“It is thus that I look back upon our first walk at Chamouni,
to the Source of the Arveron” (MS VIII; Works [1903])—The Arveyron,
a glacial tributary that rises from the
Mer de Glace, which in the nineteenth century extended to the village of
Bois and was there called the
Glacier du Bois.
On
14 August 1833, the Ruskins set out from
Geneva for the valley of
Chamonix (
Chamouni, in their spelling), the final major excursion of their summer journey.
They arrived in the village on
15 August in rainy weather, prompting
Salvador to procure a loan of books, which included a set of
Voyages dans les Alpes by
Horace‐Bénédict de Saussure,
a copy of which
Ruskin would receive for his birthday in
1834 (
Burd, ed., Ruskin Family Letters, 278, 280 n. 1).
Shortly after arrival,
John and
John James ventured out on a walk to view the
source of the Arveyron,
while
Margaret and cousin
Mary stayed behind at the inn. Their courier,
Salvador,
also remained behind, so it is likely that
Ruskin and his father
were attended by the youths whom John mentions as competing to lead them to the riverʼs source.
Children also swarmed
Mary and
Margaret when they set out (likewise without
Salvador, apparently) to catch up with
John and
John James.
The ladies walked alongside the
Arve until they reached a village, where they were told the view lay another quarter‐hourʼs walk ahead, so they decided to turn back,
“to the great regret of our little man” who was guiding them “and a number of children who continually kept saying that it was a fine sight well worth seeing,
using many times the terms ‘superbe, magnifique’ &c &c”. Returned to the inn,
Mary and
Margaret were soon reunited with
John and
John James,
who returned “much pleased with the sight”
(
Diary of Mary Richardson, 1833, 128–30).
According to
John Murray III (
1808–92), in his
1838 guidebook to
Switzerland,
the excursion to the source of the
Arveyron was “a delightful walk of an hour, along the plain of the valley,
crossing beautiful meadows, and a little forest.” The so‐called source is an “affluent of the
Arve” that “issues from below the vault of ice with which the
Glacier du Bois,
the
Mer de Glace terminates. . . . The vault of ice varies greatly in different seasons, and the author, at different times, has remarked a change
of from 30 to 100 feet of height in the arch. It may be entered, but this is dangerous, and some have suffered for their temerity. . . . The danger is, that blocks
of ice may detach themselves from the vault. . . . The scenery around the source is very grand, the deep blackness of the depth of vault, the bright and beautiful azure
where the light is transmitted through the ice. The enormous rocks brought down by the glacier from the mountains above, here tumble over,
and are deposited in the bed of the
Arve. Here, too, the dark forest, and the broken trunks of pines, add to the wild character of the scene”.
Through this forest, a steeper and more difficult path also descended to the riverʼs glacier source, leading “active and strong” visitors who had set out first for the
Montanvert
to visit the riverʼs source before they returned to
Chamonix village
(
Hand‐book for Travellers in Switzerland, 297).