OpenLLM-France/wikimedia huggingface dataset:
# Mount Margaret (Skamania County, Washington)

Mount Margaret is a 5,850-ft (1,780 m) mountain summit located in Mount St. Helens National Volcanic Monument, in the Gifford Pinchot National Forest, in Skamania County of southwest Washington state. It is situated in the Cascade Range, 2 mi (3.2 km) north of Spirit Lake, and 2.4 mi (3.9 km) northeast of Coldwater Peak. Its nearest higher neighbor is Mount Whittier, 0.93 mi (1.50 km) to the north, and Mount St. Helens rises 8 mi (13 km) to the south. Precipitation runoff from Mount Margaret drains into Coldwater Creek, a tributary of the North Fork Toutle River. A hiking trail provides access to this mountain. This peak was named some time before 1900 by an admiring prospector for Margaret "Maggie" Shultz Layton (1877-1965), a pioneering resident of Toledo, Washington.

## Geology

The history of the formation of the Cascade Mountains dates back millions of years ago to the late Eocene Epoch. Geological events occurring many years ago created the diverse topography and drastic elevation changes over the Cascade Range leading to various climate differences. During the Pleistocene period dating back over two million years ago, glaciation advancing and retreating repeatedly scoured and shaped the landscape. With the North American Plate overriding the Pacific Plate, episodes of volcanic igneous activity occurred. The lateral blast from the 1980 eruption of Mount St. Helens was pointed toward Mount Margaret and stripped the vegetation from its slopes. Due to Mount Saint Helens' proximity to Mount Margaret, volcanic ash is common in the area.

## Climate

Coldwater Peak is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall.
During winter months, weather is usually cloudy, but due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. The months July through September offer the most favorable weather for viewing or climbing this peak.
# Mount Mathias

Mount Mathias is a 7,156-foot (2,181-metre) mountain summit located within Olympic National Park in Jefferson County of Washington state. Its nearest higher neighbor is Mount Olympus, 1.76 mi (2.83 km) to the east. Mount Mathias is wedged between the massive Blue Glacier below its west slope, and the Hoh Glacier on the east side. Precipitation runoff from the mountain drains into the Hoh River.

## History

This mountain was originally named "Apollo", for one of the Olympian deities in Greek and Roman mythology who made Mount Olympus home. It was renamed in honor of Francis Wayland "Matt" Mathias (1884–1959), a mountaineer, naturalist, and Grays Harbor County civic leader. The Mathias name was officially adopted in 1960 by the U.S. Board on Geographic Names.
The first ascent of this peak was made in 1957 by Yves Eriksson and Jim Hawkins.

## Climate

Based on the Köppen climate classification, Mount Mathias is located in the marine west coast climate zone of western North America. Weather fronts originating in the Pacific Ocean travel northeast toward the Olympic Mountains. As fronts approach, they are forced upward by the peaks (orographic lift), causing them to drop their moisture in the form of rain or snow. As a result, the Olympics experience high precipitation, especially during the winter months in the form of snowfall. Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger. During winter months weather is usually cloudy, but due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. The months of July through September offer the most favorable weather for viewing or climbing this peak.

## Geology

The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and basaltic oceanic crust. The mountains were sculpted during the Pleistocene era by erosion and glaciers advancing and retreating multiple times.
# Mount McAdie

Mount McAdie is a summit on the crest of the Sierra Nevada, and is located 2.1 miles (3.4 km) south of Mount Whitney. It has three summits, with the north peak being the highest. The summit ridge marks the boundary between Sequoia National Park and the John Muir Wilderness. It is also on the boundary between Inyo and Tulare counties. Lone Pine, 12.4 miles (20.0 km) to the northeast, is in the Owens Valley on U.S. 395.
In 1905, the mountain was named in honor of Alexander G. McAdie by James E. Church. McAdie ran the U.S. Weather Bureau in San Francisco at the time, and had visited the summit of Mount Whitney in 1903. The name first appeared on a map in 1956 with the publication of the USGS, 15 minute, Mount Whitney Quadrangle topographic map.
The north summit can be reached from Arc Pass, and was first climbed by Norman Clyde in 1922. The west face was first climbed in 1954, and is a class 4 ascent. In 1968, capable rock climber 27-year-old Anita Ossofsky and a fellow climber, who were well qualified and properly equipped, ascended class 3 terrain on Mt. McAdie in good weather from Arc Pass, traversed from the east face of Middle Peak to the gulley (which divides Middle and North Peaks), and at the top of the gulley, apparently a hand-hold of Ossofsky's gave way. She fell approximately 10 feet to a ledge, from which she rolled off and fell about an additional 150 feet before coming to rest in the gulley, dying immediately.
# Mount McCausland

