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Exit 40, Chavez Siding Rd, I-19 Southbound


Bild von Ken Lund
Interstate 19 (I-19) is an intrastate Interstate Highway located entirely within the state of Arizona. I-19 runs from Nogales, at the Mexican border to Tucson, at Interstate 10.

In Nogales, Arizona, the southern terminus of I-19 is adjacent to the international port of entry, and southbound travelers can continue into Nogales, Sonora, Mexico, and connect with the northern terminus of Mexico Federal Highway 15. I-19 initially heads west through Nogales before making the turn to head north. It interchanges with two other state highways near the southern end of the route, SR 189 at exit 4 and SR 289 at exit 12. As I-19 enters the Tucson city limits, it has an interchange at SR 86 at exit 99 before reaching its northern terminus at a junction with I-10.

Nearly the entire route of I-19 follows, or is adjacent to, the former routing of U.S. Route 89 and the Santa Cruz River, which flows northward from Mexico, through Tucson and eventually disperses into the desert between Tucson and Phoenix. Most of the time, much of the river is dry, but heavy storms can cause it to overflow its banks.

The official "completion" date of the I-19 segment between Tucson (km 100) and Green Valley, Arizona (actually Helmet Peak Road at km 75) was February 12, 1972. A 1978 Project Report for the Arizona Department of Transportation lists entire I-19 project as "completed," which includes segments between Green Valley and Nogales, Arizona.

Interstate 19 is unique amongst US Interstates, because signed distances are given in meters (hundreds or thousands as distance-to-exit indications) or kilometers (as distance-to-destination indications), and not miles. Speed limit signs give speeds in miles-per-hour, however. According to the Arizona Department of Transportation (ADOT), metric signage was originally placed because of the "metric system push" in the United States at the time of the original construction of the highway.[citation needed]

I-19 had originally been signed as it was constructed, in a series of small signing contracts which used customary units.[3] In 1980, Arizona DOT awarded a single contract to install new signs which used metric units, to overlay English-unit expressions on some existing signs with metric-unit expressions, to install kilometerposts, and to provide bilingual signing in select locations. The signing scheme used in 1980 provided explicit units on advance guide signs, but not on interchange sequence signs or post-interchange confirmation (distance) signs. The expressions on advance guide signs were of the form "2 km" for distances over 1 km and "500 m" for distances under 1 km, with no provision for fractional kilometrages. On advance guide signs, the metric unit expressions "km" and "m" were placed on the baseline where "MILES" would otherwise have gone, but were sized so that their lowercase loop height matched the uppercase letter height of "MILES" on customary-unit signs. The exception was a handful of advance guide signs for the SR 86 Ajo Way exit, which used "KM" (in uppercase, contrary to SI nomenclature) on the same baseline and at the same letter height as "MILES." The 1980 signing plans also provided design details for speed limit and advisory speed signs using metric units, with the limit values enclosed in a red circle on the speed limit sign and a black circle on the yellow-background advisory signs. These speed signs all had explicit units, with "km/h" below the circle enclosing the limit value. However, the advisory signs were cancelled by change order and not installed. Had the metric speed limit sign been installed, the signed speed limit on I-19 would have been 88 km/h, which is a close soft-conversion of the then-existing 55 MPH "double nickel" national maximum speed limit. Information signs, to three distinct designs, were also placed at various locations on or near I-19 to advise motorists that the highway was signed in metric. Notwithstanding the metric legends, the signing plans were dimensioned entirely in feet and inches.[4]

In 1999, Arizona DOT awarded two contracts (administered as a single construction project) to renew signing along the full length of I-19. The general approach toward metric signing differed from that taken in 1980. Explicit units were given not just on advance guide signs, but also on interchange sequence signs, post-interchange confirmation signs, and community interchange signs (the last-listed had not been used in 1980). On the distance signs, "km" appeared after each kilometrage except when one or more of the distances was a fractional kilometrage. In such cases all the distances were given in meters with "meters" (written out in full, not "m") after each distance value. On distance signs in general, "km" or "meters" appeared on the same baseline and with the same letter height as the distance values, while advance guide signs were formatted as in 1980. Since a typical Arizona DOT freeway guide sign rehabilitation contract also replaces surface road signing near those roads’ interchanges with the freeway, metric-unit signs also appeared on local roads near I-19, giving distances in kilometers to tourist attractions such as Mission San Xavier del Bac. As was the case in 1980, the signing plans were dimensioned in feet and inches.[5] However, a number of signs near the Valencia Road interchange were replaced or amended when it was converted from a partial cloverleaf to a SPUI in 2000. One of these signs has a fractional kilometrage greater than 1 km, rendered as "1500 m," while others use "m" rather than "meters" as the unit expression. Metric unit expressions on the advance guide signs installed or modified as part of this contract appear on the same baseline as the metric values, rather than on a raised baseline as on other I-19 advance guide signs. Again, the plans were dimensioned in feet and inches.[6]

Citing motorist confusion arising from the metric signs on I-19, Arizona DOT’s Tucson district announced that new signs on I-19 would use United States customary units. To avoid the cost of replacing the metric signs all at once, signs would be replaced in specific areas of the freeway during construction projects in those areas.[7] New signs were put into place between Exit 99 (Ajo Way) and Exit 101 (Interstate 10) in 2004 after the completion of the new Interstate 10–Interstate 19 interchange.

A recent reconstruction project at the Interstate’s northern terminus with Interstate 10 in Tucson, Arizona (at the interchange commonly called "The Crossing") was begun in 2002 and completed in August 2004.

en.wikipedia.org/wiki/Interstate_19

Nogales Exits, I-19 Southbound, Nogales, Arizona


Bild von Ken Lund
Interstate 19 (I-19) is an intrastate Interstate Highway located entirely within the state of Arizona. I-19 runs from Nogales, at the Mexican border to Tucson, at Interstate 10.

In Nogales, Arizona, the southern terminus of I-19 is adjacent to the international port of entry, and southbound travelers can continue into Nogales, Sonora, Mexico, and connect with the northern terminus of Mexico Federal Highway 15. I-19 initially heads west through Nogales before making the turn to head north. It interchanges with two other state highways near the southern end of the route, SR 189 at exit 4 and SR 289 at exit 12. As I-19 enters the Tucson city limits, it has an interchange at SR 86 at exit 99 before reaching its northern terminus at a junction with I-10.

Nearly the entire route of I-19 follows, or is adjacent to, the former routing of U.S. Route 89 and the Santa Cruz River, which flows northward from Mexico, through Tucson and eventually disperses into the desert between Tucson and Phoenix. Most of the time, much of the river is dry, but heavy storms can cause it to overflow its banks.

The official "completion" date of the I-19 segment between Tucson (km 100) and Green Valley, Arizona (actually Helmet Peak Road at km 75) was February 12, 1972. A 1978 Project Report for the Arizona Department of Transportation lists entire I-19 project as "completed," which includes segments between Green Valley and Nogales, Arizona.

Interstate 19 is unique amongst US Interstates, because signed distances are given in meters (hundreds or thousands as distance-to-exit indications) or kilometers (as distance-to-destination indications), and not miles. Speed limit signs give speeds in miles-per-hour, however. According to the Arizona Department of Transportation (ADOT), metric signage was originally placed because of the "metric system push" in the United States at the time of the original construction of the highway.[citation needed]

I-19 had originally been signed as it was constructed, in a series of small signing contracts which used customary units.[3] In 1980, Arizona DOT awarded a single contract to install new signs which used metric units, to overlay English-unit expressions on some existing signs with metric-unit expressions, to install kilometerposts, and to provide bilingual signing in select locations. The signing scheme used in 1980 provided explicit units on advance guide signs, but not on interchange sequence signs or post-interchange confirmation (distance) signs. The expressions on advance guide signs were of the form "2 km" for distances over 1 km and "500 m" for distances under 1 km, with no provision for fractional kilometrages. On advance guide signs, the metric unit expressions "km" and "m" were placed on the baseline where "MILES" would otherwise have gone, but were sized so that their lowercase loop height matched the uppercase letter height of "MILES" on customary-unit signs. The exception was a handful of advance guide signs for the SR 86 Ajo Way exit, which used "KM" (in uppercase, contrary to SI nomenclature) on the same baseline and at the same letter height as "MILES." The 1980 signing plans also provided design details for speed limit and advisory speed signs using metric units, with the limit values enclosed in a red circle on the speed limit sign and a black circle on the yellow-background advisory signs. These speed signs all had explicit units, with "km/h" below the circle enclosing the limit value. However, the advisory signs were cancelled by change order and not installed. Had the metric speed limit sign been installed, the signed speed limit on I-19 would have been 88 km/h, which is a close soft-conversion of the then-existing 55 MPH "double nickel" national maximum speed limit. Information signs, to three distinct designs, were also placed at various locations on or near I-19 to advise motorists that the highway was signed in metric. Notwithstanding the metric legends, the signing plans were dimensioned entirely in feet and inches.[4]

