Hell Creek Formation includes an isolated section that was designated a monument on which date?
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Hell Creek Formation The Hell Creek Formation is an intensively-studied division of mostly Upper Cretaceous and some lower Paleocene rocks in North America, named for exposures studied along Hell Creek, near Jordan, Montana. The formation includes portions of Montana, North Dakota, South Dakota, and Wyoming. In Montana, the Hell Creek Formation overlies the Fox Hills Formation. "Pompey's Pillar" at the Pompeys Pillar National Monument is a small isolated section of the Hell Creek Formation.
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Pompeys Pillar National Monument Pompeys Pillar National Monument is a rock formation located in south central Montana, United States. Designated a National Monument on January 17, 2001, and managed by the U.S. Bureau of Land Management, it consists of only 51 acre , making it one of the smallest National Monuments in the U.S. It was previously designated a National Historic Landmark on July 25, 1965. The new Pompeys Pillar Interpretive Center opened in 2006. Exhibits in the 5,700-square foot center relate the journey of Captain William Clark and his detachment, including Sacagawea and her son Pomp, down the Yellowstone River Valley in 1806.
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Independence Rock (Wyoming) Independence Rock is a large granite rock, approximately 130 ft high, 1900 ft long and 850 ft wide, in southwestern Natrona County, Wyoming, along Wyoming Highway 220. During the middle of the 19th century, the rock was a prominent and well-known landmark on the Oregon, Mormon, and California emigrant trails. Many of these emigrants carved their names on the rock, and it was described by early missionary and explorer Father Pierre-Jean De Smet in 1840 as the "Register of the Desert". The site was designated a National Historic Landmark on January 20, 1961. It is now part of Independence Rock State Historic Site, owned and operated by the state of Wyoming.
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Cascade–Siskiyou National Monument The Cascade–Siskiyou National Monument is a national monument that protects 86,774 acre of forest and grasslands at the junction of the Cascade Range and the Siskiyou Mountains in southwestern Oregon and northwestern California, United States. The monument is managed by the Bureau of Land Management as part of the National Landscape Conservation System and was established in a presidential proclamation by President Bill Clinton on June 9, 2000.
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Sitka National Historical Park Sitka National Historical Park (earlier known as Indian River Park and Totem Park) is a national historical park in Sitka in the U.S. state of Alaska. It was redesignated as a national historical park from its previous status as national monument on October 18, 1972. The park in its various forms has sought to commemorate the Tlingit and Russian experiences in Alaska.
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Boulder Creek Formation The Boulder Creek Formation is a geologic formation in northeastern British Columbia. It was named for a tributary to Commotion Creek in the Pine Pass area by E.M. Spieker in 1921. At one time considered to be a member of the Commotion Formation, it was elevated to formation status by D.F. Stott in 1982.
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Monument, Colorado The Town of Monument is a statutory town situated at the base of the Rampart Range in El Paso County, Colorado, United States. Monument is bordered by Pike National Forest on the west, Colorado Springs and the United States Air Force Academy to the south, foothills and rock outcroppings to the north, and rolling plains to the east. Monument was first settled as a stop along the Rio Grande Railroad in 1872, and the area was incorporated as a town called Henry's Station in 1879, but the name was later changed to Monument. The town population was 5,530 at the 2010 United States Census, an increase of 181% from the population of 1,971 in 2000.
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Newberry National Volcanic Monument Newberry National Volcanic Monument was designated on November 5, 1990, to protect the area around the Newberry Volcano in the United States. It was created within the boundaries of the Deschutes National Forest and is managed by the U.S. Forest Service. It includes 50000 acre of lakes, lava flows, and spectacular geologic features in central Oregon.
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Billman Creek Formation The Billman Creek Formation is a Mesozoic geologic formation in south-central Montana. Dinosaur remains are among the fossils that have been recovered from the formation, although none have yet been referred to a specific genus.
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Paint Creek Formation The Paint Creek Formation is a geologic formation in Illinois. It preserves fossils dating back to the Carboniferous period.
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Garita Creek Formation The Garita Creek Formation is a Mesozoic geologic formation in New Mexico. Dinosaur remains are among the fossils that have been recovered from the formation, although none have yet been referred to a specific genus.
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Browns Canyon National Monument Browns Canyon National Monument is a 21,586 acre national monument in Chaffee County, Colorado that was designated as such by President Barack Obama under the Antiquities Act on February 19, 2015. The site will be centered along the Arkansas River between Buena Vista and Salida. Browns Canyon is the most popular destination for whitewater rafting in the country, and is also known for its fishing and hiking. The monument will provide habitat protection for bighorn sheep, peregrine falcons, elk, and golden eagles.
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32nd Indiana Monument The 32nd Indiana Monument, also known as the August Bloedner Monument, honors the Union soldiers of the 32nd Indiana Volunteer Infantry Regiment, also known as Indiana's "1st German" regiment, who died in the Battle of Rowlett's Station on 17 December 1861, near Munfordville, Kentucky. Originally placed at Fort Willich, near Munfordville, in January 1862, the monument was moved to Cave Hill National Cemetery at Louisville, Kentucky, in June 1867. Due to its fragile condition, the monument was removed from the national cemetery in 2008. After undergoing conservation treatment at the University of Louisville, it was placed on display at the Frazier History Museum lobby in August 2010. Although it is no longer in its original location, the 32nd Indiana Monument is generally considered to be the oldest surviving memorial to the American Civil War. A replacement monument at Cave Hill National Cemetery was dedicated in December 2011.
