photographs and ankle bracelets, but also performers who solicit donations.

The rule attracted little notice at first. But the enforcement in Washington Square Park in the past two months has generated summonses ranging from $250 to $1,000. And it has started a debate about the rights of parkgoers seeking refuge from the bustle of the streets versus those looking for entertainment.

At a news conference in the park on Sunday organized by NYC Park Advocates, the artists waved fistfuls of pink summonses while their advocates, including civil rights lawyers, called on the city to stop what they called harassment of the performers.

“This is a heavy-handed solution to a nonexistent problem,” said Ronald L. Kuby, one of the lawyers.

The rule is especially problematic in Washington Square Park, performers say, because there are few locations across its 10 acres that are beyond 50 feet from a memorial or fountain — whether the bust of Alexander Lyman Holley, who introduced the Bessemer steel process to this country, or the statue of the Italian liberator Giuseppe Garibaldi.

Then there is the park’s international reputation as a gathering place for folk music pioneers and the Beats.

“Washington Square is the live-music park of New York City, and it would be close to impossible for any one of us to follow these regulations,” said Mr. Huggins, who has received nine summonses with fines totaling $2,250.

But Adrian Benepe, the parks commissioner, argues that there is ample room for performers away from the monuments. And, he added, a musician who is not putting out a tin cup is welcome to sit on the edge of the fountain or under a monument.

“It’s the whole issue of the ‘tragedy of the commons,’ ” he said. “If you allow all the performers and all the vendors to do whatever they want to do, pretty soon there’s no park left for people who want to use them for quiet enjoyment. This is a way of having some control and not 18 hours of carnival-like atmosphere.”

Gary Behrens, an amateur photographer visiting from New Jersey, applauded the city’s efforts to rein in the performers. “I’m O.K. with the guitar, but the loud instruments have taken over the park,” he said.

The lawyers and advocates, however, challenged the idea that street performers were selling a product as a vendor does. And threatening a lawsuit, they faulted the city for creating what they called “First Amendment zones” through the rules.

“Is this place zany?” asked Norman Siegel, the former director of the New York Civil Liberties Union. “You bet. Public parks are quintessential public forums. Zaniness is something we should cherish and protect.”

Park visitation has soared along with the rise of tourism in the last 15 years, and with it vendors and artists interested in a lucrative market.

Mr. Benepe insisted that the rules would not scare off future music legends.

“If Bob Dylan wanted to come play there tomorrow, he could,” he said, “although he might have to move away from the fountain.”

Oddly, the dispute coincided with the 50th anniversary of the so-called Folk Riot in Washington Square Park, when the parks commissioner tried to squelch Sunday folk performances. Hundreds of musicians gathered in protest, the police were called in and a melee ensued.

In April, Mayor Michael R. Bloomberg wrote a letter commemorating the Folk Riot, saying he applauded “the folk performers who changed music, our city and our world beginning half a century ago.”

The cotton pygmy goose or cotton teal is a small perching duck which breeds in Pakistan, India, Bangladesh, southeast Asia and south to northern Australia.

Small individuals of this species are the smallest waterfowl on earth, at as little as 160 g (5.6 oz) and 26 cm (10 in). White predominates in this bird's plumage. Bill short, deep at base, and goose-like.

Male in breeding plumage is glossy blackish green crown, with white head, neck, and underparts; a prominent black collar and white wing-bar. Rounded head and short legs. In flight, the wings are green with a white band, making the male conspicuous even amongst the huge flying flocks of the lesser whistling duck, which share the habitat. Female paler, without either black collar and only a narrow or nonexistent strip of white wing-bar. In non-breeding plumage (eclipse) male resembles female except for his white wing-bar. Flocks on water bodies (jheels), etc.

The call is a peculiar clucking, uttered in flight IUCN: LC

As a public service to that tiny (possibly nonexistent) group of people who (a) own this record, (b) own a jukebox, and (c) desire to have said record in said jukebox, I offer up this handy, ready-to-print title strip. You're welcome.

The concrete ship that ran aground in 1926, Cape May, NJ Note the pelican or pelicans. They are a bird unknown in New Jersey, at least to me. I didn't notice till later or might have tried a longer lens. Edit: Since pic was taken pelicans have become less rare in NJ. They were nonexistent so far north previously.

This chap has worked this estero many times, its stench is likely nonexistent to him. Same for the folks living here. Bahala na.

Cedars of Lebanon State Park is a state park in Wilson County, Tennessee, in the southeastern United States. It consists of 900 acres situated amidst the 9,420-acre Cedars of Lebanon State Forest. The park and forest are approximately 10 miles (16 km) south of Lebanon, Tennessee.