In 1999, Arizona DOT awarded two contracts (administered as a single construction project) to renew signing along the full length of I-19. The general approach toward metric signing differed from that taken in 1980. Explicit units were given not just on advance guide signs, but also on interchange sequence signs, post-interchange confirmation signs, and community interchange signs (the last-listed had not been used in 1980). On the distance signs, "km" appeared after each kilometrage except when one or more of the distances was a fractional kilometrage. In such cases all the distances were given in meters with "meters" (written out in full, not "m") after each distance value. On distance signs in general, "km" or "meters" appeared on the same baseline and with the same letter height as the distance values, while advance guide signs were formatted as in 1980. Since a typical Arizona DOT freeway guide sign rehabilitation contract also replaces surface road signing near those roads’ interchanges with the freeway, metric-unit signs also appeared on local roads near I-19, giving distances in kilometers to tourist attractions such as Mission San Xavier del Bac. As was the case in 1980, the signing plans were dimensioned in feet and inches.[5] However, a number of signs near the Valencia Road interchange were replaced or amended when it was converted from a partial cloverleaf to a SPUI in 2000. One of these signs has a fractional kilometrage greater than 1 km, rendered as "1500 m," while others use "m" rather than "meters" as the unit expression. Metric unit expressions on the advance guide signs installed or modified as part of this contract appear on the same baseline as the metric values, rather than on a raised baseline as on other I-19 advance guide signs. Again, the plans were dimensioned in feet and inches.[6]

Citing motorist confusion arising from the metric signs on I-19, Arizona DOT’s Tucson district announced that new signs on I-19 would use United States customary units. To avoid the cost of replacing the metric signs all at once, signs would be replaced in specific areas of the freeway during construction projects in those areas.[7] New signs were put into place between Exit 99 (Ajo Way) and Exit 101 (Interstate 10) in 2004 after the completion of the new Interstate 10–Interstate 19 interchange.

A recent reconstruction project at the Interstate’s northern terminus with Interstate 10 in Tucson, Arizona (at the interchange commonly called "The Crossing") was begun in 2002 and completed in August 2004.

en.wikipedia.org/wiki/Interstate_19

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Exit 34, Tubac, I-19 Southbound


Bild von Ken Lund
Interstate 19 (I-19) is an intrastate Interstate Highway located entirely within the state of Arizona. I-19 runs from Nogales, at the Mexican border to Tucson, at Interstate 10.

In Nogales, Arizona, the southern terminus of I-19 is adjacent to the international port of entry, and southbound travelers can continue into Nogales, Sonora, Mexico, and connect with the northern terminus of Mexico Federal Highway 15. I-19 initially heads west through Nogales before making the turn to head north. It interchanges with two other state highways near the southern end of the route, SR 189 at exit 4 and SR 289 at exit 12. As I-19 enters the Tucson city limits, it has an interchange at SR 86 at exit 99 before reaching its northern terminus at a junction with I-10.

Nearly the entire route of I-19 follows, or is adjacent to, the former routing of U.S. Route 89 and the Santa Cruz River, which flows northward from Mexico, through Tucson and eventually disperses into the desert between Tucson and Phoenix. Most of the time, much of the river is dry, but heavy storms can cause it to overflow its banks.

The official "completion" date of the I-19 segment between Tucson (km 100) and Green Valley, Arizona (actually Helmet Peak Road at km 75) was February 12, 1972. A 1978 Project Report for the Arizona Department of Transportation lists entire I-19 project as "completed," which includes segments between Green Valley and Nogales, Arizona.

Interstate 19 is unique amongst US Interstates, because signed distances are given in meters (hundreds or thousands as distance-to-exit indications) or kilometers (as distance-to-destination indications), and not miles. Speed limit signs give speeds in miles-per-hour, however. According to the Arizona Department of Transportation (ADOT), metric signage was originally placed because of the "metric system push" in the United States at the time of the original construction of the highway.[citation needed]

I-19 had originally been signed as it was constructed, in a series of small signing contracts which used customary units.[3] In 1980, Arizona DOT awarded a single contract to install new signs which used metric units, to overlay English-unit expressions on some existing signs with metric-unit expressions, to install kilometerposts, and to provide bilingual signing in select locations. The signing scheme used in 1980 provided explicit units on advance guide signs, but not on interchange sequence signs or post-interchange confirmation (distance) signs. The expressions on advance guide signs were of the form "2 km" for distances over 1 km and "500 m" for distances under 1 km, with no provision for fractional kilometrages. On advance guide signs, the metric unit expressions "km" and "m" were placed on the baseline where "MILES" would otherwise have gone, but were sized so that their lowercase loop height matched the uppercase letter height of "MILES" on customary-unit signs. The exception was a handful of advance guide signs for the SR 86 Ajo Way exit, which used "KM" (in uppercase, contrary to SI nomenclature) on the same baseline and at the same letter height as "MILES." The 1980 signing plans also provided design details for speed limit and advisory speed signs using metric units, with the limit values enclosed in a red circle on the speed limit sign and a black circle on the yellow-background advisory signs. These speed signs all had explicit units, with "km/h" below the circle enclosing the limit value. However, the advisory signs were cancelled by change order and not installed. Had the metric speed limit sign been installed, the signed speed limit on I-19 would have been 88 km/h, which is a close soft-conversion of the then-existing 55 MPH "double nickel" national maximum speed limit. Information signs, to three distinct designs, were also placed at various locations on or near I-19 to advise motorists that the highway was signed in metric. Notwithstanding the metric legends, the signing plans were dimensioned entirely in feet and inches.[4]

In 1999, Arizona DOT awarded two contracts (administered as a single construction project) to renew signing along the full length of I-19. The general approach toward metric signing differed from that taken in 1980. Explicit units were given not just on advance guide signs, but also on interchange sequence signs, post-interchange confirmation signs, and community interchange signs (the last-listed had not been used in 1980). On the distance signs, "km" appeared after each kilometrage except when one or more of the distances was a fractional kilometrage. In such cases all the distances were given in meters with "meters" (written out in full, not "m") after each distance value. On distance signs in general, "km" or "meters" appeared on the same baseline and with the same letter height as the distance values, while advance guide signs were formatted as in 1980. Since a typical Arizona DOT freeway guide sign rehabilitation contract also replaces surface road signing near those roads’ interchanges with the freeway, metric-unit signs also appeared on local roads near I-19, giving distances in kilometers to tourist attractions such as Mission San Xavier del Bac. As was the case in 1980, the signing plans were dimensioned in feet and inches.[5] However, a number of signs near the Valencia Road interchange were replaced or amended when it was converted from a partial cloverleaf to a SPUI in 2000. One of these signs has a fractional kilometrage greater than 1 km, rendered as "1500 m," while others use "m" rather than "meters" as the unit expression. Metric unit expressions on the advance guide signs installed or modified as part of this contract appear on the same baseline as the metric values, rather than on a raised baseline as on other I-19 advance guide signs. Again, the plans were dimensioned in feet and inches.[6]

Citing motorist confusion arising from the metric signs on I-19, Arizona DOT’s Tucson district announced that new signs on I-19 would use United States customary units. To avoid the cost of replacing the metric signs all at once, signs would be replaced in specific areas of the freeway during construction projects in those areas.[7] New signs were put into place between Exit 99 (Ajo Way) and Exit 101 (Interstate 10) in 2004 after the completion of the new Interstate 10–Interstate 19 interchange.

A recent reconstruction project at the Interstate’s northern terminus with Interstate 10 in Tucson, Arizona (at the interchange commonly called "The Crossing") was begun in 2002 and completed in August 2004.

en.wikipedia.org/wiki/Interstate_19

Exit 12, Pena Blanca Lake, I-19 Southbound, Nogales, Arizona


Bild von Ken Lund
Interstate 19 (I-19) is an intrastate Interstate Highway located entirely within the state of Arizona. I-19 runs from Nogales, at the Mexican border to Tucson, at Interstate 10.

In Nogales, Arizona, the southern terminus of I-19 is adjacent to the international port of entry, and southbound travelers can continue into Nogales, Sonora, Mexico, and connect with the northern terminus of Mexico Federal Highway 15. I-19 initially heads west through Nogales before making the turn to head north. It interchanges with two other state highways near the southern end of the route, SR 189 at exit 4 and SR 289 at exit 12. As I-19 enters the Tucson city limits, it has an interchange at SR 86 at exit 99 before reaching its northern terminus at a junction with I-10.

Nearly the entire route of I-19 follows, or is adjacent to, the former routing of U.S. Route 89 and the Santa Cruz River, which flows northward from Mexico, through Tucson and eventually disperses into the desert between Tucson and Phoenix. Most of the time, much of the river is dry, but heavy storms can cause it to overflow its banks.

The official "completion" date of the I-19 segment between Tucson (km 100) and Green Valley, Arizona (actually Helmet Peak Road at km 75) was February 12, 1972. A 1978 Project Report for the Arizona Department of Transportation lists entire I-19 project as "completed," which includes segments between Green Valley and Nogales, Arizona.

