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Copiapoa in Habitat
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Copiapoathon 2006

16 November

Taltal:
Quebrada San Ramon

The Quebrada San Ramon is one of my favourite places on earth. Many visitors march straight to the point where arguably one of the nicest Copiapoa, C. krainziana, can be found. For those who take their time and observe the cacti that others have marched past, there is an amazing range of variability of plants that can only be described as forms of C. cinerea: white waxed or green bodied plants, depending on their location's exposure to the sun; white spined plants that seem to be half way between C. cinerea and C. krainziana, plants with white (C. cinerea ssp. cinerea) or yellow / orange (C. cinerea ssp. haseltoniana) wool in the apex, some plants apparently spineless forms, until they turn out to be stems growing on the same plant as normal spined stems, while some plants seem to have twice as many spines per areole as appears to be the norm; with the occasional crested plant that has been overlooked by past visitors. While most of these plants form clumps, starting on the terraces, some 2 m (6 ft) above the floor of the Quebrada, some are huge pendant specimens, fit for the largest hanging baskets you can think of, growing several hundred meters above us on the steep rock faces. None are found on the floor of the Quebrada, presumably because they were washed away whenever an occasional flash-flood rushes through here. If only the canyon walls could tell us the stories of what they had observed over the millions of years.

The visitor to San Ramon has to walk on a very uneven surface of debris left by historic flash-floods; rocks of all sorts of different sizes, some as big as a camper van, to fine gravel sand. In one or two places, these are piled up to form water falls during water-filled episodes. After walking some 7 km from the entrance, the visitor has climbed some 400 m (1200 ft) from the sea-level entrance overlooking the Ocean. This is where the various cinerea forms give way to C. krainziana and C. taltalensis (syn. C. rupestris). Other cacti seen include Eriosyce rodentiophila, although the number spotted becomes less with each visit, and Eriosyce taltalensis (syn. Neoporteria neohankianus), small and quite plentiful, and the only cactus that I found growing on the Quebrada floor, suggesting that they grow much faster than Copiapoa, having established themselves since the last flood. There are Eulychnia (E. taltalensis) decorating many of the north facing rocks faces. Since posting this report, I should point out that the lack of cacti on the Quebrada floor applies to the 6 km or so before reaching the point where the canyon opens up and becomes a stone quary, used to source material for the road building activities. Higher up, where C. krainziana starts to appear, plants of C. krainziana and C. taltalensis DO grow on the valley floor. This includes all sorts of krainziana forms, including the 'soft wispy snow-white spined plants' that are often regarded in the hobby as 'the true krainziana'. Thanks to Benjy for pointing out the need to clarify this point.

All in all, the Quebrada San Ramon provides the ideal location for a one day hike and the visitor will leave exhausted, but fulfilled by the sights that have been absorbed; water bottles are empty, digital camera storage cards are full and the batteries exhausted.

In 2003, at the start of the hike, Angie was so distracted by the plants she saw, just calling her to take their picture, that she ran out of steam half way along the Quebrada and never saw the C. krainziana. This time, she was determined to get to these plants, did not stop for distractions or chat with others, but marched along like a little panzer tank and was ever so pleased to reach her objective. With the pictures taken in 2003 and this time round, she has an enviable set of cactus images.

No, this is not an advert for a bar and ice cream parlour that I'm setting up at the end of the Quebrada, although it is a tempting thought....

Stops today: S566, S567, S568

Google Earth image, showing stops from 2001 (1), 2003 (3), 2004 (4) and 2006 (6)


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  © 2001-2006 Paul Klaassen
 
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