Cedars of Lebanon State Forest is known for its cedar glades, a unique type of ecosystem that has adapted to the thin (or nonexistent) soil layers that often occur in the eastern Central Basin. These glades are typically flanked by thick stands of red cedar, a type of juniper tree that can survive in soil layers too thin to support most large wooded plants. The presence of the red cedar in the basin reminded the region's early Euro-American settlers of the Lebanese cedar forests of Biblical fame.

Cedars of Lebanon State Forest is underlain by Ordovician period limestone, formed roughly 460 million years ago from calcareous ooze deposited by a primordial sea that once covered Middle Tennessee. Weathering of this rock has led to the creation of karst formations such as joints, underground streams, caves, and sinkholes, which are common throughout the park and forest. The forest is located in a flat section of the Central Basin characterized by thin soil layers where the limestone bedrock is often exposed.

Cedar glade communities have adapted to the basin's harsh barrens, where the soil is too thin to support most plant types, especially large wooded plants. The glades are typically open areas resembling rock or gravel-strewn meadows. Most glades include small areas of bare rock where nothing grows, gravelly areas where only grasses grow, and patches of very thin soil that support shrubs and small red cedars. Cedar glades are typically surrounded by stands of red cedar known as cedar thickets. Beyond the cedar thickets, the soil is thick enough to support a hardwood forest consisting primarily of oak and hickory.

The cedar glades of Cedars of Lebanon State Forest are home to 350 plant species, 29 of which are endemic to the cedar glades. Flowering plant species living in the glades include the formerly endangered Tennessee Coneflower (Echinacea tennesseensis), the Prickly Pear cactus (Opuntia humifusa), Limestone flame flower (Phemeranthus calcaricus), Gattinger's Prairie Clover (Dalea gattingeri), Glade Phlox (Phlox bifida), and Nashville Breadroot (Pediomelum subacaule). Nonflowering plants include reindeer moss and glade moss. Along with the red cedar, trees in the surrounding forest include white oak and shagbark hickory. Wildlife chiefly consists of rodents and birds.

en.wikipedia.org/wiki/Cedars_of_Lebanon_State_Park

LINK: youtu.be/VGpha2SEhe4

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The 17th and 18th of January 2023 would see two LSL steam locomotives transfer to the north and south, these being ex-BR built LNER B1 no. '61306, Mayflower' and ex-LMS/BR Black Five 5MT no. '45231, The Sherwood Forester'.

We first view 'Mayflower' at Lichfield Trent Valley on the 17th of January during its LE movement to LSL's Southall depot to work charters under the 'Steam Dreams' name. I had planned to go to an off-station location for this view, but a nonexistent bus meant I had no time to get to the location.

Our second view is of 'The Sherwood Forester' at Rugeley Trent Valley on its way to LSL's home base in Crewe after spending some time at their Southall depot. Not my finest shot, but it'll do.

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.

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.

NY Times, Dec. 4 2011

Colin Huggins was there with his baby grand, the one he wheels into Washington Square Park for his al fresco concerts. So were Tic and Tac, a street-performing duo, who held court in the fountain — dry for the winter. And Joe Mangrum was pouring his elaborate sand paintings on the ground near the Washington Arch.

Follow @NYTMetro

Connect with @NYTMetro on Twitter for New York breaking news and headlines.

Enlarge This Image

Hiroko Masuike/The New York Times

Kareem Barnes of Tic and Tac collected donations on Sunday.

Enlarge This Image

Hiroko Masuike/The New York Times

Joe Mangrum showed his sand paintings on Sunday.

In other words, it was a typical Sunday afternoon in the Greenwich Village park, where generations of visitors have mingled with musicians, artists, activists, poets and buskers.

Yet this fall, that urban harmony has grown dissonant as the city’s parks department has slapped summonses on the four men and other performers who put out hats or buckets, for vending in an unauthorized location — specifically, within 50 feet of a monument.

The department’s rule, one of many put in place a year ago, was intended to control commerce in the busiest parks. Under the city’s definition, vending covers not only those peddling photographs and ankle bracelets, but also performers who solicit donations.

The rule attracted little notice at first. But the enforcement in Washington Square Park in the past two months has generated summonses ranging from $250 to $1,000. And it has started a debate about the rights of parkgoers seeking refuge from the bustle of the streets versus those looking for entertainment.

At a news conference in the park on Sunday organized by NYC Park Advocates, the artists waved fistfuls of pink summonses while their advocates, including civil rights lawyers, called on the city to stop what they called harassment of the performers.

“This is a heavy-handed solution to a nonexistent problem,” said Ronald L. Kuby, one of the lawyers.

