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Founded in 1906, Mesa Verde National Park was created to conserve and protect the Ancestral Puebloan archaeological sites and cliff dwellings within the present-day park on the sides and top of a large tree-covered cuesta, known as Mesa Verde, that rises approximately 1,500 feet (785 meters) above the surrounding canyons and valleys, with rugged canyons cutting through the cuesta, lined with sandstone cliffs and ledges.
The area was inhabited by indigenous people for thousands of years prior to the rise of the Ancestral Puebloan culture, whom developed villages and farmsteads within what is today Mesa Verde National Park beginning around the year 750, with the structures built by the Ancestral Puebloans growing in complexity and durability, especially due to contact with the nearby culture centered around Chaco Canyon. The famous cliff dwellings for which the area is famous, however, were built between approximately 1020 and 1260, especially after a major drought in the region between 1130 and 1180, which led to a major migration of people from Chaco Canyon to Mesa Verde. The people of Chaco Canyon brought their culture, construction techniques, and goods with them, which is evident at archaeological sites on the cuesta.
The area began to depopulate between 1260 and 1285 due to environmental conditions becoming less favorable, with the people of Mesa Verde moving to the lowlands of what is today New Mexico and Arizona, with many founding or joining Pueblo settlements in these regions that still exist today. The stone houses were left to the elements, and were left uninhabited, only remembered by the descendants of the Ancestral Puebloans and the other indigenous groups who called the area home, most notably the Utes.
The ancient ruins were discovered by European-Americans in 1873, and were documented between 1875 and 1888, with various cliff dwellings and archaeological sites being relatively well-preserved and recognizable to explorers, archaeologists, and scientists whom visited the modern-day park. However, the removal of artifacts from the cuesta became a major concern, and efforts began in 1889 to protect the area as a National Park.
The park covers an area of 82 square miles (212 square kilometers), and features multiple Ancestral Puebloan and other indigenous archaeological sites, and was taken from the Ute people, with land being taken from the Utes after the establishment of the park to expand its borders. The park long struggled with proper interpretation and inclusion of the voices of the Puebloan people, whose ancestors built the ancient dwellings and lived at what are today archaeological sites, with work presently ongoing to redress these issues.
The ruins at the park underwent reconstitution and stabilization between 1908 and 1922, with extensive work being done on Spruce Tree House, Cliff Palace, and Sun Temple. Further work was carried out by the New Deal-era Civilian Conservation Corps starting in 1932 and extending through World War II, which included the construction of various park facilities for visitors and staff, and constructing roads atop the cuesta. The Wetherill Mesa ruins, meanwhile, were stabilized with work being carried out between 1958 and 1965, coinciding with the construction of the Far View accommodations atop the cuesta to the east.
The park today features a modern entrance road from US Highway 160, which climbs up the rugged slopes at the north end of the park to the top of the cuesta, stretching across the top of the cuesta to the south, where it connects to various roads that allow visitors to access the overlooks and trails for various cliff dwellings and archaeological sites on Chapin Mesa and Wetherill Mesa. Two areas of tourist accommodation also exist at Far View in the northern section of the park, and the administrative district at Spruce Tree Point at the southern end of the park.
The park was listed on the National Register of Historic Places in 1966, and was designated a UNESCO World Heritage Site in 1978. Today, the park sees over half a million visitors annually, and continues to preserve and maintain the ancient structures built by the Ancestral Puebloans.
Founded in 1906, Mesa Verde National Park was created to conserve and protect the Ancestral Puebloan archaeological sites and cliff dwellings within the present-day park on the sides and top of a large tree-covered cuesta, known as Mesa Verde, that rises approximately 1,500 feet (785 meters) above the surrounding canyons and valleys, with rugged canyons cutting through the cuesta, lined with sandstone cliffs and ledges.
The area was inhabited by indigenous people for thousands of years prior to the rise of the Ancestral Puebloan culture, whom developed villages and farmsteads within what is today Mesa Verde National Park beginning around the year 750, with the structures built by the Ancestral Puebloans growing in complexity and durability, especially due to contact with the nearby culture centered around Chaco Canyon. The famous cliff dwellings for which the area is famous, however, were built between approximately 1020 and 1260, especially after a major drought in the region between 1130 and 1180, which led to a major migration of people from Chaco Canyon to Mesa Verde. The people of Chaco Canyon brought their culture, construction techniques, and goods with them, which is evident at archaeological sites on the cuesta.
The area began to depopulate between 1260 and 1285 due to environmental conditions becoming less favorable, with the people of Mesa Verde moving to the lowlands of what is today New Mexico and Arizona, with many founding or joining Pueblo settlements in these regions that still exist today. The stone houses were left to the elements, and were left uninhabited, only remembered by the descendants of the Ancestral Puebloans and the other indigenous groups who called the area home, most notably the Utes.
