OpenLLM-France/wikimedia huggingface dataset:
# Navajo Mountain

Navajo Mountain (Navajo: Naatsisʼáán meaning "Earth Head") is a peak in San Juan County, Utah, with its southern flank extending into Coconino County, Arizona, in the United States. It holds an important place in the traditions of three local Native American tribes. The summit is the highest point on the Navajo Nation.

## Geologic history

Navajo Mountain is a prominent free-standing laccolith, a dome-shaped body of igneous rock that intruded into sedimentary layers and lifted up the overlying layer. The igneous rock at the core of the mountain is wrapped in sedimentary layers. Such igneous intrusions have been exposed by erosion and well studied in similar mountain ranges on the Colorado Plateau, such as the Henry Mountains, the Abajo Mountains, and the La Sal Range.
The Colorado Plateau is made of mostly flat-lying layers of sedimentary rock that record paleoclimate extremes ranging from oceans to widespread deserts over the last 1.8 billion years. The peak of Navajo Mountain, at approximately 10,388 feet (3,166 m), is made up of uplifted Dakota Sandstone deposited during the Cretaceous Period (approximately 66-138 million years ago). Other formations exposed on the surface of the mountain include the Jurassic sequence of the Morrison Formation, Entrada Sandstone, Carmel Formation, and Navajo Sandstone.

## Cultural history

The Navajo Mountain region has special cultural significance to the Navajo people, who know it as Naatsisʼáán ("Earth Head" or "Pollen Mountain"). Together with Rainbow Bridge to the northwest, Navajo Mountain figures prominently as the first settlement area in western Navajo origin stories. Following the military defeat of the Diné (Navajo people) by United States forces in 1863, the political landscape was changed by new boundaries and major physical alterations. The establishment of Rainbow Bridge National Monument (1910), and the filling of Glen Canyon by Lake Powell in 1963, has facilitated tourism of this previously remote region. Access to Navajo Mountain is still regulated by the sovereign Navajo Nation, and a permit is required to hike in the region. Climbing the mountain itself is forbidden.
Before becoming part of the Navajo Nation, the area was inhabited by the Ancestral Puebloans. Their descendants, the Hopi, call Navajo Mountain Tokonave, or "Heart of the Earth". Ruins in the area of Navajo Mountain are still strongly associated with certain Hopi clans, with priests still making pilgrimages to shrines in the area.
Before 1933, when the area between the Colorado and San Juan Rivers and the Arizona border was added to the Navajo reservation, the area was known as the Paiute Strip, and the mountain itself was known as Paiute Mountain, due to the population of San Juan Paiutes living between the mountain and Monument Valley.
The community of Navajo Mountain, Utah is to the east.

## Ecology

The Navajo Mountain beardtongue (Penstemon navajoa) is a rare plant limited mainly to the upper elevation slopes of Navajo Mountain.
# Newton Butte

Newton Butte, in the Grand Canyon, Arizona, United States is a prominence below the South Rim, northwest of Grandview Point, and north on a ridgeline from Shoshone Point which is one mile east of Yaki Point, East Rim Drive. Shoshone Point and Yaki are both on access roads from East Rim Drive, with Yaki being the more advantageous to different viewing directions.
Newton Butte is 5,940 feet (1,811 m), and located on a point/ridge, just south of Granite Gorge on the Colorado River. The point location of Newton Butte extends due north from an intermediate point on the South Rim, Shoshone Point, which at the end of the Newton Butte point ridgeline, also forms the west perimeter of the Lonetree Canyon drainage, into Granite Gorge.
Just north of Newton Butte, 3/4 mi on the end of the point, is Pattie Butte, a lower elevation prominence, 5,306 feet (1,617 m).
Two hiking trails are closest to Newton Butte. Across Granite Gorge, views south can be made from the Clear Creek Trail, at lower elevations or as it climbs past Zoroaster Canyon to ridgelines at the west of Clear Creek. The Tonto Trail on the Tonto Platform, south side of Granite Gorge, has the closest hiking points near the bottom elevations of Newton Butte.
Newton Butte is named for Sir Isaac Newton (1642–1727), and was officially adopted in 1906 by the U.S. Board on Geographic Names.

