There are few sights on Earth’s landscapes as awe-inspiring as a volcano – energetic or dormant.

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And a brand new ebook underscores this, providing ‘a visible celebration of probably the most spectacular, notorious and energetic volcanoes from all corners of the globe’.

Volcano, by Robert J Ford (www.amberbooks.co.uk), takes the reader on an eye-opening photographic tour from Hawaii to Chile and from Portugal to New Zealand, taking in phenomena that, as Ford says in his introduction, are reminders of Earth’s uncooked energy.

He writes: ‘We people have felt for hundreds of years that we have now mastery over our world – remodeling it to go well with our wants and methods of life. But our planet from time to time sends reminders that we’re however residents upon its again.

‘Volcanoes are probably the most highly effective of those, which people snuggled up towards over time as we broaden our constructed surroundings into each nook of the pure world.’

Scroll all the way down to see MailOnline Journey’s decide of the photographs within the mesmerising tome… 

PUYEHUE-CORDON CAULLE, RANCO PROVINCE, CHILE: A stunning photograph of one of this century's most colossal eruptions. Ford writes: 'Puyehue-Cordon Caulle in the Southern Volcanic Zone is a complex of two volcanoes: Puyehue and the fissure system of Cordon Caulle. After 51 years of inactivity, in 2011–12, it exploded in what became the biggest eruption of the 21st century so far. An estimated 100million tons of ash, sand and pumice were ejected, some of which circled the globe, reaching other parts of South America, South Africa, Papua New Guinea, Australia and New Zealand'

PUYEHUE-CORDON CAULLE, RANCO PROVINCE, CHILE: A shocking {photograph} of one among this century’s most colossal eruptions. Ford writes: ‘Puyehue-Cordon Caulle within the Southern Volcanic Zone is a fancy of two volcanoes: Puyehue and the fissure system of Cordon Caulle. After 51 years of inactivity, in 2011–12, it exploded in what grew to become the most important eruption of the twenty first century thus far. An estimated 100million tons of ash, sand and pumice had been ejected, a few of which circled the globe, reaching different elements of South America, South Africa, Papua New Guinea, Australia and New Zealand’

LAGOA DE SANTIAGO, SETE CITADES, SAO MIGUEL ISLAND, AZORES, PORTUGAL: 'The Lagoa de Santiago fills one of the cones that arose in the caldera of the Sete Citades Massif, an ancient stratovolcanic complex at the western end of Sao Miguel Island,' writes Ford. 'The caldera is dominated by the twin lake of Lagoa das Sete Citades (seen in the background), which is said to have been created by the tears of two young lovers forbidden to see each other by the king'

LAGOA DE SANTIAGO, SETE CITADES, SAO MIGUEL ISLAND, AZORES, PORTUGAL: ‘The Lagoa de Santiago fills one of many cones that arose within the caldera of the Sete Citades Massif, an historic stratovolcanic advanced on the western finish of Sao Miguel Island,’ writes Ford. ‘The caldera is dominated by the dual lake of Lagoa das Sete Citades (seen within the background), which is alleged to have been created by the tears of two younger lovers forbidden to see one another by the king’

MOUNT ST HELENS, WASHINGTON, USA: 'The landslide that preceded and triggered the blast of pyroclastic material in the 1980 eruption,' writes Ford, 'was caused by the collapse of the entire north face of the mountain after an earthquake and carried with it debris that covered an area of 62 square km (24 sq miles) with many metres of rubble. It was the largest landslide in recorded history and left a clear view into the volcano's crater for the first time'

MOUNT ST HELENS, WASHINGTON, USA: ‘The landslide that preceded and triggered the blast of pyroclastic materials within the 1980 eruption,’ writes Ford, ‘was attributable to the collapse of your complete north face of the mountain after an earthquake and carried with it particles that lined an space of 62 sq. km (24 sq miles) with many metres of rubble. It was the biggest landslide in recorded historical past and left a transparent view into the volcano’s crater for the primary time’

