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Nicely restored and repainted Missouri Kansas Texas Extended-Vision Caboose 134 rests at the preserved MKT Boonville, Missouri depot on September 12, 2010.
Built by Darby Corp. of Kansas City, KS, the #134 was part of an order for ten MKT cabooses, (125-134) built in 1968. Retired by the Union Pacific after the August, 1988 UP-MKT merger, caboose 134 was donated to the city of Boonville and placed on display at the Katy Depot in 1991 where it still resides.
The Palouse extends into the western part of Idaho and, while there are not as many photographic opportunities as there are in Washington, there are still a few gems to be found.. This "salt box" barn is one of them and sits all alone in this little valley and stands out primarily due to its bright red color. It contrasts quite well with the surrounding green farmland and blue sky. For those of you who follow me regularly, you know that I often wonder how things got their names. So here are a couple of useless tidbits. The term "salt box" is a reference to the old wooden boxes that were used to store salt (no, I am not old enough to remember them). This style of barns and houses originated in New England, and were built that way so that snow would slide down the steep roofs. The other arcane tidbit is the name of the town that this barn is located in, Moscow. It turns out that one of the original traders was born in Moscow, Russia, and he opened the first trading post in the area. I had never heard of the town before my visit, but was surprised to also find out that it is the home of the University of Idaho.
Source: en.wikipedia.org/wiki/Chicago
Chicago, officially the City of Chicago, is the most populous city in the U.S. state of Illinois, and the third-most-populous city in the United States. With an estimated population of 2,705,994 (2018), it is also the most populous city in the Midwestern United States. Chicago is the county seat of Cook County, the second-most-populous county in the US, with a small portion of the northwest side of the city extending into DuPage County near O'Hare Airport. Chicago is the principal city of the Chicago metropolitan area, often referred to as Chicagoland. At nearly 10 million people, the metropolitan area is the third most populous in the United States.
Located on the shores of freshwater Lake Michigan, Chicago was incorporated as a city in 1837 near a portage between the Great Lakes and the Mississippi River watershed and grew rapidly in the mid-19th century. After the Great Chicago Fire of 1871, which destroyed several square miles and left more than 100,000 homeless, the city made a concerted effort to rebuild. The construction boom accelerated population growth throughout the following decades, and by 1900, less than 30 years after the great fire, Chicago was the fifth-largest city in the world. Chicago made noted contributions to urban planning and zoning standards, including new construction styles (including the Chicago School of architecture), the development of the City Beautiful Movement, and the steel-framed skyscraper.
Chicago is an international hub for finance, culture, commerce, industry, education, technology, telecommunications, and transportation. It is the site of the creation of the first standardized futures contracts, issued by the Chicago Board of Trade, which today is the largest and most diverse derivatives market in the world, generating 20% of all volume in commodities and financial futures alone. Depending on the particular year, the city's O'Hare International Airport is routinely ranked as the world's fifth or sixth busiest airport according to tracked data by the Airports Council International. The region also has the largest number of federal highways and is the nation's railroad hub. Chicago was listed as an alpha global city by the Globalization and World Cities Research Network, and it ranked seventh in the entire world in the 2017 Global Cities Index. The Chicago area has one of the highest gross domestic products (GDP) in the world, generating $689 billion in 2018. In addition, the city has one of the world's most diversified and balanced economies, with no single industry employing more than 14% of the workforce. Chicago is home to several Fortune 500 companies, including Allstate, Boeing, Caterpillar, Exelon, Kraft Heinz, McDonald's, Mondelez International, Sears, United Airlines Holdings, and Walgreens.
Chicago's 58 million domestic and international visitors in 2018 made it the second most visited city in the nation, as compared with New York City's 65 million visitors in 2018. The city was ranked first in the 2018 Time Out City Life Index, a global quality of life survey of 15,000 people in 32 cities. Landmarks in the city include Millennium Park, Navy Pier, the Magnificent Mile, the Art Institute of Chicago, Museum Campus, the Willis (Sears) Tower, Grant Park, the Museum of Science and Industry, and Lincoln Park Zoo. Chicago's culture includes the visual arts, literature, film, theatre, comedy (especially improvisational comedy), food, and music, particularly jazz, blues, soul, hip-hop, gospel, and electronic dance music including house music. Of the area's many colleges and universities, the University of Chicago, Northwestern University, and the University of Illinois at Chicago are classified as "highest research" doctoral universities. Chicago has professional sports teams in each of the major professional leagues, including two Major League Baseball teams.
Source: en.wikipedia.org/wiki/John_Hancock_Center
875 North Michigan Avenue, formerly the John Hancock Center, is a 100-story, 1,128-foot supertall skyscraper located in Chicago, Illinois. Located in the Magnificent Mile district, its name was changed to 875 North Michigan Avenue on February 12, 2018.
It was constructed under the supervision of Skidmore, Owings and Merrill, with Peruvian-American chief designer Bruce Graham and Bangladeshi structural engineer Fazlur Rahman Khan. When the building topped out on May 6, 1968, it was the second-tallest building in the world and the tallest outside New York City. It is currently the fourth-tallest building in Chicago and the ninth-tallest in the United States, after One World Trade Center, the Willis Tower, 432 Park Avenue, the Trump Tower Chicago, the Empire State Building, the Bank of America Tower, 30 Hudson Yards and the Aon Center. When measured to the top of its antenna masts, it stands at 1,500 feet (457 m). The building is home to several offices and restaurants, as well as about 700 condominiums. It also contains the third-highest residence in the world, after the Burj Khalifa in Dubai and the Trump Tower in Chicago. The building was named for John Hancock Mutual Life Insurance Company, a developer and original tenant of the building. In 2018, John Hancock Insurance requested that its name be removed and the owner is seeking another naming rights deal.
From the 95th floor restaurant, diners can look out at Chicago and Lake Michigan. The observatory (360 Chicago), which competes with the Willis Tower's Skydeck, has a 360° view of the city, up to four states, and a distance of over 80 miles (130 km). 360 Chicago is home to TILT, a moving platform that leans visitors over the edge of the skyscraper to a 30-degree angle, a full bar with local selections, Chicago's only open-air SkyWalk, and also features free interactive high definition touch screens in six languages. The 44th-floor sky lobby features America's highest indoor swimming pool.
@designeour : Neon Square UI Kit by tintins Licenses Offered Standard Extended File Types PSD File Size 19… bit.ly/1UdMMhX (via Twitter twitter.com/designeour/status/743200446421032964)
Picture taken with the Nikon V1 + M42 adapter + 2x extender Vivitar + Auto Chinon 135mm and edited in LR + Nik Software Plugin.
Mixed up fills and black/white lines. Drawed using mousegestures.
Colors based on this one
Generated with actionscript
Orginal size: 8000x8000px
Extended version of my previously folded model
www.flickr.com/photos/48817677@N04/43732545690
EH paper, hexagon from 40x40 cm, 80 division grid.
Work was well along in February 2023 to extend the length of the siding at Campellstown, Ohio. The view is made from Oxford-Gettysburg Road looking railroad westward.
Yellowstone National Park (Arapaho: Henihco'oo or Héetíhco'oo) is a national park located primarily in the U.S. state of Wyoming, although it also extends into Montana and Idaho. It was established by the U.S. Congress and signed into law by President Ulysses S. Grant on March 1, 1872. Yellowstone, widely held to be the first national park in the world, is known for its wildlife and its many geothermal features, especially Old Faithful Geyser, one of the most popular features in the park. It has many types of ecosystems, but the subalpine forest is most abundant. It is part of the South Central Rockies forests ecoregion.
Yellowstone National Park spans an area of 3,468.4 square miles (8,983 km2), comprising lakes, canyons, rivers and mountain ranges. Yellowstone Lake is one of the largest high-altitude lakes in North America and is centered over the Yellowstone Caldera, the largest supervolcano on the continent. The caldera is considered an active volcano. It has erupted with tremendous force several times in the last two million years. Half of the world's geothermal features are in Yellowstone, fueled by this ongoing volcanism. Lava flows and rocks from volcanic eruptions cover most of the land area of Yellowstone. The park is the centerpiece of the Greater Yellowstone Ecosystem, the largest remaining nearly-intact ecosystem in the Earth's northern temperate zone.
Hundreds of species of mammals, birds, fish and reptiles have been documented, including several that are either endangered or threatened. The vast forests and grasslands also include unique species of plants. Yellowstone Park is the largest and most famous megafauna location in the Continental United States. Grizzly bears, wolves, and free-ranging herds of bison and elk live in the park. The Yellowstone Park bison herd is the oldest and largest public bison herd in the United States. Forest fires occur in the park each year; in the large forest fires of 1988, nearly one third of the park was burnt. Yellowstone has numerous recreational opportunities, including hiking, camping, boating, fishing and sightseeing. Paved roads provide close access to the major geothermal areas as well as some of the lakes and waterfalls. During the winter, visitors often access the park by way of guided tours that use either snow coaches or snowmobiles.
The park is located at the headwaters of the Yellowstone River, from which it takes its historical name. Near the end of the 18th century, French trappers named the river "Roche Jaune", which is probably a translation of the Hidatsa name "Mi tsi a-da-zi" (Rock Yellow River). Later, American trappers rendered the French name in English as "Yellow Stone". Although it is commonly believed that the river was named for the yellow rocks seen in the Grand Canyon of the Yellowstone, the Native American name source is not clear.
The first detailed expedition to the Yellowstone area was the Cook–Folsom–Peterson Expedition of 1869, which consisted of three privately funded explorers. The Folsom party followed the Yellowstone River to Yellowstone Lake. The members of the Folsom party kept a journal and based on the information it reported, a party of Montana residents organized the Washburn-Langford-Doane Expedition in 1870. It was headed by the surveyor-general of Montana Henry Washburn, and included Nathaniel P. Langford (who later became known as "National Park" Langford) and a U.S. Army detachment commanded by Lt. Gustavus Doane.
The expedition spent about a month exploring the region, collecting specimens and naming sites of interest. A Montana writer and lawyer named Cornelius Hedges, who had been a member of the Washburn expedition, proposed that the region should be set aside and protected as a national park; he wrote a number of detailed articles about his observations for the Helena Herald newspaper between 1870 and 1871. Hedges essentially restated comments made in October 1865 by acting Montana Territorial Governor Thomas Francis Meagher, who had previously commented that the region should be protected. Others made similar suggestions. In an 1871 letter from Jay Cooke to Ferdinand V. Hayden, Cooke wrote that his friend, Congressman William D. Kelley had also suggested "Congress pass a bill reserving the Great Geyser Basin as a public park forever".
By 1915, 1,000 automobiles per year were entering the park, resulting in conflicts with horses and horse-drawn transportation. Horse travel on roads was eventually prohibited.
The Civilian Conservation Corps (CCC), a New Deal relief agency for young men, played a major role between 1933 and 1942 in developing Yellowstone facilities. CCC projects included reforestation, campground development of many of the park's trails and campgrounds, trail construction, fire hazard reduction, and fire-fighting work. The CCC built the majority of the early visitor centers, campgrounds and the current system of park roads.
During World War II, tourist travel fell sharply, staffing was cut, and many facilities fell into disrepair. By the 1950s, visitation increased tremendously in Yellowstone and other national parks. To accommodate the increased visitation, park officials implemented Mission 66, an effort to modernize and expand park service facilities. Planned to be completed by 1966, in honor of the 50th anniversary of the founding of the National Park Service, Mission 66 construction diverged from the traditional log cabin style with design features of a modern style. During the late 1980s, most construction styles in Yellowstone reverted to the more traditional designs. After the enormous forest fires of 1988 damaged much of Grant Village, structures there were rebuilt in the traditional style. The visitor center at Canyon Village, which opened in 2006, incorporates a more traditional design as well.
A large arch made of irregular-shaped natural stone over a road
The 1959 Hebgen Lake earthquake just west of Yellowstone at Hebgen Lake damaged roads and some structures in the park. In the northwest section of the park, new geysers were found, and many existing hot springs became turbid. It was the most powerful earthquake to hit the region in recorded history.
In 1963, after several years of public controversy regarding the forced reduction of the elk population in Yellowstone, United States Secretary of the Interior Stewart Udall appointed an advisory board to collect scientific data to inform future wildlife management of the national parks. In a paper known as the Leopold Report, the committee observed that culling programs at other national parks had been ineffective, and recommended management of Yellowstone's elk population.
The wildfires during the summer of 1988 were the largest in the history of the park. Approximately 793,880 acres (321,272 ha; 1,240 sq mi) or 36% of the parkland was impacted by the fires, leading to a systematic re-evaluation of fire management policies. The fire season of 1988 was considered normal until a combination of drought and heat by mid-July contributed to an extreme fire danger. On "Black Saturday", August 20, 1988, strong winds expanded the fires rapidly, and more than 150,000 acres (61,000 ha; 230 sq mi) burned.