The ancient ruins were discovered by European-Americans in 1873, and were documented between 1875 and 1888, with various cliff dwellings and archaeological sites being relatively well-preserved and recognizable to explorers, archaeologists, and scientists whom visited the modern-day park. However, the removal of artifacts from the cuesta became a major concern, and efforts began in 1889 to protect the area as a National Park.
The park covers an area of 82 square miles (212 square kilometers), and features multiple Ancestral Puebloan and other indigenous archaeological sites, and was taken from the Ute people, with land being taken from the Utes after the establishment of the park to expand its borders. The park long struggled with proper interpretation and inclusion of the voices of the Puebloan people, whose ancestors built the ancient dwellings and lived at what are today archaeological sites, with work presently ongoing to redress these issues.
The ruins at the park underwent reconstitution and stabilization between 1908 and 1922, with extensive work being done on Spruce Tree House, Cliff Palace, and Sun Temple. Further work was carried out by the New Deal-era Civilian Conservation Corps starting in 1932 and extending through World War II, which included the construction of various park facilities for visitors and staff, and constructing roads atop the cuesta. The Wetherill Mesa ruins, meanwhile, were stabilized with work being carried out between 1958 and 1965, coinciding with the construction of the Far View accommodations atop the cuesta to the east.
The park today features a modern entrance road from US Highway 160, which climbs up the rugged slopes at the north end of the park to the top of the cuesta, stretching across the top of the cuesta to the south, where it connects to various roads that allow visitors to access the overlooks and trails for various cliff dwellings and archaeological sites on Chapin Mesa and Wetherill Mesa. Two areas of tourist accommodation also exist at Far View in the northern section of the park, and the administrative district at Spruce Tree Point at the southern end of the park.
The park was listed on the National Register of Historic Places in 1966, and was designated a UNESCO World Heritage Site in 1978. Today, the park sees over half a million visitors annually, and continues to preserve and maintain the ancient structures built by the Ancestral Puebloans.
I managed to mount the surge protector out of the way. It holds pretty good on the flimsy back wall.
(HGM 493 M, Heisey Glass Museum, Newark, Ohio, USA)
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"355 Quator" is the designation for a specific glass product design made in Newark, Ohio by the Heisey Glass Company (1896 to 1957). Heisey glass designs are called "patterns". Pattern designations include a number (not necessarily consecutively numbered during the history of the glass factory) and a name. Some pattern names were given by the Heisey company, while others were given by Heisey glass researchers.
"Conserve dish" refers to a dish for jams composed of a mix of different fruits.
The source of silica for Heisey glass is apparently undocumented, but was possibly a sandstone deposit in the Glassrock area (Glenford & Chalfants area) of Perry County, Ohio (if anyone can provide verfication of this, please inform me). Quarries in the area targeted the Pennsylvanian-aged Massillon Sandstone (Pottsville Group) and processed it into glass sand suitable for glass making.
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From museum signage:
Augustus H. Heisey (1842-1922) emigrated from Germany with his family in 1843. They settled in Merrittown, Pennsylvania and after graduation from the Merrittown Academy, he worked for a short time in the printing business.
In 1861, he began his life-long career in the glass industry by taking a job as a clerk with the King Glass Company of Pittsburgh. After a stint in the Union Army, Heisey joined the Ripley Glass Company as a salesman. It was there that he earned his reputation of "the best glass salesman on the road".
In 1870, Heisey married Susan Duncan, daughter of George Duncan, then part-owner of the Ripley Company and later full owner, at which time he changed its name to George Duncan & Sons. A year later, he deeded a quarter interest to each of his two children. A few years after his death, A.H. Heisey and James Duncan became sole owners. In 1891, the company joined the U.S. Glass Company to escape its financial difficulties. Heisey was the commercial manager.
Heisey began to formulate plans for his own glass company in 1893. He chose Newark, Ohio because there was an abundance of natural gas nearby and, due to the efforts of the Newark Board of Trade, there was plenty of low cost labor available. Construction of the factory at 301 Oakwood Avenue began in 1895 and it opened in April of 1896 with one sixteen-pot furnace. In its heyday, the factory had three furnaces and employed nearly seven hundred people. There was a great demand for the fine glass and Heisey sold it all over the world.
The production in the early years was confined to pressed ware, in the style of imitation cut glass. The company also dealt extensively with hotel barware. By the late 1890s, Heisey revived the colonial patterns with flutes, scallops, and panels which had been so popular decades earlier. These were so well accepted that from that time on, at least one colonial line was made continuously until the factory closed.
