quiet lanes and tracks that criss-cross this wonderfully varied region. This guidebook aims to introduce the reader to some of these wonderful routes, covering between 15km (10 miles) and 65km (40 miles) in a day and leading up to a finale of the multi-day Tour de Peak District – a five-day route running roughly around the edge of this fantastic region and within the grasp of anyone of average fitness.
Typical limestone scenery in the White Peak (Cheedale, near Route 11)
Geology
The Peak District was once a shallow tropical sea, and had you been riding 350 million years ago you would have been close to the Equator and completely underwater (perhaps that’ll be more believable to those visiting on a dull wet day!). Fringed by coral reefs and sea lilies (crinoids) with shellfish swimming around, the calcium carbonate of their remains went on to form limestone.
Later on (325–300 million years ago) the tropical sea slowly drained away when a huge river delta to the north advanced slowly southwards. This river delta dropped first mud, then coarser layers of sand and grits, today known as gritstone.
These two types of rock – limestone and gritstone – are the main constituents of the Peak District. The differences in colour and the distinctive separation of the two types of rock – roughly gritstone to the northern, western and eastern fringes, and limestone in the central and southern areas – led to the popular names of ‘White Peak’ and ‘Dark Peak’ for the southern limestone and northern gritstone regions respectively. Gritstone is sometimes also called ‘millstone grit’ due its long-standing use for millstones.
Abandoned millstones at Lawrencefield (near Route 16) – a common use for gritstone, hence its alternative name ‘millstone grit’
There is also a third, lesser known type of rock: an area of shale, formed from the early mud layers deposited by the encroaching river delta. This is often exposed on the boundary between the older limestone and more recent gritstone – the ‘shivering mountain’ of Mam Tor (Route 17) is a good example of this intermediate layer.
More recently (geologically speaking) the region was lifted and folded to form a gentle dome. Overlying deposits of coal were eroded, followed by some of the gritstone and shales, revealing the weaker limestone beneath the higher parts of the region. Being weaker, this limestone has eroded more quickly, leaving behind gritstone edges such as Froggatt, Stanage (Route 16) and Windgather Rocks (Route 18).
Wildlife
There is a surprising variety of animals to be seen in Derbyshire and the Peak District. Aside from the ubiquitous Derbyshire sheep, llamas and alpacas are farmed at many locations across the region, and there are even a few ostrich farms. Wilder creatures such as deer, foxes and rabbits are all frequently seen, but quiet footsteps can also reward you with glimpses of startled stoats and even adders.
Other less common sightings are of mountain hares and red-neck wallabies. The original group of wallabies escaped into the wild from a private zoo near the Roaches (Routes 15, 20 and TdPD) in the late 1940s. Their descendants were thought to have become extinct around 2000, but recent sightings in the Roaches and Buxton areas suggest otherwise. At least one yak also escaped at the same time; it was last seen on the moorlands in 1951, so yaks are unlikely to be part of Peak District wildlife these days – but like Scottish wildcats, you never know!
Near water or hay meadows, dragonflies and all sorts of butterflies are frequently sighted. More rarely, water voles can sometimes be seen beside streams, and the strange sucker-mouthed river lamphrey exist in our waterways (although these are usually only sighted by experts).
Any cyclist interested in birdlife will find the Peak District a fantastic location, with a wide abundance of species, from the tiny goldcrest, the redstart and the brightly coloured siskin to curlews, buzzards and geese. Kestrels are frequently seen hovering over fields and moorlands, waiting to pounce on unsuspecting small mammals. Grouse are a common sight and sound on the moorlands, but more common still is the pleasant warble of the skylark, high above the ground; lower down, the weaving acrobatics of swallows also provide entertainment.
The bright yellow siskin can frequently be seen near the River Derwent; Finches, like this chaffinch, are a common sight
In the vales and dales, dippers are often seen bobbing alongside limestone streams. Ducklings, stonechats (named for their distinctive call which sounds like small stones knocking together) and finches of all descriptions are a common sight, especially in early to mid-summer, and the lucky viewer may get to see a kingfisher along the banks of the River Derwent. On the reservoirs and other larger bodies of water, goshawks often hover high above honking geese on Ladybower (Route 1), while osprey in the migratory season and lapwings in winter grace Carsington Water (Route 4).
Plants and flowers
While snowdrops are often the first to flower, it’s usually March before more wild flowers are in evidence, with daffodils being among the first (Route 19 has a surprisingly good display up the hill to Wessenden Moor). Soon after that, bluebells form carpets of blue for a few brief spring weeks (Grenoside woods, just north of Sheffield, is a good place to see these), and wild garlic often goes rampant, creating pungent swathes of white. (Both bluebells and wild garlic prefer limestone woodlands.)
Derbyshire bluebells
Come late spring/early summer, many fields explode into flower as hay meadows take advantage of increasing sunshine and one of the Peak District’s many rare species – the early purple orchid – comes into flower. A short detour into one of the many limestone dales will be rewarded with a view of this small purple flower: Monks Dale (near Route 11) is especially renowned for them. Meanwhile hawthorn trees create a profusion of white-flowered hedges.
Later on, the verges of many country lanes gain an infusion of pink (from rosebay willowherb, foxgloves, campion), blue-purple (vetch, cranesbill and harebells – especially towards Staffordshire/Cheshire), white (cow parsley and daisies of all sizes) or yellow (from humble dandelions and buttercups to poisonous ragwort). Many of the rough upland moorlands also turn shimmering white with cotton grass and the purple blush of moorland heather turning the harsh upland landscape into a much softer and more colourful scene needs no introduction to anyone who has seen tourist brochure images of the Peak District: this is best seen in late July to early September.
From August onwards, purple-stained fingers and lips give away those who have been enjoying the deliciously ripe wild bilberries (moorlands) and brambles (lower-lying lands); but nettles, brambles, bracken and butterbur (huge rhubarb-like leaves lining limestone dales) threaten to take over any path not frequently ridden.
Autumn then brings beautiful leafy shades of red, yellow and brown – especially on beech and chestnut trees, whose nuts are now ripe and falling before winter claims a harsh quietness in the floral world and the cycle starts once again in January.
History
Cyclists would be forgiven for thinking the Peak District was named for its abundance of hilly routes, but in fact this has nothing to do with topography, and everything to do with an ancient tribe called the Paec. These Paec-saetna were Anglo-Saxons from further south, who moved up the Dove and Derwent valleys and settled in what became known as the Peak District from roughly AD400. Over time they became a distinctly separate tribe from their southern, lowland cousins and the term Paec-saetna (or Pec-saetan) was used to distinguish them from other Dark-Age inhabitants of Mercia. (At this time England was divided into three kingdoms: Mercia formed the middle kingdom between Northumberland and Wessex.) The regional name of ‘Peak District’ is thought to come directly from this ancient ‘Paec’ tribe.
Going back much further in time, Creswell Crags is