OL DOINYO LENGAI, TANZANIA: 'Ol Doinyo Lengai varies between eruptions of liquid lava that form lava lakes and fountains (known as effusive eruptions) and explosive eruptions that create large cinder and ash cones,' writes Ford. 'An episode of the latter type in 2007 spewed ash thousands of metres into the air, which also fell on the surrounding countryside, forcing local residents to flee with their livestock. Explosive eruptions continued into 2008, building a cone over 100m (330ft) high that encircled a steep-sided crater'

OL DOINYO LENGAI, TANZANIA: ‘Ol Doinyo Lengai varies between eruptions of liquid lava that kind lava lakes and fountains (often called effusive eruptions) and explosive eruptions that create massive cinder and ash cones,’ writes Ford. ‘An episode of the latter sort in 2007 spewed ash 1000’s of metres into the air, which additionally fell on the encompassing countryside, forcing native residents to flee with their livestock. Explosive eruptions continued into 2008, constructing a cone over 100m (330ft) excessive that encircled a steep-sided crater’

MOUNT VESUVIUS, CAMPANIA, ITALY: This volcano poses a deadly threat to millions. Ford writes: 'Mount Vesuvius, part of the Campanian Volcanic Arc, dominates the Bay of Naples and the population centres lying within its reach. It is these nearby settlements that make Vesuvius one of the most dangerous volcanoes in the world, with three million people in Naples near enough to be threatened by an eruption and the mountain being the only mainland European volcano to have erupted in the past 100 years (1944 being the last incident)'

MOUNT VESUVIUS, CAMPANIA, ITALY: This volcano poses a lethal menace to tens of millions. Ford writes: ‘Mount Vesuvius, a part of the Campanian Volcanic Arc, dominates the Bay of Naples and the inhabitants centres mendacity inside its attain. It’s these close by settlements that make Vesuvius probably the most harmful volcanoes on the earth, with three million individuals in Naples close to sufficient to be threatened by an eruption and the mountain being the one mainland European volcano to have erupted previously 100 years (1944 being the final incident)’

DEVILS TOWER, WYOMING, USA: It's a volcanic tower that's out of this world, having made an appearance in Steven Spielberg’s Close Encounters of the Third Kind. Ford reveals that this 264m (867ft) geological feature is considered sacred by Northern Plains Indians and is thought to have been formed 'by an intrusion of magma into surrounding sedimentary rock' and 'would only have become a visible landmark when all the sedimentary material eroded away'. Ford adds: 'Some believe, however, that Devils Tower is all that remains of what was once a huge explosive volcano'

DEVILS TOWER, WYOMING, USA: It is a volcanic tower that is out of this world, having made an look in Steven Spielberg’s Shut Encounters of the Third Variety. Ford reveals that this 264m (867ft) geological characteristic is taken into account sacred by Northern Plains Indians and is believed to have been shaped ‘by an intrusion of magma into surrounding sedimentary rock’ and ‘would solely have turn into a visual landmark when all of the sedimentary materials eroded away’. Ford provides: ‘Some imagine, nevertheless, that Devils Tower is all that is still of what was as soon as an enormous explosive volcano’

BARDARBUNGA VOLCANIC SYSTEM, VATNAJOKULL NATIONAL PARK, ICELAND: ‘Baroarbunga is a stratovolcano located under the Vatnajokull ice cap (known as a subglacial volcano), Iceland’s biggest,' explains Ford. 'During the 2014–15 eruption, the emptying of Baroarbunga's magma chamber saw a subsidence of its caldera by around 65m (213ft), which also caused a sinking of the surface of the glacier under which the volcano sits'

BARDARBUNGA VOLCANIC SYSTEM, VATNAJOKULL NATIONAL PARK, ICELAND: ‘Baroarbunga is a stratovolcano positioned beneath the Vatnajokull ice cap (often called a subglacial volcano), Iceland’s greatest,’ explains Ford. ‘Throughout the 2014–15 eruption, the emptying of Baroarbunga’s magma chamber noticed a subsidence of its caldera by round 65m (213ft), which additionally triggered a sinking of the floor of the glacier beneath which the volcano sits’