Mount McCausland is a mountain in the U.S state of Washington located in the Okanogan-Wenatchee National Forest east of Stevens Pass. It's a popular hike that has views of nearby Lake Valhalla and Lichtenberg Mountain.
# Jōetsumyōkō Station

Jōetsumyōkō Station (上越妙高駅, Jōetsumyōkō-eki) is an interchange railway station in Jōetsu, Niigata, Japan, operated by East Japan Railway Company (JR East), West Japan Railway Company (JR West) and the third-sector railway operator Echigo Tokimeki Railway. It opened in March 2015.

## Lines

Jōetsumyōkō Station is served by the Echigo Tokimeki Railway Myōkō Haneuma Line and the high-speed Hokuriku Shinkansen, which opened for service on 14 March 2015. It replaced Wakinoda Station on the Shinetsu Main Line, located approximately 120 m away. The journey from Tokyo via the Hokuriku Shinkansen takes 1 hour 48 minutes. Only Hakutaka services stop at Jōetsumyōkō on the Hokuriku Shinkansen.

## Station layout

The new station consists of two elevated island platforms serving four tracks on the Hokuriku Shinkansen, with a ground-level island platform serving two tracks for the Myōkō Haneuma Line. The station has a "Midori no Madoguchi" staffed ticket office and also a "View Plaza" travel agent.

### Platforms

| 1 | ■ Myōkō Haneuma Line | for Myōkō-Kōgen |
| 2 | ■ Myōkō Haneuma Line | for Naoetsu |
| 11/12 | ■ Hokuriku Shinkansen | for Nagano, Takasaki, Tokyo |
| 13/14 | ■ Hokuriku Shinkansen | for Toyama, Kanazawa, Tsuruga |
* The ticket barriers leading to the Shinkansen platforms
* The ticket barriers leading to the Haneuma Line platform
* The Haneuma Line platform in January 2015
* View from the observation deck

## History

Initially provisionally named Jōetsu Station (上越駅), the name Jōetsumyōkō Station was formally announced in June 2013. Construction was completed in October 2014. It opened on 14 March 2015, coinciding with the opening of the Hokuriku Shinkansen extension from Nagano.

## Passenger statistics

In fiscal year 2017, the Myōkō Hanauma Line portion of the station was used by an average of 934 passengers daily (boarding passengers only). In fiscal year 2017, the JR portion of the station was used by an average of 2,131 passengers daily (boarding passengers only).

## Surrounding area

The station is located on the southern side of the Takada district of Jōetsu city, about 1.5 km from the border with Myōkō. The area was largely rice paddies with some houses, shops and factories along nearby Japan National Route 18; however, with the opening of the Shinkansen line, the area is rapidly urbanising.
# Mount Minsi

Mount Minsi forms the Pennsylvania side of the Delaware Water Gap, and is the eastern extent of the Blue Mountain. It is composed of sandstone and conglomerates of the Shawangunk Formation.

## Hiking

The easiest route to the summit of Minsi is by way of the Appalachian Trail, from the Lake Lenape trailhead near the town of Delaware Water Gap. The Mount Minsi fire road shares and parallels parts of the same route on the same northwest slopes. Both travel about 5 miles (8 km) round trip, and gain 1,020 feet (310 m) of elevation.

## Climbing

The band of exposed metaquartzite cliffs on east face of Minsi hold a number of traditional climbing routes. The earliest of these were put up in 1975, and established routes range from 5.0 to 5.12+. Winter can offer some mixed and ice climbing as well.
# Caccothryptus arakawae

Caccothryptus arakawae is a species of minute marsh-loving beetle in the subfamily Limnichinae. The species was described alongside five other Caccothryptus species by Natural History Museum entomologist Keita Matsumoto in 2021, using specimens gathered by Martin J. D. Brendell at Kathmandu, Nepal in 1983. Six of Brendell's specimens were distinguished from its initial classification of Caccothryptus testudo due to distinct genital structures. The species was named for Hiromu Arakawa, the creator of manga series Fullmetal Alchemist.

