While in Australia recently, I took my boys on a trip up the Maroochy River into the Maroochy wetlands. We had all enjoyed our canoe trip into the Noosa Everglades the previous year (https://mountainsrivers.com/2018/09/06/canoeing-in-the-noosa-everglades/) but this time we had a solar-powered canoe. The solar panel charges a battery that runs an electric outboard motor. It produces a reasonable speed and is very quiet. And we certainly appreciated the ease of gliding upriver without effort.
After walking from the White Horse across Uffington Castle perched on the hilltop (see previous post Iron Age hillforts), I walked for about a kilometre to join the Ridgeway track that leads across the Wessex Downs in southern England. I followed this west for about a mile to another Neolithic chambered long barrow known as Wayland’s Smithy. The Smithy is about 100 metres off the Ridgeway nestled in a grove of trees.
The ancient Ridgeway track
Some forest near the Ridgeway
The first version of the barrow was built between 3,590 and 3,555 BC. It was 20m long and the remains of 14 people were buried here in a stone and timber box over a period of less than 15 years. Between 3,460 and 3,400 BC a second larger barrow 56m in length with a stone chamber was constructed over it, and the chambers contained the jumbled remains of several people.
While in Wiltshire earlier this month, I stayed in the village of Avebury, which lies within the world’s largest megalithic stone circle, and is about a mile north of Silbury Hill (see previous post at Exploring-the-barrow-downs-of-wessex
Constructed over several hundred years during the Neolithic period from around 3,000 BC to 2,600 BC, a large henge (a bank and a ditch) with a large outer stone circle encircles part of Avebury village. Two separate smaller stone circles are located closer to the centre of the henge.
The ditch and mound surrounding the Avebury outer stone circle
The outer stone circle is 332 metres in diameter with a circumference just over 1,000 metres and encloses two smaller stone circles near its centre. The available evidence suggests that in the early Neolithic, Avebury and the surrounding hills were covered in dense oak woodland, and as the Neolithic progressed, the woodland around Avebury and the nearby monuments receded and was replaced by grassland.
After the day of reasonably heavy snow in Geneva last week, I decided to head up to Verbier to take advantage of the new snow. Verbier is a bit under two hours drive from Geneva and has spectacular scenery and skiing. In the first few years I was in Geneva, Verbier was my regular ski destination, and for a couple of years I rented a small studio apartment there so I could go up for weekends and longer periods when possible.
From Lausanne onwards, the ground in the Rhone Valley was completely covered in snow, and the trees and mountains were all dusted with fresh powder. I parked in the valley below Verbier and caught the cable car up past Verbier to the mid-level pistes.
Heading up in the cable car
Verbier is part of the “Four Valleys” (“4 Vallées”) ski area, which is the biggest ski domain in Switzerland with extensive off-piste and back country routes.
After a warm and sunny March, the snow has returned to Geneva. It started to snow in the evening and continued overnight. When I woke the world was transformed. I took my dog for a walk in the snow, she loves it. And I could not resist taking too many photos.
I have recently been cleaning up old external drives that I’ve used over the years for backups and found a folder of photographs from a 2003 ski trip to Champèry. Champéry lies in a side valley of the Rhone valley under the Dents du Midi (“Teeth of Midday”) mountain range. Some of the photos really capture the beauty of skiing in this region, which is part of the Portes du Soleil (The Doors of the Sun). So I decided to put them up in this post. The Portes du Soleil is one of Europe’s two largest ski areas, around 1000 square kilometres, with 13 interconnected ski resorts and around 650 km of marked pistes, and includes Les Gets where we skied in February this year.
Looking down towards Champéry lying under the Dents du Midi on the other side of the valley
Continuing to head upwards from where the above photo was taken will bring you to the ridgeline which marks the Swiss border with France. Later in the day I skied down the other side into France and ended up in the Morzine valley, where I caught a chairlift back up to the top.
Schools in Geneva have a one-week mid-term break in February, and the ski slopes are normally crowded. I took my boys for a week skiing in the French Alps at Les Gets, which is a little over 60 kilometres from Geneva, in the direction of Chamonix. The slopes were even more crowded as usual, as it was also the British mid-term break, and Les Gets is a popular destination.
Looking towards Mont Blanc from Mont Chéry.
The village of Les Gets, visible in the valley below my younger son in the photo above, is relatively low at 1,170m above sea level, and the highest points accessible on ski are at around 2000 m. The photo above was taken near the summit of Mont Chéry at around 1,800 m. In the distance to the south-east Mont Blanc (4,810 m) is visible on the horizon. I stood on its summit in 2010 (Mont Blanc), 3000 metres higher than where I and my son are now standing. Below is another photo taken using the zoom lens.