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Castle Rock (San Juan County, Utah)
Castle Rock is a summit in San Juan County, Utah, United States. Description Castle Rock is situated north-northeast of the Monument Valley Tribal Park Visitor Center, on Navajo Nation land. It is an iconic landform of Monument Valley and can be seen from Highway 163. Precipitation runoff from this landform's slopes drains into the San Juan River drainage basin. Topographic relief is significant as the summit rises above the surrounding terrain in 0.25 mile (0.4 km). This landform's toponym has been officially adopted by the United States Board on Geographic Names. It is so named because the butte resembles the silhouette of a castle. The first ascent of the summit was made on May 8, 1960, by Harvey T. Carter, Layton Kor, and John Auld. Geology Castle Rock is composed of three principal strata. The bottom layer is slope-forming Organ Rock Shale, the next stratum is cliff-forming De Chelly Sandstone, and the upper layer is Moenkopi Formation. The rock ranges in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brighams Tomb
Brighams Tomb is a summit in San Juan County, Utah, United States. Description Brighams Tomb is situated northeast of Oljato–Monument Valley, Utah, on Navajo Nation land. It is an iconic landform of Monument Valley and can be seen from Highway 163. Precipitation runoff from this landform's slopes drains into the San Juan River drainage basin. Topographic relief is significant as the summit rises above the surrounding terrain in 0.25 mile (0.4 km). The mountain's name refers to Brigham Young, the first governor of the Utah Territory. This landform's toponym was officially adopted/revised in 1988 by the United States Board on Geographic Names after having been officially named "Saddleback" from 1964 through 1987. Some older maps will still show the Saddleback name. Geology Brighams Tomb is composed of three principal strata. The bottom layer is slope-forming Organ Rock Shale, the next stratum is cliff-forming De Chelly Sandstone, and the upper layer is Moenkopi For ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Harvey T
Harvey, Harveys or Harvey's may refer to: Arts, entertainment, and media * ''Harvey'' (play), a 1944 play by Mary Chase about a man befriended by an invisible anthropomorphic rabbit * Harvey Awards ("Harveys"), one of the most important awards in American comic industry, founded in 1988 * "Harvey", a song by Her's off the album ''Invitation to Her's'', 2018 Films * ''Harvey'' (1950 film), a 1950 film adapted from Mary Chase's play, starring James Stewart * ''Harvey'' (1996 film), a 1996 American made-for-television remake of the 1950 film * ''Harvey'' (2023 film), a Canadian animated short film * ''Harvey'' (Hallmark), a 1972 adaptation of Mary Chase's play for the ''Hallmark Hall of Fame'' Characters * Harvey (''Farscape''), a character in the TV show ''Farscape'' * Harvey, a crane engine in ''Thomas & Friends'' * Harvey Beaks, in the Nickelodeon animated series '' Harvey Beaks'' * Harvey Birdman, title character from the teen-adult animated series ''Harvey Birdman, A ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
King-on-his-Throne
King-on-his-Throne is a summit in San Juan County, Utah, United States. Description King-on-his-Throne is situated north-northeast of the Monument Valley Tribal Park Visitor Center, on Navajo Nation land. It is an iconic landform of Monument Valley and can be seen from Highway 163. Precipitation runoff from this landform's slopes drains into the San Juan River drainage basin. Topographic relief is significant as the summit rises above the surrounding terrain in 0.2 mile (0.32 km). This landform's toponym has been officially adopted by the United States Board on Geographic Names. It is so named because the butte resembles a king sitting on a throne looking south to the valley. The first ascent of the summit was made in 1967 by Fred Beckey, Marlene Dalluge, Joe Brown, and Don Liska. Geology King-on-his-Throne is composed of two principal strata. The bottom layer is slope-forming Organ Rock Shale and the upper stratum is cliff-forming De Chelly Sandstone. The rock ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Castle Butte (Valley Of The Gods)
Castle Butte is a summit in San Juan County, Utah, United States. Description Castle Butte is situated west of Bluff, Utah, in the Valley of the Gods, on land administered by the Bureau of Land Management. Precipitation runoff from this iconic landform's slopes drains to the San Juan River via Lime Creek. Access to the butte is via the 17-mile Valley of the Gods Road which makes a change of direction loop around this butte. Topographic relief is significant as the summit rises above the surrounding terrain in 0.15 mile (0.24 km). This landform's toponym has been officially adopted as Castle Butte by the United States Board on Geographic Names, however it is also known as Eagle Plume Tower. The first ascent of the summit was made in 1976 by Bill Forrest and Frank Luptom via the South Face. Geology Castle Butte is composed of two principal strata of the Cutler Formation. The bottom layer is slope-forming Halgaito Formation and the upper stratum is cliff-forming C ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Appearances Of Monument Valley In The Media
Monument Valley, located on the Navajo Nation within Arizona and Utah, has been featured in many forms of media since the 1930s. It is perhaps most famous for its use in many John Ford films, such as ''Stagecoach'' (1939) and ''The Searchers'' (1956). It has also been featured in such films as '' Easy Rider'' (1969), directed by and co-starring Dennis Hopper; ''Forrest Gump'' (1994), directed by Robert Zemeckis, and '' The Eiger Sanction'' (1975), directed by and starring Clint Eastwood; and in two episodes of the popular United Kingdom television show ''Doctor Who'': " The Impossible Astronaut" (23 April 2011) and " Day of the Moon" (30 April 2011). The twin buttes of Monument Valley (" the Mittens"), the "Totem Pole", and the "Ear of the Wind" arch, among other features, have developed iconic status. They have appeared in many television programs, commercials, and Hollywood movies, especially Westerns. Motion pictures Films *'' The Vanishing American'' (1925) *'' The Lone ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Forrest Gump