Interstate 19 is unique amongst US Interstates, because signed distances are given in meters (hundreds or thousands as distance-to-exit indications) or kilometers (as distance-to-destination indications), and not miles. Speed limit signs give speeds in miles-per-hour, however. According to the Arizona Department of Transportation (ADOT), metric signage was originally placed because of the "metric system push" in the United States at the time of the original construction of the highway.[citation needed]

I-19 had originally been signed as it was constructed, in a series of small signing contracts which used customary units.[3] In 1980, Arizona DOT awarded a single contract to install new signs which used metric units, to overlay English-unit expressions on some existing signs with metric-unit expressions, to install kilometerposts, and to provide bilingual signing in select locations. The signing scheme used in 1980 provided explicit units on advance guide signs, but not on interchange sequence signs or post-interchange confirmation (distance) signs. The expressions on advance guide signs were of the form "2 km" for distances over 1 km and "500 m" for distances under 1 km, with no provision for fractional kilometrages. On advance guide signs, the metric unit expressions "km" and "m" were placed on the baseline where "MILES" would otherwise have gone, but were sized so that their lowercase loop height matched the uppercase letter height of "MILES" on customary-unit signs. The exception was a handful of advance guide signs for the SR 86 Ajo Way exit, which used "KM" (in uppercase, contrary to SI nomenclature) on the same baseline and at the same letter height as "MILES." The 1980 signing plans also provided design details for speed limit and advisory speed signs using metric units, with the limit values enclosed in a red circle on the speed limit sign and a black circle on the yellow-background advisory signs. These speed signs all had explicit units, with "km/h" below the circle enclosing the limit value. However, the advisory signs were cancelled by change order and not installed. Had the metric speed limit sign been installed, the signed speed limit on I-19 would have been 88 km/h, which is a close soft-conversion of the then-existing 55 MPH "double nickel" national maximum speed limit. Information signs, to three distinct designs, were also placed at various locations on or near I-19 to advise motorists that the highway was signed in metric. Notwithstanding the metric legends, the signing plans were dimensioned entirely in feet and inches.[4]

In 1999, Arizona DOT awarded two contracts (administered as a single construction project) to renew signing along the full length of I-19. The general approach toward metric signing differed from that taken in 1980. Explicit units were given not just on advance guide signs, but also on interchange sequence signs, post-interchange confirmation signs, and community interchange signs (the last-listed had not been used in 1980). On the distance signs, "km" appeared after each kilometrage except when one or more of the distances was a fractional kilometrage. In such cases all the distances were given in meters with "meters" (written out in full, not "m") after each distance value. On distance signs in general, "km" or "meters" appeared on the same baseline and with the same letter height as the distance values, while advance guide signs were formatted as in 1980. Since a typical Arizona DOT freeway guide sign rehabilitation contract also replaces surface road signing near those roads’ interchanges with the freeway, metric-unit signs also appeared on local roads near I-19, giving distances in kilometers to tourist attractions such as Mission San Xavier del Bac. As was the case in 1980, the signing plans were dimensioned in feet and inches.[5] However, a number of signs near the Valencia Road interchange were replaced or amended when it was converted from a partial cloverleaf to a SPUI in 2000. One of these signs has a fractional kilometrage greater than 1 km, rendered as "1500 m," while others use "m" rather than "meters" as the unit expression. Metric unit expressions on the advance guide signs installed or modified as part of this contract appear on the same baseline as the metric values, rather than on a raised baseline as on other I-19 advance guide signs. Again, the plans were dimensioned in feet and inches.[6]

Citing motorist confusion arising from the metric signs on I-19, Arizona DOT’s Tucson district announced that new signs on I-19 would use United States customary units. To avoid the cost of replacing the metric signs all at once, signs would be replaced in specific areas of the freeway during construction projects in those areas.[7] New signs were put into place between Exit 99 (Ajo Way) and Exit 101 (Interstate 10) in 2004 after the completion of the new Interstate 10–Interstate 19 interchange.

A recent reconstruction project at the Interstate’s northern terminus with Interstate 10 in Tucson, Arizona (at the interchange commonly called "The Crossing") was begun in 2002 and completed in August 2004.

en.wikipedia.org/wiki/Interstate_19

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Going to the Sun U-Valley B&W


Bild von Ken Lund
Going to the Sun Road, Glacier National Park.

Glacier National Park is located in the U.S. state of Montana, bordering the Canadian provinces of Alberta and British Columbia. Glacier National Park contains two mountain ranges, sometimes referred to as the southern extension of the Canadian Rockies mountain ranges, with over 130 named lakes, more than 1,000 different species of plants and hundreds of species of animals. This vast pristine ecosystem, spread across 1,584 mi² (4,101 km²), is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 mi² (44,000 km²).[1] The famed Going-to-the-Sun Road, a National Historic Civil Engineering Landmark, traverses through the heart of the park and crosses the Continental Divide, allowing visitors breathtaking views of the rugged Lewis and Livingston mountain ranges, as well as dense forests, alpine tundra, waterfalls and two large lakes. Along with the Going-to-the-Sun Road, five historic hotels and chalets are listed as National Historic Landmarks, and a total of 350 locations are on the National Register of Historic Places.

Glacier National Park borders Waterton Lakes National Park in Canada—the two parks are known as the Waterton-Glacier International Peace Park, and were designated as the world’s first International Peace Park in 1932. Both parks were designated by the United Nations as Biosphere Reserves in 1976, and in 1995 as World Heritage sites.[2]

The earliest occupants with lineage to current tribes were the Salish, Flathead, Shoshone and Cheyenne. The Blackfeet arrived around the beginning of the 18th century and soon dominated the eastern slopes of what later became the park, as well as the Great Plains immediately to the east. The park region provided the Blackfeet shelter from the harsh winter winds of the plains, and supplemented their traditional bison hunts with other game meat. Today, the Blackfeet Indian Reservation borders the park in the east, while the Flathead Indian Reservation is located west and south of the park. When the Blackfeet Reservation was first established in 1855 by the Lame Bull Treaty, it included the eastern area of the current park up to the Continental Divide.[4] To the Blackfeet, the mountains of this area, especially Chief Mountain and the region in the southeast at Two Medicine, were considered the "Backbone of the World" and were frequented during vision quests. In 1895, Chief White Calf of the Blackfeet authorized the sale of the mountain area, some 800,000 acres (3,200 km²), to the U.S. government for .5 million. This established the current boundary between the park and the reservation.

While exploring the Marias River in 1806, the Lewis and Clark Expedition came within 50 miles (80 km) of the area that is now the park. A series of explorations after 1850 helped to shape the understanding of the area that later became the park. George Bird Grinnell came to the region in the late 1880s and was so inspired by the scenery that he spent the next two decades working to establish a national park. In 1901, Grinnell wrote a description of the region, in which he referred to it as the "Crown of the Continent", and his efforts to protect the land make him the premier contributor to this cause.[2] A few years after Grinnell first visited, Henry L. Stimson and two companions, including a Blackfeet Indian, climbed the steep east face of Chief Mountain in 1892.

In 1891, the Great Northern Railway crossed the Continental Divide at Marias Pass (5,213 ft/1,589 m), which is along the southern boundary of the park. In an effort to stimulate use of the railroad, the Great Northern soon advertised the splendors of the region to the public. The company lobbied the United States Congress, and in 1900, the park was designated as a forest preserve. Under the forest designation mining was still allowed, but was not commercially successful. Meanwhile, proponents of protecting the region kept up their efforts, and in 1910, under the influence of George Bird Grinnell, Henry L. Stimson and the railroad, a bill was introduced into the U.S. Congress which redesignated the region from a forest reserve to a national park. This bill was signed into law by President William Howard Taft on May 11, 1910. From May until August, the forest reserve supervisor, Fremont Nathan Haines, managed the Park’s resources as the first acting superintendent. In August of 1910, William Logan was appointed the Park’s first superintendent.

The Great Northern Railway, under the supervision of president Louis W. Hill, built a number of hotels and chalets throughout the park in the 1910s to promote tourism. These buildings, constructed and operated by a Great Northern subsidiary called the Glacier Park Company, were modeled on Swiss architecture as part of Hill’s plan to portray Glacier as "America’s Switzerland". Vacationers commonly took pack trips on horseback between the lodges or utilized the seasonal stagecoach routes to gain access to the Many Glacier area in the northeast.[5]

The chalets, built between 1910 and 1913, included Belton, St. Mary, Going-to-the-Sun, Many Glacier, Two Medicine, Sperry, Granite Park, Cut Bank, and Gunsight Lake. The railway also built Glacier Park Lodge, adjacent to the park on its east side, and the Many Glacier Hotel on the east shore of Swiftcurrent Lake. Louis Hill personally selected the sites for all of these buildings, choosing each for their dramatic scenic backdrops and views. Another developer, John Lewis, built the Lewis Glacier Hotel on Lake McDonald in 1913–1914. The Great Northern Railway bought the hotel in 1930, and it was later renamed Lake McDonald Lodge. Some of the chalets were in remote backcountry locations accessible only by trail. Today, only Sperry, Granite Park, and Belton Chalets are still in operation, while a building formerly belonging to Two Medicine Chalet is now Two Medicine Store.[6] The surviving chalet and hotel buildings within the park are now designated as National Historic Landmarks.[7] In total, 350 buildings and structures within the park are listed on the National Register of Historic Places, including ranger stations, backcountry patrol cabins, fire lookouts, and concession facilities.