## Taxonomy

The Limnichidae (minute marsh-loving beetle) genus Caccothryptus was first described by David Sharp in 1902. In 2014, the genus was divided into five species groups by Carles Hernando and Ignacio Ribera.
A group of Caccothryptus specimens were collected in 1983 in Kathmandu, Nepal by Martin J. D. Brendell, curator of Coleoptera Department of Entomology at the Natural History Museum, London. These were labeled as C. ripicola and C. testudo, first described by forester Harry George Champion in 1923. These were stored at the Natural History Museum. In 2021, museum entomologist Keita Matsumoto identified a number of distinct species from these specimens. A male specimen from Kathmandu was labeled as the holotype for Caccothryptus arakawae. Five specimens (comprising three males and two females) were labeled paratypes. C. arakawae was placed in the species group C. testudo and named for Japanese manga artist Hiromu Arakawa, the creator of Fullmetal Alchemist.

## Description

The Caccothryptus arakawae specimens identified by Matsumoto have elytral lengths of 3.39–3.68 mm, and elytral widths of 2.32–2.52 mm. Their prothoraces are 0.90–1 mm in length and 2.03–2.11 mm in width. C. arakawae has an elongated oval body, brown in colour except for reddish tibia and long, white setae, which are distributed across both the upper and lower sides of the beetle. Its tarsi are divided into five segments, of increasing length, with the fifth segment as long as the others combined. It has long, narrow, light brown tarsal claws. The beetle's head, smooth and punctured, is slightly retracted into its pronotum, and features eleven-segment antennae. Little sexual dimorphism exists between the male and female specimen, beyond a longer fifth abdominal ventrite on the female.
The beetle's genitals display a number of differences from the original classification of C. testudo, which enabled its classification as a separate species. C. arakawae's median lobe narrows to a slightly pointed tip. It has a U-shaped depression between the V-shaped notches on the tip of the genitalia. The genitals' dorsum are wavy, forming two concave curves. Females have a long ovipositor.
# Laguna Amarga

Laguna Amarga is a caldera and associated ignimbrite in the Andes of northwestern Argentina.
Laguna Amarga is part of the southern Central Volcanic Zone and one among several Miocene-Pliocene-Pleistocene volcanic centres of this volcanic region. The formation of magma chambers and thus of large volcanic systems has apparently been influenced by tectonic changes. The Laguna Amarga caldera is associated with the Cordillera Claudio Gay faults together with the Laguna Escondida and Wheelwright calderas, all of which are between 6.5 and 4 mya old. Laguna Amarga and Laguna Verde are sometimes associated with the Vallecito ignimbrite instead. The formation of the Laguna Amarga volcanic centre was probably influenced by orogenic changes in the Andes which triggered the formation of fractures in the crust.
The Laguna Amarga caldera has a diameter of 33 kilometres (21 mi) and is linked to the Laguna Escondida caldera. It is the largest caldera in the area and may be part of an eastward migrating volcanic complex. Tephras erupted during its formation have been found hundreds of kilometres from Laguna Amarga.
The 630 km$^3$ (150 cu mi) Laguna Verde ignimbrite was erupted 4-3 mya ago and is associated with these two calderas. Other dates are 4.5 ± 0.5 to 3.0 ± 0.2 mya. The ignimbrite covers an area of 86.46 km$^2$ (33.38 sq mi), cropping out southwest of the Laguna Amarga ignimbrite. The Laguna Verde ignimbrite ranges from dacite to rhyolite in composition, containing biotite, pumice, quartz and sanidine. Hydrothermally altered rocks occur in the area.
The Laguna Amarga ignimbrite was erupted 5.1 mya ago, or 3.7-4.1 mya, and it has a volume of over 70 km$^3$ (17 cu mi). It extends north-northwest from Peinado volcano. The ignimbrite is somewhat welded and contains vesicular pumice, and bears some similarity with the Cyclops ignimbrite 50 km (31 mi) away. Further, the Laguna Amarga ignimbrites like the Cerro Blanco and Galan ignimbrites are rich in sodium. It covers a surface area of 611.02 km$^2$ (235.92 sq mi), cropping out around the Laguna Amarga. Another ignimbrite, Los Colorados, is located at the edge of the Amarga caldera but its eruptive centre is unknown. After its formation, lava flows from Peinado and Cerro El Condor overran the floor of the caldera and monogenetic volcanos developed both on the caldera floor and on its ignimbrite.
# Mount Nebo (Oregon)

Mount Nebo is a 8,261-foot (2,518 m) mountain in the Eagle Cap Wilderness of Oregon, in the United States. Named after the biblical Mount Nebo overlooking Israel, which is said to be the place of Moses' death. It is the centerpiece of the Imnaha Divide, inside the Wallowa–Whitman National Forest. Mount Nebo is one of the important areas where sheep and cattle graze throughout Eagle Cap Wilderness.

