Tag Archives: The Kimmeridge Pliosaur

Jurassic Coast: the Mystery of the Freshwater Steps

see also
Anfibio Sigma TXL+ main page
English South Coast Day Paddles
Kimmeridge Ledges with Zelgear Igla IK
Packrafting Kimmeridge to Chapman’s Pool
In Search of the Kimmeridge Pliosaur

Punta Pliosaurus

Unsatisfied with my bank holiday paddle-by, two days later we hiked back to Chapman’s and packrafted back round to Punta P. We left right on LW spring, but either my tide timings were wrong (don’t start me on that) or Chapman’s shore doesn’t dramatically transform, like Kimmeridge beach.
It was less than a mile’s paddle, but a strong SSE was blowing and once out of the Pool, it got choppy around Egmont Point, especially into the wind on the way back. It didn’t help that I had the TXL’s floor mat fitted for extra glide, but which I know doesn’t work well for a rear paddler: higher floor = less or no backrest = not relaxing.

Once at the cliff face and with the boat resting in the shade of the Freshwater rock spur, the Mrs easily found fragments of ammonites in the shingle (why always ammonites?). We edged round the spur’s tidal shelf onto Pliosaur beach where a woman looked down from above and asked
‘Ow d’you get down there?’
‘We paddled.’
‘Uh..?’


Despite an exceedingly dry spring and summer, a cascade was still dribbling down the cliff face through tendrils of moss, ferns and algae (below). It was the end of the South Gwyle, a short stream with a big catchment. Augmented by a couple of landscaped fish ponds up the valley at Encombe House (more below), ‘gwyle’ is an old Dorset word for a tree-lined stream.

Fallen and weathered concrete slabs below a protruding step on the cliff edge: the remains of the mysterious ‘Freshwater Steps’

With nothing more to learn about the pliosaur, I was curious about the odd limestone wall up on the clifftop, seemingly bridging the stream. Clearly visible on aerial imagery, I’d noticed it walking back the other day to Kimmeridge, but was too hot and bothered to explore. Perhaps the ruin of an old mill?

Landslide into Egmont Bight

On the east (other) side of the dark shaly spur from which the cascade falls, the protruding end of the wall is being undermined, and now hangs over the cliff edge (below). Cracking under its own weight, one day it’ll collapse and fall to the beach. We parked the packraft here, in the shade of the spur. The face was full of fossils, but bits of grit were constantly dropping from above.
While here I had a look at the probable site of the landslide I’d seen on Saturday (left), but it must have looked more dramatic than it was on the beach, and these little slides must happen all the time.

Overhanging east end of the wall from above and the beach, slowly being undermined by the receding cliff (2025)

Photos by Phil Champion on Geograph from 2008. On the left note the ‘other’Ladies’ Steps’ (‘for ladies to climb easily to a path leading to the Carriage road‘) descending to the wall: the old footpath still part of the SWCP in the 1970s but now under thick brambles or thin air. The wire fence and all the pillars seen above have disappeared, bar one. It’s amazing it’s all lasted so long, given its exposure, but the east side of the spur has lost several feet in height and width in 17 years.

Freshwater Steps and the Hydraulic Ram, map 1901 (Source)
Map 1811 (Source)

Back on the west side of the spur, ‘Freshwater Steps’ is a name I’ve seen on older maps (above) and, as expected, locally born geologist Ian West’s geological and historical page had some answers, as well as many fascinating old photos.
In fact ‘Freshwater’ seems to have been a name for this locality (left) which preceded the Steps. Perhaps a place a boat could pull in to top up the water barrels? I’ve noticed another ‘Freshwater’ on the south coast of Devon.

Encombe House, 1857, photolithograph, John Pouncy (source)

As far as I can unravel, the story goes that round 1840, the Freshwater Steps were built down to the beach by John Scott, the 2nd Lord Eldon whose Encombe estate enveloped a grand Georgian mansion (above) bought in 1807 by his grandfather, former Chancellor Lord Eldon (also John Scott; d. 1838; right). History has not judged the first Lord too fondly according to usually impartial Wikipedia, as well as this writer who puts him alongside the famously loathed Castlereagh of the late Regency era. Since those days the estate has grown greatly.