After the park was well established and visitors began to rely more on automobiles, work was begun on the 53 mile (85 km) long Going-to-the-Sun Road, completed in 1932. Also known simply as the Sun Road, the road bisects the park and is the only route that ventures deep into the park, going over the Continental Divide at Logan Pass (6,646 feet, 2025 m) at the midway point. The Sun Road is also listed on the National Register of Historic Places, and in 1985 was designated a National Historic Civil Engineering Landmark.[8] Another route, along the southern boundary between the park and National Forests is U.S. Route 2, which crosses the Continental Divide at Marias Pass and connects the towns of West Glacier and East Glacier. During the 1930s, the Civilian Conservation Corps assisted in the development of many of the park’s trails and campgrounds. The increase in motor vehicle traffic through the park during the 1930s also resulted in the construction of new concession facilities at Swiftcurrent and Rising Sun, both designed for automobile-based tourism. These early "auto camps" are now also listed on the National Register.[9]

In 2003, wildfires on the western side of the Continental Divide burned 10% of Glacier National Park. There were also extensive fires in the surrounding forests.

Glacier National Park is managed by the National Park Service; park headquarters is in West Glacier, Montana. The National Park Service has the smallest staff of any major federal agency, yet oversees over 84 million acres (340,000 km²).[10] Visitation to Glacier National Park averages slightly less than 2 million visitors annually, however a relative few venture far from main roadways and hotels.

Glacier National Park had an operating budget of ,885,000 for fiscal year 2006. Most of this budget was used to provide a minimal number of staff and to make minor improvements to structures and roadways in immediate need of repair. More than 60% of the employees are employed for only a few months per year during the summer. Only 20% of the park’s annual funding comes from entrance and campground fees. The remaining funding comes from federal tax dollars, grants and donations. According to reports presented to the U.S. House of Representatives in 1999, the cost of deferred maintenance, not including repairs to roads and hotels, was million. Restoring the five hotels in the park by bringing them up to the current fire codes and performing stabilization work, would cost another 0–135 million.

The mandate of the National Park Service is to ‘…preserve and protect natural and cultural resources’. The Organic Act of August 25, 1916, established the National Park Service as a federal agency. One major section of the Act has often been summarized as the "Mission", "…to promote and regulate the use of the…national parks…which purpose is to conserve the scenery and the natural and historic objects and the wild life therein and to provide for the enjoyment of the same in such manner and by such means as will leave them unimpaired for the enjoyment of future generations."[11] In keeping with this mandate, hunting is illegal in the park, as are mining, logging and removal of natural or cultural resources. Additionally, oil and gas exploration and extraction are not permitted. In 1974, a wilderness study was submitted to congress which identified 95% of the area of the park as qualifying for wilderness designation. Unlike a few other parks, Glacier National Park has yet to be protected as wilderness, but National Park Service policy requires that identified areas listed in the report be managed as wilderness until Congress renders a full decision."[12]

In anticipation of the 100th anniversary of the park in 2010, major reconstruction of the Going-to-the-Sun Road is underway, and temporary road closures are expected in the 2007 season. Some rehabilitation of major structures such as visitor centers and historic hotels, as well as improvements in wastewater treatment facilities and campgrounds, are expected to be completed by the anniversary date. Also planned are fishery studies for Lake McDonald, updates of the historical archives and restoration of trails.

The park is bordered on the north by Waterton Lakes National Park in Alberta, and the Flathead Provincial Forest and Akamina-Kishinena Provincial Park in British Columbia. To the west, the north fork of the Flathead River forms the western boundary, while its middle fork is part of the southern boundary. The Blackfeet Indian Reservation provides most of the eastern boundary, and the Lewis and Clark and the Flathead National Forests form the southern and western boundary. The remote Bob Marshall Wilderness Complex is located in the two forests immediately to the south.

The park contains a dozen large lakes and 700 smaller ones, but only 131 lakes have been named. Lake McDonald, St. Mary Lake, Bowman Lake and Kintla Lake are the four largest lakes. Numerous smaller lakes, known as tarns, are located in cirques formed by glacial erosion. Some of these lakes, like Avalanche Lake and Cracker Lake, are colored an opaque turquoise by suspended glacial silt, which also causes a number of streams to run milky white. The lakes of Glacier National Park remain cold year round, with temperatures rarely above 50 °F (10 °C) at their surface. Cold water lakes such as these support little plankton growth, ensuring that the lake waters are remarkably clear. The lack of plankton, however, lowers the rate of pollution filtration, and pollutants have a tendency to linger longer. Consequently, the lakes are considered environmental bellwethers as they can be quickly affected by even minor increases in pollutants.[13]

Two hundred waterfalls are scattered throughout the park, however, during dryer times of the year, many of these are reduced to a trickle. The largest falls include those in the Two Medicine region, McDonald Falls in the McDonald Valley and Swiftcurrent Falls in the Many Glacier area, which is easily observable and close to the Many Glacier Hotel. One of the tallest waterfalls is Bird Woman Falls, which drops 492 feet (150 m) from a hanging valley beneath the north slope of Mount Oberlin.[14] Bird Woman Falls can be easily seen from the Going-to-the-Sun Road.

The rocks found in the park are primarily sedimentary in origin, having been laid down in shallow seas over 1.6 billion to 800 million years ago. During the formation of the Rocky Mountains the Lewis Overthrust, commencing 170 million years ago, moved an enormous region of rocks three miles (4.8 km) thick and 160 miles (257 km) long, eastward more than 50 miles (80 km).[15] This resulted in older rocks being displaced over newer ones, and today the overlying Proterozoic rocks are over 1.4 billion years older than the underlying Cretaceous age rocks.

One of the most dramatic evidences of this overthrust is visible in the form of Chief Mountain, an isolated peak on the edge of the eastern boundary of the park rising 4,500 feet (1,372 m) above the Great Plains. There are seven mountains in the park over 10,000 feet (3,048 m) in elevation, with Mount Cleveland at 10,466 feet (3,190 m) being the tallest. Appropriately named Triple Divide Peak sends waters towards the Pacific Ocean, Hudson Bay, and Gulf of Mexico watersheds, and can effectively be considered to the be the apex of the North American continent, although the mountain is only 8,020 feet (2,444 m) above sea level.

The rocks in Glacier National Park are the best preserved Proterozoic sedimentary rocks in the world, and have proved to be some of the world’s most fruitful sources for records of early life. Sedimentary rocks of similar age located in other regions have been greatly altered by mountain building and other metamorphic changes, and consequently fossils are less common and more difficult to observe. The rocks in the park preserve such features as millimeter-scale lamination, ripple marks, mud cracks, salt-crystal casts, raindrop impressions, oolites and other sedimentary bedding characteristics. Six fossilized species of Stromatolites, which were early organisms consisting primarily blue-green algae, have been documented and dated at about 1 billion years.[16] The discovery of the Appekunny Formation, a well preserved rock stratum in the park, pushed back the established date for the origination of animal life a full billion years. This rock formation has bedding structures which are believed to be the remains of the earliest identified metazoan (animal) life on Earth.[17]

Glacier National Park is dominated by mountains which were carved into their present shapes by the huge glaciers of the last ice age; these glaciers have largely disappeared over the 15,000 years. Evidence of widespread glacial action is found throughout the park in the form of U-shaped valleys, glacial cirques, arêtes and large outflow lakes radiating like fingers from the base of the highest peaks. Since the end of the ice ages, various warming and cooling trends have occurred. The last recent cooling trend was during the Little Ice Age which took place approximately between 1550 and 1850.[18] During the Little Ice Age, the glaciers in the park expanded and advanced, although to nowhere near as great an extent as they had during the Ice Age. Coincidentally, the park region was first explored in detail near the end of the Little Ice Age and a systematized survey began in which the number and size of glaciers was documented on maps and by photographic evidence. Much of this late 19th century work, however, was undertaken to lure tourism into the region or to search for mineral wealth, not out of a particular desire to document glaciers.

During the middle of the 20th century, examination of the maps and photographs from the previous century provided clear evidence that the 150 glaciers known to have existed in the park a hundred years earlier had greatly retreated, and in many cases disappeared altogether.[19] Repeat photography of the glaciers, such as the pictures taken of Grinnell Glacier between 1938 and 2005 as shown, help to provide visual confirmation of the extent of glacier retreat.

In the 1980s, the U.S. Geological Survey began a more systematic study of the remaining glaciers, which continues to the present day. By 2005, only 27 glaciers remained, and scientists generally agree that if the current greenhouse warming continues, all the glaciers in the park will be gone by 2030.[19] This glacier retreat follows a worldwide pattern that has accelerated even more since 1980. The extensive glacier retreat that has been observed in Glacier National Park, as well as in other regions worldwide, is a key indicator of climatic changes on a worldwide scale. Without a major climatic change in which cooler and moister weather returns and persists, the mass balance (accumulation rate versus melting rate) of glaciers will continue to be negative and the glaciers will eventually disappear, leaving behind only barren rock.[19]

After the end of the Little Ice Age in 1850, the glaciers in the park retreated moderately until the 1910s. Between 1917 and 1926, the retreat rate rose rapidly and continued to accelerate through the 1930s. A slight cooling trend from the 1940s until 1979, helped to slow the rate of retreat and in a few examples some glaciers even advanced a few tens of meters. However, during the 1980s, the glaciers in the park began a steady period of loss of glacial ice, which continues into the 2000s. In 1850, the glaciers in the region near Blackfoot and Jackson Glaciers covered 5,337 acres (21.6 km²), but by 1979, the same region of the park had glacier ice covering only 1,828 acres (7.4 km²). Between 1850 and 1979, 73 percent of the glacial ice had melted away.[20] At the time the park was created, Jackson Glacier was part of Blackfoot Glacier, but the two separated into different glaciers by 1939.