## Access

Newton Butte can be viewed from the South Rim viewpoints from Yavapai Point, Yaki Point, Shoshone Point, or Grandview Point. Access to East Rim Drive. South Rim, is from the east, on Arizona State Route 64, from US 89. A west access to East Rim Drive is from Williams, Arizona, or Flagstaff, by way of U.S. Route 180 in Arizona.

## Gallery

* Newton Butte in bullseye, from Yaki Point. (Pattie Butte lower left)
* Newton Butte on the right
* Newton Butte centered, from the east. (Lyell Butte to left, Newberry Butte to right)
* O'Neill Butte, (above Supai Group 'redbeds'), on ridgeline from Yaki Point; (Newton Butte prominence off photo, right) View northeast, with Cape Royal (point) on Walhalla Plateau (Kaibab Plateau), and flat-top of Wotans Throne and Vishnu Temple prominence. (from Yavapai Point, west of Yaki Point, South Rim)
* (view east-northeast, from Mather Point-(Yavapai Point)) O'Neill Butte, on ridgeline north, from Newton Butte. Pattie Butte sits on an upper platform of Redwall Limestone, overlain by a 2nd-platform of Surprise Canyon Formation. (partly eroded)
# Notch Mountain (Utah)

Notch Mountain is an 11,263-foot-elevation (3,433-meter) mountain summit in Summit County, Utah, United States.

## Description

Notch Mountain is located 50 miles (80 km) east of Salt Lake City in the Uinta-Wasatch-Cache National Forest. It is situated in the western Uinta Mountains which are a subrange of the Rocky Mountains. Precipitation runoff from this mountain drains north into headwaters of the Weber River and south into headwaters of the Provo River. Topographic relief is significant as the summit rises 1,100 feet (335 meters) above Wall Lake (source of the Provo River) in 0.75 mile (1.2 km). Access to the mountain is via the Mirror Lake Highway and hiking the 10-mile Notch Mountain Trail which passes through "The Notch", but does not lead to the summit. The Notch is a 10,621-foot-elevation gap between the 11,263-ft east peak and the 11,258-ft west peak. The mountain's descriptive toponym was officially adopted in 1932 by the U.S. Board on Geographic Names.

## Geology

Notch Mountain is composed of metasedimentary rock of the Mount Watson Formation. Fluvial sediment processes deposited a sequence of nearly white quartz arenite and subarkose interbedded with minor amounts of pale-red arkosic arenite and grayish-green shale during the Late Precambrian. The Uintas were uplifted during the Laramide orogeny about 70 to 50 million years ago. Numerous glacial cycles during the Quaternary Period sculpted the mountain and scoured the surrounding land forming many depressions that are now lakes.

## Climate

Based on the Köppen climate classification, Notch Mountain is located in a subarctic climate zone with cold snowy winters and mild summers. Tundra climate characterizes the summit and highest slopes. The months of July through early October offer the most favorable weather to visit the mountain.
# Ostler Peak

Ostler Peak is a 12,718-foot elevation (3,876 m) mountain summit located in Summit County, Utah, United States.

## Description

Ostler Peak is set within the High Uintas Wilderness on land managed by Uinta-Wasatch-Cache National Forest. It is situated along the crest of the Uinta Mountains which are a subset of the Rocky Mountains, and it ranks as the 37th-highest summit in Utah. Topographic relief is significant as the summit rises over 1,900 feet (580 meters) above Amethyst Lake in one-half mile. Neighbors include Spread Eagle Peak 1.4 mile to the southwest, Hayden Peak four miles west, and line parent Lamotte Peak two miles north-northeast. Precipitation runoff from this mountain drains into the Ostler and Stillwater forks of the Bear River.

## Etymology

The landform's toponym was officially adopted in 1932 by the U.S. Board on Geographic Names to remember the late James Rulon "Dick" Ostler (1900–1931), Uinta National Forest ranger in the Grandaddy Lake region of the Uinta Mountains.