The rule is especially problematic in Washington Square Park, performers say, because there are few locations across its 10 acres that are beyond 50 feet from a memorial or fountain — whether the bust of Alexander Lyman Holley, who introduced the Bessemer steel process to this country, or the statue of the Italian liberator Giuseppe Garibaldi.

Then there is the park’s international reputation as a gathering place for folk music pioneers and the Beats.

“Washington Square is the live-music park of New York City, and it would be close to impossible for any one of us to follow these regulations,” said Mr. Huggins, who has received nine summonses with fines totaling $2,250.

But Adrian Benepe, the parks commissioner, argues that there is ample room for performers away from the monuments. And, he added, a musician who is not putting out a tin cup is welcome to sit on the edge of the fountain or under a monument.

“It’s the whole issue of the ‘tragedy of the commons,’ ” he said. “If you allow all the performers and all the vendors to do whatever they want to do, pretty soon there’s no park left for people who want to use them for quiet enjoyment. This is a way of having some control and not 18 hours of carnival-like atmosphere.”

Gary Behrens, an amateur photographer visiting from New Jersey, applauded the city’s efforts to rein in the performers. “I’m O.K. with the guitar, but the loud instruments have taken over the park,” he said.

The lawyers and advocates, however, challenged the idea that street performers were selling a product as a vendor does. And threatening a lawsuit, they faulted the city for creating what they called “First Amendment zones” through the rules.

“Is this place zany?” asked Norman Siegel, the former director of the New York Civil Liberties Union. “You bet. Public parks are quintessential public forums. Zaniness is something we should cherish and protect.”

Park visitation has soared along with the rise of tourism in the last 15 years, and with it vendors and artists interested in a lucrative market.

Mr. Benepe insisted that the rules would not scare off future music legends.

“If Bob Dylan wanted to come play there tomorrow, he could,” he said, “although he might have to move away from the fountain.”

Oddly, the dispute coincided with the 50th anniversary of the so-called Folk Riot in Washington Square Park, when the parks commissioner tried to squelch Sunday folk performances. Hundreds of musicians gathered in protest, the police were called in and a melee ensued.

In April, Mayor Michael R. Bloomberg wrote a letter commemorating the Folk Riot, saying he applauded “the folk performers who changed music, our city and our world beginning half a century ago.”

joe mangrum

washington square park

© branko

www.a2b1.com

youtube channel: www.youtube.com/a2b1

NY Times, Dec. 4 2011

Colin Huggins was there with his baby grand, the one he wheels into Washington Square Park for his al fresco concerts. So were Tic and Tac, a street-performing duo, who held court in the fountain — dry for the winter. And Joe Mangrum was pouring his elaborate sand paintings on the ground near the Washington Arch.

Follow @NYTMetro

Connect with @NYTMetro on Twitter for New York breaking news and headlines.

Enlarge This Image

Hiroko Masuike/The New York Times

Kareem Barnes of Tic and Tac collected donations on Sunday.

Enlarge This Image

Hiroko Masuike/The New York Times

Joe Mangrum showed his sand paintings on Sunday.

In other words, it was a typical Sunday afternoon in the Greenwich Village park, where generations of visitors have mingled with musicians, artists, activists, poets and buskers.

Yet this fall, that urban harmony has grown dissonant as the city’s parks department has slapped summonses on the four men and other performers who put out hats or buckets, for vending in an unauthorized location — specifically, within 50 feet of a monument.

The department’s rule, one of many put in place a year ago, was intended to control commerce in the busiest parks. Under the city’s definition, vending covers not only those peddling photographs and ankle bracelets, but also performers who solicit donations.

The rule attracted little notice at first. But the enforcement in Washington Square Park in the past two months has generated summonses ranging from $250 to $1,000. And it has started a debate about the rights of parkgoers seeking refuge from the bustle of the streets versus those looking for entertainment.

At a news conference in the park on Sunday organized by NYC Park Advocates, the artists waved fistfuls of pink summonses while their advocates, including civil rights lawyers, called on the city to stop what they called harassment of the performers.

“This is a heavy-handed solution to a nonexistent problem,” said Ronald L. Kuby, one of the lawyers.

The rule is especially problematic in Washington Square Park, performers say, because there are few locations across its 10 acres that are beyond 50 feet from a memorial or fountain — whether the bust of Alexander Lyman Holley, who introduced the Bessemer steel process to this country, or the statue of the Italian liberator Giuseppe Garibaldi.

Then there is the park’s international reputation as a gathering place for folk music pioneers and the Beats.

“Washington Square is the live-music park of New York City, and it would be close to impossible for any one of us to follow these regulations,” said Mr. Huggins, who has received nine summonses with fines totaling $2,250.

