Dendrosenecio johnstonii, formerly Senecio johnstonii, is a giant groundsel found in the middle altitudes of Mount Kilimanjaro in Africa.
 A recent botanical reclassification split off some species formerly in "Senecio", putting the giant groundsels in the new genus "Dendrosenecio".
 It also redefined the former species Senecio cottonii, as a subspecies of "Dendrosenecio johnstonii".
 Both genera are in the family "Asteraceae".
 The giant grounsels of the genus "Dendrosenecio" evolved, about a million years ago, from a "Senecio" that established itself on Mount Kilimanjaro, with those that survived adapting into "Dendrosenecio kilimanjari".
 As it moved down the mountain, the adaptations necessary for the new environment created the new species, "Dendrosenecio johnstonii".
 Various subspecies are found on other mountains.
Dendrosenecio kilimanjari is a giant groundsel found atop Mount Kilimanjaro in Africa.
 It was originally known as Senecio kilimanjari, but a recent botanical reclassification split off some species formerly in "Senecio", putting it and various other species in the new genus "Dendrosenecio".
 Both genera are in the family "Asteraceae".
 The giant grounsels of the genus "Dendrosenecio" evolved, about a million years ago, from a "Senecio" that established itself on Mount Kilimanjaro, with those that survived adapting into "Dendrosenecio kilimanjari".
 This later colonised other mountains by some means - the standard distance for wind dispersal of seeds is a few metres - and these isolated populations adapted in ways different from the parent population, creating new species.
Tanzania ( ), officially the United Republic of Tanzania (Swahili: "Jamhuri ya Muungano wa Tanzania" ), is a country in eastern Africa within the African Great Lakes region.
 It borders Kenya and Uganda to the north; Rwanda, Burundi, and the Democratic Republic of the Congo to the west; Zambia, Malawi, and Mozambique to the south; and the Indian Ocean to the east.
 Mount Kilimanjaro, Africa's highest mountain, is in north-eastern Tanzania.
Mount Meru is a dormant stratovolcano located 70 km west of Mount Kilimanjaro in the country of Tanzania.
 At a height of 4,562.13 m , it is visible from Mount Kilimanjaro on a clear day, and is the fifth-highest mountain in Africa, dependent on definition.
The Northern Ice Field is near the summit of Mount Kilimanjaro in Tanzania, on the west slope of the peak.
 The Northern Ice Field and Eastern Ice Fields were connected to the Southern Ice Field and formed part of a continuous body of glacial ice atop Mount Kilimanjaro when first scientifically examined in 1912.
 By 1962 the Southern Ice Field separated from the Northern Ice Field and then by 1975 the Eastern Ice Field did as well.
 In 1912, the glaciated areas atop Mount Kilimanjaro covered 11.40 sqkm ; by 2011 this had been reduced to 1.76 sqkm , an 85 percent loss.
 At one time, ice flowing off the Northern Ice Field fed numerous glaciers, including, north to south, the Credner, Drygalski, Great Penck and Little Penck Glaciers.
Lake Chala, also known as Dschalla, is a crater lake in a caldera on the borders of Kenya and Tanzania on the eastern edge of Mount Kilimanjaro, 8km north of Taveta and 55 kms from the town of Moshi.
 Depending on the time of year, it ranges in colour from deep blue to turquoise and green, it is surrounded by a 100 metres high crater rim.
 The lake is fed by groundwater flows, which come from Mount Kilimanjaro, fed and drained under ground with a rate of about 10 million m³ / year.
 Even the Chala loses volume.
 Its level had dropped in the last 6 years, by 2.4 metres, at the start of 2011 the water level has risen again by over 1 metre.
Credner Glacier is on Mount Kilimanjaro in Tanzania, on the northwest slope of the peak and is a remnant of an icecap which once crowned the top of Mount Kilimanjaro.
 The glacier is situated at an elevation of between 5800 and .
 Credner Glacier is one of the largest glaciers on the mountain and descends from the Northern Ice Field.
 Credner is rapidly retreating due to its high exposure point on the northwest slope of Mount Kilimanjaro.
 A report published in 2013 indicated that in another decade the glacier may no longer exist.
The Rebmann Glacier is located near the summit of Mount Kilimanjaro in Tanzania and is a small remnant of an enormous icecap which once crowned the summit of Mount Kilimanjaro.
 This icecap has retreated significantly over the past century and between 1912 and the 2000, 82 percent of the glacial ice on the mountain has disappeared.
 Rebmann Glacier is named for the German missionary and explorer, Johann Rebmann who was the first European explorer to report of snow and glaciers atop Mount Kilimanjaro in 1848.
Baraeus orientalis is a species of beetle in the family Cerambycidae.
 It was described by Per Olof Christopher Aurivillius in 1907.
 It is known from Tanzania, Malawi, Kenya, Namibia, Zimbabwe, Somalia, Cameroon, Ethiopia, and Zambia.
Drygalski Glacier was on Mount Kilimanjaro in Tanzania, on the northwest slope of the peak.
 The glacier terminus once extended to an elevation of 4800 m with an origination point near the summit of Mount Kilimanjaro and was fed by the Northern Ice Field.
 The Great Penck Glacier once flanked Drygalski Glacier to the south and until recently, the Credner Glacier did as well to the north.
 Drygalski Glacier is named for German geographer Erich von Drygalski.

Question: The Baraeus orientalis, a species of beetle, is found in which country, home of Mount Kilimanjaro?
Answer: Tanzania