A.H. Heisey's name appears on many different design patents including some when he was with George Duncan & Sons. Heisey patterns that he was named the designer include 1225 Plain Band, 305 Punty and Diamond Point, and 1776 Kalonyal.
Other innovations instituted by A.H. Heisey were the pioneering in advertising glassware in magazines nationally, starting as early as 1910 and the first glass company to make fancy pressed stems. That idea caught on quickly and most hand-wrought stemware is made in this manner, even now.
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Info. at:
en.wikipedia.org/wiki/Heisey_Glass_Company
and
The packaging to jam ratio is quite steep, ancient hands have to resort to teeth or a friendly waitress to tear open the darned thing, and, if the manufacturer seals the bloody seal below rather than above the tear strip one is still buggered. Portion control gone made I tell ‘ee. Back in olden times one might have had a pocket knife about one but these days…. I suppose I was just grouchy about it because in talking to the waitress I got brain-fog and spoke of condiments rather than conserves which error kept coming back to me throughout the morning. Pfft!
CONSERVER at Banavie 24th June 2016
Name:
Conserver
MMSI:235009391 [UK]
Callsign:MBKY5
Speed/Dir:8 kts / 34° NE
Status:Default (15)
Dest:Unknown
ETA:unknown
Type:Local Vessel (57)
Size:18m x 5m x 0m
Received:11:23:46 28 Jun 16 BST
Founded in 1906, Mesa Verde National Park was created to conserve and protect the Ancestral Puebloan archaeological sites and cliff dwellings within the present-day park on the sides and top of a large tree-covered cuesta, known as Mesa Verde, that rises approximately 1,500 feet (785 meters) above the surrounding canyons and valleys, with rugged canyons cutting through the cuesta, lined with sandstone cliffs and ledges.
The area was inhabited by indigenous people for thousands of years prior to the rise of the Ancestral Puebloan culture, whom developed villages and farmsteads within what is today Mesa Verde National Park beginning around the year 750, with the structures built by the Ancestral Puebloans growing in complexity and durability, especially due to contact with the nearby culture centered around Chaco Canyon. The famous cliff dwellings for which the area is famous, however, were built between approximately 1020 and 1260, especially after a major drought in the region between 1130 and 1180, which led to a major migration of people from Chaco Canyon to Mesa Verde. The people of Chaco Canyon brought their culture, construction techniques, and goods with them, which is evident at archaeological sites on the cuesta.
The area began to depopulate between 1260 and 1285 due to environmental conditions becoming less favorable, with the people of Mesa Verde moving to the lowlands of what is today New Mexico and Arizona, with many founding or joining Pueblo settlements in these regions that still exist today. The stone houses were left to the elements, and were left uninhabited, only remembered by the descendants of the Ancestral Puebloans and the other indigenous groups who called the area home, most notably the Utes.
The ancient ruins were discovered by European-Americans in 1873, and were documented between 1875 and 1888, with various cliff dwellings and archaeological sites being relatively well-preserved and recognizable to explorers, archaeologists, and scientists whom visited the modern-day park. However, the removal of artifacts from the cuesta became a major concern, and efforts began in 1889 to protect the area as a National Park.
The park covers an area of 82 square miles (212 square kilometers), and features multiple Ancestral Puebloan and other indigenous archaeological sites, and was taken from the Ute people, with land being taken from the Utes after the establishment of the park to expand its borders. The park long struggled with proper interpretation and inclusion of the voices of the Puebloan people, whose ancestors built the ancient dwellings and lived at what are today archaeological sites, with work presently ongoing to redress these issues.
The ruins at the park underwent reconstitution and stabilization between 1908 and 1922, with extensive work being done on Spruce Tree House, Cliff Palace, and Sun Temple. Further work was carried out by the New Deal-era Civilian Conservation Corps starting in 1932 and extending through World War II, which included the construction of various park facilities for visitors and staff, and constructing roads atop the cuesta. The Wetherill Mesa ruins, meanwhile, were stabilized with work being carried out between 1958 and 1965, coinciding with the construction of the Far View accommodations atop the cuesta to the east.
The park today features a modern entrance road from US Highway 160, which climbs up the rugged slopes at the north end of the park to the top of the cuesta, stretching across the top of the cuesta to the south, where it connects to various roads that allow visitors to access the overlooks and trails for various cliff dwellings and archaeological sites on Chapin Mesa and Wetherill Mesa. Two areas of tourist accommodation also exist at Far View in the northern section of the park, and the administrative district at Spruce Tree Point at the southern end of the park.
The park was listed on the National Register of Historic Places in 1966, and was designated a UNESCO World Heritage Site in 1978. Today, the park sees over half a million visitors annually, and continues to preserve and maintain the ancient structures built by the Ancestral Puebloans.