But Adrian Benepe, the parks commissioner, argues that there is ample room for performers away from the monuments. And, he added, a musician who is not putting out a tin cup is welcome to sit on the edge of the fountain or under a monument.

“It’s the whole issue of the ‘tragedy of the commons,’ ” he said. “If you allow all the performers and all the vendors to do whatever they want to do, pretty soon there’s no park left for people who want to use them for quiet enjoyment. This is a way of having some control and not 18 hours of carnival-like atmosphere.”

Gary Behrens, an amateur photographer visiting from New Jersey, applauded the city’s efforts to rein in the performers. “I’m O.K. with the guitar, but the loud instruments have taken over the park,” he said.

The lawyers and advocates, however, challenged the idea that street performers were selling a product as a vendor does. And threatening a lawsuit, they faulted the city for creating what they called “First Amendment zones” through the rules.

“Is this place zany?” asked Norman Siegel, the former director of the New York Civil Liberties Union. “You bet. Public parks are quintessential public forums. Zaniness is something we should cherish and protect.”

Park visitation has soared along with the rise of tourism in the last 15 years, and with it vendors and artists interested in a lucrative market.

Mr. Benepe insisted that the rules would not scare off future music legends.

“If Bob Dylan wanted to come play there tomorrow, he could,” he said, “although he might have to move away from the fountain.”

Oddly, the dispute coincided with the 50th anniversary of the so-called Folk Riot in Washington Square Park, when the parks commissioner tried to squelch Sunday folk performances. Hundreds of musicians gathered in protest, the police were called in and a melee ensued.

In April, Mayor Michael R. Bloomberg wrote a letter commemorating the Folk Riot, saying he applauded “the folk performers who changed music, our city and our world beginning half a century ago.”

youtu.be/tTVWQ8dxPW0

Starring Richard Garland, Pamela Duncan, Russell Johnson, Leslie Bradley, Mel Welles, and Ed Nelson. Directed by Roger Corman.

ATTACK OF THE CRAB MONSTERS is one of a handful of B films that Roger Corman did for Allied Artists when he wasn't churning 'em out for Nicholson and Arkoff at AIP. It also happens to be one of his most beloved 50s monster efforts. Frequent collaborator Charles Griffith concocted the script and strays from the abundant humor present in LITTLE SHOP OF HORRORS and CREATURE FROM THE HAUNTED SEA, playing it straight this time (that is if you can accept a giant talking crab as serious). Griffith also appears in the film (he gets decapitated early on) and directed some underwater scenes.

A group of scientists find themselves marooned on a nuclear-affected atoll in the Pacific where they have come searching for members of a previous expedition. After doing some research, they learn that the other scientists were eaten by giant mutated land crabs, and that these creatures have also absorbed their minds. The menacing crustaceans begin to snack on this new set of guests, using telepathy (articulating with the voices of the person they just devoured) in order to summon their next victim.

Like all of the early Corman films, this was made on shoestring but was reportedly his highest grosser up until that time. It's a tight 60+ minute effort with very little time for chat, and the giant crabs don't look too bad at all in comparison with other 50s sleaze creatures. The film boasts a classic Corman stock ensemble: Richard Garland (PANIC IN YEAR ZERO) and Pamela Duncan (THE UNDEAD) are the heroic love interests, the vastly underrated Russell Johnson (still years away from "Gilligan's Island") is a life-saving technician, Mel Welles and Leslie Bradley are scientists with accents (you haven't lived until you've heard a giant crab speak with Welles' Mushnik persona, and Beach Dickerson and Ed Nelson are in there as well. Nelson also operated the crab and legend has it that Jack Nicholson did as well!

ATTACK OF THE CRAB MONSTERS has been released on DVD by Allied Artists Classics, a company whose legitimacy is still in question. Previously released on VHS, they utilize the same substandard transfer and it fairs no better on the digital format. The full frame black and white image is looks generations down in quality, with nonexistent black levels and video tape dropouts during the start of the show. The print source is in decent shape, but the overall appearance is dark and dingy. Sound quality is OK, if you can get past some hiss. This would be fine if this was an under-$10 budget release, but this baby retails for about $25! If you're willing to shell out the bucks, the quality is acceptable and this title is essential to any 50s monster movie buff's collection. Also included is the original trailer and a still gallery

A group of scientists travel to a remote island to study the effects of nuclear weapons tests, only to get stranded when their airplane explodes. The team soon discovers that the island has been taken over by crabs that have mutated into enormous, intelligent monsters. To add to their problems, the island is slowly sinking into the ocean. Will any of them manage to escape?