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England Landscape Photography
Walking Hiking England

Hermit’s Cave, Ecclesbourne Glen, Hastings

Introduction

Ecclesbourne Glen is one of those places that feels completely removed from the town above. Within a few minutes of leaving the cliff top, you drop into a narrow, wooded valley with a running stream, small waterfalls, and steep sandstone sides.

On this walk, I came down a footpath I’d never used before and finally found the Hermit’s Cave — tucked into the rock face, half hidden by vegetation and easy to miss if you didn’t know it was there.

It’s not large, but it has presence. The surrounding sandstone is heavily weathered and pitted, with a natural overhang that forms a shallow cave. Combined with the woodland setting, it feels like a place that belongs to a different time.

A short clip from the walk:

After filming, I’ve included the exact location below so you can find it yourself, along with the full map of all the places I’ve explored.


The Story of the Hermit

The cave is most commonly linked to John Hancox, often referred to as the East Hill Hermit.

He was originally a London draper who fell on hard times in the late 1800s and came to Hastings. At some point in the 1890s, he took up residence in this cave in Ecclesbourne Glen.

Sandstone overhang at Hermit’s Cave Ecclesbourne Glen showing textured rock formation
The textured sandstone overhang that forms the natural shelter of Hermit’s Cave

Local records suggest the landowner, Rev. Sayer-Milward, later allowed him to stay and even gave him a small patch of land in front of the cave. Here, Hancox lived a quiet, isolated life, growing some of his own food and becoming something of a local curiosity.

He remained here until his death in 1918.

Standing in front of the cave today, it’s easy to see why someone might choose this spot. It’s sheltered, tucked away, and surrounded by woodland and water — completely separate from the town just below.


The Landscape

Ecclesbourne Glen is part of the wider Hastings Country Park Nature Reserve, where the High Weald meets the coast.

This landscape is defined by soft sandstone, which erodes easily and creates the steep-sided valleys, overhangs, and rock formations you see throughout the area. The cave itself is simply a natural feature shaped over time, later adapted as a shelter.

The glen is also classic gill woodland — a damp, sheltered valley with its own microclimate. You’ll find ferns, moss, and early spring growth covering the ground, with the stream cutting through the centre.

It’s this combination of geology and woodland that makes the area feel so enclosed and atmospheric.


Visiting the Cave

The Hermit’s Cave works best as part of a walk through Ecclesbourne Glen rather than a standalone destination.

Close view of Hermit’s Cave Ecclesbourne Glen showing weathered sandstone and surrounding ferns
Weathered sandstone and ferns surrounding the entrance to Hermit’s Cave in Ecclesbourne Glen

The approach is what makes it — following the stream, hearing the water before you see it, then suddenly coming across the cave set into the rock.

For photography, a wider composition works well to show the cave in context with the surrounding sandstone. A lower angle helps emphasise the overhang and the texture in the rock face.

Spring is ideal when the valley is fresh and green, but it would also suit autumn colours or damp winter conditions.


Practical Info

Location
Ecclesbourne Glen, Hastings Country Park, East Sussex

Access
Reached via public footpaths through Ecclesbourne Glen. Paths can be uneven, muddy, and steep in places.

Safety
This is an area of soft sandstone and ongoing erosion. Keep well back from cliff edges and avoid unstable sections.

Best Time to Visit
Spring for greenery and water flow, autumn for colour, winter for mood and atmosphere.


Nearby

If you’re exploring Ecclesbourne Glen, these are all close by and worth combining into the same walk:

  • Covehurst Bay – A quiet, remote beach below the cliffs, far less busy than Hastings seafront
  • Dripping Well – A small but interesting water feature cut into the rock, hidden along the cliff paths
  • Hastings Old Town – Historic streets, fishing quarter, and one of the best preserved old towns on the south coast
  • East Hill – Cliff-top views, coastal paths, and access down into the glens
  • Rock-a-Nore – Fishing boats, net huts, and one of the most distinctive coastal scenes in Sussex

Final Thoughts

The Hermit’s Cave is one of those places that you could easily walk past without ever knowing it’s there.

But once you find it, it adds another layer to the landscape — not just geology and woodland, but a real human story tied into it.