The expansive cultural history of the park has been documented by the 1,000 archeological sites that have been discovered. The park has 1,106 historic structures and features, and of these Obsidian Cliff and five buildings have been designated National Historic Landmarks. Yellowstone was designated an International Biosphere Reserve on October 26, 1976, and a UN World Heritage Site on September 8, 1978. The park was placed on the List of World Heritage in Danger from 1995 to 2003 due to the effects of tourism, infection of wildlife, and issues with invasive species. In 2010, Yellowstone National Park was honored with its own quarter under the America the Beautiful Quarters Program.
Heritage and Research Center
The Heritage and Research Center is located at Gardiner, Montana, near the north entrance to the park. The center is home to the Yellowstone National Park's museum collection, archives, research library, historian, archeology lab, and herbarium. The Yellowstone National Park Archives maintain collections of historical records of Yellowstone and the National Park Service. The collection includes the administrative records of Yellowstone, as well as resource management records, records from major projects, and donated manuscripts and personal papers. The archives are affiliated with the National Archives and Records Administration.
Approximately 96 percent of the land area of Yellowstone National Park is located within the state of Wyoming. Another three percent is within Montana, with the remaining one percent in Idaho. The park is 63 miles (101 km) north to south, and 54 miles (87 km) west to east by air. Yellowstone is 2,219,789 acres (898,317 ha; 3,468.420 sq mi) in area, larger than the states of Rhode Island or Delaware. Rivers and lakes cover five percent of the land area, with the largest water body being Yellowstone Lake at 87,040 acres (35,220 ha; 136.00 sq mi). Yellowstone Lake is up to 400 feet (120 m) deep and has 110 miles (180 km) of shoreline. At an elevation of 7,733 feet (2,357 m) above sea level, Yellowstone Lake is the largest high altitude lake in North America. Forests comprise 80 percent of the land area of the park; most of the rest is grassland.
The Continental Divide of North America runs diagonally through the southwestern part of the park. The divide is a topographic feature that separates Pacific Ocean and Atlantic Ocean water drainages. About one third of the park lies on the west side of the divide. The origins of the Yellowstone and Snake Rivers are near each other but on opposite sides of the divide. As a result, the waters of the Snake River flow to the Pacific Ocean, while those of the Yellowstone find their way to the Atlantic Ocean via the Gulf of Mexico.
The park sits on the Yellowstone Plateau, at an average elevation of 8,000 feet (2,400 m) above sea level. The plateau is bounded on nearly all sides by mountain ranges of the Middle Rocky Mountains, which range from 9,000 to 11,000 feet (2,700 to 3,400 m) in elevation. The highest point in the park is atop Eagle Peak (11,358 feet or 3,462 metres) and the lowest is along Reese Creek (5,282 feet or 1,610 metres). Nearby mountain ranges include the Gallatin Range to the northwest, the Beartooth Mountains in the north, the Absaroka Range to the east, and the Teton Range and the Madison Range to the southwest and west. The most prominent summit on the Yellowstone Plateau is Mount Washburn at 10,243 feet (3,122 m).
Yellowstone National Park has one of the world's largest petrified forests, trees which were long ago buried by ash and soil and transformed from wood to mineral materials. This ash and other volcanic debris, are believed to have come from the park area itself. This is largely due to the fact that Yellowstone is actually a massive caldera of a supervolcano. There are 290 waterfalls of at least 15 feet (4.6 m) in the park, the highest being the Lower Falls of the Yellowstone River at 308 feet (94 m).
Three deep canyons are located in the park, cut through the volcanic tuff of the Yellowstone Plateau by rivers over the last 640,000 years. The Lewis River flows through Lewis Canyon in the south, and the Yellowstone River has carved two colorful canyons, the Grand Canyon of the Yellowstone and the Black Canyon of the Yellowstone in its journey north.
Yellowstone is at the northeastern end of the Snake River Plain, a great U-shaped arc through the mountains that extends from Boise, Idaho some 400 miles (640 km) to the west. This feature traces the route of the North American Plate over the last 17 million years as it was transported by plate tectonics across a stationary mantle hotspot. The landscape of present-day Yellowstone National Park is the most recent manifestation of this hotspot below the crust of the Earth.
The Yellowstone Caldera is the largest volcanic system in North America. It has been termed a "supervolcano" because the caldera was formed by exceptionally large explosive eruptions. The magma chamber that lies under Yellowstone is estimated to be a single connected chamber, about 37 miles (60 km) long, 18 miles (29 km) wide, and 3 to 7 miles (5 to 12 km) deep. The current caldera was created by a cataclysmic eruption that occurred 640,000 years ago, which released more than 240 cubic miles (1,000 km³) of ash, rock and pyroclastic materials. This eruption was more than 1,000 times larger than the 1980 eruption of Mount St. Helens. It produced a caldera nearly five eighths of a mile (1 km) deep and 45 by 28 miles (72 by 45 km) in area and deposited the Lava Creek Tuff, a welded tuff geologic formation. The most violent known eruption, which occurred 2.1 million years ago, ejected 588 cubic miles (2,450 km³) of volcanic material and created the rock formation known as the Huckleberry Ridge Tuff and created the Island Park Caldera. A smaller eruption ejected 67 cubic miles (280 km³) of material 1.3 million years ago, forming the Henry's Fork Caldera and depositing the Mesa Falls Tuff.
Each of the three climactic eruptions released vast amounts of ash that blanketed much of central North America, falling many hundreds of miles away. The amount of ash and gases released into the atmosphere probably caused significant impacts to world weather patterns and led to the extinction of some species, primarily in North America.
Wooden walkways allow visitors to closely approach the Grand Prismatic Spring.
A subsequent caldera-forming eruption occurred about 160,000 years ago. It formed the relatively small caldera that contains the West Thumb of Yellowstone Lake. Since the last supereruption, a series of smaller eruptive cycles between 640,000 and 70,000 years ago, has nearly filled in the Yellowstone Caldera with >80 different eruptions of rhyolitic lavas such as those that can be seen at Obsidian Cliffs and basaltic lavas which can be viewed at Sheepeater Cliff. Lava strata are most easily seen at the Grand Canyon of the Yellowstone, where the Yellowstone River continues to carve into the ancient lava flows. The canyon is a classic V-shaped valley, indicative of river-type erosion rather than erosion caused by glaciation.
Each eruption is part of an eruptive cycle that climaxes with the partial collapse of the roof of the volcano's partially emptied magma chamber. This creates a collapsed depression, called a caldera, and releases vast amounts of volcanic material, usually through fissures that ring the caldera. The time between the last three cataclysmic eruptions in the Yellowstone area has ranged from 600,000 to 800,000 years, but the small number of such climactic eruptions cannot be used to make an accurate prediction for future volcanic events.
The most famous geyser in the park, and perhaps the world, is Old Faithful Geyser, located in Upper Geyser Basin. Castle Geyser, Lion Geyser and Beehive Geyser are in the same basin. The park contains the largest active geyser in the world—Steamboat Geyser in the Norris Geyser Basin. A study that was completed in 2011 found that at least 1283 geysers have erupted in Yellowstone. Of these, an average of 465 are active in a given year. Yellowstone contains at least 10,000 geothermal features altogether. Half the geothermal features and two-thirds of the world's geysers are concentrated in Yellowstone.
In May 2001, the U.S. Geological Survey, Yellowstone National Park, and the University of Utah created the Yellowstone Volcano Observatory (YVO), a partnership for long-term monitoring of the geological processes of the Yellowstone Plateau volcanic field, for disseminating information concerning the potential hazards of this geologically active region.
In 2003, changes at the Norris Geyser Basin resulted in the temporary closure of some trails in the basin. New fumaroles were observed, and several geysers showed enhanced activity and increasing water temperatures. Several geysers became so hot that they were transformed into purely steaming features; the water had become superheated and they could no longer erupt normally. This coincided with the release of reports of a multiple year United States Geological Survey research project which mapped the bottom of Yellowstone Lake and identified a structural dome that had uplifted at some time in the past. Research indicated that these uplifts posed no immediate threat of a volcanic eruption, since they may have developed long ago, and there had been no temperature increase found near the uplifts. On March 10, 2004, a biologist discovered 5 dead bison which apparently had inhaled toxic geothermal gases trapped in the Norris Geyser Basin by a seasonal atmospheric inversion. This was closely followed by an upsurge of earthquake activity in April 2004. In 2006, it was reported that the Mallard Lake Dome and the Sour Creek Dome— areas that have long been known to show significant changes in their ground movement— had risen at a rate of 1.5 to 2.4 inches (3.8 to 6.1 cm) per year from mid–2004 through 2006. As of late 2007, the uplift has continued at a reduced rate. These events inspired a great deal of media attention and speculation about the geologic future of the region. Experts responded to the conjecture by informing the public that there was no increased risk of a volcanic eruption in the near future. However, these changes demonstrate the dynamic nature of the Yellowstone hydrothermal system.
Yellowstone experiences thousands of small earthquakes every year, virtually all of which are undetectable to people. There have been six earthquakes with at least magnitude 6 or greater in historical times, including a 7.5‑magnitude quake that struck just outside the northwest boundary of the park in 1959. This quake triggered a huge landslide, which caused a partial dam collapse on Hebgen Lake; immediately downstream, the sediment from the landslide dammed the river and created a new lake, known as Earthquake Lake. Twenty-eight people were killed, and property damage was extensive in the immediate region. The earthquake caused some geysers in the northwestern section of the park to erupt, large cracks in the ground formed and emitted steam, and some hot springs that normally have clear water turned muddy. A 6.1‑magnitude earthquake struck inside the park on June 30, 1975, but damage was minimal.
For three months in 1985, 3,000 minor earthquakes were detected in the northwestern section of the park, during what has been referred to as an earthquake swarm, and has been attributed to minor subsidence of the Yellowstone caldera. Beginning on April 30, 2007, 16 small earthquakes with magnitudes up to 2.7 occurred in the Yellowstone Caldera for several days. These swarms of earthquakes are common, and there have been 70 such swarms between 1983 and 2008. In December 2008, over 250 earthquakes were measured over a four-day span under Yellowstone Lake, the largest measuring a magnitude of 3.9. In January 2010, more than 250 earthquakes were detected over a two-day period. Seismic activity in Yellowstone National Park continues and is reported hourly by the Earthquake Hazards Program of the U.S. Geological Survey.
On March 30, 2014, a magnitude 4.8 earthquake struck almost the very middle of Yellowstone near the Norris Basin at 6.34am; reports indicated no damage. This was the biggest earthquake to hit the park since February 22, 1980.
Over 1,700 species of trees and other vascular plants are native to the park. Another 170 species are considered to be exotic species and are non-native. Of the eight conifer tree species documented, Lodgepole Pine forests cover 80% of the total forested areas. Other conifers, such as Subalpine Fir, Engelmann Spruce, Rocky Mountain Douglas-fir and Whitebark Pine, are found in scattered groves throughout the park. As of 2007, the whitebark pine is threatened by a fungus known as white pine blister rust; however, this is mostly confined to forests well to the north and west. In Yellowstone, about seven percent of the whitebark pine species have been impacted with the fungus, compared to nearly complete infestations in northwestern Montana. Quaking Aspen and willows are the most common species of deciduous trees. The aspen forests have declined significantly since the early 20th century, but scientists at Oregon State University attribute recent recovery of the aspen to the reintroduction of wolves which has changed the grazing habits of local elk.
There are dozens of species of flowering plants that have been identified, most of which bloom between the months of May and September. The Yellowstone Sand Verbena is a rare flowering plant found only in Yellowstone. It is closely related to species usually found in much warmer climates, making the sand verbena an enigma. The estimated 8,000 examples of this rare flowering plant all make their home in the sandy soils on the shores of Yellowstone Lake, well above the waterline.
In Yellowstone's hot waters, bacteria form mats of bizarre shapes consisting of trillions of individuals. These bacteria are some of the most primitive life forms on earth. Flies and other arthropods live on the mats, even in the middle of the bitterly cold winters. Initially, scientists thought that microbes there gained sustenance only from sulfur. In 2005 researchers from the University of Colorado at Boulder discovered that the sustenance for at least some of the diverse hyperthermophilic species is molecular hydrogen.
Thermus aquaticus is a bacterium found in the Yellowstone hot springs that produces an important enzyme (Taq polymerase) that is easily replicated in the lab and is useful in replicating DNA as part of the polymerase chain reaction (PCR) process. The retrieval of these bacteria can be achieved with no impact to the ecosystem. Other bacteria in the Yellowstone hot springs may also prove useful to scientists who are searching for cures for various diseases.
