There is a large farm called, "Farm for education." All first year "Freshman" students must take a horticulture class. They learn to grow vegetables and flowers on this farm.
Students can pick herbs and sometimes drink herbal teas in this garden. It is also a popular place for students to eat lunch.
Keisen University has educational links with these universities:
Smuglyanka
Smuglyanka (Russian: Смугля́нка, meaning "the dark girl") is a Russian song. The lyrics tell of a man who met a pretty woman gathering grapes and tries to seduce her, but finds out that she is a partisan. She then convinces him to join the partisans as well. It was written in 1940 by Yakov Shvedov (lyrics) and Anatoliy Grigoryevich Novikov (music). The song was meant to glorify female partisans in the Russian Civil War. The song is still very popular.
Mimikyu
Mimikyu is a Pokémon which was first encountered in the game "Pokémon Sun and Moon."
Mimikyu is one of the strangest Pokémon as its true identity is hidden under the disguise it has on. There has been many fan art works of what fans believed to be Mimikyu's true form. However, recently in a anime episode it is shown that it is a ghostly orb and anyone who looks at its yellow eyes will die of shock.
Thomas Bloodworth
Sir Thomas Bloodworth (sometimes spelled Bludworth) was an English merchant and politician. He was Lord Mayor of London from October 1665 to October 1666. He was in the House of Commons from 1660 to 1679.
He was blamed for the spread of the Great Fire of London. This is because, as the Mayor, he did not give approval to stop the fire.
Pothole (landform)
Potholes (also called kettles or kettle holes) are shallow bodies of water. They are filled with sediment. They are formed by retreating glaciers or by draining floodwaters.
Potholes can be formed when big blocks of ice break off of glaciers. The blocks become covered by sediment the glacier leaves behind. When the block melts, the hole it leaves behind is a pothole.
Potholes can also be formed when an ice-dammed lake suddenly drains away. As the ice melts, ramparts can form around the edge of the pothole. The lakes that fill these holes are usually deep or less. They eventually become filled with sediment. In acid conditions, a bog may form. In alkaline conditions, it will be peatland.
Kettles are landforms created by melted water from glaciers, a process called "fluvioglacial." When warming weather conditions cause a glacier to start melting, large blocks of ice can break off in a process called "calving." Rather than melting on the surface of the ground, the ice block can get partially or totally buried by dirt, rocks, and plant matter - the "sediment" carried in the glacier together with its ice content. This sediment piles up on the land where the glacier had been, a broad, smooth stretch called an "outwash plain" (or "sandur"). The kettle hole occurs when the exposed or buried ice block melts so that the surface of the sandur sinks. Multiple kettle holes can form near each other, and with the ridges and mounds of sediment around them the smooth surface of the sandur becomes irregular. Kettle holes can also occur in ridge-shaped deposits of loose rock chunks called "till."
Kettle holes can also form when a lake has a large amount of ice blocking the outlet where water drains from it, and the ice breaks up all at once. The flood that this causes can carry blocks of ice and sediment similar to the glacier-calf activity described above. These floods are called "jökulhlaups," an Islandic term used wherever this occurs. In 1992, the geologist Judith Maizels made outdoor observations and reproduced the conditions in a laboratory simulation. She found that protective walls (called ramparts) (protective walls) form around the edge of kettle holes made by jökulhlaup floods. The type of ramparts that develop depends on the how concentrated are the rock fragments contained in the melted ice block, and also on how deeply the block was buried by sediment.
Most kettle holes are less than two kilometres in diameter, although some in the U.S. Midwest exceed ten kilometres. Puslinch Lake in Ontario, Canada, is the largest kettle lake in Canada, covering . Fish Lake in the north-central Cascade Mountains of the U.S. state of Washington is .
The depth of most kettles is less than ten meters. In most cases, kettle holes eventually fill with water, sediment, or plant growth (vegetation). If the kettle gets more water from surface or underground rivers or streams, it becomes a kettle lake. If the kettle gets its water from rainfall and/or snowfall (precipitation), existing groundwater, or a combination of the two, it is termed a kettle pond. A kettle wetland is a kettle pond in which plant matter grows. Kettle ponds that are not affected by the local groundwater table will usually become dry during the warm summer months, in which case they are called "ephemeral" (something which disappears on its own).
If water in a kettle becomes acidic due to decomposing organic plant matter, it becomes a kettle bog. Otherwise, if underlying soils are lime-based, which has the effect of neutralizing the acidic conditions somewhat, it becomes a kettle peatland. Kettle bogs are closed ecosystems because they have no water source other than precipitation (rainfall and snowfall). Both acidic kettle bogs and fresh water kettles are important ecological niches for some symbiotic (mutually dependent) species of flora and fauna.
The Kettle Moraine, a region of Wisconsin covering an area from Green Bay at Lake Michigan to south-central Wisconsin, has numerous kettles, moraines and other glacial features. It has many kettle lakes, some of which are 100 to deep. Kettle Point, Ontario, Canada, has rock concretions (where sediment naturally cements into hard masses) locally named 'kettles', but there are no kettle lakes in this region.
The Prairie Pothole Region extends from northern Alberta, Canada to Iowa, United States and includes thousands of small sloughs (shallow bodies of usually stagnant water in a wetland) and lakes.
Fischenthal
Fischenthal is a municipality in the district of Hinwil in the canton of Zurich in Switzerland.
Besides the village of Fischenthal, it includes the villages of Gibswil and Steg, as well as nearly 100 smaller settlements.
Flaach
Flaach is a municipality in the district of Andelfingen in the canton of Zurich in Switzerland.
Lee Weissenborn
Lee Edward Weissenborn (March 19, 1929 – May 7, 2017) was an American Democratic Party politician in the state of Florida. He was a member of the member of the Florida House of Representatives for Dade County from 1963 through 1966. He later served as a member of the Florida Senate from 1967 through 1971.
Weissenborn was born in St. Louis, Missouri. He studied at University of Florida. Weissenborn died at his home in Palmetto Bay, Florida on May 7, 2017 from stroke complications at the age of 88.
Édouard Philippe
Édouard Charles Philippe (born 28 November 1970) is a French lawyer and politician. He was the Prime Minister of France from 15 May 2017 to 3 July 2020.
Philippe is a member of the Union for a Popular Movement, later the Republicans. He has served as a member of the National Assembly representing the 7th constituency of Seine-Maritime since 2012, as well as mayor of Le Havre and president of the agglomeration community of Le Havre since 2010.
On 15 May 2017, President Emmanuel Macron appointed him Prime Minister. He resigned on 3 July 2020. Two days later, he became Mayor of Le Havre.
Callista Gingrich
Callista Louise Gingrich ("née" Bisek; born March 4, 1966) is an American politician and businesswoman. She is the current United States Ambassador to the Holy See since December 22, 2017. She was the President of Gingrich Productions. She is married to former Speaker of the U.S. House of Representatives and 2012 Republican Presidential candidate Newt Gingrich.