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Hagerman Fossil Beds National Monument Hagerman Fossil Beds National Monument near Hagerman, Idaho, contains the largest concentration of Hagerman horse fossils in North America. The fossil horses for which the monument is famous have been found in only one locale in the northern portion of the monument called the Hagerman Horse Quarry. The 4,351-acre (17.6 km) monument is internationally significant because it protects the world's richest known fossil deposits from the late Pliocene epoch, 3.5 million years ago. These plants and animals represent the last glimpse of that time that existed before the Ice Age, and the earliest appearances of modern flora and fauna. This is also significant because the fossils present during this period of the Pliocene represent species which were alive during the early stages in the evolution of man, albeit on a different continent. The fossil beds were designated a National Natural Landmark in 1975.
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Pennsylvania State Memorial, Gettysburg The Pennsylvania State Memorial is a monument in Gettysburg National Military Park that commemorates the 34,530 Pennsylvania soldiers who fought in the July 1 to 3, 1863 Battle of Gettysburg during the American Civil War. The memorial stands along Cemetery Ridge, the Union battle line on July 2, 1863. Completed in 1914, it is the largest of the state monuments on the Gettysburg Battlefield.
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Sir Bevil Grenville's Monument Sir Bevil Grenville's Monument is a monument erected in 1720 on Lansdown, then called "Lansdowne Hill", 4 mi north-west of the city of Bath, in Somerset, England. It was designated a Grade II* listed building on 1 February 1956, and a scheduled monument on 12 December 1950.
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Coon Creek Formation The Coon Creek Formation is a geologic formation located in western Tennessee and extreme northeast Mississippi. It is a sedimentary sandy marl deposit, Late Cretaceous (Maastrichtian) in age, about 70 million years old. The formation is known for producing mosasaurs and plesiosaurs, particularly at Coon Creek in McNairy County, Tennessee, which the formation is named for. Additionally, the formation produces many other marine invertebrates such as "Turritella" and the state fossil of Tennessee, the bivalve "Pterotrigonia thoracica", as well as other fossils such as crabs.
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Devil's Garden Devils Garden is an area of Arches National Park, located near Moab, Utah, United States, that features a series of rock fins and arches formed by erosion. The Devils Garden Trail, including more primitive sections and spurs, meanders through the area for 7.2 mi . The trailhead leads directly to Landscape Arch after a 0.8 mi outbound hike, while Tunnel Arch and Pine Tree Arch can be seen on spur trails on the way to Landscape Arch. Several other arches, including Partition, Navajo, Double O, and Private Arch, as well as the Dark Angel monolith and Fin Canyon, are accessed via the primitive loop trail and its spurs.
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Arch Creek Petroglyphs The Arch Creek Petroglyphs, also known as Site 48CK41 are Native American rock art figures located in Crook County, Wyoming. The site, in the southern Black Hills, is unusual in featuring comparatively long, narrow line figures incised on the rock, compared to more common V-necked anthropomorphs and shield figures. The site is particularly well preserved and is protected.
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Hermits Rest Hermits Rest is a structure built in 1914 at the western end of Hermit Road at the south rim of the Grand Canyon in Arizona, United States. The Hermit Trail, a hiking trail that extends to the Colorado River, begins about ¼ mile beyond the shuttle bus stop at Hermit's Rest. Hermits Rest also represents the western terminus of the Rim Trail. The location was named for Louis Boucher. Around 1891, Boucher - a Canadian-born prospector - staked claims below present-day Hermits Rest. With help, Boucher carved the aforementioned trail into the canyon, and for years lived alone at nearby Dripping Springs. The main structure currently standing at Hermits Rest was designed by architect Mary Colter. Hermits Rest is the westernmost point on the canyon's south rim that is accessible by paved road. It was built as a rest area for tourists on coaches operated by the Fred Harvey Company on the way to the now-vanished Hermit Camp. The building was designed to appear to be a natural stone formation, closely tied to the land. Colter selected furnishings that are included in the National Historic Landmark designation.
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Hole in the Rock Trail The Hole in the Rock Trail (often hyphenated as Hole-in-the-Rock) is a historic trail running east-southeast from the town of Escalante in southern Utah in the western United States. The Mormon trailblazers who established this trail crossed the Colorado River and ended their journey in the town of Bluff. The Hole-in-the-Rock expedition established the trail in 1879. The trail is located within the borders of the Grand Staircase-Escalante National Monument, the adjacent Glen Canyon National Recreation Area and federal Bureau of Land Management (BLM) public land to the east of the Colorado River. A geologic feature called the Hole in the Rock gave the trail its name. A modern unpaved road called the Hole-in-the-Rock Road (BLM Road 200) closely follows this historic trail to the point where it enters the Glen Canyon National Recreation Area. The modern road is an important access route for visiting the Canyons of the Escalante and the Devil's Garden. The trail is listed on the National Register of Historic Places, being added to that list in 1982.
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Jonathan Creek archaeological site Jonathan Creek archaeological site is an important Mississippian-era (ca. A.D. 1000-1500) village and burial mound site, situated on the banks of the Tennessee River, located in the unincorporated town of Aurora in Marshall county, Kentucky. It was originally discovered and noted by Robert Loughridge in the late 19th century. C.B. Moore returned in 1914-1915; however, his work failed to recover many significant artifacts. Further research of the site was initiated by William S. Webb with William D. Funkhouser in the 1930s, with excavations beginning in 1940 by the Civilian Conservation Corps. The project ended only 2 years later when the US entered into WWII. Webb published his findings in 1952. The reports revealed the remnants of 89 structures within a fortified stockade enclosure. The approximate occupation of this area dates from approximately 1200 AD to 1300 AD The original analysis of Dr. Webb was expanded upon by Dr. Sissel Schroeder who continued this work in the 1990s.