The falls today at Freshwater Steps. The last hanging step visible top left

The surviving stone wall is actually the portal of a finely built, 60-metre, stone-lined culvert passing under the South West Coast Path (gallery above). Downstream, a cobbled canal once redirected the stream over the promontory’s tip (another image from 1965), though the 2004 Purbeck Revealed book (see below) seems to explain this as a natural feature, despite the stone-lined canal.
Freshwater and sea storms eroded the spur and the stream receded to its current position (left) – the same geological process which, decades later, saw a pliosaur snout drop to the shore with an unheard thud.

Google Earth historical imagery. In 2002 the coast path still took the old way close to the cliffs and through the scrub (as still shown of Google Maps today), the wall and canal appear intact with a pillar at each end of the wall and another (which has been moved but still survives in the grass) marking a gateway to the Steps whose lower have have collapsed to the beach. At least 2 metres of cliff have also slipped down from the eastern side of the spur. Another, more overgrown image from 2005; the canal wall remains intact and the waterfall tips off towards the end. Note the gully above the as-yet unfound pliosaur, it may have contributed to the erosion which eventually exposed the snout. By 2014 the SWCP had rerouted north, the western canal wall had collapsed, littering the beach below and putting the waterfall in its current position, although the upper Steps are still evident. The wall is collapsing on the east side. Current GE imagery appears to extend the east wall which suggests artificial enhancement, possibly AI?

Mid-19th century ‘carriage roads’

Why all this work diverting the gwyle through a culvert and building the Steps? Perhaps, along with the estate’s fine gardens and numerous carriage roads (one cutting right across long subsided Houns Tout cliff to Chapman’s; left), it was all about impressing visitors with picturesque ‘follies’ along with the supposed health benefits of bathing in sea water (see pump house below) which had helped put nearby Weymouth on the map.
Purbeck Revealed (2004) by Ilay Cooper may have another explanation. Born in Swanage during WW2, the author describes larking about on the Encombe estate as a boy. According to his research, the second Lord was responding to water shortages on the estate with bold Victorian engineering, not engaging in late Regency frippery. The gwyle’s catchment was not so broad after all, necessitating the digging of long, stone-lined tunnels and laying pipes into adjacent valleys in search of springs. The Freshwater project may have been little more than a spin off while the builders and masons were in. Certainly Encombe sat right on top of lashing of Purbeck stone from which the house itself was originally built.

The Steps and Falls may have modestly been trying to outdo the 1831 Clavell Tower folly (right), three miles west along the SWCP on the adjacent Smedmore Estate. The Tower survived a little better than the Freshwater infrastructure, but a century on, it was a ruined, burned out shell. By 2007, in poor shape internally and fast becoming the ‘Leaning Tower of Purbeck’, a funding campaign finally succeeded in having it dismantled brick by brick and moved back from the cliff edge.

Note that especially on the east side, the cliff is much more receded than this modified map, based on the Definitive County Map, shows
Near the Steps, this doesn’t look like a ‘hydraulic ram’ as shown on maps.

On another visit here, exploring the area just north of the wall, a friend noticed a rusted iron fence and overgrown steps (left) leading down to a domed chamber. Inside a heavily corroded crank and flywheel (above) looked like the ‘Hydraulic Ram‘ noted on late-1800s maps (below) and listed on Dorset Heritage. But the position doesn’t line up with old maps and I must admit, the device we saw doesn’t resemble any vintage ram pumps found online, each with their distinctive bulbous ‘accumulator’ chamber. With the hand wheel and crank, this looked more like a means to vertically open a sluice valve. Maybe there’s more elsewhere or below the stone floor.
At Encombe, old sources say the pump was used secondarily to move sea water up to the house where people could bathe in privacy, not on the beach like the hoi polloi. It may explain the small side shaft I noticed passing through the culvert probably directly under the pump house – an outlet for the sluice or the ram’s ‘waste valve’ perhaps? Assuming sea water bathing didn’t go on round the clock at Encombe, the chamber we found may have been a valve to get the hydraulic ram pumping.
The pump house was also alongside a shorter trail to the SWCP, joining it just before the steps climb westwards.

Map late 1800s Source

A ‘hydram’ is an ingenious ‘uphill water pump’ invented by one of the Mongolfier brothers in 1796, a decade or more after their famous hot air balloon flight (left) also turned the concept of gravity upside down. The pump uses the free energy of a constant water source and the ‘water hammer’ effect (the bang when you shut off a tap quickly) feeding pipes fitted with a pair of one-way valves. Once balanced, it slowly but surely pumps water way above the inlet source with a little wastage from the first valve – see vid below.
Requiring no external power and little maintenance, hydraulic rams and similar devices were common in the pre-electric 19th century, and have been rediscovered today by off-griders and remote villages in the developing world.