## Climate

Based on the Köppen climate classification, Ostler Peak is located in a subarctic climate zone with cold snowy winters and mild summers. Tundra climate characterizes the summit and highest slopes.
Climate data for Ostler Peak 40.7434 N, 110.7697 W, Elevation: 12,224 ft (3,726 m) (1991–2020 normals) :
| Month | Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec | Year |
| Mean daily maximum °F (°C) | 23.0 (−5.0) | 23.2 (−4.9) | 29.5 (−1.4) | 35.0 (1.7) | 43.3 (6.3) | 53.9 (12.2) | 61.7 (16.5) | 60.1 (15.6) | 52.2 (11.2) | 40.8 (4.9) | 29.2 (−1.6) | 23.1 (−4.9) | 39.6 (4.2) |
| Daily mean °F (°C) | 13.3 (−10.4) | 12.5 (−10.8) | 17.7 (−7.9) | 22.6 (−5.2) | 31.1 (−0.5) | 41.4 (5.2) | 49.2 (9.6) | 47.8 (8.8) | 40.4 (4.7) | 29.8 (−1.2) | 19.5 (−6.9) | 13.3 (−10.4) | 28.2 (−2.1) |
| Mean daily minimum °F (°C) | 3.6 (−15.8) | 1.9 (−16.7) | 6.0 (−14.4) | 10.2 (−12.1) | 18.9 (−7.3) | 28.9 (−1.7) | 36.7 (2.6) | 35.6 (2.0) | 28.5 (−1.9) | 18.7 (−7.4) | 9.8 (−12.3) | 3.5 (−15.8) | 16.9 (−8.4) |
| Average precipitation inches (mm) | 5.63 (143) | 5.36 (136) | 4.99 (127) | 4.98 (126) | 4.27 (108) | 2.95 (75) | 2.17 (55) | 2.00 (51) | 3.33 (85) | 4.33 (110) | 4.13 (105) | 5.02 (128) | 49.16 (1,249) |
| Source: PRISM Climate Group ||||||||||||||

## Gallery

* Ostler Peak and Spread Eagle Peak seen from Christmas Meadows Stillwater Fork of the Bear River in foreground
* Ostler Peak and Spread Eagle Peak seen from Christmas Meadows
* Ostler Peak in autumn
* Amethyst Lake viewed from Ostler Peak
* Lamotte Peak (left), Ostler Peak (center), Spread Eagle Peak (right).
* Ostler Peak in autumn
* Northeast aspect of Ostler Peak viewed from airliner.
# Picketpost Mountain

Picketpost Mountain is located just outside the town of Superior, Arizona approximately 40 miles (64 km) east of the Phoenix Metro Area. The summit stands at an elevation of 4,375 feet (1,133 meters) above sea level, with a prominence 2000 feet above its base. The mountain is located in the southern desert region of Tonto National Forest near, but not within the Superstition Mountains, and is popular with hikers. The mountain is known for an oddly placed mailbox at the top of the mountain, which contains the log books for the Picketpost Mountain Trail.
The mountain's name stems from an early military camp established at the base of the mountain by General George Stoneman in 1870. The soldiers nicknamed the mountain “Picket Post” due to its use as a sentinel position to guard their camp from attacks. This military camp eventually grew into the town of Superior.
# Kalanchoe tetraphylla

Kalanchoe tetraphylla is a species of Kalanchoe native to Madagascar. It is a small shrub with a simple stout stem and usually two pairs of opposite leaves, closely related to Kalanchoe synsepala. Its scientific name is often misapplied by horticulturists to the continental southern African species Kalanchoe luciae.
# Sulphur Peak (Utah)

Sulphur Peak is a summit in the south end of the Pavant Range in Millard County, Utah. It reaches an elevation of 7,020 feet (2,140 m)
# Tetzlaff Peak

Tetzlaff Peak is a 6,267-foot elevation (1,910 m) mountain summit located in Tooele County, Utah, United States.