It’s a reminder that these glens aren’t just natural features. People have lived, hidden, and survived in them, often in ways that feel completely removed from modern life.

The Sandstone Ridges of the High Weald

Introduction

Across Tunbridge Wells and the Kent–East Sussex border lies a hidden geological landscape — a chain of sandstone ridges formed over 100 million years ago.

From the open commons above the town to woodland reserves and climbing crags, these formations are all part of the same system: the Tunbridge Wells Sand Formation. What appears as separate locations — Wellington Rocks, Toad Rock, Eridge Rocks, High Rocks and Harrison’s Rocks — are in fact different expressions of one ancient landscape.

This post brings them together as a single journey through geology, history and place.


Watch the Film

Short film exploring the sandstone ridges of the High Weald:

Explore all locations on the map:
[View all mapped locations]


Wellington Rocks

Tunbridge Wells Common

Wellington Rocks sit on Tunbridge Wells Common, right on the edge of the historic spa town. These sandstone outcrops are among the most accessible in the area, rising directly from open heathland and woodland.

Wellington rocks tunbridge wells common
Sandstone outcrops on Tunbridge Wells Common, known as Wellington Rocks, part of the Tunbridge Wells Sand Formation in the High Weald. These weathered iron-rich rocks rise from open heathland just above the historic spa town of Royal Tunbridge Wells, Kent.

The name “Wellington Rocks” is linked to the nearby Wellington Hotel, reflecting the Victorian period when Tunbridge Wells was a fashionable destination and the Common was part of everyday leisure life.

Here, geology is woven into the town itself. Visitors have walked these rocks for centuries, long before they were understood scientifically. Today they remain a quiet introduction to the wider sandstone landscape beneath the High Weald.


Toad Rock & Rusthall Common

Rusthall Common

A short walk west from Tunbridge Wells Common leads to Rusthall Common and the distinctive Toad Rock.

Toad Rock, Rusthall Common, Kent
Toad Rock on Rusthall Common near Royal Tunbridge Wells, Kent. This distinctive weathered sandstone formation is part of the Tunbridge Wells Sand Formation within the High Weald, shaped over millions of years into one of the area’s most recognisable natural landmarks.

Shaped by differential erosion, the rock’s perched form gives it its name. By the early 19th century it had already become a local curiosity, appearing in guidebooks and attracting visitors who tried to interpret its unusual shape.

Rusthall Common contains far more than a single landmark. Nearby features such as Bull’s Hollow reveal sheer sandstone faces and remnants of past quarrying activity. It is a landscape where geology, folklore and human use overlap.


Eridge Rocks Nature Reserve

Eridge Rocks Nature Reserve

Just across the county border into East Sussex, Eridge Rocks reveals a more atmospheric side of the sandstone landscape.

distinctive sandstone rocks at Eridge high weald
Sandstone formations at Eridge Rocks Nature Reserve near Eridge, East Sussex. Part of the Tunbridge Wells Sand Formation within the High Weald, these weathered Cretaceous sandstones rise through woodland and heath, shaped over millions of years by natural erosion into one of Sussex’s most distinctive geological landscapes.

Here the formations rise as towers, cliffs and narrow passages through woodland and heath. The setting feels quieter and more enclosed, with the rock emerging unexpectedly from the trees.

Now protected as a National Nature Reserve, the site is valued not only for its geology but also for its habitats. Mosses, lichens and ferns thrive on the sandstone surfaces, while the surrounding woodland supports a diverse ecosystem.

Eridge Rocks shows how this ancient geology has become part of a living natural environment.


High Rocks

High Rocks

High Rocks is the most dramatic expression of the sandstone ridge system.

high rocks inscriptions royal tunbridge wells kent
Sandstone formations at High Rocks near Royal Tunbridge Wells, Kent. Part of the Tunbridge Wells Sand Formation within the High Weald, these dramatic Cretaceous sandstone cliffs and narrow fissures have been shaped over millions of years by natural erosion, forming one of the most distinctive geological landscapes in the area.

Here the rock forms towering cliffs, narrow gullies and enclosed passages that can be walked through. The scale and structure of the formations make it one of the most visually striking sites in the region.