The impact of glacier retreat on the park’s ecosystems is not fully known, but cold water dependent plant and animal species could suffer due to a loss of habitat. Reduced seasonal melting of glacial ice may also affect stream flow during the dry summer and fall seasons, reducing water table levels and increasing the risk of forest fires. The loss of glaciers will also reduce the aesthetic visual appeal that glaciers provide to visitors.[21]

Many areas are only accessible during the summer, and possibly the late spring and early fall, depending on snowfall and elevation. Rainfall is frequent in the tourist season during the summer and may persist for days, averaging two to three inches (5–7.6 cm) each month. Snowfall can occur at any time of the year, even in the summer, and especially at higher altitudes. Visiting in the early summer is a way to avoid some but not all of the wet weather. In the spring, however, the nights and early mornings will be substantially cooler, and high-elevation trails, including the popular Hidden Lake Trail at Logan Pass, may still be snow covered. Thunderstorms are common all summer, and normal safety precautions for lightning and hail should be taken. The mountainous terrain ensures that tornadoes are very rare. The winter can bring prolonged cold waves, especially on the eastern side of the Continental Divide. Snowfalls are significant over the course of the winter, with the largest accumulation occurring in the west. During the tourist season daytime high temperatures average in the 60s and 70s °F (15 to 25 °C), and nighttime lows usually drop into the 40s (7 °C). Temperatures in the high country may be much cooler. In the lower valleys, on the other hand, daytime highs over 90 °F (32 °C) are not unusual.[22]

Rapid temperature changes have been noted in the region, and in Browning, Montana, which is just east of the park in the Blackfeet Indian Reservation, a world record temperature drop of 100 degrees Fahrenheit (56 °C) in only 24 hours occurred on the night of January 23–24, 1916, when thermometers plunged from 44 °F to -56 °F (7 to -49 °C).[23]

Glacier National Park has a highly regarded global climate change research program. Based in West Glacier, with its main headquarters in Bozeman, Montana, the U.S. Geological Survey has performed scientific research on specific climate change studies since 1992. In addition to the study of the retreating glaciers, research performed includes forest modeling studies in which fire ecology and habitat alterations are analyzed. Additionally, changes in alpine vegetation patterns are documented, watershed studies in which stream flow rates and temperatures are recorded frequently at fixed gauging stations, and atmospheric research in which UV-B radiation, ozone and other atmospheric gases are analyzed over time. The research compiled all contribute to a broader understanding of climate changes in the park. The data collected, when compared to other facilities scattered around the world, help to correlate these climatic changes on a global scale.[24]

Glacier is considered to have excellent air and water quality. No major areas of dense human population exist anywhere near the region and industrial effects are minimized due to a scarcity of factories and other potential contributors of pollutants. However, the sterile and cold lakes found throughout the park are easily contaminated by airborne pollutants that fall whenever it rains or snows, and some evidence of these pollutants have been found in park waters. The pollution level is currently viewed as negligible, and the park lakes and waterways have a water quality rating of A-1, the highest rating given by the state of Montana.[25]

Glacier is part of a large preserved ecosystem collectively known as the "Crown of the Continent Ecosystem", all of which is primarily untouched wilderness of a pristine quality. Virtually all the plants and animals which existed at the time white explorers first entered the region are present in the park today.[26]

A total of over 1,132 plant species have been identified parkwide. The predominantly coniferous forest is home to various species of trees such as the Engelmann spruce, Douglas fir, subalpine fir, limber pine and western larch, which is a deciduous conifer, producing cones but losing its needles each fall. Cottonwood and aspen are the more common deciduous trees and are found at lower elevations, usually along lakes and streams. The timberline on the eastern side of the park is almost 800 feet (244 m) lower than on the western side of the Continental Divide, due to exposure to the colder winds and weather of the Great Plains. West of the Continental Divide, the forest receives more moisture and is more protected from the winter, resulting in a more densely populated forest with taller trees. Above the forested valleys and mountain slopes, alpine tundra conditions prevail, with grasses and small plants eking out an existence in a region that enjoys as little as three months without snow cover. Thirty species of plants are found only in the park and surrounding National Forests. Beargrass, a tall flowering plant, is commonly found near moisture sources, and is relatively widespread during July and August. Wildflowers such as monkeyflower, glacier lily, fireweed, balsamroot and Indian paintbrush are also common.[27]

The forested sections fall into three major climatic zones. The west and northwest are dominated by spruce and fir and the southwest by redcedar and hemlock; the areas east of the Continental Divide are a combination of mixed pine, spruce, fir and prairie zones. The cedar-hemlock groves along the Lake McDonald valley are the easternmost examples of this Pacific climatic ecosystem.[28]

Whitebark pine communities have been heavily damaged due to the effects of blister rust, a non native fungus. In Glacier and the surrounding region, 30% of the Whitebark pine trees have died and over 70% of the remaining trees are currently infected. The Whitebark pine provides a high fat pine cone seed, commonly know as the pine nut, that is a favorite food of red squirrels and Clark’s nutcracker. Both grizzlies and black bears are known to raid squirrel caches of the pine nuts, and it is one of the bears’ favorite foods. Between 1930 and 1970, efforts to control the spread of blister rust were unsuccessful, and continued destruction of whitebark pines appears likely, with attendant negative impacts on dependent species.[29]

Virtually all the historically known plant and animal species, with the exception of the bison and woodland caribou, are present, providing biologists an intact ecosystem for plant and animal research. Two threatened species of mammals, the grizzly bear and the Canadian lynx, are found in the park. Although their numbers remain at historical levels, both are listed as threatened because in virtually every other region of the U.S. outside of Alaska, they are either extremely rare or absent from their historical range. On average, one or two bear attacks on humans occur each year; since the creation of the park in 1910, there have been a total of 10 bear related deaths.[30] The number of grizzlies and lynx in the park is not known for certain, but park biologists believe that there are slightly less than 350 grizzlies parkwide, and a study commenced in 2001 hoped to determine the number of lynx in the park.[31] Another study has indicated that the wolverine, another very very rare mammal in the lower 48 states, continues to reside in the park.[32] An estimated 800 black bears are believed to exist parkwide. The black bear is less aggressive than the grizzly and a recent study using DNA to identify hair samples indicated that there are about six times as many black bears as there are grizzlies.[33] Other large mammals such as the mountain goat (the official park symbol), bighorn sheep, moose, elk, mule deer, white-tailed deer, coyote, and the rarely seen mountain lion, are either plentiful or common. Unlike in Yellowstone National Park, which commenced a wolf reintroduction program in the 1990s, wolves have existed almost continuously in Glacier. 62 species of mammals in all have been documented including badger, river otter, porcupine, mink, marten, fisher, six species of bats and numerous other smaller mammals.[34]

A total 260 species of birds have been recorded, with raptors such as the bald eagle, golden eagle, peregrine falcon, osprey and several species of hawks residing year round. The harlequin duck is a colorful species of waterfowl found in the lakes and waterways. The great blue heron, tundra swan, Canada goose and American wigeon are species of waterfowl more commonly encountered in the park. Great horned owl, Clark’s nutcracker, Steller’s jay, pileated woodpecker and cedar waxwing reside in the dense forests along the mountainsides, and in the higher altitudes, the ptarmigan, timberline sparrow and rosy finch are the most likely to be seen. The Clark’s nutcracker is less plentiful than in past years due to the reduction in the number of whitebark pines.[35]

Because of the colder climate, ectothermic reptiles are all but absent, with two species of garter snakes and the western painted turtle being the only three reptile species proven to exist. Similarly, only six species of amphibians are documented, although those species exist in large numbers. After a forest fire in 2001, a few park roads were temporarily closed the following year to allow thousands of Western toads to migrate to other areas.[36]

Glacier is also home to the endangered bull trout which is illegal to possess and must be returned to the water if caught inadvertently.[37] A total of 23 species of fish reside in park waters and native game fish species found in the lakes and streams include the cutthroat trout, northern pike, mountain whitefish, Kokanee salmon and grayling. Introduction in previous decades of Lake trout and other non-native fish species have greatly impacted some native fish populations, especially the bull trout and west slope cutthroat trout.

Forest fires were viewed for many decades as a threat to protected areas such as forests and parks. As a better understanding of fire ecology developed after the 1960s, forest fires were understood to be a natural part of the ecosystem. The earlier policies of suppression resulted in the accumulation of dead and decaying trees and plants which would normally have been reduced had fires been allowed to burn. Many species of plants and animals actually need wildfires to help replenish the soil with nutrients and to open up areas that allow grasses and smaller plants to thrive.[38] Glacier National Park has a fire management plan which ensures that human caused fires are generally suppressed as they always have been. In the case of natural fires, the fire is monitored and suppression is dependent on the size and threat a fire may pose to human safety and structures. Major fires that require the assistance of other resources are coordinated through the National Interagency Fire Center.