Non-native plants sometimes threaten native species by using up nutrient resources. Though exotic species are most commonly found in areas with the greatest human visitation, such as near roads and at major tourist areas, they have also spread into the backcountry. Generally, most exotic species are controlled by pulling the plants out of the soil or by spraying, both of which are time consuming and expensive.
Yellowstone is widely considered to be the finest megafauna wildlife habitat in the lower 48 states. There are almost 60 species of mammals in the park, including the gray wolf, the threatened lynx, and grizzly bears. Other large mammals include the bison (often referred to as buffalo), black bear, elk, moose, mule deer, white-tailed deer, mountain goat, pronghorn, bighorn sheep, and mountain lion.
Bison graze near a hot spring
The Yellowstone Park bison herd is the largest public herd of American bison in the United States. The relatively large bison populations are a concern for ranchers, who fear that the species can transmit bovine diseases to their domesticated cousins. In fact, about half of Yellowstone's bison have been exposed to brucellosis, a bacterial disease that came to North America with European cattle that may cause cattle to miscarry. The disease has little effect on park bison, and no reported case of transmission from wild bison to domestic livestock has been filed. However, the Animal and Plant Health Inspection Service (APHIS) has stated that bison are the "likely source" of the spread of the disease in cattle in Wyoming and North Dakota. Elk also carry the disease and are believed to have transmitted the infection to horses and cattle. Bison once numbered between 30 and 60 million individuals throughout North America, and Yellowstone remains one of their last strongholds. Their populations had increased from less than 50 in the park in 1902 to 4,000 by 2003. The Yellowstone Park bison herd reached a peak in 2005 with 4,900 animals. Despite a summer estimated population of 4,700 in 2007, the number dropped to 3,000 in 2008 after a harsh winter and controversial brucellosis management sending hundreds to slaughter. The Yellowstone Park bison herd is believed to be one of only four free roaming and genetically pure herds on public lands in North America. The other three herds are the Henry Mountains bison herd of Utah, at Wind Cave National Park in South Dakota and on Elk Island in Alberta.
Elk Mother Nursing Her Calf
To combat the perceived threat of brucellosis transmission to cattle, national park personnel regularly harass bison herds back into the park when they venture outside of the area's borders. During the winter of 1996–97, the bison herd was so large that 1,079 bison that had exited the park were shot or sent to slaughter. Animal rights activists argue that this is a cruel practice and that the possibility for disease transmission is not as great as some ranchers maintain. Ecologists point out that the bison are merely traveling to seasonal grazing areas that lie within the Greater Yellowstone Ecosystem that have been converted to cattle grazing, some of which are within National Forests and are leased to private ranchers. APHIS has stated that with vaccinations and other means, brucellosis can be eliminated from the bison and elk herds throughout Yellowstone.
A reintroduced northwestern wolf in Yellowstone National Park
Starting in 1914, in an effort to protect elk populations, the U.S. Congress appropriated funds to be used for the purposes of "destroying wolves, prairie dogs, and other animals injurious to agriculture and animal husbandry" on public lands. Park Service hunters carried out these orders, and by 1926 they had killed 136 wolves, and wolves were virtually eliminated from Yellowstone. Further exterminations continued until the National Park Service ended the practice in 1935. With the passing of the Endangered Species Act in 1973, the wolf was one of the first mammal species listed. After the wolves were extirpated from Yellowstone, the coyote then became the park's top canine predator. However, the coyote is not able to bring down large animals, and the result of this lack of a top predator on these populations was a marked increase in lame and sick megafauna.
Bison in Yellowstone National Park
By the 1990s, the Federal government had reversed its views on wolves. In a controversial decision by the U.S. Fish and Wildlife Service (which oversees threatened and endangered species), northwestern wolves, imported from Canada, were reintroduced into the park. Reintroduction efforts have been successful with populations remaining relatively stable. A survey conducted in 2005 reported that there were 13 wolf packs, totaling 118 individuals in Yellowstone and 326 in the entire ecosystem. These park figures were lower than those reported in 2004 but may be attributable to wolf migration to other nearby areas as suggested by the substantial increase in the Montana population during that interval. Almost all the wolves documented were descended from the 66 wolves reintroduced in 1995–96. The recovery of populations throughout the states of Wyoming, Montana and Idaho has been so successful that on February 27, 2008, the U.S. Fish and Wildlife Service removed the Northern Rocky Mountain wolf population from the endangered species list.
An estimated 600 grizzly bears live in the Greater Yellowstone Ecosystem, with more than half of the population living within Yellowstone. The grizzly is currently listed as a threatened species, however the U.S. Fish and Wildlife Service has announced that they intend to take it off the endangered species list for the Yellowstone region but will likely keep it listed in areas where it has not yet recovered fully. Opponents of delisting the grizzly are concerned that states might once again allow hunting and that better conservation measures need to be implemented to ensure a sustainable population. Black bears are common in the park and were a park symbol due to visitor interaction with the bears starting in 1910. Feeding and close contact with bears has not been permitted since the 1960s to reduce their desire for human foods. Yellowstone is one of the few places in the United States where black bears can be seen coexisting with grizzly bears. Black bear observations occur most often in the park's northern ranges and in the Bechler area which is in the park's southwestern corner.
Population figures for elk are in excess of 30,000—the largest population of any large mammal species in Yellowstone. The northern herd has decreased enormously since the mid‑1990s; this has been attributed to wolf predation and causal effects such as elk using more forested regions to evade predation, consequently making it harder for researchers to accurately count them. The northern herd migrates west into southwestern Montana in the winter. The southern herd migrates southward, and the majority of these elk winter on the National Elk Refuge, immediately southeast of Grand Teton National Park. The southern herd migration is the largest mammalian migration remaining in the U.S. outside of Alaska.
In 2003 the tracks of one female lynx and her cub were spotted and followed for over 2 miles (3.2 km). Fecal material and other evidence obtained were tested and confirmed to be those of a lynx. No visual confirmation was made, however. Lynx have not been seen in Yellowstone since 1998, though DNA taken from hair samples obtained in 2001 confirmed that lynx were at least transient to the park. Other less commonly seen mammals include the mountain lion and wolverine. The mountain lion has an estimated population of only 25 individuals parkwide. The wolverine is another rare park mammal, and accurate population figures for this species are not known. These uncommon and rare mammals provide insight into the health of protected lands such as Yellowstone and help managers make determinations as to how best to preserve habitats.
Eighteen species of fish live in Yellowstone, including the core range of the Yellowstone cutthroat trout—a fish highly sought by anglers. The Yellowstone cutthroat trout has faced several threats since the 1980s, including the suspected illegal introduction into Yellowstone Lake of lake trout, an invasive species which consume the smaller cutthroat trout. Although lake trout were established in Shoshone and Lewis lakes in the Snake River drainage from U.S. Government stocking operations in 1890, it was never officially introduced into the Yellowstone River drainage. The cutthroat trout has also faced an ongoing drought, as well as the accidental introduction of a parasite—whirling disease—which causes a terminal nervous system disease in younger fish. Since 2001, all native sport fish species caught in Yellowstone waterways are subject to a catch and release law. Yellowstone is also home to six species of reptiles, such as the painted turtle and Prairie rattlesnake, and four species of amphibians, including the Boreal Chorus Frog.
311 species of birds have been reported, almost half of which nest in Yellowstone. As of 1999, twenty-six pairs of nesting bald eagles have been documented. Extremely rare sightings of whooping cranes have been recorded, however only three examples of this species are known to live in the Rocky Mountains, out of 385 known worldwide. Other birds, considered to be species of special concern because of their rarity in Yellowstone, include the common loon, harlequin duck, osprey, peregrine falcon and the trumpeter swan.
As wildfire is a natural part of most ecosystems, plants that are indigenous to Yellowstone have adapted in a variety of ways. Douglas-fir have a thick bark which protects the inner section of the tree from most fires. Lodgepole Pines —the most common tree species in the park— generally have cones that are only opened by the heat of fire. Their seeds are held in place by a tough resin, and fire assists in melting the resin, allowing the seeds to disperse. Fire clears out dead and downed wood, providing fewer obstacles for lodgepole pines to flourish. Subalpine Fir, Engelmann Spruce, Whitebark Pine, and other species tend to grow in colder and moister areas, where fire is less likely to occur. Aspen trees sprout new growth from their roots, and even if a severe fire kills the tree above ground, the roots often survive unharmed because they are insulated from the heat by soil. The National Park Service estimates that in natural conditions, grasslands in Yellowstone burned an average of every 20 to 25 years, while forests in the park would experience fire about every 300 years.
About thirty-five natural forest fires are ignited each year by lightning, while another six to ten are started by people— in most cases by accident. Yellowstone National Park has three fire lookout towers, each staffed by trained fire fighters. The easiest one to reach is atop Mount Washburn, though it is closed to the public. The park also monitors fire from the air and relies on visitor reports of smoke and/or flames. Fire towers are staffed almost continuously from late June to mid-September— the primary fire season. Fires burn with the greatest intensity in the late afternoon and evening. Few fires burn more than 100 acres (40 ha), and the vast majority of fires reach only a little over an acre (0.5 ha) before they burn themselves out. Fire management focuses on monitoring dead and down wood quantities, soil and tree moisture, and the weather, to determine those areas most vulnerable to fire should one ignite. Current policy is to suppress all human caused fires and to evaluate natural fires, examining the benefit or detriment they may pose on the ecosystem. If a fire is considered to be an immediate threat to people and structures, or will burn out of control, then fire suppression is performed.
In an effort to minimize the chances of out of control fires and threats to people and structures, park employees do more than just monitor the potential for fire. Controlled burns are prescribed fires which are deliberately started to remove dead timber under conditions which allow fire fighters an opportunity to carefully control where and how much wood is consumed. Natural fires are sometimes considered prescribed fires if they are left to burn. In Yellowstone, unlike some other parks, there have been very few fires deliberately started by employees as prescribed burns. However, over the last 30 years, over 300 natural fires have been allowed to burn naturally. In addition, fire fighters remove dead and down wood and other hazards from areas where they will be a potential fire threat to lives and property, reducing the chances of fire danger in these areas. Fire monitors also regulate fire through educational services to the public and have been known to temporarily ban campfires from campgrounds during periods of high fire danger. The common notion in early United States land management policies was that all forest fires were bad. Fire was seen as a purely destructive force and there was little understanding that it was an integral part of the ecosystem. Consequently, until the 1970s, when a better understanding of wildfire was developed, all fires were suppressed. This led to an increase in dead and dying forests, which would later provide the fuel load for fires that would be much harder, and in some cases, impossible to control. Fire Management Plans were implemented, detailing that natural fires should be allowed to burn if they posed no immediate threat to lives and property.
1988 started with a wet spring season although by summer, drought began moving in throughout the northern Rockies, creating the driest year on record to that point. Grasses and plants which grew well in the early summer from the abundant spring moisture produced plenty of grass, which soon turned to dry tinder. The National Park Service began firefighting efforts to keep the fires under control, but the extreme drought made suppression difficult. Between July 15 and 21, 1988, fires quickly spread from 8,500 acres (3,400 ha; 13.3 sq mi) throughout the entire Yellowstone region, which included areas outside the park, to 99,000 acres (40,000 ha; 155 sq mi) on the park land alone. By the end of the month, the fires were out of control. Large fires burned together, and on August 20, 1988, the single worst day of the fires, more than 150,000 acres (61,000 ha; 230 sq mi) were consumed. Seven large fires were responsible for 95% of the 793,000 acres (321,000 ha; 1,239 sq mi) that were burned over the next couple of months. A total of 25,000 firefighters and U.S. military forces participated in the suppression efforts, at a cost of 120 million dollars. By the time winter brought snow that helped extinguish the last flames, the fires had destroyed 67 structures and caused several million dollars in damage. Though no civilian lives were lost, two personnel associated with the firefighting efforts were killed.
Contrary to media reports and speculation at the time, the fires killed very few park animals— surveys indicated that only about 345 elk (of an estimated 40,000–50,000), 36 deer, 12 moose, 6 black bears, and 9 bison had perished. Changes in fire management policies were implemented by land management agencies throughout the United States, based on knowledge gained from the 1988 fires and the evaluation of scientists and experts from various fields. By 1992, Yellowstone had adopted a new fire management plan which observed stricter guidelines for the management of natural fires.
from Wikipedia
A somewhat serendipitous photo, from my recent visual culture project.