There’s a good account extracted from local born Bob Dorey’s (1892-1995) memoir – Odds & Ends from My Century (1992) – on the Kingston history page. Here, the old village pub was renamed the Scott’s Arms after WW2. OS maps also show ‘Eldon’s Seat’ half a mile to the northwest of the Steps, the first Eldon’s private viewpoint.

Finely built culvert, nearly 200 years old. Crawling through here was all a bit ‘Famous Five and the Mystery of the Freshwater Steps’. At the end of the tunnel I was expecting to find a lost smugglers’ hoard draped by a couple of skeletons. Maybe I’ve read too many books.

Storms raged and the soft shale crumbled, slowly taking the Steps, and parts of the wall and channel with them. The falls broke through to spill down the mossy cliff some time after 2005, and around 1978 (according to Purbeck Revealed) the Steps, long undercut, collapsed entirely, never to be trod again.

A castaway’s last desperate attempt at rescue.

Deary me, we have drifted a long way from packrafting and adventures in packboats. We set off back to Chapman’s, the TXL riding over bigger waves like a dead pliosaur. The Mrs was not at ease and next day Poole Coastguard reported being swamped with incidents.
I was also surprised how sore the shoulders were next day after just 2.5 kms there and back in the wind and waves, compared to Saturday’s calm 6-kilo ride over from Kimmeridge. Seems it was more effort than it felt, like a short but rough MTB ride vs a longer road ride. Repeating that crossing today in a packraft would’ve been utterly exhausting if not an outright Bad Idea. But that’s why we wait and wait for the 10% chance of <10mph tailwinds with favourable tides.

Chapman’s mule

In Search of the Kimmeridge Pliosaur

Anfibio Sigma TXL+ main page
English South Coast Day Paddles
Kimmeridge Ledges with Zelgear Igla IK
Packrafting Kimmeridge to Chapman’s Pool
The Mystery of the Freshwater Steps

They say everyone remembers where they were when the BBC aired ‘Attenborough and the Giant Sea Monster‘ on New Year’s Day, 2024. ICYMI, it’s still on iPlayer and having watched it, you’ll realise the profile of the famously fossil-rich Kimmeridge cliffs along Dorset’s Jurassic Coast has been raised further. Come high summer it’s impossible to find a park at the local Sainsbury’s.

Attenborough and the Giant Sea Monster – on BBC iPlayer last time I looked

The story goes that in 2022, fossil enthusiast Phil Jacobs was fossicking along a difficult-to-access beach at low tide when he discovered a huge, crocodile-like snout in the shingle (left).
He contacted Steve Etches (below) at the nearby Etches Collection fossil museum in Kimmeridge and, long story short, a two-metre pliosaur skull was laboriously excavated from the friable cliff-face from which the snout had dropped. The BBC and Attenborough recorded it all as over months, the skull was painstaking restored and primed to go on display at the Collection the day after the documentary aired. Good article.

Steve Etches dwarfed by the massive pliosaur skull

I’d visited the usually deserted museum over Christmas a week earlier, finding another similarly huge pliosaur jaw and many other amazing marine fossils on display. Returning on a stormy January 2nd after the broadcast, the place was packed with curious visitors blithely ignoring the ‘No Photos’ edicts right under Steve Etches’ nose. Since then the Pliosaur has been rebranded as the ‘Sea Rex‘.

Smedmore Estate signs at Kimmeridge Bay (left) warn against doing many things, including fossil hunting, and yet the museum has a video on how to do this safely. So I wondered how permission worked in the technically ‘neutral’ or Crown-owned intertidal zone (ITZ) where the fossil-rich Kimmeridge Ledges lie, and further east where the snout was found. A member of staff explained that protected SSSI status (see map or below) extended into the ITZ (as it might do for coral reefs) and Etches, a local man with decades of fossil collecting behind him, is the only person with permission from the Smedmore Estate (who help fund his museum) to excavate fossils, presumably in the cliffs fringing their land above the ITZ.

Kimmeridge SSSI includes ITZ

Perhaps finding tiny, loose fossils while beach combing is tolerated. When I was packing up my packraft the other day at Chapman’s Pool, I flicked off a wet flake stuck to the boat and could swear it was a thumbnail-sized ammonite fossil, DoB: 150,000,000 BC. I tried to find it among the shingle, but the fast-rising tide was lapping at my feet, so it got away. Another time down at Chapman’s (below left), the geef easily found a curl of ammonite shell the size of a thumb. Ammonites embedded in the exposed grey bedrock are everywhere (above left).

