Hedgehope Hill

Hedgehope Hill

Hedgehope Hill rises to 714.4 m in the Cheviot Hills of Northumberland National Park, above the Harthope Valley southwest of Wooler. Its summit, rocky approaches and neighbouring valleys bring together several different landscapes: exposed upland, a wooded burn, ancient settlement remains and rocks formed deep inside a Devonian volcanic complex.

Summit and geography

An OS trig point stands on an ancient cairn. The summit-feature grid reference is NT 94386 19787; the measured height refers to the cairn’s edge at NT 94381 19798, the highest visible natural ground. These are distinct locations, and the height is not a measurement to the top of the trig pillar. The recorded prominence is 147.3 m.

The Cheviot lies west-northwest, across the Harthope Valley. Comb Fell lies to the southwest and is linked to Hedgehope by a broad col. The summit cairn’s date and original purpose are not established here.

Geology: granite, hot fluids and a later dyke

Hedgehope belongs to the Devonian Cheviot igneous complex. Granite formed as magma cooled below ground; volcanic rocks formed from eruptions at the surface. The granitic core was injected into the older volcanic rocks, heating and changing them around its margins.

Around Hedgehope’s summit, granitic boulders contain conspicuously larger crystals within a finer crystalline mass, a texture called porphyritic. Hot fluids subsequently altered these rocks: some original minerals were replaced, and minerals including chlorite and tourmaline developed. A quartz-porphyry dyke cuts through the granitic rock near the summit. Fragments of granite enclosed in the dyke help reveal the sequence: the host rock existed before the later intrusion. This gives Hedgehope a more intricate geological story than its smooth outline suggests.

The shape of the landscape

The Harthope Valley follows a major fault through the Cheviot massif. Its linear course and steep sides contrast with the rounded uplands. Weathering, ice and meltwater helped shape this landscape long after the igneous rocks formed. Nearby tors also differ in composition: Housey Crags and Long Crags expose altered volcanic rock, whereas Great Standrop, south of Hedgehope, is a granite tor.

The Harthope Burn rises on The Cheviot’s southern slopes and runs northeast through the valley, passing Langleeford Hope and Langleeford. Farther downstream it joins Carey Burn, becoming Wooler Water and eventually reaching the River Till. Isolated farms, rather than villages, characterise the upper valley.

Archaeology around Hedgehope

The surrounding slopes preserve a much longer human history than the modern walking paths suggest. On a terrace below Long Crags, 600 m southeast of Langleeford, are the remains of a native farmstead occupied during the Roman period. Its irregular enclosure measures up to 67 by 40 m, with two circular house sites and a scooped courtyard inside, plus another circular house outside. This was a farming settlement in the local landscape; the Roman-period date does not identify it as a Roman military camp.

East of Hedgehope, near Threestoneburn House, a stone circle and associated alignment belong to the Late Neolithic or Early Bronze Age. The oval ring measures roughly 36 by 30 m and comprises 16 stones of local pink granite. Partial excavation in 1856 recovered charcoal and a flint tool; peat had accumulated over the original ground surface. The circle and the Long Crags farmstead are separate monuments away from the summit cairn, and neither is included as a visit in the two walking circuits below. Their presence illustrates different uses of this landscape across prehistoric and later farming communities.

Habitats and wildlife

The alder-fringed Harthope Burn provides a sheltered contrast to the open slopes above. Around the valley, birds to watch and listen for include curlews, stonechats, meadow pipits, whinchats and skylarks. Buzzards may be seen overhead, and merlins are a possibility. Adders also occur in the valley. These are wildlife possibilities, rather than promised sightings or a list of species confined to Hedgehope’s summit. Take time to look from the path and avoid disturbing animals.

Views

On a clear day the outlook reaches across the Cheviots to the Northumberland coast, including Bamburgh Castle and the Farne Islands. The Cheviot is the prominent neighbouring hill across the valley.

Two complete walking circuits

Both walks below include Comb Fell as well as Hedgehope. Distances, ascent and times describe the whole return circuit, not a direct summit out-and-back. Treat times as planning estimates and allow for your pace, stops, weather and ground conditions. Both are moderate-to-hard hill walks.

From Langleeford: upper Harthope Valley and Comb Fell

About 14.5 km, 667 m ascent; allow around 6 hours 20 minutes. Start and finish at roadside parking NT953225, before Langleeford.

Follow the valley through Langleeford and Langleeford Hope, continuing beside Harthope Burn to Scotsman’s Knowe. Cross Comb Fell and the intervening col to Hedgehope. Descend north, then northeast past Long Crags and Housey Crags, returning across the Harthope Burn footbridge to the start.

From Hartside: Linhope Spout and the southern approaches

About 17.2 km, 727 m ascent; allow around 7 hours 10 minutes. Start and finish at roadside parking NT975162 near Hartside, beyond Ingram.

Walk through Linhope to Linhope Spout, then follow the Linhope Burn and Standrop Burn approach towards Comb Fell. Continue over Hedgehope and return by Dunmoor Hill, Cunyan Crags and Greensidehill to the Hartside road. The extra summits and waterfall make this a substantial full-day circuit. Expect rough heather and intermittent paths.

Access, preparation and safety

Use a detailed map to plan either circuit; these outlines are not turn-by-turn navigation. Check current access notices and the condition of paths and crossings before setting out. Park only where permitted, leave entrances clear and follow signs. Wooler has shops, places to eat and public toilets; carry food and drink for the hill walk.

Steep slopes, wet ground and intermittent paths require care. Carry a map and compass and know how to use them. Take suitable footwear, warm layers and waterproofs, check the hill forecast and leave enough daylight for the whole return. Snow or ice can change the difficulty considerably and may require winter equipment and skills. Choose a route and turnaround time that leave a margin for deteriorating conditions.

Credits

Hill data: The Database of British and Irish Hills v18.6 (https://www.hill-bagging.co.uk/dobih/), CC BY 4.0 (https://creativecommons.org/licenses/by/4.0/); wording adapted.

Heritage information: Historic England. Contains public sector information licensed under the Open Government Licence v3.0 (https://www.nationalarchives.gov.uk/doc/open-government-licence/version/3/).