Increased population and the growth of suburban areas near parklands, has led to the development of what is known as Wildland Urban Interface Fire Management, in which the park cooperates with adjacent property owners in improving safety and fire awareness. This approach is common to many other protected areas. As part of this program, houses and structures near the park are designed to be more fire resistant. Dead and fallen trees are removed from near places of human habitation, reducing the available fuel load and the risk of a catastrophic fire, and advance warning systems are developed to help alert property owners and visitors about forest fire potentials during a given period of the year.[39] In 2003, 136,000 acres (550 km²) burned in the park after a five year drought and a summer season of almost no precipitation. This was the most area transformed by fire since the creation of the park in 1910.

Glacier is distant from major cities, and the closest airport is at Kalispell, Montana, southwest of the park. Amtrak trains stop at East and West Glacier. A fleet of restored 1930s White Motor Company coaches, called Reds, offer tours on all the main roads in the park. The drivers of the buses are called "Jammers," due to the gear-jamming that formerly occurred during the vehicles’ operation. The tour buses were rebuilt in 2001 to run on propane, to lessen their environmental impact.[40]

A number of historic wooden tour boats, some dating back to the 1920s, operate on several of the larger lakes.

Hiking is a popular activity in the park. Over half of the visitors to the park report taking a hike on the park’s nearly 700 miles (1,127 km) of trails.[41] 110 miles (177 km) of the Continental Divide National Scenic Trail spans most of the distance of the park north to south, with a few alternate routes at lower elevations if high altitude passes are closed due to snow. Due to the presence of bears and other large mammals, dogs are not permitted on any trails in the park, though they are permitted at front country campsites that can accessed by a vehicle, and along paved roads.

Numerous day hiking options are available throughout the park. Backcountry camping is allowed at campsites along the trails. A permit is required, which can be obtained from certain visitor centers or arranged for in advance. Much of Glacier’s backcountry is usually inaccessible to hikers until early June due to accumulated snowpack and potential avalanche risk, and many trails at higher altitudes remain snow packed until July. The major campgrounds that allow vehicle access are found throughout the park, most of which are near one of the larger lakes. The campground at St. Mary and at Apgar are open year round, but conditions are considered primitive in the off-season, as the restroom facilities are closed and there is no running water. All campgrounds with vehicle access are usually open from mid June until mid September.[42] Guide and shuttle services are also available.

Fishing is a popular activity in the park and some of the finest fly fishing in North America can be found in the streams that flow through the park. Though the park requires that those fishing understand the regulations, no permit is required to fish the waters within the park boundary. The endangered bull trout must be released immediately back to the water if caught, otherwise, the regulations on limits of catch per day are liberal.[43]

Winter recreation activities in Glacier are limited. Snowmobiling is illegal in the park, but cross-country skiing is permitted in the lower altitude valleys on the east and western sides of the park.

From: en.wikipedia.org/wiki/Glacier_National_Park_(U.S.)

Badwater


Bild von skinnylawyer
Badwater, located 282 feet or 86 meters below sea level, is the lowest part of the Western Hemisphere.

Water from nearby mountains flows here and evaporates, leaving a salty crust. The name "Badwater" came about because a survey team found that its mules would not even come close to drinking the water due to the bad taste.

As seen here, it is possible to walk on the salty valley floor out to the middle of nowhere.

In the distance can be seen Telescope Peak, which makes the western wall of Death Valley. Telescope Peak stands over 11,000 feet tall, for one of the most extreme changes of elevations anywhere in the world.

Jackson Lake, Grand Teton National Park


Bild von pmsyyz
Bit of a steep climb down to the shoreline, probably due to seasonal lake level changes caused by the dam. This was in the afternoon and the light was bad for taking photos of the mountains.

Jackson Lake is a lake located in north western Wyoming in Grand Teton National Park. The lake is natural, except for the top 33 feet (10 m), which is due to the construction of Jackson Lake Dam, built in 1911. This top level of the lake is utilized by farmers in Idaho for irrigation purposes. The lake is the remnant of large glacial gouging from the neighboring Teton Range, and is still fed by runoff from small glaciers near the peaks of those mountains. The main source of water is the Snake River, which flows in from the North. Jackson Lake is one of the largest high altitude lakes in the U.S. at an elevation of 6,772 feet (2,064 m) above sea level. The lake is up to 15 miles (25 km) long, 7 miles (11.25 km) wide and 438 feet (134 m) deep. The water of the lake averages below 60 degrees even during the hottest summer months and can freeze to more than 6 feet (1.8 m) thick in the winter.

IMG_2390

Gute peak flow Photos:

St. George, Utah (10)


Bild von Ken Lund
St. George is a city located in the southwestern part of the U.S. state of Utah, and the county seat of Washington County, Utah. It is the principal city of and is included in the St. George, Utah Metropolitan Statistical Area. The city is 119 miles (192 km) northeast of Las Vegas, Nevada, and 303 miles (488 km) south of Salt Lake City on Interstate 15.

According to the U.S. Census Bureau, St. George had a population of 72,718 in 2007, up from 49,728 in 2000. In 2005, St. George surpassed Layton as the eighth-largest city in Utah. From 1990 to 2000, St. George beat Las Vegas by a mere 0.6% as the fastest-growing metropolitan area in the U.S. This trend has continued, with St. George being declared the second fastest-growing metropolitan area in the U.S. (behind Greeley, Colorado) in September 2005. In 2007, the metropolitan area (defined as Washington County) had an estimated 140,908 residents. The population of St. George and surrounding cities in 2050 is projected to be at more than 700,000 residents.

St. George is the population and commercial center of Utah’s Dixie, a nickname given to the area when Mormon pioneers grew cotton in the warm climate. St. George’s trademark is its geology — red bluffs make up the northern part of the city with two peaks covered in lava rock in the city’s center. The northeastern edges of the Mojave Desert are visible to the south. Zion National Park can be seen to the east, and the Pine Valley Mountains loom over the city to the north and northwest. The climate has more in common with the Desert Southwest than the rest of the state, with scorching hot summers and mild, mostly snowless winters. The city has recently developed into a major retirement destination.

St. George was founded as a cotton mission in 1861 under the direction of Brigham Young, the President of The Church of Jesus Christ of Latter-day Saints (the Mormons or LDS Church)— part of a greater church effort to become self-sufficient. While the early settlers did manage to grow cotton, it was never produced at competitive market rates; consequently, cotton farming was eventually abandoned.

At the outbreak of the Civil War in 1861, Brigham Young organized the settlement of what is now Washington County, Utah.

“Fearing that, the war would take away the cotton supply, he began plans for raising enough in this western country to supply the needs of his people. Enough favorable reports had come to him from this warm country below the rim of the [Great] Basin, that he was convinced cotton could be raised successfully here. At the general church conference in Salt Lake City on October 6th, [1861], about three hundred families were “called" to the Dixie mission to promote the cotton industry. Most of the people knew nothing of this expedition until their names were read from the pulpit; but in nearly every case, they responded with good will, and made ready to leave within the month’s time allotted to them. The families were selected so as to ensure the communities the right number of farmers, masons, blacksmiths, businessmen, educators, carpenters, as needed.”

The settlement was named after George A. Smith, an apostle of The Church of Jesus Christ of Latter-day Saints.

In April 1877, the LDS Church completed the St. George Utah Temple. It is the Church’s third temple, and, currently, its longest continually-operating temple.

According to the United States Census Bureau, the city has a total area of 64.9 square miles (168.0 km²), of which, 64.4 square miles (166.8 km²) of it is land and 0.5 square miles (1.2 km²) of it (0.72%) is water.

St. George lies in the lowest elevation region of the state, Dixie, with most of the city lying below 3,000 feet (900 m). The city is surrounded by mountains and red sandstone buttes, and it lies at the very northeastern edge of the Mojave Desert. The Virgin River flows through the city. The Santa Clara River also flows on the east side of the city before merging with the Virgin River to the south. In early 2005, major flooding occurred within these two rivers. One person was killed and several houses were destroyed by the raging Santa Clara River.

The city borders Arizona, and is located between the towns of Santa Clara and Ivins to the west and Washington to the east. The core of the city, including its downtown, Dixie State College, convention center, and hospital, are located in a small valley overlooking the Virgin River and surrounded by low lava and sandstone bluffs. The city’s southern section, Bloomington, is more typical of the Mojave Desert, with desert scrub and gravel dominating the landscape. The southeast part of the city contains some farming along the Virgin River, but like the west and northwest parts of the city has become increasingly dominated by suburban-style development.

In Southern Utah, soil and rock formations are red in appearance due to the presence of iron oxide.[11] Although portions of the older section of the city (particularly the southern part near the Virgin River) lie on floodplain alluvium, much of St. George is built directly upon Jurassic, Triassic, and Permian period sedimentary bedrock. The following formations—listed in chronological order—can be found within the city limits.

Kaibab Limestone (Permian): Grey fossiliferious limestone, exposed at the center of the Virgin River anticline along Horseman Park Drive and in the low hills to the south of South Bloomington Hills.

Moenkopi Formation (Triassic): Chocolatey-red and white banded mudstone, shale, limestone, and siltstone containing thick layers of gypsum, exposed at Bloomington, South Bloomington Hills, and the south side of Webb Hill.