## Description

Tetzlaff Peak is situated in the Silver Island Mountains which are a subset of the Great Basin Ranges, and it is set on land managed by the Bureau of Land Management. The community of Wendover, Utah, is 10 miles to the southwest and the Bonneville Speedway is five miles to the southeast. Topographic relief is significant as the summit rises 2,000 feet (610 meters) above the Bonneville Salt Flats in one mile. This landform's toponym was officially adopted in 1960 by the U.S. Board on Geographic Names to honor American racecar driver Teddy Tetzlaff (1883–1929). On August 12, 1914, Tetzlaff set a land speed record by driving the Blitzen Benz 142.8 miles per hour (229.8 kilometres per hour) at the Bonneville Salt Flats (then known as Salduro, Utah).

## Climate

Tetzlaff Peak is set in the Great Salt Lake Desert which has hot summers and cold winters. The desert is an example of a cold desert climate as the desert's elevation makes temperatures cooler than lower elevation deserts. Due to the high elevation and aridity, temperatures drop sharply after sunset. Summer nights are comfortably cool. Winter highs are generally above freezing, and winter nights are bitterly cold, with temperatures often dropping well below freezing.

## Gallery

* Tetzlaff Peak (center), Pilot Peak (distant left) from Bonneville Salt Flats
* Southwest aspect
* Rishel Peak (left) and Tetzlaff Peak (center) seen from Volcano Peak. Further in the distance are Graham Peak and Jenkins Peak.
* Volcano Peak (left), Rishel Peak (left of center) and Tetzlaff Peak (right) from Bonneville Salt Flats
* South aspect
* Rishel Peak (left) and Tetzlaff Peak (right)
* Tetzlaff Peak and Bonneville Salt Flats
* Tetzlaff Peak (center), Pilot Peak (distant left) from Bonneville Salt Flats
# Journal of Lutheran Ethics

The Journal of Lutheran Ethics (JLE) is a bimonthly, open access ecclesial academic journal that covers ethical issues from Christian perspectives with special attention to the confessional tradition of the Evangelical Lutheran Church in America (ELCA). It is published by the Theological Discernment Team in the ELCA's Office of the Presiding Bishop. The current editor-in-chief is Jennifer Hockenbery.

## History

The Journal of Lutheran Ethics was established in September 2001 and was published monthly. In 2011 it moved to a bimonthly rhythm. Each issue features book reviews and, since 2019, special features for use in the congregation.
Past editors of the Journal of Lutheran Ethics include Carmelo Santos, James Kenneth Echols, Victor Thasia, and Kaari Reinertson.
Past topics discussed in the Journal of Lutheran Ethics include economic inequality, immigration, abortion, gun control, technology, natural law, genetics and stem cell research, foreign policy, ecumenism, just war, climate change and ecojustice, addiction, end-of-life issues, and Israel-Palestine.
# Shinchi Station

Shinchi Station (新地駅, Shinchi-eki) is a railway station in the town of Shinchi, Fukushima Prefecture, Japan, operated by East Japan Railway Company (JR East). Operation of the station was suspended due to severe damage to the railway and station facilities caused by the 2011 Tōhoku earthquake and tsunami in March 2011. The station reopened at a new location in December 2016.

## Lines

Shinchi Station is served by the Jōban Line and is 315.8 kilometers from the starting point of the line at Nippori in Tokyo. The station is attended.

## Station layout

Prior to the 2011 Tōhoku earthquake and tsunami, Shinchi Station previously had a single island platform and a single side platform connected to the station building by a footbridge. The station was rebuilt with two opposed side platforms.

### Platforms

| 1 | ■ Jōban Line | for Iwanuma and Sendai |
| 2 | ■ Jōban Line | for Sōma and Haranomachi |

## History

Shinchi Station opened on November 10, 1897. The station was absorbed into the JR East network upon the privatization of the Japanese National Railways (JNR) on April 1, 1987.
The station was totally destroyed by the 2011 Tōhoku earthquake and tsunami on 11 March 2011. It reopened at a new location further inland on 10 December 2016.
* The station building in January 2008
* The remains of Shinchi Station, including an E721 series train, after the tsunami in 2011

## Passenger statistics

In 2018, the station was used by an average of 281 passengers daily (boarding passengers only).

## Surrounding area

* National Route 6
* Shinchi town hall
* Shinchi post office
* Tsurushi fishing port
# Kokuryō Station

Kokuryō Station (国領駅, Kokuryō-eki) is a passenger railway station located in the city of Chōfu, Tokyo, Japan, operated by the private railway operator Keio Corporation.