COTOPAXI, COTOPAXI PROVINCE, ECUADOR: 'Cotopaxi’s biggest known eruptions were in 1742, 1744, 1768 and 1877,' reveals Ford. 'The latter three events destroyed Latacunga town on each occasion. During the 1877 eruption, pyroclastic flows on all sides of the mountain melted the entire ice cap to cause lahars [mudflows] that travelled more than 100km (62 miles) to the Pacific Ocean. Modern eruptions threaten flash-melts of the new glacier and lahars that pose a great risk to the land and population nearby'

COTOPAXI, COTOPAXI PROVINCE, ECUADOR: ‘Cotopaxi’s greatest recognized eruptions had been in 1742, 1744, 1768 and 1877,’ reveals Ford. ‘The latter three occasions destroyed Latacunga city on every event. Throughout the 1877 eruption, pyroclastic flows on all sides of the mountain melted your complete ice cap to trigger lahars [mudflows] that travelled greater than 100km (62 miles) to the Pacific Ocean. Fashionable eruptions threaten flash-melts of the brand new glacier and lahars that pose an awesome threat to the land and inhabitants close by’

TEIDE, TENERIFE, CANARY ISLANDS, SPAIN: The summit of Teide is the highest point in Spain and the islands of the Atlantic at 3,718m (12,198ft). It rises out of the caldera of another giant volcano that helped birth Tenerife, reveals Ford. He continues: ‘The island was created through the accretions of three large shield volcanoes that formed their own small landmasses. Between these another volcano, Las Canadas, formed, joining all four together in a small island, which then grew over the millennia. Las Canadas later collapsed to create the caldera, out of which Teide grew over the course of the last 160,000 years’

TEIDE, TENERIFE, CANARY ISLANDS, SPAIN: The summit of Teide is the best level in Spain and the islands of the Atlantic at 3,718m (12,198ft). It rises out of the caldera of one other large volcano that helped delivery Tenerife, reveals Ford. He continues: ‘The island was created by the accretions of three massive defend volcanoes that shaped their very own small landmasses. Between these one other volcano, Las Canadas, shaped, becoming a member of all 4 collectively in a small island, which then grew over the millennia. Las Canadas later collapsed to create the caldera, out of which Teide grew over the course of the final 160,000 years’

ZENDAN-E SOLEYMAN, WEST AZERBAIJAN PROVINCE, IRAN: 'The hollow cone of Zendan-e Soleyman is a 107m- (351ft) tall ancient extinct volcano formed of mostly calcium sediments,' writes Ford, 'with the remains of various temple buildings surrounding the peak. Its crater, 65m (213ft) wide and 85m (279ft) deep, was filled with water centuries ago but has long since dried up. The mountain takes its name – "the Prison of Solomon" – from the biblical king Solomon, after a local legend that tells how the Hebrew king imprisoned monsters within the mountain’s deep cone'

ZENDAN-E SOLEYMAN, WEST AZERBAIJAN PROVINCE, IRAN: ‘The hole cone of Zendan-e Soleyman is a 107m- (351ft) tall historic extinct volcano shaped of largely calcium sediments,’ writes Ford, ‘with the stays of varied temple buildings surrounding the height. Its crater, 65m (213ft) large and 85m (279ft) deep, was stuffed with water centuries in the past however has lengthy since dried up. The mountain takes its identify – “the Jail of Solomon” – from the biblical king Solomon, after an area legend that tells how the Hebrew king imprisoned monsters inside the mountain’s deep cone’

MAZZARO, SICILY, ITALY: This stunning picture shows a smoking Mount Etna looming over the ruins of Teatro Antico di Taormina, an ancient Greek theatre. Ford adds: ‘The mountain consists of two volcanoes: a shield volcano that began erupting here about 500,000 years ago sits under a 35,000-year-old stratovolcano. Etna experiences a variety of eruption styles, including violent Strombolian explosions and frequent lava flows’