Like many who know the area, I was curious to know exactly where the fossil was found – or more accurately, solving the geo-locating challenge was a bit of ‘Wherewozit’ fun. Not surprisingly, the location was conspicuously absent from mainstream reports, but within the first minute of the BBC doc the excavation site is shown, and a couple of minutes later, snout finder Phil Jacobs’ shaky phone video pans past a waterfall in the background with a limestone wall bridging it (more below), and a mention of ‘east of Kimmeridge’. Ah Ha! The waterfall appears again in the BBC doc, so all in all you don’t have to work for GCHQ to pin down a possible location.

Fast forward a year and I finally got to paddle past what looked like Punta Pliosaurus on my way to Chapman’s from Kimmeridge. Beforehand, I’d wondered what would be there: disingenuous ‘Danger, Keep Away, Loose Cliff’ signs, evidence of excavation to retrieve the rest of the megafish’s body, or a huddle of day tourists from Swanage?

Although a late-afternoon sun was casting a shadow across the cliff (above right), all I can say is, assuming I’d got the right place, they’ve done an superb job of disguising the excavation of the pliosaur skull and restoring the cliff’s natural appearance until they get a chance to come back and finish the job. That said, a couple of weeks later a regular walker who knew the story here thought natural processes had quickly obliterated the excavation but either way, once done, they’re gonna need a bigger display case. Meanwhile, something else above the beach had caught my eye. More about that here.

Packrafting Jurassic: Kimmeridge to Chapman’s Pool

Anfibio Sigma TXL+ main page
English South Coast Day Paddles
Kimmeridge Ledges with Zelgear Igla IK
The Kimmeridge Pliosaur
Packrafting the Jurassic Coast (video)
Packrafting Lulworth Cove to Kimmeridge
Dancing Ledge and Sea Caves

Action Stations and man the pumps. Conditions are finally benign for a paddle from Kimmeridge Bay to Chapman’s Pool – a distance of over three point six miles. It’s not exactly rowing the Pacific, but in a dumpy packraft you need to pick your moments when there are no take-outs from one end to the other, followed it’s a stiff, four-mile walk back.
A big spring tide was inbound for HW about 8pm and the wind was forecast at just 8mph SSW (onshore) and dropping by late afternoon. Plus it was sunny, too. Which was nice.

I packed a paddle in my pack and rode down to Kimmeridge Bay.
At Kimmeridge Bay’s massive car park field, bikes are only £1.20, but it’s a choka bank holiday weekend so I hope the lad at the pay shed was on a percentage today. I asked him about tides which have been doing my under-stimulated brain in. ‘Err, there’s a board over there’ said laddy. At last, the Kimmeridge Question was solved, I thought, admiring the first apostrophe, but sighing at the second. It turned out the board lazily repeated UKHO Mupe Bay/Lulworth Cove timings, about 5 miles west. You’d think that would be adequate for an estimate, but not necessarily.
I’m still baffled by the tides on Purbeck’s eastern Jurassic Coast. The problem is getting reliable times for Kimmeridge Bay or Chapman’s Pool, the most useful put-ins hereabouts, and timings matter the longer you’re on the water. The UKHO posts times for Mupe Bay and also Lulworth Cove which is less than a mile away. The times are identical. And then there’s nothing until Swanage, about 12 miles to the east as the black-tipped tern flies and a doable day’s paddle in a long boat. Such gaps in UKHO stations are fairly normal along the UK coast, and you’d think just estimating Mupe Bay ± ~30 mins will give a time for Kimmeridge. But around here the tidosphere is all warped. Above, a few days before neap tide, it looks like Swanage rises in synch with Mupe and then ‘holds on’ to HW for hours, before dumping five hours ‘late’.
And then I found this Insta post (above) from Sharon Lee in Brighton who makes tide times posters. But not for Kimmeridge because, as she observes: ‘Notice an arc of weirdness around Dorset? That’s an amphidromic point. Which basically means the tides around Dorset (particularly the Isles of Purbeck and Portland) are utterly mad.’ Amphidromic (or a tidal node) was a new one on me, but may explain the Mupe-Swanage Incongruity (MSI), as tidal philosophers have called it since Pytheas skimmed pebbles with Posidonius. You’ll find many tide times websites supposedly offering times for non-UKHO locations, but many just list the nearest UKHO location with no real-world adjustment. As unless I am over-thinking it, Mupe Bay to Swanage needs quite a bit of Amphidromic adjustment.
And while I have your attention, what is the point of UKHO listing identical times for Lulworth Cove and Mupe Bay, just a mile apart? Is it because one is civilian-touristy and the other military most days of the year? So what? Yes, there are no less than four UKHO tidal locations in western Poole Harbour (+ Wareham) as closely bunched, but it’s a busy area that drains out to mud flats at low water and the timings are all different.
Mysterious tidal nodes appear all over the world. They are the Black Holes of the Oceans; go there and nothing happens. Spooky. Source