Nikon Z6, Nikkor 24-70mm f/4 S
Capture One
New Adventure Travel's unique Ikarus-bodied DAF SB220 was retired from local bus work in 2015 and became a driver trainer, donning the registration H20 KFJ.
This shot from June of that year was taken as she was passing Bargoed Railway Station with a new recruit at the wheel, having just passed the company's East Lancs Kinetic-bodied MAN on Rail Replacement duties.
One of the first photos taken with an OM Zuiko mounted on the E-5. 28mm f/2.8 opened up "because I could".
The Cheetah is credited as being the fastest land animal over short distances, and can reach speeds of up to 90 km/h (55.9 m/h) in pursuit of prey. This cat is characterized by a slender body, long legs, and a distinctly rounded head with small rounded ears which are set wide apart. It measures two meters from the snout to the tip of the tail, has a mass of 40 - 60 Kg's, and stands about 800 mm high. It has a concave back and lower hind quarters. This Cat is characterized by a strongly spotted coat and by a long tail which is half as long as the length of its head and body. The tail has a unique pattern of striped markings.
Steve Hackett and his band from last year's 'Genesis Extended' gig at the Armadillo in Glasgow.
Left to right here are: Rob Townsend (lurking in the shadows); Roger King; Nad Sylvan; Steve Hackett; Gary O'Toole (also in the shadows); and Nick Beggs.
This was the seventh of eight gigs I shot on the Genesis Revisited/Extended tours over 2013/2014. My third gig was a Steve Hackett gig, so it was a joy for me to be able to shoot these gigs.
My thanks are due to Steve and Jo Hackett for arranging my photography access, and also to Brian Coles, Steve's Tour Manager for his help on the night. :-)
You can see other pics in my Steve Hackett set.
Try out met de Canon Extender 2x in combinatie met de Canon 70-200mm 2.8L.
Try out with the Canon Extender 2x in combination with the Canon 70-200mm 2.8L.
De kauw (Corvus mon edula, ook Coloeus monedula) behoort tot de kraaiachtigen en is een van de kleinste leden van deze familie.
The western jackdaw (Corvus monedula), also known as the Eurasian jackdaw, European jackdaw, or simply jackdaw, is a passerine bird in the crow family.
Interpreting a drawing of a distorted found object (shoe) through the application of a different medium, to further alter the depiction. Focussing on texture, tone and line.
Foundation course.
Size: Two A3 pages of sketchbook
Media: Paint, ink, charcoal
During previous visits to the area around Tromso I fell in love with the Island of Senja and surrounding archipelago. So, with summer having arrived I jumped north for an extended weekend and a wander for some fishing, photography, and walks. These photos are the result.
For licensing or usage requests, please reach out directly.
Sony A7R with Metabones Adapter and Canon 100-400 lense looks a little bit funny ;)
mein privater Blog: tasche.photography
KC-10A “Extender”
BLUE01
86-0028
RAF Mildenhall
USAF 514th Air Mobility Wing
USAF 305th Air Mobility Wing
86-0028 taxis after landing at RAF Mildenhall from Travis Air Force Base,California.
23rd February 2022
newcastlephotos.blogspot.com/2006/06/all-saints-cemetery....
All Saints Cemetery
This Cemetery stands on Jesmond Road, opposite Jesmond Old Cemetery and was the first cemetery in Newcastle to be instigated by the Burial Board. Consecrated in 1855 and opened in 1856 this was very much a rural part of Newcastle. The residential housing surrounding the cemetery on 3 sides were built later.
Noted Newcastle architect Benjamin Green designed the cemetery, its buildings and the fine Gothic archway over the entrance from Jesmond Road. The cemetery is surrounded by cast iron railings with fleur-de-lys heads.
The cemetery was extended to Osborne Avenue, from just under 10 acres by another 1.3 hectares in 1881.
In 1924 Carliol Square Gaol was demolished and the bodies of its executed criminals were transferred into unmarked graves in the cemetery.
In total around 90,000 burials have taken place here.
Thomas Harrison Hair (1810-1875) the artist best known for his Views of the Collieries of Northumberland and Durham, is buried here in an unmarked grave.
Two Small Chapels:
2 chapels. 1856 by Green. Coursed squared sandstone with ashlar turrets and dressings; Welsh slate roofs. T-plan with additional porch on side away from centre of cemetery, and corner turret on innermost side at south end. Aligned north-south. Decorated style. Double doors, with elaborate hinges,on inner fronts have nook shafts and head-stopped dripmoulds; similar surround to plainer door in outward-facing porch; windows of 3 lights facing gateway, 2 lights on other fronts, have similar dripmoulds. Lancets to corner turrets with gabled belfry under octagonal spirelets. Buttresses. Steeply-pitched roofs with cross finials. LISTED GRADE 2.
1 of the Chapels is now the Russian Orthodox Church Of St. George.
Gate, walls, piers, gates and railings.
Cemetery gateway, walls, piers, gates and railings. Dated 1856; by Green. Coursed squared sandstone with ashlar dressings; wrought iron gates; cast iron railings. Gothic style. High gable over 2-centred arch with 12 shafts each side and many mouldings; gabled ends have fantastic beasts climbing down kneelers; head-stopped dripmoulds, buttresses and finials.
High, pointed coping to flanking walls containing pedestrian doors in arches; end piers have gables with fleur-de-lis moulding. Chamfered coping to dwarf quadrant walls and similar walls along cemetery front, with 4 square piers at each side having pyramidal coping. High gates are Gothic-patterned; railings have fleur-de-lis heads.
Burials:
Samuel Smith.
Celtic Cross monument. Samuel Smith OBE JP (1872-1949) was the founder of Rington's Tea. He was born in Leeds and became an errand boy for a tea merchants on leaving school at 11. In 1908 he moved to Newcastle and set up a small shop in Heaton with William Titterington. They called the company Ringtons. The tea was imported from India and Sri Lanka then tasted, blended and packaged. It was delivered by the company's black, gold and green horse-drawn coaches. In 1926 the business moved to purpose-built premises in Algernon Road. Eventually there were 26 branches of Ringtons in the North. The firm moved into coachbuilding during the World Wars, which led to the creation of Smith's Electric Vehicles at Team Valley Trading Estate.
Alexander Gardner.
Cross monument. Alexander Gardner (1877-1921) was a footballer for Newcastle United. Before the First World War, Newcastle United were in the First Division, won three league titles and won one FA Cup final of three. Alexander was the captain and played at right half (midfielder). He made 268 appearances and scored 20 goals. He was born in Leith in 1899. The 1904/5 team won 23 out of 34 league games. In 1909 Alexander broke his leg, which ended his football career. He became landlord of the Dun Cow Inn in Claremont Road.
Michael Joseph Quigley.
Gravestone of Michael Joseph Quigley (1837-1924), American Civil War veteran. Michael was born in Bradford and emigrated to America with his wife shortly before the outbreak of civil war. He served under General Robert E. Lee in Virginia but was wounded in his left arm. He was later employed in Government Service. He returned to Britain in 1876. He lived in St. Lawrence Square off Walker Road. His income was subsidised by a pension from the American Government.
James Skinner.
Obelisk monument to James Skinner (1836-1920), shipbuilder. James was born in London. He moved to Newcastle aged 14 to begin an apprenticeship at Coutts shipyard at Low Walker. He went on to manage Andrew Leslie's shipyard at Hebburn then opened a yard at Bill Quay with William Wood, shipyard cashier. The firm Wood Skinner & Co. built 330 vessels over 42 years up to 1925. They also built the 30-bed Tyne Floating Hospital for Infectious Diseases at Jarrow Slake, designed by Newcastle Civil Engineer, George Laws. The hospital ship was launched on 2 August 1885. It sank in 1888. She was refloated and remained moored there for over 40 years.
Francis Batey.
Urn monument to Francis Batey (1841-1915), steam tug boat owner. Francis joined his father's tug boat business at the age of 11 and eventually gained his master's certificate. When the Albert Edward Dock opened in 1884, he was assistant pilot on the Rio Amazonas, the first ship to enter the dock. He went on to be chairman of several tug related companies on the River Tyne. One of his sons, John Thomas Batey, became Managing Director of Hawthorn Leslie's Hebburn shipyard.
Antonio Marcantonio.
Impressive monument of a statue of a monk or friar holding an infant. Antonio Marcantonio (1886-1960), ice cream manufacturer, arrived in Newcastle in 1895 to join a small colony of Italians living in Byker. In the early 1900s he returned to Italy to marry Angela. He returned to Newcastle and began making ice cream in a room in his house using small pans of salt and ice to freeze it. Eventually he took over a small factory on Stepney Bank. 500 gallons of ice cream were made daily. He also owned five ice cream parlours, the first one was in the Grainger Arcade. The Mark Toney business still flourishes (factory at Benton Square).
George Henry Carr.
A 13 feet high monument to George Henry Carr (1867-1889), racing cyclist. There is a shield on each side depicting a bicycle, flowers, the badge of the Jubilee Rovers Bicycle Club and the badge of Clarence Bicycle Club. Carr was a prominent figure on the racing circuit. He died aged 22 of inflammation of the brain.
John James Lightfoot,
Monument of an angel to John James Lightfoot (1877-1897), apprentice joiner. John James was crushed to death aged 19 during restoration of the 200 year old Green Tree beerhouse in Robson's Entry, Sandgate.The building collapsed killing 4 people and injuring 12. The disaster was sketched by the Chronicle's artist and published on 6 March 1897 the day after the accident. The article describes the scene - 'in the house to the east there was a yawning space where the wall had tumbled in; behind the hole a staircase stood, but seemed, like the sword of Damocles, to have no more than a hair-strength to support it'.
Josephine Esther Salisse.
Family vault of M. and H.M. Salisse. A stone sarcophagus with a bronze female figure mourning over it. Josephine Esther Salisse (1905-1924) was from Thornton Heath in Surrey. She died suddenly at her aunt's home in Stratford Road, Heaton, aged 19.
John and Benjamin Green were a father and son who worked in partnership as architects in North East England during the early nineteenth century. John, the father was a civil engineer as well as an architect. Although they did carry out some commissions separately, they were given joint credit for many of their projects, and it is difficult to attribute much of their work to a single individual. In general, John Green worked on civil engineering projects, such as road and rail bridges, whereas Benjamin worked on projects that were more purely architectural. Their work was predominantly church and railway architecture, with a sprinkling of public buildings that includes their masterpiece, Newcastle's Theatre Royal.
Drawings by John and Benjamin Green are held by the Laing Art Gallery in Newcastle upon Tyne.
Biographies
John Green was born on 29 June 1787 at Newton Fell House, Nafferton, two miles north of Ovington, Northumberland. He was the son of Benjamin Green, a carpenter and maker of agricultural implements. After finishing school, he worked in his father's business. The firm moved to the market town of Corbridge and began general building work with young John concentrating on architectural work. About 1820, John set up business as an architect and civil engineer in nearby Newcastle upon Tyne.
John Green married Jane Stobart in 1805, and they had two sons, John (c.1807–68) and Benjamin (c1811-58), both of whom became architects. Little is known about the career of John, but Benjamin worked in partnership with his father on many projects.
In 1822 John Green designed a new building for the Newcastle Literary and Philosophical Society. The building, which houses the society's substantial library, is still in use today. He also designed a number of farmhouses, being employed on the Beaufront estate near Hexham and also on the Duke of Northumberland’s estates.
John Green was principally a civil engineer, and built several road and rail bridges. In 1829–31 he built two wrought-iron suspension bridges crossing the Tyne (at Scotswood) and the Tees (at Whorlton). The bridge at Scotswood was demolished in 1967 but the one at Whorlton still survives. When the High Level Bridge at Newcastle was proposed ten years later, John Green submitted plans, but those of Robert Stephenson were accepted by the York, Newcastle and Berwick Railway. Green also built a number of bridges using an innovative system of laminated timber arches on masonry piers, the Weibeking system, based on the work of Bavarian engineer C.F. Weibeking. The two he built for the Newcastle and North Shields Railway, at the Ouseburn and at Willington Quay remain in use, though the timbers were replaced with wrought iron in a similar lattice pattern in 1869. In 1840 he was elected to the Institution of Civil Engineers, and in 1841 he was awarded the institution's Telford Medal for his work on laminated arch design.
John Green died in Newcastle on 30 September 1852.
Benjamin Green
Benjamin Green was a pupil of Augustus Charles Pugin, father of the more famous Augustus Welby Northmore Pugin. In the mid-1830s he became a partner of his father and remained so until the latter's death in 1852. The two partners differed somewhat. John has been described as a 'plain, practical, shrewd man of business' with a 'plain, severe and economical' style, whereas Benjamin was 'an artistic, dashing sort of fellow', with a style that was 'ornamental, florid and costly'.