Shinarump Conglomerate (Triassic): Yellow to brown cliff-forming sandstone and conglomerate containing fossilized oyster shells and petrified wood. Forms the cliff faces north of Bloomington, on Webb Hill, and along the Virgin River south of 1450 South Street. This is actually the lowest member of the Chinle formation.

Chinle Formation (Triassic): Purple, white, grey and locally green bentonitic shale weathering to clay. Because of the softness of the strata, structures built on this formation run a higher risk of settling or slippage. The Chinle formation underlies large portions of St. George, including North Bloomington Hills, much of Green Valley, and much of the east part of the city around Riverside Drive and Pine View High School.

Moenave Formation (Jurassic): Red and orange sandstone, siltstone, and mudstone. There is some confusion about distinguishing between the Springdale sandstone member of the Moenave formation and the overlying Navajo sandstone, which is similar in appearance, in the St. George area. It is now generally assumed that the red cliffs to the north of the old part of the city (north of Red Hills Parkway) and at the Dixie Red Hills golf course are part of the Moenave formation. Other exposures include cuts into the east and west Black Hills and the southern part of Dixie Downs.

Kayenta Formation (Jurassic): Red, orange, and purple sandstone, shale, and mudstone. Forms slopes below the massive Navajo sandstone in the northern part of the city including northern Dixie Downs and along Snow Canyon Parkway.

Navajo Sandstone (Jurassic): Grey to brown, red, and (in its upper layers) white massive sandstone. Forms cliff faces above Snow Canyon Parkway and white outcrops at Winchester Hills.

Basaltic lava flows from the Quaternary period form the black ridges to the east and west of the old part of St. George city. The volcanic eruptions producing these flows are thought to date back 1.2 million years.

St. George straddles the line between the Colorado Plateau region to the east with its mesas, and the basin and range to the west with its broad landscapes and cactus forests. Other points of geologic interest include the Virgin River anticline; the rock has eroded away in the center leaving shear walls surrounding the "Purgatory Flats" area to the east of St. George. Another geologic feature is Pine Valley Mountain, composed of one solid piece of granite, it is one of the largest laccoliths in the world.

Along with its increasing population, the economy of St. George and surrounding areas has boomed in recent years.

One of St. George’s most significant corporations is SkyWest Airlines, which has its corporate headquarters in St. George. Wal-Mart has a large distribution center located near St. George. In 2003, Intermountain Health Care opened a new 0 million, 196 bed, 420,000-square-foot (39,000 m2) hospital building.

A large part of the economy of southwestern Utah comes from tourism. St. George is in proximity to Zion National Park and Bryce Canyon National Park, as well as several state parks and recreational areas. It is a little less than an hour drive from the Tony award winning Utah Shakespearean Festival. Golf also plays a large part in the city’s tourism industry. St. George offers one of the highest number of golf courses per capita in the country. Special events such as the St. George Marathon and the Huntsman Senior Games draw thousands to St. George each year. The St. George Marathon is currently the 13th largest marathon in the country.

en.wikipedia.org/wiki/St._George,_Utah

St. George, Utah (13)


Bild von Ken Lund
St. George is a city located in the southwestern part of the U.S. state of Utah, and the county seat of Washington County, Utah. It is the principal city of and is included in the St. George, Utah Metropolitan Statistical Area. The city is 119 miles (192 km) northeast of Las Vegas, Nevada, and 303 miles (488 km) south of Salt Lake City on Interstate 15.

According to the U.S. Census Bureau, St. George had a population of 72,718 in 2007, up from 49,728 in 2000. In 2005, St. George surpassed Layton as the eighth-largest city in Utah. From 1990 to 2000, St. George beat Las Vegas by a mere 0.6% as the fastest-growing metropolitan area in the U.S. This trend has continued, with St. George being declared the second fastest-growing metropolitan area in the U.S. (behind Greeley, Colorado) in September 2005. In 2007, the metropolitan area (defined as Washington County) had an estimated 140,908 residents. The population of St. George and surrounding cities in 2050 is projected to be at more than 700,000 residents.

St. George is the population and commercial center of Utah’s Dixie, a nickname given to the area when Mormon pioneers grew cotton in the warm climate. St. George’s trademark is its geology — red bluffs make up the northern part of the city with two peaks covered in lava rock in the city’s center. The northeastern edges of the Mojave Desert are visible to the south. Zion National Park can be seen to the east, and the Pine Valley Mountains loom over the city to the north and northwest. The climate has more in common with the Desert Southwest than the rest of the state, with scorching hot summers and mild, mostly snowless winters. The city has recently developed into a major retirement destination.

St. George was founded as a cotton mission in 1861 under the direction of Brigham Young, the President of The Church of Jesus Christ of Latter-day Saints (the Mormons or LDS Church)— part of a greater church effort to become self-sufficient. While the early settlers did manage to grow cotton, it was never produced at competitive market rates; consequently, cotton farming was eventually abandoned.

At the outbreak of the Civil War in 1861, Brigham Young organized the settlement of what is now Washington County, Utah.

“Fearing that, the war would take away the cotton supply, he began plans for raising enough in this western country to supply the needs of his people. Enough favorable reports had come to him from this warm country below the rim of the [Great] Basin, that he was convinced cotton could be raised successfully here. At the general church conference in Salt Lake City on October 6th, [1861], about three hundred families were “called" to the Dixie mission to promote the cotton industry. Most of the people knew nothing of this expedition until their names were read from the pulpit; but in nearly every case, they responded with good will, and made ready to leave within the month’s time allotted to them. The families were selected so as to ensure the communities the right number of farmers, masons, blacksmiths, businessmen, educators, carpenters, as needed.”

The settlement was named after George A. Smith, an apostle of The Church of Jesus Christ of Latter-day Saints.

In April 1877, the LDS Church completed the St. George Utah Temple. It is the Church’s third temple, and, currently, its longest continually-operating temple.

According to the United States Census Bureau, the city has a total area of 64.9 square miles (168.0 km²), of which, 64.4 square miles (166.8 km²) of it is land and 0.5 square miles (1.2 km²) of it (0.72%) is water.

St. George lies in the lowest elevation region of the state, Dixie, with most of the city lying below 3,000 feet (900 m). The city is surrounded by mountains and red sandstone buttes, and it lies at the very northeastern edge of the Mojave Desert. The Virgin River flows through the city. The Santa Clara River also flows on the east side of the city before merging with the Virgin River to the south. In early 2005, major flooding occurred within these two rivers. One person was killed and several houses were destroyed by the raging Santa Clara River.

The city borders Arizona, and is located between the towns of Santa Clara and Ivins to the west and Washington to the east. The core of the city, including its downtown, Dixie State College, convention center, and hospital, are located in a small valley overlooking the Virgin River and surrounded by low lava and sandstone bluffs. The city’s southern section, Bloomington, is more typical of the Mojave Desert, with desert scrub and gravel dominating the landscape. The southeast part of the city contains some farming along the Virgin River, but like the west and northwest parts of the city has become increasingly dominated by suburban-style development.

In Southern Utah, soil and rock formations are red in appearance due to the presence of iron oxide.[11] Although portions of the older section of the city (particularly the southern part near the Virgin River) lie on floodplain alluvium, much of St. George is built directly upon Jurassic, Triassic, and Permian period sedimentary bedrock. The following formations—listed in chronological order—can be found within the city limits.

Kaibab Limestone (Permian): Grey fossiliferious limestone, exposed at the center of the Virgin River anticline along Horseman Park Drive and in the low hills to the south of South Bloomington Hills.

Moenkopi Formation (Triassic): Chocolatey-red and white banded mudstone, shale, limestone, and siltstone containing thick layers of gypsum, exposed at Bloomington, South Bloomington Hills, and the south side of Webb Hill.

Shinarump Conglomerate (Triassic): Yellow to brown cliff-forming sandstone and conglomerate containing fossilized oyster shells and petrified wood. Forms the cliff faces north of Bloomington, on Webb Hill, and along the Virgin River south of 1450 South Street. This is actually the lowest member of the Chinle formation.

Chinle Formation (Triassic): Purple, white, grey and locally green bentonitic shale weathering to clay. Because of the softness of the strata, structures built on this formation run a higher risk of settling or slippage. The Chinle formation underlies large portions of St. George, including North Bloomington Hills, much of Green Valley, and much of the east part of the city around Riverside Drive and Pine View High School.

Moenave Formation (Jurassic): Red and orange sandstone, siltstone, and mudstone. There is some confusion about distinguishing between the Springdale sandstone member of the Moenave formation and the overlying Navajo sandstone, which is similar in appearance, in the St. George area. It is now generally assumed that the red cliffs to the north of the old part of the city (north of Red Hills Parkway) and at the Dixie Red Hills golf course are part of the Moenave formation. Other exposures include cuts into the east and west Black Hills and the southern part of Dixie Downs.

Kayenta Formation (Jurassic): Red, orange, and purple sandstone, shale, and mudstone. Forms slopes below the massive Navajo sandstone in the northern part of the city including northern Dixie Downs and along Snow Canyon Parkway.

Navajo Sandstone (Jurassic): Grey to brown, red, and (in its upper layers) white massive sandstone. Forms cliff faces above Snow Canyon Parkway and white outcrops at Winchester Hills.

