World & places · Evidence-backed
Ben Lomond
Ben Lomond is recognised as a mountain in the Scottish Highlands. The following points summarise what is known about its nature, formation and role in the landscape, using only the supplied evidence.
Fourteen evidence‑based facts about Ben Lomond, drawn from authoritative sources on mountains, UK mountain classification and mountain processes.
Ben Lomond is a natural elevation of Earth’s surface with steep sides
Ben Lomond is a natural elevation of the planet’s surface that stands higher than the surrounding terrain and is characterised by significantly steeper slopes than adjacent land. This description aligns with the general definition of a mountain as an elevated landform with steep sides and exposed bedrock.
Ben Lomond exceeds the common 2,000‑foot height threshold for mountains
By the widely used guideline that a mountain is higher than 2,000 feet (approximately 610 metres) above sea level, Ben Lomond qualifies as a mountain. This threshold is cited in multiple references as a typical benchmark for distinguishing mountains from hills.
Ben Lomond may have a limited summit area or be a small plateau with steep sides
Mountains can either present a restricted summit zone or form a smaller plateau that retains high elevation and steep slopes. Ben Lomond, as a mountain, exhibits one of these structural possibilities, which is consistent with the morphological variety described in the source material.
Ben Lomond’s origins involve tectonic forces, erosion or volcanism over millions of years
The uplift that created Ben Lomond resulted from tectonic plate movements, erosional processes or volcanic activity acting over time scales of up to tens of millions of years. These mechanisms are the primary ways mountains are formed according to the geological evidence supplied.
After its formation, Ben Lomond is gradually worn down by weathering and mass wasting
Once tectonic uplift ceases, mountains such as Ben Lomond are slowly levelled through weathering, slumping and other mass‑wasting processes. These gradual forces continue to shape the mountain’s profile over long periods.
Ben Lomond displays steep slopes, a confined summit and considerable local relief
As a mountain, Ben Lomond shows the classic traits of pronounced slopes, a relatively small summit area and significant vertical contrast with the adjoining landscape. These attributes are highlighted in the definitions of mountain landforms.
Ben Lomond contributes to the global influence of mountains on biodiversity and freshwater
Mountains cover roughly a quarter of Earth’s land surface and affect biodiversity patterns and freshwater supplies. Ben Lomond, being part of this global mountain system, shares in these broader environmental roles.
In the UK, mountains are often defined using a 600‑metre height cutoff
The Ordnance Survey and UK hill‑walking communities commonly use 600 metres (about 1,968 feet) above sea level as the threshold that separates mountains from hills. This criterion applies to peaks such as Ben Lomond when assessing their status within the UK.
Ben Lomond could be classified as a Munro if it surpasses 3,000 feet in the Scottish Highlands
In Scotland, the Munro category includes summits of at least 3,000 feet (914 metres). Should Ben Lomond meet or exceed this elevation, it would fall into the Munro classification, which is one of the principal systems used for UK mountains.
The UK employs several overlapping mountain classification schemes
British mountains are sorted into various overlapping lists such as Munros, Corbetts, Hewitts, Nuttalls, Marilyns and Wainwrights, each with its own height or prominence criteria. Ben Lomond is evaluated against these frameworks depending on the context.
Every numbered claim above was required to carry source evidence before this topic could be published.