Then I saw in Kimmeridge’s Etches Fossil Museum shop a locally published tide tables booklet. ‘… West Dorset’ said the cover, but ‘Covers the coast from Swanage, Dorset through to Salcombe, East Devon‘ claimed the shop’s online blurb. The publisher’s website said as much (… the whole of the Dorset and South Devon coast…). Not in the copy I bought. The tables give every day of the published year, but only for Exmouth, Lyme and Portland. There’s nothing east of Portland in the booklet, unless you include a spot check on Portsmouth or Dover. No mention of Swanage, Lulworth or other local adjustments for Purbeck. You’d think I’d not be the first to notice this, I’d have saved my money for two more moto parkings were it not for chappy behind the shop counter advising: add an hour to Portland for BST, then 15-25 minutes for Kimmeridge. It’s Portland’s sticky out Bill that puts a spanner in Purbeck’s tidal flow, he explained. The formula was not Mupe Bay ± 30 minutes, as I’d guesstimated, but Portland + 15-25. I coughed up my £2.50 as an offering for this handy tip – I’ll appreciate it and the booklet when AI implodes the internet.
But hold your paddles, there’s more! Also on the Etches website I found a link to Willy Weather with a page for Kimmeridge Bay that wasn’t just a paste from Mupe Bay, but believably adjusted times. I compared KB times many months in the future using the Portland booklet formula and Willy, and found them to be within 3-13 minutes of each other. Assuming both are broadly correct, that will do me. Willy don’t list Chapman’s Pool but do have adjacent Egmont Point which seems to be KB + 2 minutes.
I’d heard of Willy Weather, but it wasn’t in my tidal bookmarks. It is now.
Still reading? At the jetty by the Wild Seas Centre a pair of well prepared sea anglers were setting out in their double outrigger SoTs. Talking of gear, this is a proper sea paddle so I’m in my proper Kokatat Leviathan pfd, but it feels like wearing a folded tractor inner tube full of ice cream. Leviathan – it’s in the name. At least I won’t be too gear-shamed when the RNLI fish me out by my ear and shake me dry.
I head out of the Bay and turn east. Oh MG, breaking offshore waves already! But I needn’t have worried today. There were a few more later on, but nothing the TXL+ couldn’t ride out. I actually think tackling this stage with a rising tide flooding the Ledges is the way to do it (in either direction), as any waves will diminish as the ledges submerge – won’t they? It’s more down to the wind of which there was little today, but as you paddle along you still want to glance offshore once in a while in case you’ve gotten on the inside of a building wave which can pop up out anytime, any place, any where. This is why I stayed quite far out. Not normally what I like to do alone in a packraft.
The Ledges from above.
And on a windy day west of Kimmeridge. Frothier than a Costa cappuccino with sprinkle.
The waters are clear and green. At many points I could have hopped out and waded along.
In fact, I did for a bit.
It took me back to Shark Bay, 2011. Jeff and Sharon and me in my Gumotex Sunny wading north to a unearth a cache near Peron Point after battling a stiff headwind all morning. What a great paddle adventure that was. Easily doable in a packraft too, with added dolphins, dugongs, rays and yes, sharks.
I’m on the look out for ‘Iron Skeg Beach’ I found with the Igla IK a couple of years back. Above looks similar but is not it. In the Igla I turned back at ISB to Kimmeridge as paddling on to Chapman’s would’ve meant paddling back. First time out here and with a head full of Ledge Lore, I didn’t want to get caught out as tides and winds turned, and hauling the 17-kilo boat back along the coast path would have been too much. As I was about to find out.
There is the rusty triangular ‘skeg’ (also below) sticking up. This is actually called Clavell’s Hard and studying Ian West’s page for this area, I think the object (below) may have been something to do with oil shale mining right here in the 1890. There’s a semi-naked castaway looking for treasure. I hope he knows how to get back.
The strange cast iron object that looked like a ship’s skeg – from the SS Treveal, wrecked at nearby Egmont Point in 1920? It’s more likely a piece mining gear, a winch stand perhaps.
The soft, shaly grey cliffs, rich with ancient marine remnants.
Four colourful kayakers close to shore, like I should be. There’s more to see there.
I pass what could be Punta Pliosaurus.
Two days later we came back for a closer look.