''Forrest Gump'' is a 1994 American comedy-drama film directed by Robert Zemeckis. An adaptation of the Forrest Gump (novel), 1986 novel by Winston Groom, the screenplay of the film is written by Eric Roth. It stars Tom Hanks in the title role, alongside Robin Wright, Gary Sinise, Mykelti Williamson, and Sally Field in lead roles. The film follows the life of an Alabama man named Forrest Gump (Hanks) and his experiences in the 20th century in the United States, 20th-century United States. Principal photography took place between August and December 1993, mainly in Georgia (U.S. state), Georgia, North Carolina, and South Carolina. Extensive visual effects were used to incorporate Hanks into archived footage and to develop other scenes. The Forrest Gump (soundtrack), soundtrack features songs reflecting the different periods seen in the film. Various interpretations have been made of the protagonist and the film's political symbolism. ''Forrest Gump'' was released in the Unite ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Diurnal Temperature Variation
In meteorology, diurnal temperature variation is the variation between a high air temperature and a low temperature that occurs during the same day. Temperature lag Temperature lag, also known as thermal inertia, is an important factor in diurnal temperature variation. Peak daily temperature generally occurs ''after'' noon, as air keeps absorbing net heat for a period of time from morning through noon and some time thereafter. Similarly, minimum daily temperature generally occurs substantially after midnight, indeed occurring during early morning in the hour around dawn, since heat is lost all night long. The analogous annual phenomenon is seasonal lag. As solar energy strikes the Earth's surface each morning, a shallow layer of air directly above the ground is heated by conduction. Heat exchange between this shallow layer of warm air and the cooler air above is very inefficient. On a warm summer's day, for example, air temperatures may vary by from just above the ground t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Semi-arid Climate
A semi-arid climate, semi-desert climate, or steppe climate is a dry climate sub-type. It is located on regions that receive precipitation below potential evapotranspiration, but not as low as a desert climate. There are different kinds of semi-arid climates, depending on variables such as temperature, and they give rise to different biomes. Defining attributes of semi-arid climates A more precise definition is given by the Köppen climate classification, which treats steppe climates (''BSh'' and ''BSk'') as intermediates between desert climates (BW) and humid climates (A, C, D) in ecological characteristics and agricultural potential. Semi-arid climates tend to support short, thorny or scrubby vegetation and are usually dominated by either grasses or shrubs as they usually cannot support forests. To determine if a location has a semi-arid climate, the precipitation threshold must first be determined. The method used to find the precipitation threshold (in millimeters): * ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Köppen Climate Classification
The Köppen climate classification divides Earth climates into five main climate groups, with each group being divided based on patterns of seasonal precipitation and temperature. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (temperate), ''D'' (continental), and ''E'' (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' indicates a tropical rainforest climate. The system assigns a temperature subgroup for all groups other than those in the ''A'' group, indicated by the third letter for climates in ''B'', ''C'', ''D'', and the second letter for climates in ''E''. Other examples include: ''Cfb'' indicating an oceanic climate with warm summers as indicated by the ending ''b.'', while ''Dwb'' indicates a semi-Monsoon continental climate, monsoonal continental climate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Triassic
The Triassic ( ; sometimes symbolized 🝈) is a geologic period and system which spans 50.5 million years from the end of the Permian Period 251.902 million years ago ( Mya), to the beginning of the Jurassic Period 201.4 Mya. The Triassic is the first and shortest period of the Mesozoic Era and the seventh period of the Phanerozoic Eon. Both the start and end of the period are marked by major extinction events. The Triassic Period is subdivided into three epochs: Early Triassic, Middle Triassic and Late Triassic. The Triassic began in the wake of the Permian–Triassic extinction event, which left the Earth's biosphere impoverished; it was well into the middle of the Triassic before life recovered its former diversity. Three categories of organisms can be distinguished in the Triassic record: survivors from the extinction event, new groups that flourished briefly, and other new groups that went on to dominate the Mesozoic Era. Reptiles, especially archosaurs, were the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Permian
The Permian ( ) is a geologic period and System (stratigraphy), stratigraphic system which spans 47 million years, from the end of the Carboniferous Period million years ago (Mya), to the beginning of the Triassic Period 251.902 Mya. It is the sixth and last period of the Paleozoic Era; the following Triassic Period belongs to the Mesozoic Era. The concept of the Permian was introduced in 1841 by geologist Sir Roderick Murchison, who named it after the Perm Governorate, region of Perm in Russia. The Permian witnessed the diversification of the two groups of amniotes, the synapsids and the Sauropsida, sauropsids (reptiles). The world at the time was dominated by the supercontinent Pangaea, which had formed due to the collision of Euramerica and Gondwana during the Carboniferous. Pangaea was surrounded by the superocean Panthalassa. The Carboniferous rainforest collapse left behind vast regions of desert within the continental interior. Amniotes, which could better cope with these ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moenkopi Formation
The Moenkopi Formation is a geological formation that is spread across the U.S. states of New Mexico, northern Arizona, Nevada, southeastern California, eastern Utah and western Colorado. This unit is considered to be a Geological unit, group in Arizona. Part of the Colorado Plateau and Basin and Range Province, Basin and Range, this red sandstone was laid down in the Early Triassic, Lower Triassic and possibly part of the Middle Triassic, around 240 million years ago. History of investigation There is no designated Type locality (geology), type locality for this formation. It was named for a development at the mouth of Moencopie Wash in the Grand Canyon area by Ward in 1901. In 1917 a 'substitute' type locality was located by Gregory in the wall of the Little Colorado Canyon, about 5 miles below Tanner Crossing in Coconino County, Arizona. While in the Great Basin, Bassler and Reeside characterized and named the Rock Canyon Conglomerate, Virgin Limestone, and Shnabkaib Shale ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
