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MONTGOMERY, Alabama (March 23, 2016) – Against the backdrop of the Alabama River at the Union Station Train Shed, 300 conservation district supervisors, conservation partners, and students gathered to hear the Alabama Soil & Water Conservation Committee (SWCC) launch a new initiative to continue its mission of conserving Alabama’s natural resources: Conserve Alabama.
Visit conservealabama.gov to learn more about the campaign.
44OR249-21518-AH
Cooking hook which hung from a hearth crane or trammel and was used to hang pots and pans over an open fire.
Kumquat Marmalade, confiture, citrus, fortunella, kumquat, 金橘, 桔子, fruit preserves, conserve, jam, canning, pectin
Conserving the stonework at Silves castle. I couldn't see what she was doing, but it was certainly painstaking.
At this seminar, Susmita Dasgupta (World Bank) discussed how her research develops and applies a spatial econometric model that links road upgrading to forest clearing and biodiversity loss in the moist tropical forests of Bolivia, Cameroon and Myanmar.
Details at iems.ust.hk/forests
El 22 de desembre de 2022 el grup de l'espai de cuina sostenible i memòria, Conserves Litorals, va visitar el Moll del Rellotge i la llotja de la Barceloneta per conèixer el funcionament de la llotja i la flota.
Kumquat Marmalade, confiture, citrus, fortunella, kumquat, 金橘, 桔子, fruit preserves, conserve, jam, canning, pectin
Yay! My grocery store came out with reusable bags. They are sturdy and extra wide. I'm helping one step at a time.
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.
Here is the conserved and restored water feature, a former font or bird bath? Enough survived to allow replacement columns to be accurately made. Compare to the previous photo prior to restoration.
Kickstarter supporters of the Lark cookbook are getting roughcuts of recipes. This conserve is part of a Meyer lemon parfait
To conserve the foothill yellow-legged frog (Rana boylii), a wildlife crew on the Tahoe National Forest surveys for the frogs and their egg masses in a stream bed where illegal off-highway driving occurs, further damaging this ecosystem impacted by the legacy of historical hydraulic mining. The egg masses are at risk of being run over, so the crew looks for signs of tire tracks, like this one, to determine what egg masses need to be moved to a safer part of the stream. There are many places in the forest to enjoy off-high way driving, but sensitive aquatic ecosystems like this one are not the place. Tahoe National Forest, April 24, 2020. (USDA Forest Service photo by Lauren Hoyle)
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.
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.
That’s what we’re all about at Huron Pines. Visit www.huronpines.org/ to learn more.
Photo credit: David Smith