## Location

Mount Nebo is located in the northern ridge of the Imnaha Divide, approximately 2 miles North of the confluence of the north and south forks of the Imnaha River. The slopes and meadows that surround Mount Nebo reach towards the Tenderfoot Wagon Road and Mine south of McCully Basin.

## Ecology

Mount Nebo has an open grassy south-facing slope. It was a target of a significant fire in the early 1900s. Since then, mountain big sagebrush has invaded most of the open grassy slope. Stands of subalpine fir mixed with Engelmann spruce, scattered lodgepole pine and small pockets of whitebark pine near the summit are the most notorious trees on the mountain and its surrounding ridges.

## Lookout tower

Several fire lookout towers were built in the early 1900s throughout the Wallowa–Whitman National Forest. Mount Nebo had a lookout tower and 10x10 cabin built in the 1920s. Maintenance and cabin occupation was reported through the 1950s. The tower and the cabin were removed in the 1970s.
# Mount Newcomb

Mount Newcomb is a 13,422-foot-elevation (4,091-meter) mountain summit located just west of the crest of the Sierra Nevada mountain range in Tulare County, California. It is situated in Sequoia National Park, and is 2.8 miles (4.5 km) south of Mount Whitney, 1.1 miles (1.8 km) northeast of Mount Chamberlin, and 3.5 miles west of Mount Corcoran. Mt. Newcomb ranks as the 70th highest summit in California. Topographic relief is significant as it rises 2,083 feet (635 meters) above the second Crabtree Lake in approximately one mile. This mountain's name was officially adopted in 1940 by the U.S. Board on Geographic Names to honor American astronomer Simon Newcomb (1835–1909). The first ascent of the summit was made August 22, 1936, by Max Eckenburg and Bob Rumohr.

## Climbing

Established climbing routes:
* Southwest Slope – class 2 – 1936 by Max Eckenburg and Bob Rumohr
* Southwest Ridge – class 3 – 1956 by George O. Hale
* Northeast Ridge – class 3 – 2004 by Bob Sumner
* South Ridge – class 3
* The Keep – class 5.10 – 2001 by Dave Nettle, Aaron Zanto

## Climate

According to the Köppen climate classification system, Mount Newcomb has an alpine climate. Most weather fronts originate in the Pacific Ocean, and travel east toward the Sierra Nevada mountains. As fronts approach, they are forced upward by the peaks, causing them to drop their moisture in the form of rain or snowfall onto the range (orographic lift). Precipitation runoff from this mountain drains west to the Kern River via Whitney and Rock Creeks.
# Mount Newhall

Mount Newhall is a 1,916-foot-elevation (584-meter) summit in Alaska, United States.

## Description

Mount Newhall is a landmark of the Dutch Harbor area set 2.25 miles (3.62 km) east of Unalaska on Unalaska Island of the Aleutian Islands. Mount Newhall is part of the Aleutian Range. Precipitation runoff from the mountain drains into Iliuliuk Bay. Topographic relief is significant as the summit rises over 1,900 feet (579 meters) above tidewater in approximately 1.3 miles (2.1 km). The mountain's toponym was a local name published in 1951 on an U.S. Geological Survey map and has been officially adopted by the United States Board on Geographic Names. Dr. Albert Warren Newhall (1872–1929) and his wife Agnes were early residents of Unalaska who managed the Jesse Lee Home in Unalaska in the late 1800s and early 1900s. He was the local physician, dentist, and minister.

## Climate

According to the Köppen climate classification system, Mount Newhall is located in a subpolar oceanic climate zone with cold, snowy winters, and cool summers. Winter temperatures can drop to 0 °F with wind chill factors below −10 °F.

## Gallery

* Mt. Newhall
* Mt. Newhall (left) and Unalaska
* Newhall (left) and Unalaska
# Tampa Heights

Tampa Heights is one of the oldest neighborhoods within the city limits of Tampa, situated in the central part of the city. As of the 2000 census, the neighborhood had a population of 16,393.
Historic buildings in the area include the Tampa Free Library. Redevelopment efforts are underway in the community and include an extension of Tampa Riverwalk and renovation of Water Works Park (Tampa, Florida).