The Greens worked as railway architects and it is believed that all the main line stations between Newcastle and Berwick upon Tweed were designed by Benjamin. In 2020 Morpeth Station was restored to Green's original designs following a £2.3M investment. They also designed a number of Northumbrian churches, the best examples being at Earsdon and Cambo.
The Green's most important commissions in Newcastle were the Theatre Royal (1836–37) and the column for Grey's Monument (1837–38). Both of these structures were part of the re-development of Newcastle city centre in neo-classical style by Richard Grainger, and both exist today. Although both of the partners were credited with their design, it is believed that Benjamin was the person responsible.
Another well-known structure designed by the Greens is Penshaw Monument (1844). This is a folly standing on Penshaw Hill in County Durham. It was built as a half-sized replica of the renowned Temple of Hephaestus in Athens, and was dedicated to John George Lambton, first Earl of Durham and the first Governor of the Province of Canada. The monument, being built on a hill is visible for miles around and is a famous local landmark. It is now owned by the National Trust.
Benjamin Green survived his father by only six years, and died in a mental home at Dinsdale Park, County Durham on 14 November 1858.
Major works
Presbyterian Chapel, Newcastle upon Tyne, 1822 (demolished 2011)
Literary and Philosophical Society, Newcastle upon Tyne, 1822–1825
St Peter's Church, Falstone, 1824–1825
Westgate Hill Cemetery, Newcastle upon Tyne, 1825–1829 (lodge demolished 1970, railings and gates removed, piers and basic layout remains)
Ingram Farm, Ingram, 1826
Whorlton Suspension Bridge, Wycliffe, County Durham, 1829–1831
Hawks Cottages, Gateshead, 1830 (demolished 1960)
Scotswood Chain Bridge, Newcastle upon Tyne, 1831, (demolished 1967)
Church of St Mary and St Thomas Aquinas, Stella, 1831–1832[1]
Bellingham Bridge, Bellingham, 1834
Holy Trinity Church, Stockton-On-Tees, 1834–1835[2]
Holy Trinity Church, Dalton (near Stamfordham), 1836
Vicarage of St Alban, Earsdon, 1836
Church of St Alban, Earsdon, 1836–1837
St Mary's Roman Catholic Church, Alnwick, 1836
Church of the Holy Saviour, Newburn, 1836–1837
Poor Law Guardians Hall, North Shields, 1837
Master Mariners Homes, Tynemouth, 1837–1840[3]
Theatre Royal, Newcastle upon Tyne, 1837
Parish Hall of the Church of the Holy Saviour, Newburn, 1838
Column of Grey's Monument, Newcastle upon Tyne, 1838
Willington Viaduct, Wallsend, 1837–1839
Ouseburn Viaduct, Newcastle upon Tyne, 1837–1839
Church of the Holy Saviour, Tynemouth, 1839–1841
Ilderton Vicarage, Ilderton, 1841
The Red Cottage, Whitburn, 1842
Holy Trinity Church, Cambo, 1842
Holy Trinity Church, Horsley-on-Rede, 1844
The Earl of Durham's Monument, Sunderland, 1844
St Edwin's, Coniscliffe, Co. Durham, 1844 (restoration of mediaeval church)
40–44 Moseley Street, Newcastle upon Tyne, 1845
Witham Testimonial Hall, Barnard Castle, 1846
Old Railway Station, Tynemouth Rd, Tynemouth 1846–1847
Acklington Station, Acklington, 1847
Chathill Station, Chathill, 1847
Belford Station, Belford, Northumberland, 1847
Morpeth Station, Morpeth, Northumberland, 1847
Warkworth Station, Warkworth, Northumberland, 1847
Holy Trinity Church, Seghill, 1849
Newcastle Joint Stock Bank, St Nicholas Square, Newcastle, c.1850
Norham station, Norham, 1851
St Paul's Church, Elswick, 1854
All Saints Cemetery, Jesmond, 1854
Sailor's Home, 11 New Quay, North Shields, 1856
United Free Methodist Church, North Shields, 1857
Corn Exchange, Groat Market, Newcastle (demolished 1974)
Newcastle upon Tyne, or simply Newcastle is a cathedral city and metropolitan borough in Tyne and Wear, England. It is located on the River Tyne's northern bank, opposite Gateshead to the south. It is the most populous settlement in the Tyneside conurbation and North East England.
Newcastle developed around a Roman settlement called Pons Aelius, the settlement became known as Monkchester before taking on the name of a castle built in 1080 by William the Conqueror's eldest son, Robert Curthose. It was one of the world's largest ship building and repair centres during the industrial revolution. Newcastle was part of the county of Northumberland until 1400, when it separated and formed a county of itself. In 1974, Newcastle became part of Tyne and Wear. Since 2018, the city council has been part of the North of Tyne Combined Authority.
The history of Newcastle upon Tyne dates back almost 2,000 years, during which it has been controlled by the Romans, the Angles and the Norsemen amongst others. Newcastle upon Tyne was originally known by its Roman name Pons Aelius. The name "Newcastle" has been used since the Norman conquest of England. Due to its prime location on the River Tyne, the town developed greatly during the Middle Ages and it was to play a major role in the Industrial Revolution, being granted city status in 1882. Today, the city is a major retail, commercial and cultural centre.
Roman settlement
The history of Newcastle dates from AD 122, when the Romans built the first bridge to cross the River Tyne at that point. The bridge was called Pons Aelius or 'Bridge of Aelius', Aelius being the family name of Roman Emperor Hadrian, who was responsible for the Roman wall built across northern England along the Tyne–Solway gap. Hadrian's Wall ran through present-day Newcastle, with stretches of wall and turrets visible along the West Road, and at a temple in Benwell. Traces of a milecastle were found on Westgate Road, midway between Clayton Street and Grainger Street, and it is likely that the course of the wall corresponded to present-day Westgate Road. The course of the wall can be traced eastwards to the Segedunum Roman fort at Wallsend, with the fort of Arbeia down-river at the mouth of the Tyne, on the south bank in what is now South Shields. The Tyne was then a wider, shallower river at this point and it is thought that the bridge was probably about 700 feet (210 m) long, made of wood and supported on stone piers. It is probable that it was sited near the current Swing Bridge, due to the fact that Roman artefacts were found there during the building of the latter bridge. Hadrian himself probably visited the site in 122. A shrine was set up on the completed bridge in 123 by the 6th Legion, with two altars to Neptune and Oceanus respectively. The two altars were subsequently found in the river and are on display in the Great North Museum in Newcastle.
The Romans built a stone-walled fort in 150 to protect the river crossing which was at the foot of the Tyne Gorge, and this took the name of the bridge so that the whole settlement was known as Pons Aelius. The fort was situated on a rocky outcrop overlooking the new bridge, on the site of the present Castle Keep. Pons Aelius is last mentioned in 400, in a Roman document listing all of the Roman military outposts. It is likely that nestling in the shadow of the fort would have been a small vicus, or village. Unfortunately, no buildings have been detected; only a few pieces of flagging. It is clear that there was a Roman cemetery near Clavering Place, behind the Central station, as a number of Roman coffins and sarcophagi have been unearthed there.
Despite the presence of the bridge, the settlement of Pons Aelius was not particularly important among the northern Roman settlements. The most important stations were those on the highway of Dere Street running from Eboracum (York) through Corstopitum (Corbridge) and to the lands north of the Wall. Corstopitum, being a major arsenal and supply centre, was much larger and more populous than Pons Aelius.
Anglo-Saxon development
The Angles arrived in the North-East of England in about 500 and may have landed on the Tyne. There is no evidence of an Anglo-Saxon settlement on or near the site of Pons Aelius during the Anglo-Saxon age. The bridge probably survived and there may well have been a small village at the northern end, but no evidence survives. At that time the region was dominated by two kingdoms, Bernicia, north of the Tees and ruled from Bamburgh, and Deira, south of the Tees and ruled from York. Bernicia and Deira combined to form the kingdom of Northanhymbra (Northumbria) early in the 7th century. There were three local kings who held the title of Bretwalda – 'Lord of Britain', Edwin of Deira (627–632), Oswald of Bernicia (633–641) and Oswy of Northumbria (641–658). The 7th century became known as the 'Golden Age of Northumbria', when the area was a beacon of culture and learning in Europe. The greatness of this period was based on its generally Christian culture and resulted in the Lindisfarne Gospels amongst other treasures. The Tyne valley was dotted with monasteries, with those at Monkwearmouth, Hexham and Jarrow being the most famous. Bede, who was based at Jarrow, wrote of a royal estate, known as Ad Murum, 'at the Wall', 12 miles (19 km) from the sea. It is thought that this estate may have been in what is now Newcastle. At some unknown time, the site of Newcastle came to be known as Monkchester. The reason for this title is unknown, as we are unaware of any specific monasteries at the site, and Bede made no reference to it. In 875 Halfdan Ragnarsson, the Danish Viking conqueror of York, led an army that attacked and pillaged various monasteries in the area, and it is thought that Monkchester was also pillaged at this time. Little more was heard of it until the coming of the Normans.
Norman period
After the arrival of William the Conqueror in England in 1066, the whole of England was quickly subjected to Norman rule. However, in Northumbria there was great resistance to the Normans, and in 1069 the newly appointed Norman Earl of Northumbria, Robert de Comines and 700 of his men were killed by the local population at Durham. The Northumbrians then marched on York, but William was able to suppress the uprising. That same year, a second uprising occurred when a Danish fleet landed in the Humber. The Northumbrians again attacked York and destroyed the garrison there. William was again able to suppress the uprising, but this time he took revenge. He laid waste to the whole of the Midlands and the land from York to the Tees. In 1080, William Walcher, the Norman bishop of Durham and his followers were brutally murdered at Gateshead. This time Odo, bishop of Bayeux, William's half brother, devastated the land between the Tees and the Tweed. This was known as the 'Harrying of the North'. This devastation is reflected in the Domesday Book. The destruction had such an effect that the North remained poor and backward at least until Tudor times and perhaps until the Industrial Revolution. Newcastle suffered in this respect with the rest of the North.
In 1080 William sent his eldest son, Robert Curthose, north to defend the kingdom against the Scots. After his campaign, he moved to Monkchester and began the building of a 'New Castle'. This was of the "motte-and-bailey" type of construction, a wooden tower on top of an earthen mound (motte), surrounded by a moat and wooden stockade (bailey). It was this castle that gave Newcastle its name. In 1095 the Earl of Northumbria, Robert de Mowbray, rose up against the king, William Rufus, and Rufus sent an army north to recapture the castle. From then on the castle became crown property and was an important base from which the king could control the northern barons. The Northumbrian earldom was abolished and a Sheriff of Northumberland was appointed to administer the region. In 1091 the parish church of St Nicholas was consecrated on the site of the present Anglican cathedral, close by the bailey of the new castle. The church is believed to have been a wooden building on stone footings.
Not a trace of the tower or mound of the motte and bailey castle remains now. Henry II replaced it with a rectangular stone keep, which was built between 1172 and 1177 at a cost of £1,444. A stone bailey, in the form of a triangle, replaced the previous wooden one. The great outer gateway to the castle, called 'the Black Gate', was built later, between 1247 and 1250, in the reign of Henry III. There were at that time no town walls and when attacked by the Scots, the townspeople had to crowd into the bailey for safety. It is probable that the new castle acted as a magnet for local merchants because of the safety it provided. This in turn would help to expand trade in the town. At this time wool, skins and lead were being exported, whilst alum, pepper and ginger were being imported from France and Flanders.
Middle Ages
Throughout the Middle Ages, Newcastle was England's northern fortress, the centre for assembled armies. The Border war against Scotland lasted intermittently for several centuries – possibly the longest border war ever waged. During the civil war between Stephen and Matilda, David 1st of Scotland and his son were granted Cumbria and Northumberland respectively, so that for a period from 1139 to 1157, Newcastle was effectively in Scottish hands. It is believed that during this period, King David may have built the church of St Andrew and the Benedictine nunnery in Newcastle. However, King Stephen's successor, Henry II was strong enough to take back the Earldom of Northumbria from Malcolm IV.
The Scots king William the Lion was imprisoned in Newcastle, in 1174, after being captured at the Battle of Alnwick. Edward I brought the Stone of Scone and William Wallace south through the town and Newcastle was successfully defended against the Scots three times during the 14th century.