Shots taken during the removal of the 18th century glass in the east window for cleaning and repair by Norgrove Studios in 2017.
St Mary's at Preston on Stour is a gem of a church. The tower and nave are mostly the original late medieval work but with significant remodeling in 1752-64 (by Edward Woodward of Chipping Campden) The chancel was entirely rebuilt at this time, though the effect is surprisingly homogeneous.
Inside the chancel are several wall-mounted monuments of 17th & 18th century date, but it is the stained glass which takes centre stage, with a magnificent collection of Continental roundels in the east window, and two superb and extremely unusual side windows by William Price from the 1750s, with standing saints flanked by an eccentric collection of portrait medallions.
There is further notable glass in the west window under the tower, which seems to be indigenous work of 15th & 16th century dates, possibly original to the church, though sadly difficult to see without special access to the bell ringing chamber.
Founded in 1906, Mesa Verde National Park was created to conserve and protect the Ancestral Puebloan archaeological sites and cliff dwellings within the present-day park on the sides and top of a large tree-covered cuesta, known as Mesa Verde, that rises approximately 1,500 feet (785 meters) above the surrounding canyons and valleys, with rugged canyons cutting through the cuesta, lined with sandstone cliffs and ledges.
The area was inhabited by indigenous people for thousands of years prior to the rise of the Ancestral Puebloan culture, whom developed villages and farmsteads within what is today Mesa Verde National Park beginning around the year 750, with the structures built by the Ancestral Puebloans growing in complexity and durability, especially due to contact with the nearby culture centered around Chaco Canyon. The famous cliff dwellings for which the area is famous, however, were built between approximately 1020 and 1260, especially after a major drought in the region between 1130 and 1180, which led to a major migration of people from Chaco Canyon to Mesa Verde. The people of Chaco Canyon brought their culture, construction techniques, and goods with them, which is evident at archaeological sites on the cuesta.
The area began to depopulate between 1260 and 1285 due to environmental conditions becoming less favorable, with the people of Mesa Verde moving to the lowlands of what is today New Mexico and Arizona, with many founding or joining Pueblo settlements in these regions that still exist today. The stone houses were left to the elements, and were left uninhabited, only remembered by the descendants of the Ancestral Puebloans and the other indigenous groups who called the area home, most notably the Utes.
The ancient ruins were discovered by European-Americans in 1873, and were documented between 1875 and 1888, with various cliff dwellings and archaeological sites being relatively well-preserved and recognizable to explorers, archaeologists, and scientists whom visited the modern-day park. However, the removal of artifacts from the cuesta became a major concern, and efforts began in 1889 to protect the area as a National Park.
The park covers an area of 82 square miles (212 square kilometers), and features multiple Ancestral Puebloan and other indigenous archaeological sites, and was taken from the Ute people, with land being taken from the Utes after the establishment of the park to expand its borders. The park long struggled with proper interpretation and inclusion of the voices of the Puebloan people, whose ancestors built the ancient dwellings and lived at what are today archaeological sites, with work presently ongoing to redress these issues.
The ruins at the park underwent reconstitution and stabilization between 1908 and 1922, with extensive work being done on Spruce Tree House, Cliff Palace, and Sun Temple. Further work was carried out by the New Deal-era Civilian Conservation Corps starting in 1932 and extending through World War II, which included the construction of various park facilities for visitors and staff, and constructing roads atop the cuesta. The Wetherill Mesa ruins, meanwhile, were stabilized with work being carried out between 1958 and 1965, coinciding with the construction of the Far View accommodations atop the cuesta to the east.
The park today features a modern entrance road from US Highway 160, which climbs up the rugged slopes at the north end of the park to the top of the cuesta, stretching across the top of the cuesta to the south, where it connects to various roads that allow visitors to access the overlooks and trails for various cliff dwellings and archaeological sites on Chapin Mesa and Wetherill Mesa. Two areas of tourist accommodation also exist at Far View in the northern section of the park, and the administrative district at Spruce Tree Point at the southern end of the park.
The park was listed on the National Register of Historic Places in 1966, and was designated a UNESCO World Heritage Site in 1978. Today, the park sees over half a million visitors annually, and continues to preserve and maintain the ancient structures built by the Ancestral Puebloans.
Conserving Dryland Biodiversity: supporting the environmental services of mobile pastoralists and other indigenous peoples.
We all wear down.....This center section of the almost 100 year old Lamberton Conservatory is being reconstructed due to extreme wear and tear. It's amazing how they are able to keep the rest of the place open. Many huge palm trees have had to be taken out and stored elsewhere. You can see the bases of the 2 small waterfall, left and (distant) right center. It looks like they've had to cut down one palm in the right foreground.
NO INVITES OR ICONS PLEASE