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Emery, Utah
Emery is a town in Emery County, Utah, United States. The population was 288 at the 2010 census. History Prehistoric Emery sits at the base of the mountains that contain the North Horn Formation. Named after North Horn Mountain, near Castle Dale, this formation in Emery County contain numerous Cretaceous- and Tertiary-era fossil invertebrates, microfossils and palynomorphs. Flagstaff Peak, north of Emery, has abundant dinosaur bone material, prehistoric mammal remains, and petrified dinosaur footprints. The elevation is around 7000 Fremont people, the Old Spanish Trail, and exploration The Fremont culture or Fremont people is a pre-Columbian archeological culture who existed in the area from AD 700 to 1300. It was adjacent to, roughly contemporaneous with, but distinctly different from the Ancestral Pueblo peoples. The culture received its name from the Fremont River, where the first Fremont sites were discovered. The Fremont River in Utah flows from the Johnson Valley Reservo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Town
A town is a human settlement. Towns are generally larger than villages and smaller than cities, though the criteria to distinguish between them vary considerably in different parts of the world. Origin and use The word "town" shares an origin with the German word , the Dutch word , and the Old Norse . The original Proto-Germanic word, *''tūnan'', is thought to be an early borrowing from Proto-Celtic *''dūnom'' (cf. Old Irish , Welsh ). The original sense of the word in both Germanic and Celtic was that of a fortress or an enclosure. Cognates of ''town'' in many modern Germanic languages designate a fence or a hedge. In English and Dutch, the meaning of the word took on the sense of the space which these fences enclosed, and through which a track must run. In England, a town was a small community that could not afford or was not allowed to build walls or other larger fortifications, and built a palisade or stockade instead. In the Netherlands, this space was a garden, mor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Castle Dale, Utah
Castle Dale is a city in northwestern Emery County, Utah, United States. The population was 1,630 at the 2010 census. It is the county seat of Emery County. History The first settlement at Castle Dale was made in 1879. Geography Castle Dale lies on the north side of Cottonwood Creek, a tributary of the San Rafael River, in Castle Valley. According to the United States Census Bureau, the city has a total area of , all land. Utah State Route 10 passes through the center of town, leading northeast to Price and southwest to Interstate 70. Demographics As of the census of 2000 there were 1,657 people, 508 households, and 420 families residing in the city. The population density was 887.5 people per square mile (342.1/km2). There were 618 housing units at an average density of 331.0 per square mile (127.6/km2). The racial makeup of the city was 95.47% White, 0.06% African American, 0.66% Native American, 0.54% Asian, 0.18% Pacific Islander, 0.91% from other races, and 2. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Capitol Reef National Park
Capitol Reef National Park is an American national park in south-central Utah. The park is approximately long on its northsouth axis and just wide on average. The park was established in 1971 to preserve of desert landscape and is open all year, with May through September being the highest visitation months. Partially in Wayne County, Utah, the area was originally named "Wayne Wonderland" in the 1920s by local boosters Ephraim P. Pectol and Joseph S. Hickman. Capitol Reef National Park was designated a national monument on August 2, 1937, by President Franklin D. Roosevelt to protect the area's colorful canyons, ridges, buttes, and monoliths; however, it was not until 1950 that the area officially opened to the public. Road access was improved in 1962 with the construction of State Route 24 through the Fremont River Canyon. The majority of the nearly long up-thrust formation called the Waterpocket Folda rocky spine extending from Thousand Lake Mountain to Lake Powellis pr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fish Lake (Utah)
Fish Lake is a high alpine lake (elevation approximately ) located in the Fishlake/ Southern Wasatch Plateau region of south-central Utah, United States. It lies within and is the namesake of the Fishlake National Forest. Fish Lake, six miles long and one mile wide, lies in a geologic structure known as a graben valley. It is bounded by the Mytoge Mountains on the southeast shore which sharply rise about 1,000 feet (300 m) above the lake level. Along the northwest shore, the lake is bounded by Fish Lake Hightop Plateau (summit elevation 11,600 ft / 3,500 m). Fish Lake holds rainbow trout, splake, lake trout, kokanee salmon, brown trout, tiger trout and yellow perch. Yellow perch are regarded as an invasive species; there is no bag limit and anglers are encouraged to dispose of any yellow perch caught. The lake is stocked by the Utah Division of Wildlife Resources fish hatchery in Glenwood. The region sees heavy snowfall in the winter, with snowfall occu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fremont River (Utah)
The Fremont River is a long river in southeastern Utah, United States that flows from the Johnson Valley Reservoir, which is located on the Wasatch Plateau near Fish Lake, southeast through Capitol Reef National Park to the Muddy Creek near Hanksville where the two rivers combine to form the Dirty Devil River, a tributary of the Colorado River. Course The Johnson Valley Reservoir is fed by Sevenmile Creek (from the north) and Lake Creek (from the southwest). The Fremont River passes through Fremont, Loa, Lyman, Bicknell, Teasdale, and Torrey and provides year-round irrigation for the agricultural lands of Rabbit Valley and Caineville. Then it heads through Hanksville and afterward to its mouth. Miscellaneous The Fremont River has a drainage area of fed by spring snowmelt off Thousand Lake Mountain, Boulder Mountain, and the northern Henry Mountains. The river is named after John Charles Frémont. It gives its name to the Fremont culture, a Precolumbian archaeological c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ancestral Pueblo Peoples