High Rocks also carries a strong human history. In the Georgian and Victorian periods it became a major attraction for visitors from Tunbridge Wells. Some left behind carved inscriptions — poems and moral reflections — offering a glimpse into how people once interpreted these natural formations before modern geology.

Today, High Rocks is a managed site, used for events and open to visitors at set times. It remains a place where natural history and human history are closely intertwined.


Harrison’s Rocks

Harrison’s Rocks

South of Eridge, near Groombridge, Harrison’s Rocks forms a long sandstone ridge running through woodland.

Harrison rocks high weald kent
Sandstone formations at Harrison’s Rocks near Groombridge on the Kent–East Sussex border. Part of the Tunbridge Wells Sand Formation in the High Weald, these weathered Cretaceous sandstone cliffs form a long natural ridge through woodland and are a well-known climbing area as well as an important geological feature of the landscape.

Unlike the more sculpted formations elsewhere, this site reveals the sandstone as a continuous wall of rock, stretching through the landscape. It is one of the most important sandstone climbing areas in southern England.

Because the rock is soft and easily damaged, climbing here follows strict traditional practices designed to preserve the stone. This ongoing use makes Harrison’s Rocks a living landscape, where ancient geology continues to shape modern activity.


A Connected Landscape

Although each location feels distinct, they are all part of the same geological system.

Laid down in the Early Cretaceous period as river sediments, the sandstone was later exposed and shaped by millions of years of erosion. What we see today — cliffs, ridges, towers and fissures — are different outcomes of the same underlying processes.

Each site tells a different part of the story:

  • Wellington Rocks — geology within the town
  • Toad Rock — shape and folklore
  • Eridge Rocks — geology within nature
  • High Rocks — spectacle and interpretation
  • Harrison’s Rocks — ongoing human use

Together, they reveal a hidden sandstone world beneath the High Weald.

Crowhurst Yew Tree, East Sussex – Ancient Yew Beside St George’s Church

Introduction

The Crowhurst Yew Tree, located in the churchyard of St George’s Church in East Sussex, is one of the oldest living things in the county.

Estimated to be over 1,300 years old, it predates the Norman Conquest and may even mark a site of spiritual importance stretching back into pre-Christian Britain.

Continue reading Crowhurst Yew Tree, East Sussex – Ancient Yew Beside St George’s Church

St Helen’s Well, Hastings


Introduction

Hidden in St Helen’s Wood above Ore in Hastings is a small spring known as St Helen’s Well. Tucked away in the woodland valley below the ridge where Old St Helen’s Church stands, it’s an easy place to walk past without ever realising it’s there.

The well itself isn’t marked on modern OS maps, but the clue lies in the spring symbol in the valley. By heading towards the nearest spring relative to St Helen’s Wood, it’s possible to track down the location where the water emerges from the hillside.

Continue reading St Helen’s Well, Hastings

Eridge Rocks Nature Reserve, East Sussex

Introduction

Eridge Rocks Nature Reserve contains some of the most impressive sandstone formations in the High Weald. Located just inside the East Sussex border near Tunbridge Wells, the reserve reveals a maze of weathered sandstone towers rising through woodland and heathland.

The rock formations are part of a wider sandstone belt that runs through this landscape, linking Eridge Rocks with nearby sites such as High Rocks, Harrison’s Rocks and the formations on Tunbridge Wells and Rusthall Commons.

Continue reading Eridge Rocks Nature Reserve, East Sussex

Old St Helen’s Church Ruins, Hastings

Introduction

The church’s elevated position reflects an older landscape. In medieval times churches were often built on high ground overlooking settlements and farmland, both for visibility and for the practical benefit of dry ground above the valley below.

Standing quietly on the ridge above Ore in Hastings are the remains of Old St Helen’s Church, one of the oldest church sites in the town. Today the roofless walls and sturdy tower sit among weathered gravestones and grass, but for centuries this was the parish church serving the surrounding rural community.

Continue reading Old St Helen’s Church Ruins, Hastings

Harrison’s Rocks, Groombridge

Introduction

Harrison’s Rocks is one of the most impressive sandstone ridges in the High Weald. Located near Groombridge on the Kent–East Sussex border, the site reveals a long line of weathered sandstone cliffs rising through woodland.

