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Ashoro is a town located in Tokachi Subprefecture, Hokkaido, Japan.

As of September 2016, the town has an estimated population of 7,150 and a density of 5.1 persons per km². The total area is 1,408.09 km².

It was the largest municipality in Japan until the merger of Takayama City, Gifu Prefecture on February 1, 2005. Main industries of the town include dairying and farming of sugar beet and wheat.

Lake Onnetō is a major attraction of the town and is a part of Akan National Park.

As of January 31, 2015, the total population of The Town of Ashoro is 7,339, with a total of 3,540 men and 3,799 women. The Town of Ashoro’s population density is 5.09 people per square kilometer. The county of Ashoro’s, Ashoro-gun, population is 9,692 with a population density of 4.81per square km. Like many communities in the Tokachi prefecture, the Town of Ashoro has seen a decline in population. The 1999 census concluded there were 9,409 people living in Ashoro. The total area is 1,408.09 km²Ashoro is located in the northeastern part of the Tokachi. Kushiro and Shiranuka is to the east and to the south are Honebestu and Obihiro. Kamishiro is to the west and to the north is Oketo, Rikubestu, and Tsubetsu. Ashoro is Ashoro consists of rolling foothills and is nestled at the base of Mount Meakan. Ashoro-gun is 66.5 km wide and 48.2 km long and is 1,408.09K m². Ashoro is considered a wide town. 83 percent of the town’s land is forested. Ashoro is influenced by the Tokachi inland climate; temperature differences are large with less precipitation but have many sunny days. On average Ashoro receives 846.5 mm of rain with August being the wettest month, 151 mm of precipitation, and February being the dries, 4.5 mm of precipitation. On average temperatures vary from 23.2 degrees Celsius in August and dropping to -8 in January. Wikipedia

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An image from Ashoro-cho Hokkaido Japan

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Lombardy is one of the twenty administrative regions of Italy. It has an extent of 23,844 km² (9,206 sq mi) in the northern-central part of the country, and a population of about 10 million people, constituting more than one-sixth of the population of Italy. Over a fifth of the Italian gross domestic product is produced in the region.

The metropolitan area of Milan is the largest in the country and is among the largest in the European Union. Of the fifty-eight UNESCO World Heritage Sites in Italy, eleven are in Lombardy. Virgil, Pliny the Elder, Ambrose, Caravaggio, Claudio Monteverdi, Antonio Stradivari, Cesare Beccaria, Alessandro Volta, Alessandro Manzoni, and popes John XXIII and Paul VI are among those with origins in the area now known as Lombardy.

The word Lombardy comes from Lombard, which in turn is derived from Late Latin Longobardus, Langobardus (“a Lombard”), derived from the Proto-Germanic elements *langaz + *bardaz; equivalent to long beard. Some scholars suggest the second element instead derives from Proto-Germanic *bardǭ, *barduz (“axe”), related to German Barte (“axe”), or that the whole word comes from the Proto-Albanian *Lum bardhi “white river” (Compare modern Albanian lum i bardhë).

During the early Middle Ages, “Lombardy” referred to the Kingdom of the Lombards (Latin: Regnum Langobardorum), a kingdom ruled by the Germanic Lombards who had controlled most of Italy since their invasion of Byzantine Italy in 568. As such “Lombardy” and “Italy” were almost interchangeable; by the mid-8th century, the Lombards ruled everywhere except the Papal possessions around Rome (roughly modern Lazio and northern Umbria), Venice, and some Byzantine possessions in the south (southern Apulia and Calabria; some coastal settlements including Amalfi, Gaeta, Naples, and Sorrento; Sicily and Sardinia). The term was also used until around 965 in the form Λογγοβαρδία (Longobardia) as the name for the territory roughly covering modern Apulia which the Byzantines had recovered from the Lombard rump Duchy of Benevento.

With a surface area of 23,861 km² (9,213 sq mi), Lombardy is the fourth-largest region of Italy. It is bordered by Switzerland (north: Canton Ticino and Canton Graubünden) and by the Italian regions of Trentino-Alto Adige/Südtirol and Veneto (east), Emilia-Romagna (south), and Piedmont (west). Three distinct natural zones can be easily distinguished in Lombardy: mountains, hills, and plains—the last being divided into Alta (high plains) and Bassa (low plains). Wikipedia

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am image from Lombardy, Italy

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Mount Taranaki, less commonly known as Mount Egmont, is a dormant stratovolcano in the Taranaki region on the west coast of New Zealand’s North Island. It is the second highest point in the North Island, after Mount Ruapehu. The 2,518-metre (8,261 ft) mountain has a secondary cone, Fanthams Peak (Māori: Panitahi), 1,966 meters (6,450 ft), on its south side.

The name Taranaki comes from the Māori language. The Māori word tara means mountain peak, and Naki is thought to come from ngaki, meaning “shining”, a reference to the snow-clad winter nature of the upper slopes. It was also named Pukehaupapa and Pukeonaki by iwi who lived in the region in “ancient times”.

Captain Cook named it Mount Egmont on 11 January 1770 after John Perceval, 2nd Earl of Egmont, a former First Lord of the Admiralty who had supported the concept of an oceanic search for Terra Australis Incognita. Cook described it as “of a prodigious height and its top covered with everlasting snow,” surrounded by a “flat country … which afforded a very good aspect, being clothed with wood and verdure”.

When the French explorer Marc-Joseph Marion du Fresne saw the mountain on 25 March 1772 he named it Pic Mascarin. He was unaware of Cook’s earlier visit.

It appeared as Mount Egmont on maps until 29 May 1986, when the name officially became “Mount Taranaki or Mount Egmont” following a decision by the Minister of Lands. The Egmont name still applies to the national park that surrounds the peak and geologists still refer to the peak as the Egmont Volcano.

As part of the treaty settlement with Ngā Iwi o Taranaki the mountain will be officially named Taranaki Maunga. As of 18 July 2021, the settlement has not yet been completed.

Taranaki is geologically young, having commenced activity approximately 135,000 years ago. The most recent volcanic activity was the production of a lava dome in the crater and its collapse down the side of the mountain in the 1850s or 1860s. Between 1755 and 1800, an eruption sent a pyroclastic flow down the mountain’s northeast flanks, and a moderate ash eruption occurred about 1755, of the size of Ruapehu’s activity in 1995/1996. The last major eruption occurred around 1655. Recent research has shown that over the last 9,000 years minor eruptions have occurred roughly every 90 years on average, with major eruptions every 500 years. Wikipedia

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An image of Mount Taranaki

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