## Description

Tampa Heights is bounded by the North Boulevard to the west, Dr. Martin Luther King Jr. Boulevard to the north, Downtown Tampa to the south, and Ybor Heights, V.M. Ybor, and Ybor City to the east. The land area of the neighborhood is 3.5 square miles (9.1 km$^2$).
Thomas P. Kennedy is credited with naming the area when he moved there calling it the "Highlands" and it was developed as Tampa's first suburb in the 1880s. Today the neighborhood is known for its diversity and historic status, but gentrification of the area is causing controversy.

## Demographics

As of the census of 2010, there were 5,782 people residing in Tampa Heights. The racial makeup of Tampa Heights was 59.4% Black or African American, 32.4% White, 21.3% of the population was Hispanic or Latino of any race, 3.7% from two or more races, 3.4% from other races, 0.6% Asian and Pacific Islander and 0.3% Native American.
In Tampa Heights, the population was spread out, with 8% under 5 years; 8% 5 to 9 years; 14.7% 10 to 19 years; 29.7% 20 to 39 years; 24.7% 40 to 59 years; 11.6% 60 to 79 years; 3.3% 80 years and over.

## New development

In recent years, Tampa Heights has seen new people flow into the area aiming to restore it. Many new businesses have opened in the area such as art galleries and coffee shops. A new development called "The Heights of Tampa" has begun with some initial phases of construction. The project is mixed use for residential and commercial. It would be the northern end of the Tampa Riverwalk.
New developments also include Armature Works. Armature Works is a 73,000-square-foot space that consists of event spaces, trendy restaurants and bars, workspaces and the Heights Public Market.
The building dates back to 1910. It was originally a warehouse that stored TECO streetcars.
One way to access Armature Works is by walking along the Tampa Riverwalk.
# Edward Lewis (publisher)

Edward Lewis (born May 15, 1940) is an American business executive and former magazine publisher. He was one of the co-founders of Essence magazine, and chairman of Latina magazine. He was the first black chairman of the Magazine Publishers of America. His memoir, The Man From Essence: Creating a Magazine for Black Women, was co-authored by Audrey Edwards and published in 2014.
Lewis grew up in South Bronx, New York. He attended DeWitt Clinton High School. He was awarded a football scholarship to University of New Mexico, where he completed both a bachelor's and a master's degree. He later studied for a doctoral degree at Harvard University.
On February 9, 1991, Lewis married speech pathologist Carolyn Wright from Los Angeles.
# Mount Oso

Mount Oso (Spanish: Cerro del Oso) is a mountain in Western Stanislaus County, California, and is located on the Diablo Range. At 3,352 feet (1,022 m) feet in elevation, it is the third highest point in Stanislaus County. There are many radio stations and an unused forest fire lookout tower on the mountain. It appears in the City of Modesto's logo due to its predominance in the area's skyline.

## History

Mount Oso, (oso - Spanish for bear), was probably discovered by Gabriel Moraga during his expeditions in the Central Valley. This mountain can clearly be seen in Modesto, California, and has a beautiful contrast with the almond orchards. There is no exact date of the first ascent of the mountain.

## Location

The mountain is in Western Stanislaus County, 10 miles west of Westley, California, and is not accessible to the public due to surrounding gated private property.
# Mount Pendleton

Mount Pendleton is a 7,605-foot (2,318 m) mountain in the Alaska Range, in Denali National Park and Preserve, to the east-northeast of Denali. It lies above the Polychrome Glaciers. Mount Pendleton was named in 1961 by the U.S. Geological Survey for topographer Thomas Percy Pendleton.
# Mount Pierce (California)

Mount Pierce, sometimes called Pierce Mountain or Monument Peak at 3179 ft (949 m), is the highest point of the Monument Ridge which is part of the Coast Range in Humboldt County, California. It was named after U.S. President Franklin Pierce (1804–69). The summit offers a wide view of a wide area in Humboldt, Mendocino, Trinity and Del Norte counties north to the state of Oregon.
Due to the high visibility of the top of Mount Pierce and the inability to see Mount Diablo from the northwestern corner of the state, a new principal meridian, the Humboldt meridian was established in 1853 intersecting the survey base line at the summit of Mount Pierce which still governs the surveys in the northwestern corner of California.
The summit of Mount Pierce was marked with a tower of iron bars, now gone, but currently noted by an array of antennas, a geodetic marker and a plaque, placed on October 4, 2003, on the sesquicentennial of the establishment of the Humboldt Meridian Initial Point by Deputy Surveyor Henry Washington on October 6, 1853. The center of the Initial Point is marked by a standard US Coast and Geodetic Survey triangulation station disc, stamped “Mt. Pierce 1928.”