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Nebraska researchers are collaborating with teams in Illinois and at Princeton to aid crop producers to improve the process of deciding whether or not to irrigate. This project, supported by the USDA, is aimed at saving both financial and water resources. ow.ly/fUId50ydcpB
- @RonnieDGreen on Twitter, Feb. 4, 2020
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.
My contribution to "going green" - I will not be able to make it to the Saturday meeting. Sorry I'll miss all the great photos.
Modern skyscrapers form a contrasting backdrop to the old conserved shophouses in Chinatown, Singapore at dusk.
Fort Stewart U.S. Army Medical Department Activity, Warrior Transition Battalion and Dental Health Activity inducted 16 Non-Comissioned Officers into the ranks of the NCO Corps during the NCO Induction Ceremony at Winn Army Community Hospital.
#winnarmycommunityhospital #fortstewart #soldiers #passageintothecorpofthenco #oneteamonepurpose #ncoinductionceremony #backboneofthearmy #ncocorps
One Team. One Purpose. Conserving the fighting strength since 1775.
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This slogan was on all the benches along the pier of San Cristóbal. Who wouldn't want to help conserve an amazing animal like this lazy sea lion!?
Conserved motif analysis of Brachypodium MADS-box proteins according to the phylogenetic relationship.Each motif is represented by a number in a colored box. Motif 1 is the MADS-box domain; 2 and 3 are two different components of the K domain; 4 and 20 are I domains; 6 is a 129 amino acid MADS-box domain; 8 is a structure; 5, 7 and 9?19 are unidentified regions. Box length corresponds to motif length. Specific lengths, locations and p-values of each motif can be found in Table S4 in File S1.
Great Sand Dunes National Park and Preserve is a national park of the United States that conserves an area of large sand dunes on the eastern edge of the San Luis Valley, and an adjacent national preserve in the Sangre de Cristo Range, in south-central Colorado.[5] The park was originally designated Great Sand Dunes National Monument on March 17, 1932, by President Herbert Hoover. The original boundaries protected an area of 35,528 acres (55.5 sq mi; 143.8 km2). A boundary change and redesignation as a national park and preserve was authorized on November 22, 2000, and then established on September 24, 2004. The park encompasses 107,342 acres (167.7 sq mi; 434.4 km2) while the preserve protects an additional 41,686 acres (65.1 sq mi; 168.7 km2) for a total of 149,028 acres (232.9 sq mi; 603.1 km2). The recreational visitor total was 527,546 in 2019.
The park contains the tallest sand dunes in North America, up to 750 feet (230 m) tall. The dunes cover an area of about 30 sq mi (78 km2) and are estimated to contain over 1.2 cubic miles (5 billion cubic metres) of sand. Sediments from the surrounding mountains filled the valley over geologic time periods. After lakes within the valley receded, exposed sand was blown by the predominant southwest winds toward the Sangre de Cristos, eventually forming the dune field over an estimated tens of thousands of years.[9] The four primary components of the Great Sand Dunes system are the mountain watershed, the dune field, the sand sheet, and the sabkha. Ecosystems within the mountain watershed include alpine tundra, subalpine forests, montane woodlands, and riparian zones.
Evidence of human habitation in the San Luis Valley dates back about 11,000 years. The first historic peoples to inhabit the area were the Southern Ute Tribe; Apaches and Navajo also have cultural connections in the area. In the late 17th century, Diego de Vargas, a Spanish governor of Santa Fe de Nuevo México, became the first European on record to enter the San Luis Valley. Juan Bautista de Anza, Zebulon Pike, John C. Frémont, and John Gunnison all traveled through and explored parts of the region in the 18th and 19th centuries. The explorers were soon followed by settlers who ranched, farmed, and mined in the valley starting in the late 19th century. The park was first established as a national monument in 1932 to protect it from gold mining and the potential of a concrete manufacturing business.
Visitors must walk across the wide and shallow Medano Creek to reach the dunes in spring and summer. The creek typically has a peak flow from late May to early June. From July to April, it is usually no more than a few inches deep, if there is any water at all. Hiking is permitted throughout the dunes with the warning that the sand surface temperature may reach 150 °F (66 °C) in summer. Sandboarding and sandsledding are popular activities, both done on specially designed equipment that can be rented just outside the park entrance or in Alamosa. Visitors with street-legal four-wheel drive vehicles may continue past the end of the park's main road to Medano Pass on 22 miles (35 km) of unpaved road, crossing the stream bed of Medano Creek nine times and traversing 4 miles (6.4 km) of deep sand.
Hunting is permitted in the preserve in the autumn, but prohibited within national park boundaries at all times. The preserve encompasses nearly all of the mountainous areas north and east of the dune field, up to the ridgeline of the Sangre de Cristos.
ALC conserved 26 acres at the Big Muddy Boat Launch, creating a safe, publicly accessible launch area to the Big Muddy River with convenient access from Highway 3. From the launch boaters can navigate 4 miles to the west to the Mississippi River, or 4 miles to the east into one of the most remote sections of the Shawnee National Forest.
Conserve seu medo
Mantenha ele aceso
Se você não teme
Se você não ama
Vai acabar cedo
Esteja atento
Ao rumo da História
Mantenha em segredo
Mas mantenha viva
Sua paranóia
Conserve seu medo
Mas sempre ficando
Sem medo de nada
Porque dessa vida
De qualquer maneira
Não se leva nada
E ande pra frente
Olhando pro lado
Se entregue a quem ama
Na rua ou na cama
Mas tenha cuidado
Conserve seu medo
Mas sempre ficando
Sem medo de nada
Porque dessa vida
De qualquer maneira
Não se leva nada
E ande pra frente
Olhando pro lado
Se entregue a quem ama
Na rua ou na cama
Mas tenha cuidado
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.
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Conserved, but not restored. The carriage is a conserved (not restored) 1st class carriage from the late 1800s.
National Railway Museum, York
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.