## Lines

Kokuryō Station is served by the Keio Line, and is located 14.2 kilometers from the starting point of the line at Shinjuku Station.

## Station layout

This station consists of one underground island platforms serving two tracks, with the station building located above. The underground tracks opened on August 19, 2012, replacing the ground-level tracks.

### Platforms

| 1 | KO Keiō Line | for Chōfu and Keiō-hachiōji KO Keiō Sagamihara Line for Hashimoto (via Chōfu) KO Keiō Takao Line for Takaosanguchi (via Kitano) |
| 2 | KO Keiō Line | for Meidaimae, Sasazuka, and Shinjuku KO Keiō New Line for Shinjuku S Toei Shinjuku Line for Moto-Yawata |
* The ticket barriers in July 2015
* The underground platforms in August 2012 shortly after opening

## History

The station opened on April 15, 1913, and relocated to its present location on December 17, 1927. The station was rebuilt as an underground station in 2012.

## Passenger statistics

In fiscal 2019, the station was used by an average of 38,713 passengers daily.
The passenger figures (boarding passengers only) for previous years are as shown below.
| Fiscal year | daily average |
| 2005 | 35,086 |
| 2010 | 37,745 |
| 2015 | 38,666 |

## Surrounding area

* National Route 20
* Chōfu Post Office
# Shibasaki Station

Shibasaki Station (柴崎駅, Shibasaki-eki) is a passenger railway station located in the city of Chōfu, Tokyo, Japan, operated by the private railway operator Keio Corporation.

## Lines

Shibasaki Station is served by the Keio Line, and is located 13.3 kilometers from the starting point of the line at Shinjuku Station.

## Station layout

This station consists of two ground-level opposed side platforms serving two tracks, connected to the station building by an underground passage.

### Platforms

| 1 | KO Keiō Line | for Chōfu and Keiō-Hachiōji KO Keiō Sagamihara Line for Hashimoto (via Chōfu) KO Keiō Takao Line for Takaosanguchi (via Kitano) |
| 2 | KO Keiō Line | for Meidaimae, Sasazuka, and Shinjuku KO Keiō New Line for Shinjuku S Toei Shinjuku Line for Moto-Yawata |

## History

The station opened on April 15, 1913 and was relocated to its present location on December 17, 1927.

## Passenger statistics

In fiscal 2019, the station was used by an average of 18,042 passengers daily.
The passenger figures (boarding passengers only) for previous years are as shown below.
| Fiscal year | daily average |
| 2005 | 17,092 |
| 2010 | 17,484 |
| 2015 | 17,226 |

## Surrounding area

* National Route 20
# Kido Station

Kido Station (木戸駅, Kido-eki) is a railway station located in the town of Naraha, Fukushima Prefecture, Japan, operated by the East Japan Railway Company (JR East).

## Lines

Kido Station is served by the Jōban Line, and is located 237.8 km from the official starting point of the line at Nippori Station.

## Station layout

The station has two opposed side platforms connected by a footbridge. The station is unattended.

### Platforms

| 1 | ■ Jōban Line | for Tomioka |
| 2 | ■ Jōban Line | for Iwaki and Mito |

## History

Kido Station opened on August 23, 1898. The station was absorbed into the JR East network upon the privatization of the Japanese National Railways (JNR) on April 1, 1987.
Due to the Fukushima Daiichi nuclear disaster in 2011, operations were halted. Operations south of the station were resumed on June 1, 2014.

## Surrounding area

Tatsuta is within the evacuation zone surrounding the Fukushima Daiichi Nuclear Power Plant. Since August 2012 it has been possible to enter the area, but remaining in the area overnight is prohibited.
* Road Station Naraha
* Kido Post Office
* National Route 6
* Hirono Power Station
# Be Like That (Kane Brown, Swae Lee and Khalid song)

"Be Like That" is a song by American musicians Kane Brown, Swae Lee, and Khalid. It was released on July 10, 2020, through RCA Records Nashville as the third single from Brown's third EP Mixtape, Vol. 1.