Unlike some of the more sculpted formations nearby, Harrison’s Rocks stretches as a continuous ridge, giving a clear sense of the scale of the sandstone layers beneath the landscape. It is also one of southern England’s best-known sandstone climbing locations.

Continue reading Harrison’s Rocks, Groombridge

High Rocks, Royal Tunbridge Wells

Introduction

High Rocks is one of the most dramatic sandstone landscapes in the High Weald. Rising above Royal Tunbridge Wells, these towering formations form a maze of cliffs, narrow passages and sculpted rock faces hidden within woodland.

Although many sandstone outcrops exist across the Tunbridge Wells area, High Rocks stands out for its scale and accessibility. Visitors can walk directly beneath and between the formations, giving a rare chance to experience the full height and structure of the sandstone ridge.

Continue reading High Rocks, Royal Tunbridge Wells

Toad Rock, Rusthall Common

Introduction

Toad Rock is one of the most distinctive sandstone formations in the Tunbridge Wells area. Perched on Rusthall Common just west of Royal Tunbridge Wells, the rock appears almost sculpted — its rounded upper section balanced on a narrower base, giving it the familiar “toad-like” shape that gives the landmark its name.

It is part of the same sandstone ridge system that runs through Tunbridge Wells Common, High Rocks and Eridge Rocks, forming one of the most interesting geological landscapes in the High Weald.


Short film from Rusthall Common and Toad Rock:

Just a short walk from Wellington Rocks on Tunbridge Wells Common, Rusthall Common reveals even more dramatic sandstone formations — including Bull’s Hollow, where sheer rock faces rise abruptly from the woodland floor.

Location: Rusthall Common, Kent
[View on Google Maps]
[See all mapped locations]


The Geology

Toad Rock is formed from the Tunbridge Wells Sand Formation, laid down around 100 million years ago during the Lower Cretaceous period.

At that time, this part of southern England was a vast river delta. Sand and sediment carried by ancient rivers settled in layers and gradually compacted into sandstone. Over millions of years, erosion exposed the rock and sculpted the shapes visible today.

Toad Rock, Rusthall Common, Kent
Toad Rock on Rusthall Common near Royal Tunbridge Wells, Kent. This distinctive weathered sandstone formation is part of the Tunbridge Wells Sand Formation within the High Weald, shaped over millions of years into one of the area’s most recognisable natural landmarks.

The unusual perched shape of Toad Rock is the result of differential erosion — where softer layers of sandstone wear away more quickly than harder layers above them. The harder cap protects the rock beneath, leaving the characteristic overhanging form.

Iron minerals within the stone give the sandstone its warm brown and reddish tones, particularly visible after rain or in soft overcast light.


Victorian Visitors

Rusthall Common became a popular walking destination during the Georgian and Victorian periods, when visitors staying in Royal Tunbridge Wells would venture out to explore the surrounding countryside.

The dramatic rock formations were seen as romantic curiosities, and Toad Rock became one of the most photographed and described features in local guidebooks of the time.

Many of the surrounding rocks are just as impressive, though often overlooked by visitors focused on the famous “toad” itself.


Bull’s Hollow

Just across the Common from Toad Rock lies Bull’s Hollow, where sandstone cliffs rise sharply above the woodland.

The rock faces here reveal the scale of the sandstone ridge beneath the landscape. Unlike the more sculptural form of Toad Rock, Bull’s Hollow exposes the layered cliff structure of the formation, showing how erosion has cut through the sandstone over geological time.

It remains one of the most striking but lesser-known features of Rusthall Common.


Living With Ancient Stone

One of the most unusual aspects of the area is how closely modern life sits beside these ancient formations. Along nearby Upper Street, houses have been built directly beside and even around exposed sandstone outcrops.

The contrast is striking: homes only decades old standing next to rock formed a hundred million years ago.

It’s a reminder that these geological features long predate the town itself — and will likely remain long after.


Practical Info

Location: Rusthall Common, Kent
Access: Open common land with public access
Parking: Rusthall village or Tunbridge Wells Common
Best Time to Visit: Early morning or overcast conditions for photography
Nearby:Wellington Rocks, High Rocks, Eridge Rocks, Harrison Rocks

Toad Rock is more than just an unusual natural landmark. It is part of a wider sandstone landscape that defines the High Weald — a landscape shaped over millions of years and still quietly embedded in everyday life.