The Ancestral Puebloans, also known as the Anasazi, were an ancient Native American culture that spanned the present-day Four Corners region of the United States, comprising southeastern Utah, northeastern Arizona, northwestern New Mexico, and southwestern Colorado. They are believed to have developed, at least in part, from the Oshara tradition, which developed from the Picosa culture. The people and their archaeological culture are often referred to as ''Anasazi'', meaning "ancient enemies", as they were called by Navajo. Contemporary Puebloans object to the use of this term, with some viewing it as derogatory. The Ancestral Puebloans lived in a range of structures that included small family pit houses, larger structures to house clans, grand pueblos, and cliff-sited dwellings for defense. They had a complex network linking hundreds of communities and population centers across the Colorado Plateau. They held a distinct knowledge of celestial sciences that found form in their ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Archeological Culture
An archaeological culture is a recurring assemblage of types of artifacts, buildings and monuments from a specific period and region that may constitute the material culture remains of a particular past human society. The connection between these types is an empirical observation, but their interpretation in terms of ethnic or political groups is based on archaeologists' understanding and interpretation and is in many cases subject to long-unresolved debates. The concept of the archaeological culture is fundamental to culture-historical archaeology. Concept Different cultural groups have material culture items that differ both functionally and aesthetically due to varying cultural and social practices. This notion is observably true on the broadest scales. For example, the equipment associated with the brewing of tea varies greatly across the world. Social relations to material culture often include notions of identity and status. Advocates of culture-historical archaeology u ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pre-Columbian
In the history of the Americas, the pre-Columbian era spans from the original settlement of North and South America in the Upper Paleolithic period through European colonization, which began with Christopher Columbus's voyage of 1492. Usually, the era covers the history of Indigenous cultures until significant influence by Europeans. This may have occurred decades or even centuries after Columbus for certain cultures. Many pre-Columbian civilizations were marked by permanent settlements, cities, agriculture, civic and monumental architecture, major earthworks, and complex societal hierarchies. Some of these civilizations had long faded by the time of the first permanent European colonies (c. late 16th–early 17th centuries), and are known only through archaeological investigations and oral history. Other civilizations were contemporary with the colonial period and were described in European historical accounts of the time. A few, such as the Maya civilization, had their own wri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fremont Culture
The Fremont culture or Fremont people is a pre-Columbian archaeological culture which received its name from the Fremont River in the U.S. state of Utah, where the culture's sites were discovered by local indigenous peoples like the Navajo and Ute. In Navajo culture, the pictographs are credited to people who lived before the flood. The Fremont River itself is named for John Charles Frémont, an American explorer. It inhabited sites in what is now Utah and parts of Nevada, Idaho, Wyoming and Colorado from AD 1 to 1301 (2,000–700 years ago). It was adjacent to, roughly contemporaneous with, but distinctly different from the Ancestral Pueblo peoples located to their south. Location Fremont Indian State Park in the Clear Creek Canyon area in Sevier County Utah contains the biggest Fremont culture site in Utah. Thousand-year-old pit houses, petroglyphs, and other Fremont artifacts were discovered at Range Creek, Utah. Nearby Nine Mile Canyon has long been known for its large col ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Palynomorph
Palynology is the "study of dust" (from grc-gre, παλύνω, palynō, "strew, sprinkle" and '' -logy'') or of "particles that are strewn". A classic palynologist analyses particulate samples collected from the air, from water, or from deposits including sediments of any age. The condition and identification of those particles, organic and inorganic, give the palynologist clues to the life, environment, and energetic conditions that produced them. The term is commonly used to refer to a subset of the discipline, which is defined as "the study of microscopic objects of macromolecular organic composition (i.e., compounds of carbon, hydrogen, nitrogen and oxygen), not capable of dissolution in hydrochloric or hydrofluoric acids". It is the science that studies contemporary and fossil palynomorphs (paleopalynology), including pollen, spores, orbicules, dinocysts, acritarchs, chitinozoans and scolecodonts, together with particulate organic matter (POM) and kerogen found in sedime ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Microfossils
A microfossil is a fossil that is generally between 0.001 mm and 1 mm in size, the visual study of which requires the use of light or electron microscopy. A fossil which can be studied with the naked eye or low-powered magnification, such as a hand lens, is referred to as a macrofossil. Microfossils are a common feature of the geological record, from the Precambrian to the Holocene. They are most common in deposits of marine environments, but also occur in brackish water, fresh water and terrestrial sedimentary deposits. While every kingdom of life is represented in the microfossil record, the most abundant forms are protist skeletons or microbial cysts from the Chrysophyta, Pyrrhophyta, Sarcodina, acritarchs and chitinozoans, together with pollen and spores from the vascular plants. Overview A microfossil is a descriptive term applied to fossilized plants and animals whose size is just at or below the level at which the fossil can be analyzed by the naked eye ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Invertebrate
Invertebrates are a paraphyletic group of animals that neither possess nor develop a vertebral column (commonly known as a ''backbone'' or ''spine''), derived from the notochord. This is a grouping including all animals apart from the chordate subphylum Vertebrata. Familiar examples of invertebrates include arthropods, mollusks, annelids, echinoderms and cnidarians. The majority of animal species are invertebrates; one estimate puts the figure at 97%. Many invertebrate taxa have a greater number and variety of species than the entire subphylum of Vertebrata. Invertebrates vary widely in size, from 50 μm (0.002 in) rotifers to the 9–10 m (30–33 ft) colossal squid. Some so-called invertebrates, such as the Tunicata and Cephalochordata, are more closely related to vertebrates than to other invertebrates. This makes the invertebrates paraphyletic, so the term has little meaning in taxonomy. Etymology The word "invertebrate" comes from the Latin word ''vertebra'', whi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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