## Background and composition

Brown discussed the song's meaning in a statement to Billboard, saying: "It's about all the different feelings you can have in a relationship. And trying not to overthink it." "Be Like That" mixes country with "infectious" pop and hip-hop elements.

## Music video

The lyric video was uploaded on July 10, 2020. The official music video was released on August 19, 2020, and was directed by Alex Alvga. Being set in the 1940s, it features the three singers taking over the Pink Motel in Sun Valley, California and showcasing a classic diner, as well as an empty pool with vintage TVs.

## Personnel

Credits adapted from YouTube and Tidal.
* Charlie Handsome – Producer
* Denis Kosiak – Mixing
* Khalif Brown – Songwriting
* Alexander Izquierdo – Songwriting
* James Keely – Engineering
* Khalid Robinson – Songwriting
* Randy Lanphear – Producer / Vocal Producer
* Michael Piroli – Engineering
* Kuk Harrell – Producer / Vocal Producer
* Ryan Vojtesak – Producer / Songwriting
* Jeff Braun – Engineering / Vocal Engineering
* Mike Will – Producer / Songwriting
* Dale Becker – Mastering
* Hector Vega - Mastering

## Charts
### Weekly charts

| Chart (2020) | Peak position |
| Australia (ARIA) | 53 |
| Canada (Canadian Hot 100) | 6 |
| Canada AC (Billboard) | 31 |
| Canada CHR/Top 40 (Billboard) | 1 |
| Canada Hot AC (Billboard) | 5 |
| Global 200 (Billboard) | 44 |
| US Billboard Hot 100 | 19 |
| US Adult Pop Airplay (Billboard) | 11 |
| US Pop Airplay (Billboard) | 8 |
| US Rolling Stone Top 100 | 17 |

### Year-end charts

| Chart (2020) | Position |
| Canada (Canadian Hot 100) | 55 |
| US Billboard Hot 100 | 88 |
| US Adult Top 40 (Billboard) | 45 |
| US Mainstream Top 40 (Billboard) | 38 |
| Chart (2021) | Position |
| Canada (Canadian Hot 100) | 55 |

## Certifications

| Region | Certification | Certified units/sales |
| Australia (ARIA) | Gold | 35,000$^‡$ |
| Brazil (Pro-Música Brasil) | Gold | 20,000$^‡$ |
| Canada (Music Canada) | 6× Platinum | 480,000$^‡$ |
| New Zealand (RMNZ) | Platinum | 30,000$^‡$ |
| United Kingdom (BPI) | Silver | 200,000$^‡$ |
| United States (RIAA) | 4× Platinum | 4,000,000$^‡$ |
| $^‡$ Sales+streaming figures based on certification alone. |||
# Kado Station

Kado Station (鹿渡駅, Kado-eki)is a railway station in the town of Mitane, Yamamoto District, Akita Prefecture, Japan, operated by East Japan Railway Company (JR East).

## Lines

Kado Station is served by the Ōu Main Line, and is located 338.4 km from the terminus of the line at Fukushima Station.

## Station layout

Kado Station has one side platform and one island platform serving three tracks, connected by a footbridge. Track 2 is used primarily for freight trains changing direction. Kado Station is a simple consignment station, administered by Higashi-Noshiro Station, and operated by Mitane municipal authority, with point-of-sales terminal installed. Ordinary tickets, express tickets, and reserved-seat tickets for all JR lines are on sale (no connecting tickets).

### Platforms

| 1 | ■ Ōu Main Line | for Higashi-Noshiro and Hirosaki |
| 2 | ■ Ōu Main Line | freight train siding |
| 3 | ■ Ōu Main Line | for Akita and Ōmagari |

## History

Kado Station was opened on August 1, 1902 as a station on the Japanese Government Railways (JGR), serving the town of Kado, Akita. The JGR became the JNR (Japan National Railways) after World War II. The station was absorbed into the JR East network upon the privatization of the JNR on April 1, 1987.

## Passenger statistics

In fiscal 2018, the station was used by an average of 135 passengers daily (boarding passengers only).

## Surrounding area

* National Route 7
* Kotooka Post Office
* Kotooka Junior High School