Wellington Rocks, Tunbridge Wells Common

Introduction

Wellington Rocks are a series of weathered sandstone outcrops rising from the open heath of Tunbridge Wells Common. Just above the historic spa town, these formations are part of the same sandstone belt that runs through Eridge, Rusthall and High Rocks — a continuous geological system straddling the Sussex–Kent border.

Shaped over millions of years, the rocks remain one of the most accessible and quietly impressive natural landmarks in the area.


Short film from Wellington Rocks:

A short walk west across the Common leads to Toad Rock on Rusthall Common, making this part of the High Weald one of the richest clusters of sandstone formations in southern England.

Location: Tunbridge Wells Common, Kent
[View on Google Maps]
[See all mapped locations]


The Geology

Wellington Rocks are formed from the Tunbridge Wells Sand Formation, laid down approximately 100 million years ago during the Lower Cretaceous period.

Wellington rocks tunbridge wells common
Sandstone outcrops on Tunbridge Wells Common, known as Wellington Rocks, part of the Tunbridge Wells Sand Formation in the High Weald. These weathered iron-rich rocks rise from open heathland just above the historic spa town of Royal Tunbridge Wells, Kent.

At that time, this landscape was a vast river delta. Sand carried by ancient rivers settled in layers, eventually compacting into sandstone. Over geological time, uplift and erosion exposed the rock. Wind, rain and frost gradually sculpted the softer layers, creating the rounded forms, fissures and ledges visible today.

The iron content within the stone gives the rock its warm, earthy tones — particularly noticeable in soft overcast light or after rain.


Why “Wellington” Rocks?

The rocks were named in the 19th century after Arthur Wellesley, the Duke of Wellington, reflecting the patriotic mood of the Victorian era. Tunbridge Wells was a fashionable spa town at the time, and public features were often given commemorative names.

The Common itself became an important leisure space, with visitors walking out from The Pantiles to enjoy fresh air and views over the surrounding countryside.


Common Land & Protection

Although much of Tunbridge Wells Common is privately owned, it is registered common land. This provides strong protection and preserves public access rights.

Occasionally, parts of the Common appear on the market as freehold interests change hands. However, common land status significantly restricts development and safeguards public access.

Ownership may change over time — the rocks remain.


Photographing Wellington Rocks

Wellington Rocks are best photographed in:

  • Overcast light (to preserve texture and avoid harsh contrast)
  • Early morning or late afternoon for soft directional light
  • Autumn and winter when foliage is thinner and the rock faces are more visible

The perimeter path allows you to walk around and over the outcrops, offering a variety of angles — from close textural studies to wider compositions including heathland and woodland.


Practical Info

Location: Tunbridge Wells Common, Kent
Access: Open access common land
Parking: Town centre / Common roadside parking
Best Time to Visit: Early morning for quiet conditions and soft light
Nearby: Rusthall Common (Toad Rock), The Pantiles, High Rocks


Wellington Rocks form part of a remarkable sandstone ridge system that defines this corner of the High Weald. A landscape shaped long before county lines were drawn — and one that continues to offer geology, history and open space in equal measure.

Landscape Photography Review 2025

2025 Photography Year in Review

2025 was a year of working closer to home and learning to respond to conditions rather than chase them. From misty dawns on the South Downs to woodland waterfalls in the High Weald and long exposures on Romney Marsh, this review brings together one standout image from each month — moments that best reflect how and where I photographed across the year.

Continue reading Landscape Photography Review 2025

December 2025: Sussex Photography Monthly Review

Introduction

December 2025 was dominated by wet, cold and overcast weather across East Sussex, which quietly shaped the direction of my photography. With wider landscapes often flat and uninviting, the focus naturally shifted into woodland, following streams and revisiting places that only reveal themselves after prolonged rainfall. The result was a month spent exploring seasonal waterfalls across the High Weald, interspersed with a handful of coastal and observational shoots.

This post brings together those December walks and discoveries, from hidden ghylls and temporary cascades to a final New Year’s Eve sunset at Beachy Head.

Continue reading December 2025: Sussex Photography Monthly Review