Mont d'Amin (1,417 m) is a mountain of the Jura, located east of the Vue des Alpes in the canton of Neuchâtel.
 It lies on the range between the valleys of Saint-Imier and Val-de-Ruz.
The Gamburtsev Mountain Range (also known as the Gamburtsev Subglacial Mountains) is a subglacial mountain range located in East Antarctica, just underneath the lofty Dome A, near the Southern Pole of Inaccessibility.
 The range was discovered by the 3rd Soviet Antarctic Expedition in 1958 and is named for Soviet geophysicist Grigoriy A. Gamburtsev.
 It is approximately 1200 km long, and the mountains are believed to be about 2700 m high, although they are completely covered by over 600 m of ice and snow.
 The Gamburtsev Mountain Range is currently believed to be about the same size as the European Alps, and, as of 2008, it is unknown how the mountains were formed, though the current speculated age of the range is over 34 million years and possibly 500 million years.
 Current models suggest that the East Antarctic ice sheet was formed from the glaciers that began sliding down the Gamburtsev range at the end of the Eocene.
 Vostok Subglacial Highlands form an east extension of Gamburtsev Subglacial Mountains.
The Uri Alps (German: "Urner Alps" ) are a mountain range in Central Switzerland and part of the Western Alps.
 They extend into the cantons of Obwalden, Valais, Bern, Uri and Nidwalden and are bordered by the Bernese Alps (Grimsel Pass) and the Emmental Alps to the west (the four lakes: Lungerersee, Sarnersee, Wichelsee, and Alpnachersee), the Schwyzer Alps to the north (Lake Lucerne), the Lepontine Alps to the south (the valley of Urseren with Andermatt) and the Glarus Alps to the east (Reuss).
The Chablais Alps are a mountain range in the western Alps.
 They are situated between Lake Geneva and the Mont Blanc Massif.
 The Col des Montets separates them from the Mont Blanc Massif in the south, and the Rhône valley separates them from the Bernese Alps in the east.
Mont Chapman (elevation 658 m ) is the highest peak in the Stoke Mountains of the southern Notre Dame mountain range located in Stoke, Quebec, Canada.
 It is accessible from trails maintained by Les Sentiers de l'Estrie.
 From the summit, one is able to see Mont Ham, Mont Ste-Cécile, and Mont Mégantic.
 Neighboring Bald Peak (elevation approx. 611 m , ) is accessible by these same trails.
The Grison Alps are the mountains of the Graubünden canton of Switzerland (Grisons being the English name for the Graubünden region).
 There are many significant peaks in the Grison Alps, including the Tödi (3,614 m) and the highest peak, Piz Bernina (4,049 m).
 Many of the mountain ranges feature extensive glaciers, such as at the Adula, the Albula, the Silvretta, the Bernnina or the Rätikon range.
 The Grison Alps include parts of both the Eastern Alps and the Western Alps.
 The Eastern Alps located in Graubünden are the Rhaetian Alps, which is part to the Central Eastern Alps.
 The Rhaetian Alps consists of the following mountain ranges: Samnaun Alps, Rätikon, Silvretta, Sesvenna Range, Albula Range, Plessur Range, Oberhalbstein Range, Livigno Range, Bregaglia Range and the Bernina Range.
 The Western Alps located in Graubünden, include portions of the Lepontine Alps and the Glarus Alps.
The Bashagard Mountains or the Bashagerd Mountains (also known as Bashagird or Bashakerd) is a mountain range that is located in southeast of Iran.
 The mountain range runs in an arc almost in a northwest-southeast direction from eastern parts of Hormozgan Province along the border with Kerman Province and stretching into southern part of Sistan and Baluchestan Province.
 With an elevation of 2185 metres, Mount Buniken (Kuh-e Buniken) is the highest point of the range located in the western section of the Bashagard Mountains, east of Sardasht in Bashagard County in Hormozgan Province, and in the vicinity of a place that marks the borders of Kerman, Hormozgan, and Sistan and Baluchestan provinces.
 Made of ophiolite, an assemblage of mafic igneous rocks representing remnants of former oceanic crust, the mountain range was formed finally in the Miocene and the Pliocene during the Alpine orogeny.
 The mountain range is located in a region with a hot semi-desert climate.
The Alps ( ; French: "Alpes" ] ; German: "Alpen" ] ; Italian: "Alpi" ] ; Romansh: "Alps" ; Slovene: "Alpe" ] ) are the highest and most extensive mountain range system that lies entirely in Europe, stretching approximately 1,200 km across eight Alpine countries: Austria, France, Germany, Italy, Liechtenstein, Monaco, Slovenia, and Switzerland.
 The mountains were formed over tens of millions of years as the African and Eurasian tectonic plates collided.
 Extreme shortening caused by the event resulted in marine sedimentary rocks rising by thrusting and folding into high mountain peaks such as Mont Blanc and the Matterhorn.
 Mont Blanc spans the French–Italian border, and at 4810 m is the highest mountain in the Alps.
 The Alpine region area contains about a hundred peaks higher than 4000 metres (just over 13,000 feet).
The Vanoise massif is a mountain range of the Graian Alps, located in the Western Alps.
 After the Mont Blanc Massif and the Massif des Écrins it is the third highest massif in France, reaching a height of 3,885m at the summit of Grande Casse.
 It lies between Tarentaise Valley to the north and the Maurienne valley in the south.
 The range is the site of France's first National Park in 1963, the Vanoise National Park.
 The ski resorts of Tignes and Val-d'Isère and the 2,770m high Col de l'Iseran are located in the eastern part of the range.
The Jura Mountains (] ; ] ) French: "Massif du Jura" , (German: "Juragebirge" , Italian: "Massiccio del Giura" ) are a sub-alpine mountain range located north of the Western Alps, mainly following the course of the France–Switzerland border.

Question: Mont d'Amin is a mountain of a sub-alpine mountain range located north of the Western Alps, and mainly following what border?
Answer: France–Switzerland border