Basaltic lava flows from the Quaternary period form the black ridges to the east and west of the old part of St. George city. The volcanic eruptions producing these flows are thought to date back 1.2 million years.

St. George straddles the line between the Colorado Plateau region to the east with its mesas, and the basin and range to the west with its broad landscapes and cactus forests. Other points of geologic interest include the Virgin River anticline; the rock has eroded away in the center leaving shear walls surrounding the "Purgatory Flats" area to the east of St. George. Another geologic feature is Pine Valley Mountain, composed of one solid piece of granite, it is one of the largest laccoliths in the world.

Along with its increasing population, the economy of St. George and surrounding areas has boomed in recent years.

One of St. George’s most significant corporations is SkyWest Airlines, which has its corporate headquarters in St. George. Wal-Mart has a large distribution center located near St. George. In 2003, Intermountain Health Care opened a new 0 million, 196 bed, 420,000-square-foot (39,000 m2) hospital building.

A large part of the economy of southwestern Utah comes from tourism. St. George is in proximity to Zion National Park and Bryce Canyon National Park, as well as several state parks and recreational areas. It is a little less than an hour drive from the Tony award winning Utah Shakespearean Festival. Golf also plays a large part in the city’s tourism industry. St. George offers one of the highest number of golf courses per capita in the country. Special events such as the St. George Marathon and the Huntsman Senior Games draw thousands to St. George each year. The St. George Marathon is currently the 13th largest marathon in the country.

en.wikipedia.org/wiki/St._George,_Utah

St. George, Utah (8)


Bild von Ken Lund
St. George is a city located in the southwestern part of the U.S. state of Utah, and the county seat of Washington County, Utah. It is the principal city of and is included in the St. George, Utah Metropolitan Statistical Area. The city is 119 miles (192 km) northeast of Las Vegas, Nevada, and 303 miles (488 km) south of Salt Lake City on Interstate 15.

According to the U.S. Census Bureau, St. George had a population of 72,718 in 2007, up from 49,728 in 2000. In 2005, St. George surpassed Layton as the eighth-largest city in Utah. From 1990 to 2000, St. George beat Las Vegas by a mere 0.6% as the fastest-growing metropolitan area in the U.S. This trend has continued, with St. George being declared the second fastest-growing metropolitan area in the U.S. (behind Greeley, Colorado) in September 2005. In 2007, the metropolitan area (defined as Washington County) had an estimated 140,908 residents. The population of St. George and surrounding cities in 2050 is projected to be at more than 700,000 residents.

St. George is the population and commercial center of Utah’s Dixie, a nickname given to the area when Mormon pioneers grew cotton in the warm climate. St. George’s trademark is its geology — red bluffs make up the northern part of the city with two peaks covered in lava rock in the city’s center. The northeastern edges of the Mojave Desert are visible to the south. Zion National Park can be seen to the east, and the Pine Valley Mountains loom over the city to the north and northwest. The climate has more in common with the Desert Southwest than the rest of the state, with scorching hot summers and mild, mostly snowless winters. The city has recently developed into a major retirement destination.

St. George was founded as a cotton mission in 1861 under the direction of Brigham Young, the President of The Church of Jesus Christ of Latter-day Saints (the Mormons or LDS Church)— part of a greater church effort to become self-sufficient. While the early settlers did manage to grow cotton, it was never produced at competitive market rates; consequently, cotton farming was eventually abandoned.

At the outbreak of the Civil War in 1861, Brigham Young organized the settlement of what is now Washington County, Utah.

“Fearing that, the war would take away the cotton supply, he began plans for raising enough in this western country to supply the needs of his people. Enough favorable reports had come to him from this warm country below the rim of the [Great] Basin, that he was convinced cotton could be raised successfully here. At the general church conference in Salt Lake City on October 6th, [1861], about three hundred families were “called" to the Dixie mission to promote the cotton industry. Most of the people knew nothing of this expedition until their names were read from the pulpit; but in nearly every case, they responded with good will, and made ready to leave within the month’s time allotted to them. The families were selected so as to ensure the communities the right number of farmers, masons, blacksmiths, businessmen, educators, carpenters, as needed.”

The settlement was named after George A. Smith, an apostle of The Church of Jesus Christ of Latter-day Saints.

In April 1877, the LDS Church completed the St. George Utah Temple. It is the Church’s third temple, and, currently, its longest continually-operating temple.

According to the United States Census Bureau, the city has a total area of 64.9 square miles (168.0 km²), of which, 64.4 square miles (166.8 km²) of it is land and 0.5 square miles (1.2 km²) of it (0.72%) is water.

St. George lies in the lowest elevation region of the state, Dixie, with most of the city lying below 3,000 feet (900 m). The city is surrounded by mountains and red sandstone buttes, and it lies at the very northeastern edge of the Mojave Desert. The Virgin River flows through the city. The Santa Clara River also flows on the east side of the city before merging with the Virgin River to the south. In early 2005, major flooding occurred within these two rivers. One person was killed and several houses were destroyed by the raging Santa Clara River.

The city borders Arizona, and is located between the towns of Santa Clara and Ivins to the west and Washington to the east. The core of the city, including its downtown, Dixie State College, convention center, and hospital, are located in a small valley overlooking the Virgin River and surrounded by low lava and sandstone bluffs. The city’s southern section, Bloomington, is more typical of the Mojave Desert, with desert scrub and gravel dominating the landscape. The southeast part of the city contains some farming along the Virgin River, but like the west and northwest parts of the city has become increasingly dominated by suburban-style development.

In Southern Utah, soil and rock formations are red in appearance due to the presence of iron oxide.[11] Although portions of the older section of the city (particularly the southern part near the Virgin River) lie on floodplain alluvium, much of St. George is built directly upon Jurassic, Triassic, and Permian period sedimentary bedrock. The following formations—listed in chronological order—can be found within the city limits.

Kaibab Limestone (Permian): Grey fossiliferious limestone, exposed at the center of the Virgin River anticline along Horseman Park Drive and in the low hills to the south of South Bloomington Hills.

Moenkopi Formation (Triassic): Chocolatey-red and white banded mudstone, shale, limestone, and siltstone containing thick layers of gypsum, exposed at Bloomington, South Bloomington Hills, and the south side of Webb Hill.

Shinarump Conglomerate (Triassic): Yellow to brown cliff-forming sandstone and conglomerate containing fossilized oyster shells and petrified wood. Forms the cliff faces north of Bloomington, on Webb Hill, and along the Virgin River south of 1450 South Street. This is actually the lowest member of the Chinle formation.

Chinle Formation (Triassic): Purple, white, grey and locally green bentonitic shale weathering to clay. Because of the softness of the strata, structures built on this formation run a higher risk of settling or slippage. The Chinle formation underlies large portions of St. George, including North Bloomington Hills, much of Green Valley, and much of the east part of the city around Riverside Drive and Pine View High School.

Moenave Formation (Jurassic): Red and orange sandstone, siltstone, and mudstone. There is some confusion about distinguishing between the Springdale sandstone member of the Moenave formation and the overlying Navajo sandstone, which is similar in appearance, in the St. George area. It is now generally assumed that the red cliffs to the north of the old part of the city (north of Red Hills Parkway) and at the Dixie Red Hills golf course are part of the Moenave formation. Other exposures include cuts into the east and west Black Hills and the southern part of Dixie Downs.

Kayenta Formation (Jurassic): Red, orange, and purple sandstone, shale, and mudstone. Forms slopes below the massive Navajo sandstone in the northern part of the city including northern Dixie Downs and along Snow Canyon Parkway.

Navajo Sandstone (Jurassic): Grey to brown, red, and (in its upper layers) white massive sandstone. Forms cliff faces above Snow Canyon Parkway and white outcrops at Winchester Hills.

Basaltic lava flows from the Quaternary period form the black ridges to the east and west of the old part of St. George city. The volcanic eruptions producing these flows are thought to date back 1.2 million years.

St. George straddles the line between the Colorado Plateau region to the east with its mesas, and the basin and range to the west with its broad landscapes and cactus forests. Other points of geologic interest include the Virgin River anticline; the rock has eroded away in the center leaving shear walls surrounding the "Purgatory Flats" area to the east of St. George. Another geologic feature is Pine Valley Mountain, composed of one solid piece of granite, it is one of the largest laccoliths in the world.

Along with its increasing population, the economy of St. George and surrounding areas has boomed in recent years.

One of St. George’s most significant corporations is SkyWest Airlines, which has its corporate headquarters in St. George. Wal-Mart has a large distribution center located near St. George. In 2003, Intermountain Health Care opened a new 0 million, 196 bed, 420,000-square-foot (39,000 m2) hospital building.

A large part of the economy of southwestern Utah comes from tourism. St. George is in proximity to Zion National Park and Bryce Canyon National Park, as well as several state parks and recreational areas. It is a little less than an hour drive from the Tony award winning Utah Shakespearean Festival. Golf also plays a large part in the city’s tourism industry. St. George offers one of the highest number of golf courses per capita in the country. Special events such as the St. George Marathon and the Huntsman Senior Games draw thousands to St. George each year. The St. George Marathon is currently the 13th largest marathon in the country.

en.wikipedia.org/wiki/St._George,_Utah

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