Walking on La Gomera and El Hierro. Paddy Dillon

42 Guinea and San Andrés

       Walk 43 Las Puntas and Guinea

       Walk 44 GR131: Orchilla to Fuente de La Llanía

       Walk 45 GR131: Fuente de la Llanía to Estaca/Tamaduste

       Appendix A Route summary table

       Appendix B Topographical glossary

       Appendix C Useful contacts

INTRODUCTION

      Several routes start or finish near the church in Valverde (Walk 28–31)

      A view of the rugged coastline after climbing high above Santa Catalina (Walk 25)

      The seven sub-tropical Canary Islands bask in sunny splendour off the Atlantic coast of north-west Africa. Millions of sun-starved north Europeans flock there for beach holidays, but increasingly visitors are discovering the amazing variety of landscapes throughout the archipelago. Conditions range from semi-deserts to perpetually moist laurisilva ‘cloud forests’, from rugged cliff coasts to high mountains, from fertile cultivation terraces to awesome rocky barrancos carved deep into multi-coloured layers of volcanic bedrock. Some areas are given the highest possible protection as national parks, but there are many more types of protected landscapes, rural parks, natural monuments and nature reserves.

      More and more walkers are finding their feet, exploring the Canary Islands using centuries-old mule tracks, rugged cliff paths and forest trails. Paths pick their way between cultivation terraces, squeeze between houses and make their way to rugged coves and hidden beaches. Some paths run from village to village, following old mule tracks once used to transport goods, while other paths are based on pilgrim trails to and from remote churches and ermitas. Many have been cleared, repaired, signposted and waymarked in recent years, ready to be explored and enjoyed.

      This guidebook explores the waymarked trail networks on the islands of La Gomera and El Hierro. Despite their small size, they boast routes of all types – from easy strolls to hands-on scrambling, from simple day-walks to long-distance trails. As these routes are fully signposted and waymarked, walkers can follow them with confidence and enjoy the islands to the full. Over 700km (435 miles) of trails are described in this guidebook.

Location

      The Canary Islands are more or less enclosed in a rectangular area from 13°30′’W to 18°00′’W and 27°30′’N to 29°30′’N. As a group, they stretch west to east over 450km (280 miles). Although administered by Spain, the mother country is 1100km (685 miles) away. The narrowest strait between the Canary Islands and Africa is a mere 110km (70 miles). The total land area is almost 7500km (2900 square miles), but the sea they occupy is ten times that size.

Geology

      Most of the world’s volcanic landscapes are formed where huge continental or oceanic ‘plates’ collide with each other. When continental plates collide, the Earth’s crust crumples upwards to form mountains, and when plates are torn apart, basaltic rock from deep within the Earth’s mantle erupts to form mountains. The Canary Islands, however, are different, and have a complicated geological history.

      The African landmass is the visible part of a continental plate that extends into the Atlantic Ocean, but the Canary Islands lie within the oceanic crust of the eastern Atlantic Ocean, close to the passive junction with the African continental plate. It is thought that the islands now lie directly above a hot-spot, or mantle plume, some 2500km (1550 miles) deep within the Earth. The mantle plume is fixed, but the oceanic and African plates are drifting very slowly eastwards. Every so often a split in the oceanic crust opens above the mantle plume, allowing molten rock to vent onto the ocean floor. As more and more material erupts, it piles higher and higher until it rises from the sea. Each of the Canary Islands was formed this way.

      Lanzarote and Fuerteventura were the first Canary Islands to form, and were subsequently pulled eastwards. The next time a rift opened over the mantle plume the islands of Gran Canaria and Tenerife were formed, and these were in turn pulled eastwards. A further oceanic rift led to the formation of La Gomera, La Palma and El Hierro. Looking forward in geological time more islands will appear as other rifts are torn open in the future.

      The forces at work deep within the Earth can scarcely be imagined. Every single piece of rock throughout the Canary Islands once existed in a molten state. Consider the energy needed to melt one small stone, and multiply that to imagine the energy required to melt everything in the island chain, as well as the immense amount of rock beneath the sea that supports them all!

      El Teide on Tenerife is often seen above the clouds from La Gomera and El Hierro

      Over time huge amounts of volcanic material were piled high, but erosion has led to great instability. During recent geological time vast chunks of the islands have collapsed into the sea, creating features such as El Golfo on El Hierro, the Caldeira de Taburiente on La Palma, and the Orotava valley on Tenerife. With each catastrophic collapse, tsunamis devastated places around the Atlantic Ocean. Geologists predict that similar collapses could occur in the future on the Cumbre Nueva on La Palma or the north face of El Teide on Tenerife.

Wildlife

      Plants and flowers

      While the northern hemisphere was in the grip of an Ice Age, the Canary Islands were sluiced by rainstorms, with powerful rivers carving deep, steep-sided barrancos into unstable layers of ash and lava. As the landmasses emerged from the Ice Age the Canary Islands dried out and the vegetation had to adapt to survive. Some species are well adapted to semi-desert conditions, while on the highest parts of the islands, laurisilva cloud forests are able to trap moisture from the mists and keep themselves well watered. Laurisilva forests once spread all the way round Mediterranean and tropical regions, and one of the best remnants now crowns La Gomera, where it is protected in a national park.

      Clockwise from top left: Prickly pear fruit; Canarian lavender; Canarian tagasaste tree

      Canary pines flourish on high, dry mountainsides, sometimes in places where nothing else grows. Almost every pine you see will have a scorched trunk, but they regenerate surprisingly well after forest fires. Beware of the long pine needles on the ground, as they are slippery underfoot. Canary palms also flourish in dry places, and in the past every part of the tree had a use; today they provide delicious miel de palma, or palm honey. Every so often dragon trees occur, the last surviving descendants of the ancient prehistoric forests. They have been decimated in the wild but prove popular in gardens.

      Tagasaste trees are often found in dense plantations, always in places where livestock are grazed. They grow with little water, yet have a high nutritional content and are regularly cut for animal fodder. In recent years they have been exported to Australia. Junipers (sabinas) are common; fruit and nut trees have been established, including apples, oranges, lemons, bananas, almonds, figs and vines. The introduced prickly pears are abundant, not so much for their fruit, but for raising cochineal beetles, whose blood provides a vivid red dye.

      Bushy scrub is rich and varied, including sticky-leaved