Around 1200, stone-faced, clay-filled jetties were starting to project into the river, an indication that trade was increasing in Newcastle. As the Roman roads continued to deteriorate, sea travel was gaining in importance. By 1275 Newcastle was the sixth largest wool exporting port in England. The principal exports at this time were wool, timber, coal, millstones, dairy produce, fish, salt and hides. Much of the developing trade was with the Baltic countries and Germany. Most of the Newcastle merchants were situated near the river, below the Castle. The earliest known charter was dated 1175 in the reign of Henry II, giving the townspeople some control over their town. In 1216 King John granted Newcastle a mayor[8] and also allowed the formation of guilds (known as Mysteries). These were cartels formed within different trades, which restricted trade to guild members. There were initially twelve guilds. Coal was being exported from Newcastle by 1250, and by 1350 the burgesses received a royal licence to export coal. This licence to export coal was jealously guarded by the Newcastle burgesses, and they tried to prevent any one else on the Tyne from exporting coal except through Newcastle. The burgesses similarly tried to prevent fish from being sold anywhere else on the Tyne except Newcastle. This led to conflicts with Gateshead and South Shields.
In 1265, the town was granted permission to impose a 'Wall Tax' or Murage, to pay for the construction of a fortified wall to enclose the town and protect it from Scottish invaders. The town walls were not completed until early in the 14th century. They were two miles (3 km) long, 9 feet (2.7 m) thick and 25 feet (7.6 m) high. They had six main gates, as well as some smaller gates, and had 17 towers. The land within the walls was divided almost equally by the Lort Burn, which flowed southwards and joined the Tyne to the east of the Castle. The town began to expand north of the Castle and west of the Lort Burn with various markets being set up within the walls.
In 1400 Henry IV granted a new charter, creating a County corporate which separated the town, but not the Castle, from the county of Northumberland and recognised it as a "county of itself" with a right to have a sheriff of its own. The burgesses were now allowed to choose six aldermen who, with the mayor would be justices of the peace. The mayor and sheriff were allowed to hold borough courts in the Guildhall.
Religious houses
During the Middle Ages a number of religious houses were established within the walls: the first of these was the Benedictine nunnery of St Bartholomew founded in 1086 near the present-day Nun Street. Both David I of Scotland and Henry I of England were benefactors of the religious house. Nothing of the nunnery remains now.
The friary of Blackfriars, Newcastle (Dominican) was established in 1239. These were also known as the Preaching Friars or Shod Friars, because they wore sandals, as opposed to other orders. The friary was situated in the present-day Friars Street. In 1280 the order was granted royal permission to make a postern in the town walls to communicate with their gardens outside the walls. On 19 June 1334, Edward Balliol, claimant to be King of Scotland, did homage to King Edward III, on behalf of the kingdom of Scotland, in the church of the friary. Much of the original buildings of the friary still exist, mainly because, after the Dissolution of the Monasteries the friary of Blackfriars was rented out by the corporation to nine of the local trade guilds.
The friary of Whitefriars (Carmelite) was established in 1262. The order was originally housed on the Wall Knoll in Pandon, but in 1307 it took over the buildings of another order, which went out of existence, the Friars of the Sac. The land, which had originally been given by Robert the Bruce, was situated in the present-day Hanover Square, behind the Central station. Nothing of the friary remains now.
The friary of Austinfriars (Augustinian) was established in 1290. The friary was on the site where the Holy Jesus Hospital was built in 1682. The friary was traditionally the lodging place of English kings whenever they visited or passed through Newcastle. In 1503 Princess Margaret, eldest daughter of Henry VII of England, stayed two days at the friary on her way to join her new husband James IV of Scotland.
The friary of Greyfriars (Franciscans) was established in 1274. The friary was in the present-day area between Pilgrim Street, Grey Street, Market Street and High Chare. Nothing of the original buildings remains.
The friary of the Order of the Holy Trinity, also known as the Trinitarians, was established in 1360. The order devoted a third of its income to buying back captives of the Saracens, during the Crusades. Their house was on the Wall Knoll, in Pandon, to the east of the city, but within the walls. Wall Knoll had previously been occupied by the White Friars until they moved to new premises in 1307.
All of the above religious houses were closed in about 1540, when Henry VIII dissolved the monasteries.
An important street running through Newcastle at the time was Pilgrim Street, running northwards inside the walls and leading to the Pilgrim Gate on the north wall. The street still exists today as arguably Newcastle's main shopping street.
Tudor period
The Scottish border wars continued for much of the 16th century, so that during that time, Newcastle was often threatened with invasion by the Scots, but also remained important as a border stronghold against them.
During the Reformation begun by Henry VIII in 1536, the five Newcastle friaries and the single nunnery were dissolved and the land was sold to the Corporation and to rich merchants. At this time there were fewer than 60 inmates of the religious houses in Newcastle. The convent of Blackfriars was leased to nine craft guilds to be used as their headquarters. This probably explains why it is the only one of the religious houses whose building survives to the present day. The priories at Tynemouth and Durham were also dissolved, thus ending the long-running rivalry between Newcastle and the church for control of trade on the Tyne. A little later, the property of the nunnery of St Bartholomew and of Grey Friars were bought by Robert Anderson, who had the buildings demolished to build his grand Newe House (also known as Anderson Place).
With the gradual decline of the Scottish border wars the town walls were allowed to decline as well as the castle. By 1547, about 10,000 people were living in Newcastle. At the beginning of the 16th century exports of wool from Newcastle were more than twice the value of exports of coal, but during the century coal exports continued to increase.
Under Edward VI, John Dudley, Duke of Northumberland, sponsored an act allowing Newcastle to annexe Gateshead as its suburb. The main reason for this was to allow the Newcastle Hostmen, who controlled the export of Tyne coal, to get their hands on the Gateshead coal mines, previously controlled by the Bishop of Durham. However, when Mary I came to power, Dudley met his downfall and the decision was reversed. The Reformation allowed private access to coal mines previously owned by Tynemouth and Durham priories and as a result coal exports increase dramatically, from 15,000 tons in 1500 to 35,000 tons in 1565, and to 400,000 tons in 1625.
The plague visited Newcastle four times during the 16th century, in 1579 when 2,000 people died, in 1589 when 1700 died, in 1595 and finally in 1597.
In 1600 Elizabeth I granted Newcastle a charter for an exclusive body of electors, the right to elect the mayor and burgesses. The charter also gave the Hostmen exclusive rights to load coal at any point on the Tyne. The Hostmen developed as an exclusive group within the Merchant Adventurers who had been incorporated by a charter in 1547.
Stuart period
In 1636 there was a serious outbreak of bubonic plague in Newcastle. There had been several previous outbreaks of the disease over the years, but this was the most serious. It is thought to have arrived from the Netherlands via ships that were trading between the Tyne and that country. It first appeared in the lower part of the town near the docks but gradually spread to all parts of the town. As the disease gained hold the authorities took measures to control it by boarding up any properties that contained infected persons, meaning that whole families were locked up together with the infected family members. Other infected persons were put in huts outside the town walls and left to die. Plague pits were dug next to the town's four churches and outside the town walls to receive the bodies in mass burials. Over the course of the outbreak 5,631 deaths were recorded out of an estimated population of 12,000, a death rate of 47%.
In 1637 Charles I tried to raise money by doubling the 'voluntary' tax on coal in return for allowing the Newcastle Hostmen to regulate production and fix prices. This caused outrage amongst the London importers and the East Anglian shippers. Both groups decided to boycott Tyne coal and as a result forced Charles to reverse his decision in 1638.
In 1640 during the Second Bishops' War, the Scots successfully invaded Newcastle. The occupying army demanded £850 per day from the Corporation to billet the Scottish troops. Trade from the Tyne ground to a halt during the occupation. The Scots left in 1641 after receiving a Parliamentary pardon and a £4,000,000 loan from the town.
In 1642 the English Civil War began. King Charles realised the value of the Tyne coal trade and therefore garrisoned Newcastle. A Royalist was appointed as governor. At that time, Newcastle and King's Lynn were the only important seaports to support the crown. In 1644 Parliament blockaded the Tyne to prevent the king from receiving revenue from the Tyne coal trade. Coal exports fell from 450,000 to 3,000 tons and London suffered a hard winter without fuel. Parliament encouraged the coal trade from the Wear to try to replace that lost from Newcastle but that was not enough to make up for the lost Tyneside tonnage.
In 1644 the Scots crossed the border. Newcastle strengthened its defences in preparation. The Scottish army, with 40,000 troops, besieged Newcastle for three months until the garrison of 1,500 surrendered. During the siege, the Scots bombarded the walls with their artillery, situated in Gateshead and Castle Leazes. The Scottish commander threatened to destroy the steeple of St Nicholas's Church by gunfire if the mayor, Sir John Marley, did not surrender the town. The mayor responded by placing Scottish prisoners that they had captured in the steeple, so saving it from destruction. The town walls were finally breached by a combination of artillery and sapping. In gratitude for this defence, Charles gave Newcastle the motto 'Fortiter Defendit Triumphans' to be added to its coat of arms. The Scottish army occupied Northumberland and Durham for two years. The coal taxes had to pay for the Scottish occupation. In 1645 Charles surrendered to the Scots and was imprisoned in Newcastle for nine months. After the Civil War the coal trade on the Tyne soon picked up and exceeded its pre-war levels.
A new Guildhall was completed on the Sandhill next to the river in 1655, replacing an earlier facility damaged by fire in 1639, and became the meeting place of Newcastle Town Council. In 1681 the Hospital of the Holy Jesus was built partly on the site of the Austin Friars. The Guildhall and Holy Jesus Hospital still exist.
Charles II tried to impose a charter on Newcastle to give the king the right to appoint the mayor, sheriff, recorder and town clerk. Charles died before the charter came into effect. In 1685, James II tried to replace Corporation members with named Catholics. However, James' mandate was suspended in 1689 after the Glorious Revolution welcoming William of Orange. In 1689, after the fall of James II, the people of Newcastle tore down his bronze equestrian statue in Sandhill and tossed it into the Tyne. The bronze was later used to make bells for All Saints Church.
In 1689 the Lort Burn was covered over. At this time it was an open sewer. The channel followed by the Lort Burn became the present day Dean Street. At that time, the centre of Newcastle was still the Sandhill area, with many merchants living along the Close or on the Side. The path of the main road through Newcastle ran from the single Tyne bridge, through Sandhill to the Side, a narrow street which climbed steeply on the north-east side of the castle hill until it reached the higher ground alongside St Nicholas' Church. As Newcastle developed, the Side became lined with buildings with projecting upper stories, so that the main street through Newcastle was a narrow, congested, steep thoroughfare.
In 1701 the Keelmen's Hospital was built in the Sandgate area of the city, using funds provided by the keelmen. The building still stands today.
Eighteenth century
In the 18th century, Newcastle was the country's largest print centre after London, Oxford and Cambridge, and the Literary and Philosophical Society of 1793, with its erudite debates and large stock of books in several languages predated the London Library by half a century.
In 1715, during the Jacobite rising in favour of the Old Pretender, an army of Jacobite supporters marched on Newcastle. Many of the Northumbrian gentry joined the rebels. The citizens prepared for its arrival by arresting Jacobite supporters and accepting 700 extra recruits into the local militia. The gates of the city were closed against the rebels. This proved enough to delay an attack until reinforcements arrived forcing the rebel army to move across to the west coast. The rebels finally surrendered at Preston.
In 1745, during a second Jacobite rising in favour of the Young Pretender, a Scottish army crossed the border led by Bonnie Prince Charlie. Once again Newcastle prepared by arresting Jacobite supporters and inducting 800 volunteers into the local militia. The town walls were strengthened, most of the gates were blocked up and some 200 cannon were deployed. 20,000 regulars were billeted on the Town Moor. These preparations were enough to force the rebel army to travel south via the west coast. They were eventually defeated at Culloden in 1746.
Newcastle's actions during the 1715 rising in resisting the rebels and declaring for George I, in contrast to the rest of the region, is the most likely source of the nickname 'Geordie', applied to people from Tyneside, or more accurately Newcastle. Another theory, however, is that the name 'Geordie' came from the inventor of the Geordie lamp, George Stephenson. It was a type of safety lamp used in mining, but was not invented until 1815. Apparently the term 'German Geordie' was in common use during the 18th century.
The city's first hospital, Newcastle Infirmary opened in 1753; it was funded by public subscription. A lying-in hospital was established in Newcastle in 1760. The city's first public hospital for mentally ill patients, Wardens Close Lunatic Hospital was opened in October 1767.
In 1771 a flood swept away much of the bridge at Newcastle. The bridge had been built in 1250 and repaired after a flood in 1339. The bridge supported various houses and three towers and an old chapel. A blue stone was placed in the middle of the bridge to mark the boundary between Newcastle and the Palatinate of Durham. A temporary wooden bridge had to be built, and this remained in use until 1781, when a new stone bridge was completed. The new bridge consisted of nine arches. In 1801, because of the pressure of traffic, the bridge had to be widened.