MAZZARO, SICILY, ITALY: This beautiful image exhibits a smoking Mount Etna looming over the ruins of Teatro Antico di Taormina, an historic Greek theatre. Ford provides: ‘The mountain consists of two volcanoes: a defend volcano that started erupting right here about 500,000 years in the past sits beneath a 35,000-year-old stratovolcano. Etna experiences a wide range of eruption kinds, together with violent Strombolian explosions and frequent lava flows’

PITON DE LA FOURNAISE, RÉUNION ISLAND, INDIAN OCEAN: This shield volcano on Reunion Island, a French departement, is one of the most active volcanoes in the world, reveals Ford. He continues: 'Its name translates as "peak of the furnace", an indicator of how often it erupts, the most recent instance being in October 2019. Despite this, it is a popular tourist site, with visitors able to access the peak. A shield volcano is one with a low, broad profile with shallowly sloping sides that has been built up over time by repeated emissions of relatively fluid lava (usually basaltic). Shield volcanoes are characterized by their low explosivity and lack of pyroclastic material'

PITON DE LA FOURNAISE, RÉUNION ISLAND, INDIAN OCEAN: This defend volcano on Reunion Island, a French departement, is likely one of the most energetic volcanoes on the earth, reveals Ford. He continues: ‘Its identify interprets as “peak of the furnace”, an indicator of how usually it erupts, the latest occasion being in October 2019. Regardless of this, it’s a common vacationer web site, with guests capable of entry the height. A defend volcano is one with a low, broad profile with shallowly sloping sides that has been constructed up over time by repeated emissions of comparatively fluid lava (normally basaltic). Protect volcanoes are characterised by their low explosivity and lack of pyroclastic materials’

MOUNT DAMAVAND, IRAN: At 18,405ft (5,610m), Damavand is Asia's highest volcano. It first erupted almost 1.78million years ago, reveals Ford. He continues: 'After a number of eruptions around 600,000 and 280,000 years ago, which helped create its steep cone of ash and lava flows, Damavand’s last one was around 5300 BC. The volcano is topped by a small crater and there are adjacent fumaroles, hot springs and mineral deposits, which imply Damavand could be considered as a potentially active volcano'

MOUNT DAMAVAND, IRAN: At 18,405ft (5,610m), Damavand is Asia’s highest volcano. It first erupted nearly 1.78million years in the past, reveals Ford. He continues: ‘After plenty of eruptions round 600,000 and 280,000 years in the past, which helped create its steep cone of ash and lava flows, Damavand’s final one was round 5300 BC. The volcano is topped by a small crater and there are adjoining fumaroles, sizzling springs and mineral deposits, which indicate Damavand might be thought-about as a doubtlessly energetic volcano’

MISTI, AREQUIPA, PERU: 'The long history of eruptions from Misti and its neighbour volcanoes, Chachani and Pichu Pichu, has made the soil extremely fertile and the surrounding area one of the most agriculturally productive in Peru,' says Ford. 'Residents of Arequipa have also made use of a local white volcanic rock called sillar to construct a significant number of buildings there, which has resulted in Arequipa being nicknamed "the white city"'

MISTI, AREQUIPA, PERU: ‘The lengthy historical past of eruptions from Misti and its neighbour volcanoes, Chachani and Pichu Pichu, has made the soil extraordinarily fertile and the encompassing space probably the most agriculturally productive in Peru,’ says Ford. ‘Residents of Arequipa have additionally made use of an area white volcanic rock known as sillar to assemble a big variety of buildings there, which has resulted in Arequipa being nicknamed “the white metropolis”‘

MOUNT RINJANI, LOMBOK, INDONESIA: At 3,726m (12,224ft), this is the second-highest volcano in Indonesia. Ford reveals: 'Its caldera was formed by the 1257 eruption of Samalas in one of the largest volcanic events since the end of the last ice age 11,500 years ago, and which may have triggered a period of global cooling and failed harvests. Rinjani’s caldera is filled by Segara Anak lake, which itself saw the emergence of a cone now known as Gunung Baru Jari in 1994 and 1995 eruptions, the lava from subsequent eruptions of which has filled a part of the lake'