I see sailboat masts ahead behind big rocks and am a bit disorientated. Chapman’s is tucked in on the left somewhere? I check the GPS and am nearly there, getting ashore 80 minutes out of KB or 4.5kph average with a bit of dawdling, and quite a lot at 6kph, according to the Garmin. People want to know this stuff!.
Along with some moored yachts and beach bathers is a trio of menacing jetskiers playing their satanic music. But this is Purbeck so it’s not blaring, and at least they weren’t tearing up the Pool like houns en tout.
At Chapman’s there are ammonite fossils everywhere you step.
Even getting off the beach by the waterfall is a loose scramble, especially backpacking a holdall. As I leave, I hear the jets gun off to Kimmeridge or Swanage. I presume that’s what they did as you can’t get a trailer down here. With a packraft you can go anywhere you can walk.
Up the steep, overgrown gully and across the parched field for the 500-foot climb up to Houns-tout hill – all in less than a mile from the shore. My pulse hits the rev limiter. What does Houns-tout even mean?
Kimmeridge 3 miles. In these shoes? No way, Jose.
Tranquil Chapman’s and St Alban’s Head from Houns-tout summit. And actually my Teva Omniums are not the problem; it’s the wobbly, 8-kilo holdall hanging from my shoulders. But on the way back I have a brilliant idea. More here.
The steep decent from Le Tout gave the underworked knees what for. I could do with my packstaff. I sold the 4-part Vertex paddle which it fitted. I need to convert my Anfibio Wave 4P but it’ll require some whittling.
Then back home I dug out an old, 55/170cm telescopic monopod (£18 on amazon Basics). It’s more gear (370g) and may slip under pressure, but zero bodging required and will work for long-arm selfies.
I witness a landslide near Punta Plio. This country is falling apart! I should get down there houns tout suite and see what fossil treasures came down with the rubble. ‘Get me Professor Etches, I found the tail. That pliosaur is longer than you think!’
In places the path is very narrow: barbed wire right to spike my raft, big drop left to spike everything else. The first half from Chapmans is tricky in places. Don’t be part of the next landslide.
The SW Coast Path is cracking up. Must be the drought. Come the next deluge it could all come apart and slide into the sea, a few feet to the left.
All around as parched as southern Spain.
At one point a cheerful passing walker observes
Ooh, paddles. What’s in the bag?’
A boat‘, I reply.
Oooh, luvlay juvlay!’ she says
At last, the rotund edifice of Clavell Tower just as the battery warning light starts flashing and the legs wobble. I hobble down the steps like Steptoe with a hangover, passing pouting Instagramers capitalising on the golden hour.
I’m a sweaty, achey mess but it’s been a lovely summer evening’s walk up and down 340 metres along a tiny part of the South West Coast Path. They say the total elevation gain on the entire 630-mile trail from Minehead to Poole is a staggering 115,000 feet (over 35,000 meters). That’s like climbing Everest from sea level four times. And yet hundreds manage it every year, signing off with thighs like telegraph poles. They’ll see many amazing things, like Kimmeridge Bay an hour before spring HW: not a foot of a beach to spare.
The ride home via a refreshing ford cools me off.
There you have it: KB to Chapman’s. A lot easier to paddle than to walk.
That’s another stage of Weymouth to Poole ticked off, leaving the trickiest 8 miles for last. First, Chapman’s east around St Alban’s Head 4 miles to Dancing Ledge. Then about the same distance from there to Swanage, around Durlston Head, another tidal pinch point and with no take-outs. In a sea kayak you’d swan through in one go, slicing through whatever the tides bring. But you can’t pop it in your pack and bus home. Alone in the TXL I’d pick the neapest of neaps and lightest of winds – and still break it into two manageable stages. Summer is coming to and end. Maybe soon or maybe next year.