A permanent military presence was established in the city with the completion of Fenham Barracks in 1806. The facilities at the Castle for holding assizes, which had been condemned for their inconvenience and unhealthiness, were replaced when the Moot Hall opened in August 1812.
Victorian period
Present-day Newcastle owes much of its architecture to the work of the builder Richard Grainger, aided by architects John Dobson, Thomas Oliver, John and Benjamin Green and others. In 1834 Grainger won a competition to produce a new plan for central Newcastle. He put this plan into effect using the above architects as well as architects employed in his own office. Grainger and Oliver had already built Leazes Terrace, Leazes Crescent and Leazes Place between 1829 and 1834. Grainger and Dobson had also built the Royal Arcade at the foot of Pilgrim Street between 1830 and 1832. The most ambitious project covered 12 acres 12 acres (49,000 m2) in central Newcastle, on the site of Newe House (also called Anderson Place). Grainger built three new thoroughfares, Grey Street, Grainger Street and Clayton Street with many connecting streets, as well as the Central Exchange and the Grainger Market. John Wardle and George Walker, working in Grainger's office, designed Clayton Street, Grainger Street and most of Grey Street. Dobson designed the Grainger Market and much of the east side of Grey Street. John and Benjamin Green designed the Theatre Royal at the top of Grey Street, where Grainger placed the column of Grey's Monument as a focus for the whole scheme. Grey Street is considered to be one of the finest streets in the country, with its elegant curve. Unfortunately most of old Eldon Square was demolished in the 1960s in the name of progress. The Royal Arcade met a similar fate.
In 1849 a new bridge was built across the river at Newcastle. This was the High Level Bridge, designed by Robert Stephenson, and slightly up river from the existing bridge. The bridge was designed to carry road and rail traffic across the Tyne Gorge on two decks with rail traffic on the upper deck and road traffic on the lower. The new bridge meant that traffic could pass through Newcastle without having to negotiate the steep, narrow Side, as had been necessary for centuries. The bridge was opened by Queen Victoria, who one year later opened the new Central Station, designed by John Dobson. Trains were now able to cross the river, directly into the centre of Newcastle and carry on up to Scotland. The Army Riding School was also completed in 1849.
In 1854 a large fire started on the Gateshead quayside and an explosion caused it to spread across the river to the Newcastle quayside. A huge conflagration amongst the narrow alleys, or 'chares', destroyed the homes of 800 families as well as many business premises. The narrow alleys that had been destroyed were replaced by streets containing blocks of modern offices.
In 1863 the Town Hall in St Nicholas Square replaced the Guildhall as the meeting place of Newcastle Town Council.
In 1876 the low level bridge was replaced by a new bridge known as the Swing Bridge, so called because the bridge was able to swing horizontally on a central axis and allow ships to pass on either side. This meant that for the first time sizeable ships could pass up-river beyond Newcastle. The bridge was built and paid for by William Armstrong, a local arms manufacturer, who needed to have warships access his Elswick arms factory to fit armaments to them. The Swing Bridge's rotating mechanism is adapted from the cannon mounts developed in Armstrong's arms works. In 1882 the Elswick works began to build ships as well as to arm them. The Barrack Road drill hall was completed in 1890.
Industrialisation
In the 19th century, shipbuilding and heavy engineering were central to the city's prosperity; and the city was a powerhouse of the Industrial Revolution. Newcastle's development as a major city owed most to its central role in the production and export of coal. The phrase "taking coals to Newcastle" was first recorded in 1538; it proverbially denotes bringing a particular commodity to a place that has more than enough of it already.
Innovation in Newcastle and surrounding areas included the following:
George Stephenson developed a miner's safety lamp at the same time that Humphry Davy developed a rival design. The lamp made possible the opening up of ever deeper mines to provide the coal that powered the industrial revolution.
George and his son Robert Stephenson were hugely influential figures in the development of the early railways. George developed Blücher, a locomotive working at Killingworth colliery in 1814, whilst Robert was instrumental in the design of Rocket, a revolutionary design that was the forerunner of modern locomotives. Both men were involved in planning and building railway lines, all over this country and abroad.
Joseph Swan demonstrated a working electric light bulb about a year before Thomas Edison did the same in the USA. This led to a dispute as to who had actually invented the light bulb. Eventually the two rivals agreed to form a mutual company between them, the Edison and Swan Electric Light Company, known as Ediswan.
Charles Algernon Parsons invented the steam turbine, for marine use and for power generation. He used Turbinia, a small, turbine-powered ship, to demonstrate the speed that a steam turbine could generate. Turbinia literally ran rings around the British Fleet at a review at Spithead in 1897.
William Armstrong invented a hydraulic crane that was installed in dockyards up and down the country. He then began to design light, accurate field guns for the British army. These were a vast improvement on the existing guns that were then in use.
The following major industries developed in Newcastle or its surrounding area:
Glassmaking
A small glass industry existed in Newcastle from the mid-15th century. In 1615 restrictions were put on the use of wood for manufacturing glass. It was found that glass could be manufactured using the local coal, and so a glassmaking industry grew up on Tyneside. Huguenot glassmakers came over from France as refugees from persecution and set up glasshouses in the Skinnerburn area of Newcastle. Eventually, glass production moved to the Ouseburn area of Newcastle. In 1684 the Dagnia family, Sephardic Jewish emigrants from Altare, arrived in Newcastle from Stourbridge and established glasshouses along the Close, to manufacture high quality flint glass. The glass manufacturers used sand ballast from the boats arriving in the river as the main raw material. The glassware was then exported in collier brigs. The period from 1730 to 1785 was the highpoint of Newcastle glass manufacture, when the local glassmakers produced the 'Newcastle Light Baluster'. The glassmaking industry still exists in the west end of the city with local Artist and Glassmaker Jane Charles carrying on over four hundred years of hot glass blowing in Newcastle upon Tyne.
Locomotive manufacture
In 1823 George Stephenson and his son Robert established the world's first locomotive factory near Forth Street in Newcastle. Here they built locomotives for the Stockton and Darlington Railway and the Liverpool and Manchester Railway, as well as many others. It was here that the famous locomotive Rocket was designed and manufactured in preparation for the Rainhill Trials. Apart from building locomotives for the British market, the Newcastle works also produced locomotives for Europe and America. The Forth Street works continued to build locomotives until 1960.
Shipbuilding
In 1296 a wooden, 135 ft (41 m) long galley was constructed at the mouth of the Lort Burn in Newcastle, as part of a twenty-ship order from the king. The ship cost £205, and is the earliest record of shipbuilding in Newcastle. However the rise of the Tyne as a shipbuilding area was due to the need for collier brigs for the coal export trade. These wooden sailing ships were usually built locally, establishing local expertise in building ships. As ships changed from wood to steel, and from sail to steam, the local shipbuilding industry changed to build the new ships. Although shipbuilding was carried out up and down both sides of the river, the two main areas for building ships in Newcastle were Elswick, to the west, and Walker, to the east. By 1800 Tyneside was the third largest producer of ships in Britain. Unfortunately, after the Second World War, lack of modernisation and competition from abroad gradually caused the local industry to decline and die.
Armaments
In 1847 William Armstrong established a huge factory in Elswick, west of Newcastle. This was initially used to produce hydraulic cranes but subsequently began also to produce guns for both the army and the navy. After the Swing Bridge was built in 1876 allowing ships to pass up river, warships could have their armaments fitted alongside the Elswick works. Armstrong's company took over its industrial rival, Joseph Whitworth of Manchester in 1897.
Steam turbines
Charles Algernon Parsons invented the steam turbine and, in 1889, founded his own company C. A. Parsons and Company in Heaton, Newcastle to make steam turbines. Shortly after this, he realised that steam turbines could be used to propel ships and, in 1897, he founded a second company, Parsons Marine Steam Turbine Company in Wallsend. It is there that he designed and manufactured Turbinia. Parsons turbines were initially used in warships but soon came to be used in merchant and passenger vessels, including the liner Mauretania which held the blue riband for the Atlantic crossing until 1929. Parsons' company in Heaton began to make turbo-generators for power stations and supplied power stations all over the world. The Heaton works, reduced in size, remains as part of the Siemens AG industrial giant.
Pottery
In 1762 the Maling pottery was founded in Sunderland by French Huguenots, but transferred to Newcastle in 1817. A factory was built in the Ouseburn area of the city. The factory was rebuilt twice, finally occupying a 14-acre (57,000 m2) site that was claimed to be the biggest pottery in the world and which had its own railway station. The pottery pioneered use of machines in making potteries as opposed to hand production. In the 1890s the company went up-market and employed in-house designers. The period up to the Second World War was the most profitable with a constant stream of new designs being introduced. However, after the war, production gradually declined and the company closed in 1963.
Expansion of the city
Newcastle was one of the boroughs reformed by the Municipal Corporations Act 1835: the reformed municipal borough included the parishes of Byker, Elswick, Heaton, Jesmond, Newcastle All Saints, Newcastle St Andrew, Newcastle St John, Newcastle St Nicholas, and Westgate. The urban districts of Benwell and Fenham and Walker were added in 1904. In 1935, Newcastle gained Kenton and parts of the parishes of West Brunton, East Denton, Fawdon, Longbenton. The most recent expansion in Newcastle's boundaries took place under the Local Government Act 1972 on 1 April 1974, when Newcastle became a metropolitan borough, also including the urban districts of Gosforth and Newburn, and the parishes of Brunswick, Dinnington, Hazlerigg, North Gosforth and Woolsington from the Castle Ward Rural District, and the village of Westerhope.
Meanwhile Northumberland County Council was formed under the Local Government Act 1888 and benefited from a dedicated meeting place when County Hall was completed in the Castle Garth area of Newcastle in 1910. Following the Local Government Act 1972 County Hall relocated to Morpeth in April 1981.
Twentieth century
In 1925 work began on a new high-level road bridge to span the Tyne Gorge between Newcastle and Gateshead. The capacity of the existing High-Level Bridge and Swing Bridge were being strained to the limit, and an additional bridge had been discussed for a long time. The contract was awarded to the Dorman Long Company and the bridge was finally opened by King George V in 1928. The road deck was 84 feet (26 m) above the river and was supported by a 531 feet (162 m) steel arch. The new Tyne Bridge quickly became a symbol for Newcastle and Tyneside, and remains so today.
During the Second World War, Newcastle was largely spared the horrors inflicted upon other British cities bombed during the Blitz. Although the armaments factories and shipyards along the River Tyne were targeted by the Luftwaffe, they largely escaped unscathed. Manors goods yard and railway terminal, to the east of the city centre, and the suburbs of Jesmond and Heaton suffered bombing during 1941. There were 141 deaths and 587 injuries, a relatively small figure compared to the casualties in other industrial centres of Britain.
In 1963 the city gained its own university, the University of Newcastle upon Tyne, by act of parliament. A School of Medicine and Surgery had been established in Newcastle in 1834. This eventually developed into a college of medicine attached to Durham University. A college of physical science was also founded and became Armstrong College in 1904. In 1934 the two colleges merged to become King's College, Durham. This remained as part of Durham University until the new university was created in 1963. In 1992 the city gained its second university when Newcastle Polytechnic was granted university status as Northumbria University.
Newcastle City Council moved to the new Newcastle Civic Centre in 1968.
As heavy industries declined in the second half of the 20th century, large sections of the city centre were demolished along with many areas of slum housing. The leading political figure in the city during the 1960s was T. Dan Smith who oversaw a massive building programme of highrise housing estates and authorised the demolition of a quarter of the Georgian Grainger Town to make way for Eldon Square Shopping Centre. Smith's control in Newcastle collapsed when it was exposed that he had used public contracts to advantage himself and his business associates and for a time Newcastle became a byword for civic corruption as depicted in the films Get Carter and Stormy Monday and in the television series Our Friends in the North. However, much of the historic Grainger Town area survived and was, for the most part, fully restored in the late 1990s. Northumberland Street, initially the A1, was gradually closed to traffic from the 1970s and completely pedestrianised by 1998.
In 1978 a new rapid transport system, the Metro, was built, linking the Tyneside area. The system opened in August 1980. A new bridge was built to carry the Metro across the river between Gateshead and Newcastle. This was the Queen Elizabeth II Bridge, commonly known as the Metro Bridge. Eventually the Metro system was extended to reach Newcastle Airport in 1991, and in 2002 the Metro system was extended to the nearby city of Sunderland.
