The Grampian Mountains (Scotland) and Mount Everest (Himalayas) differ by an order of magnitude in elevation.
Highest peak: Ben Nevis — 1,345 m (4,413 ft)
Range: Scottish Highlands, ~200 km extent
Geology: Ancient metamorphic (Moine, Dalradian) + granite intrusions, Caledonian orogeny (480-400 Ma)
Elevation: 8,848.86 m (29,031.7 ft) — 2020 China/Nepal joint survey
Location: Mahalangur Himal, Nepal/China border
Geology: Tethyan sedimentary sequence thrust over Indian Plate, active Himalayan orogeny (50 Ma-present)
Everest is 6.6× higher than Ben Nevis. The vertical difference (7,504 m) exceeds the height of the Matterhorn (4,478 m) and Mont Blanc (4,808 m) combined.
"Grampian" sounds grand. Ben Nevis is the UK's highest peak. But the Himalayas operate on a different planetary scale — continental collision vs. ancient orogen remnant. The Grampians are magnificent; Everest is extraterrestrial by comparison.
No scenario makes the Grampians "as high as Everest." Not past, present, or future tectonics.