As the 20th century progressed, trade on the Newcastle and Gateshead quaysides gradually declined, until by the 1980s both sides of the river were looking rather derelict. Shipping company offices had closed along with offices of firms related to shipping. There were also derelict warehouses lining the riverbank. Local government produced a master plan to re-develop the Newcastle quayside and this was begun in the 1990s. New offices, restaurants, bars and residential accommodation were built and the area has changed in the space of a few years into a vibrant area, partially returning the focus of Newcastle to the riverside, where it was in medieval times.
The Gateshead Millennium Bridge, a foot and cycle bridge, 26 feet (7.9 m) wide and 413 feet (126 m) long, was completed in 2001. The road deck is in the form of a curve and is supported by a steel arch. To allow ships to pass, the whole structure, both arch and road-deck, rotates on huge bearings at either end so that the road deck is lifted. The bridge can be said to open and shut like a human eye. It is an important addition to the re-developed quayside area, providing a vital link between the Newcastle and Gateshead quaysides.
Recent developments
Today the city is a vibrant centre for office and retail employment, but just a short distance away there are impoverished inner-city housing estates, in areas originally built to provide affordable housing for employees of the shipyards and other heavy industries that lined the River Tyne. In the 2010s Newcastle City Council began implementing plans to regenerate these depressed areas, such as those along the Ouseburn Valley.
Fifth and final stop on our winery tour by AAA Tours and Charters (Margaret River) - Gracetown. The town is well known for its many surfing spots. The Gracetown Grommets is a popular and historical junior surfing event. Extended Family Trip to Western Australia from 7 to 16 Jun 2016. (photo by Ben Cho)
This is Part 33 of 50 in an extended, slow-moving but still going series. Be warned: This is a long one.
You know how there are some people who get about halfway through a good book, but then get so eager to see how it turns out that they flip to the back and read the last chapter? I feel like those are the people who were settling the United States in the middle of the 19th century. Here you had a thriving collection of states filling up the eastern half of the continent, and then just as wagons started crossing the Mississippi River, somebody decides to jump ahead and smear a bunch of states on the West Coast. They weren't even waiting to make sure the eastern half of the country didn't split itself in two. They just wanted to sign up and get things settled NOW!
And so, here we have Oregon. And sure, California's already a thing just to the south, but you had to go a thousand miles to get to Oregon from any other established state in 1859. It was a slog, and a lot of the people who tried it died of dysentery along the way. But still, people came.
You May: Start the Trail
The earliest artifact of humanity ever found in Oregon is a pair of sandals that date to around 13,200 years ago, which is kind of funny when you consider the state's eventual relationship with shoes. So people were in Oregon early, though native groups over the the millennia tended to stay small and isolated by the state's rugged coastal mountains or wide river valleys or vast eastern deserts. At the time the Europeans showed up, the natives mostly lived either in little fishing villages along the Columbia or Willamette Rivers, or else they were plains people who wandered the dry grasslands over toward Idaho. But I'll save any specific discussions of these people for the Washington or Idaho stories.
You May: Look At the Map
It took a while for Europeans to get to Oregon, thanks to that big, 9,000-mile wall of continent in the way. As I said a couple of states ago, the Pacific Coast of California was remote, and Oregon perched on top is just that much farther. The entire Pacific Northwest is so remote, in fact, that it's one of the last significant pieces of coastal land to be mapped. And the funny thing is, nobody's sure who got to Oregon first.
The first guess is that it was Juan Rodríguez Cabrillo, that Spaniard who poked along the California coast in 1542 and then broke his leg stepping off a boat onto Catalina Island. But most scholars say Cabrillo only made it as far north as the Russian River, which is about 260 miles short of Oregon. So it probably wasn't him.
The next option didn't come along until 1592, when a Greek navigator piloted a ship sailed by a Spanish captain under a Spanish flag up the West Coast past all the way to Vancouver Island. The navigator's name was Ioannis Phokas, which history has Spanishized into Juan de Fuca, and for some reason he gets all the credit for this voyage even though he was just the navigator. But his life serves as a good illustration of the importance of primary sources, as it's entirely possible he never actually existed. He still wound up with a strait and a tectonic plate named after him, but most of that's up in Washington, though, so I'll save his story for that post.
Once Juan de Fuca passed Oregon by, the Spanish didn't do much with the place. As I've mentioned before, while the Spanish claimed the entire western third of North America based on various treaties going all the way back to Tordesillas in 1494, they kept their attention in North America on Mexico. A few Spanish priests trickled north into places that would become Texas and the desert Southwest, and there was that whole mission network in California, but they all stopped well short of Oregon. The Spanish ships that spent a couple of centuries sailing back and forth between Acapulco and Manilla usually stopped in California for supplies, but the only ships that ever went to Oregon did it by accident when they were blown off course, and most of them wrecked. So Oregon and Washington and British Columbia all stayed blank spots on everybody's map.
You May: Change Pace
What finally kicked things into gear for Euro-Oregon was this idea the Spanish got all of the sudden that other folks might want to go there, too, especially the Russians. And really, if you're an 18th century European empire starting to feel your age and are maybe worried you've gotten a little soft in the colonies, the last thing you want to see is a bunch of backward Russians encroaching on all those lands you've been holding onto for a rainy day. But that's just what started happening in the late 1740s. The Russians, who'd pushing across Siberia since the days of Peter the Great, finally figured out boats and hopped into Alaska. They kept moving along the coast over the next several decades, and by the 1770s, Russian fur trappers were taking excursions as far south as Oregon and California.
The Spanish response was to scramble a bunch of last-minute expeditions up the coast to fill in the maps they should have drawn up a century ago while reminding everyone that they'd been there first. One 1774 expedition charted a bunch of the more famous rocks on the Oregon coast. Another expedition in 1775 finally noticed the mouth of the Columbia River. But it all came too late. And Spain would soon have other worries anyway, once France went bankrupt and then insane right next door to the homeland, and that constant cycle of European war pushed everybody back home toward economic ruin.
So nobody said anything when famous British Supercaptain James Cook came along and drew his own map of the Pacific Northwest in 1778. Or when a few dozen British and American ships associated with the maritime fur trade started hunting otters along the coast in the 1780s. Or when Lewis and Clark finished up their great expedition on the Oregon side of the mouth of the Columbia River in 1805.
And then in 1810, the colony of New Spain decided it wanted to be its own thing and started fighting a five-year war to change its name to Mexico, and that was the end of Spain in Oregon. And, it turned out, all of North America. The Spanish stopped long enough on their way out in 1819 to sign a treaty surrendering Florida to the United States, and since they were already doing the paperwork, they went ahead and finally established the official border between Alta California and the Oregon Country at the 42nd parallel, where the Oregon-California border is today. Of course, Mexico wasn't thrilled with Spain for making that kind of deal after the Mexicans thought they'd already won their independence, but they eventually went along with it and signed a treaty of their own with the U.S. a decade later.
Meanwhile, Russia's flirtation with America's West Coast turned out to be a fad, and they'd eventually sign away whatever ambitions they might have had for anything south of Alaska with a couple of treaties in the 1820s. Which whittled the fight for ownership of the Pacific Northwest to two final players: the United Kingdom of Great Britain and Ireland, and the United States of America.
Getting Furs
The first big American push into Oregon came in 1811, when a bunch of trappers and traders working for John Jacob Astor's Pacific Fur Company followed the path Lewis and Clark had charted to the mouth of the Columbia River and built a little trading post fort, which they called Fort Astoria. But this turned out to be bad timing Astor. Tensions had been running high between the U.S. and Great Britain since the Revolution, and folks back east were itching for another war. There wasn't any American military presence in the Oregon Country, and Astor figured that Great Britain would seize all his assets as soon as war was declared. So early in 1812, he jumped all the guns and sold out to the North West Company, a British fur enterprise based in Montreal that had come into Oregon overland through Canada. But American trappers stayed in the area anyway, even as the War of 1812 raged back east.
But then a weird thing happened after the war. It turned out to be a draw that didn't solve much of anything, but the British were worn out from two decades of near-constant war in Europe, and the Americans so were relieved to have not lost the Great Lakes or the Lower Mississippi that they were thrilled to have a little peace. Nobody was in a mood to fight over Oregon, so in 1818, the two powers worked out a joint custody agreement known as the Anglo-American Convention. Since nobody could decide who should own what (the Americans would have liked a line drawn at the 49th parallel; Great Britain preferred a border along the Columbia River), they decided on a co-parenting scheme where the two nations would manage the entire disputed territory jointly.
And that sounds great, except you already know it was doomed. It lasted longer than you might guess, but little arguments started breaking out in the 1820s over who should get custody of Oregon on the weekends and whether the Columbia River would spend Christmas with the Thames or the Potomac, and tensions built through the 1830s and into the 1840s. And by the time the U.S. Presidential election of 1844 came along, the "Oregon Question" had blown up into one of those all-consuming, existential dilemmas of the sort that makes an American drunk on notions of Manifest Destiny ready to start shooting some red coats ... or whatever the Brits were wearing now.
It didn't bode well when that election brought James K. Polk to the Presidency. I've talked about Polk in a couple of these state origin stories and in a few other places over the years. Polk was the guy who goaded Mexico into starting the Mexican-American War so he'd have an excuse to go grab California, and he wasn't beyond using that same kind of bluster against the British over Oregon. In December of 1845, Polk went before Congress and anticipated John Wayne by at least a century, giving the British exactly one year to get out of town. Polk wanted everything west of the Continental Divide and south of 54°40′ north latitude. Or else.
"Or else" to Great Britain might have meant using the best navy in the world to blow up a lot of American boats and maybe retake the Great Lakes. But the powers that were in Britain had other things on their minds. The 1840s were a rough time in Europe, with a deepening economic depression affecting the entire continent. On top of that, the potato harvests in Ireland were starting to look pretty bleak, and the guys in Parliament figured they might need to buy some American wheat before long. So they suggested a compromise. "54°40′ north latitude is idiotic," they said. "That would mean we'd never get to build Vancouver, and people are going to love Vancouver. So how about we split the entire continent, everything from the Lake of the Woods in Minnesota all the way to the Pacific, along that 49th parallel line that you guys asked for 30 years ago and call it a day?" It turned out that Polk didn't really want to go to war anyway, and the 49th parallel sounded pretty sweet to him, so they all shook hands and signed the Oregon Treaty of 1846. And that's how we finally got that straight line that still defines the northern border of the United States west of the Great Lakes.
The Oregon Trail
The marketing folks for the Oregon Country had one big advantage in the first half of the 19th century. People were realizing a lot of the land Jefferson had bought from Napoleon was waterless territory unfit for the kind of agriculture a 19th century farmer could manage. But the Oregon Country? With all those green trees and fertile valleys and coastal Pacific Northwest rain? Oregon was just the thing for a nation full of expansionist-minded folks following Manifest Destiny dreams.
They started coming well before the thing was made legal, with all those fur trappers and mountain men followed by misfits and criminals and outcast religious sects, all the people who always seemed to be in the colonial bow shock. By the middle of the 1830s, enough people had marched to Oregon to beat a path that new settlers could pretend was an actual road, running from Independence, Missouri, up through future Kansas, Nebraska, Wyoming and beyond all the way to the Columbia River and the Willamette Valley. And by the time the British signed the Oregon Treaty and moved north, the road had become famous as the Oregon Trail. Over the next few decades, nearly a half-million settlers would brave the broken wagon wheels and bad weather and bouts of dysentery or measles that plagued that road, all for the hope of settling in Oregon's Willamette Valley.
In 1843, these settlers put together their own representative legislature and assembled their own legal code, called the Organic Laws. One of these Organic Laws offered free land to any white people who wanted to follow the Oregon Trail. In 1846, after the treaty made Oregon an official U.S. territory, those laws became the basis of a new constitution. In 1850, an elected delegate from Oregon named Samuel Thurston talked the U.S. Congress into passing the Donation Land Claim Act, which legitimized the offer of free land and made it federal law. Any single white man who followed the trail would get 320 acres, free of charge. Any white married couple would get twice that. And any potential settler of color would get ... well, kicked out. Because while Oregon had no interest in slavery -- everybody knew Oregon was going to be a free state -- it wasn't about to let itself become some refuge for formal slaves.
But there were plenty of white people following the trail to the Columbia and the Willamette and the Oregon coast as the 1850s drew to a close, and they'd already started platting out Portland. It was enough that on February 14, 1859, Oregon was admitted to the Union as the 33rd state.
Considering where we were on the slavery issue in 1859, it's surprising that nobody back East kicked up a snit about the admission of another free state, though I suspect that Oregon's position on the issue had been set long enough before that nobody thought it was worth the argument. But that does bring our total up to 18 free states versus 15 slave states. Henry Clay's numerical balance was officially dead. The next time I write one of these, things are going to get bloody.