MOUNT RINJANI, LOMBOK, INDONESIA: At 3,726m (12,224ft), that is the second-highest volcano in Indonesia. Ford reveals: ‘Its caldera was shaped by the 1257 eruption of Samalas in one of many largest volcanic occasions because the finish of the final ice age 11,500 years in the past, and which can have triggered a interval of world cooling and failed harvests. Rinjani’s caldera is crammed by Segara Anak lake, which itself noticed the emergence of a cone now often called Gunung Baru Jari in 1994 and 1995 eruptions, the lava from subsequent eruptions of which has crammed part of the lake’

ANAK KRAKATOA, KRAKATOA ARCHIPELAGO, SUNDA STRAIT, INDONESIA: Ford writes: 'The third of the four major explosions of the 1883 Krakatoa eruption was heard as far as 4,780km (2,970 miles) away, with its pressure wave travelling around the Earth a number of times. This was said to have burst the eardrums of sailors 64km (40 miles) away. Bodies were washing up on the shores of East Africa up to a year later’

ANAK KRAKATOA, KRAKATOA ARCHIPELAGO, SUNDA STRAIT, INDONESIA: Ford writes: ‘The third of the 4 main explosions of the 1883 Krakatoa eruption was heard so far as 4,780km (2,970 miles) away, with its strain wave travelling across the Earth plenty of instances. This was stated to have burst the eardrums of sailors 64km (40 miles) away. Our bodies had been washing up on the shores of East Africa as much as a yr later’

DIAMOND HEAD, OAHU, HAWAIIAN ISLANDS, USA: This breathtaking picture shows Diamond Head, ‘a volcanic tuff or ash cone, a volcano born when magma boils water to steam to cause an explosion of ash, rock and volcanic bombs’. Ford continues: ‘The resulting pyroclastic material and eruption column fallout build the cone. Diamond Head is part of a stage of volcanism on the island that has created numerous cones and vents and is about 400,000–500,000 years old’

DIAMOND HEAD, OAHU, HAWAIIAN ISLANDS, USA: This breathtaking image exhibits Diamond Head, ‘a volcanic tuff or ash cone, a volcano born when magma boils water to steam to trigger an explosion of ash, rock and volcanic bombs’. Ford continues: ‘The ensuing pyroclastic materials and eruption column fallout construct the cone. Diamond Head is a part of a stage of volcanism on the island that has created quite a few cones and vents and is about 400,000–500,000 years previous’

FUEGO, ANTIGUA, GUATEMALA: 'Typically, eruptions of Fuego were of a Vulcanian nature (small yet violent explosions with dense clouds of ash-laden gas and rock, with both pyroclastic and thick magma flows) and lasted a few hours to several days,' explains Ford. 'From 2002, Fuego began a period of almost constant activity that saw bursts of ash and lava, which culminated in an unexpected eruption in 2018 that buried several villages and killed nearly 200 people'

FUEGO, ANTIGUA, GUATEMALA: ‘Sometimes, eruptions of Fuego had been of a Vulcanian nature (small but violent explosions with dense clouds of ash-laden gasoline and rock, with each pyroclastic and thick magma flows) and lasted a number of hours to a number of days,’ explains Ford. ‘From 2002, Fuego started a interval of virtually fixed exercise that noticed bursts of ash and lava, which culminated in an surprising eruption in 2018 that buried a number of villages and killed almost 200 individuals’

MOUNT RUAPEHU, TONGARIRO NATIONAL PARK, NORTH ISLAND, NEW ZEALAND: 'A series of very explosive Plinian eruptions occurred at Ruapehu between about 22,600 and 10,000 years ago,' says Ford. 'Since then, only one vent has probably been active, at Crater Lake in the summit region. Major eruptions in historic times seem to occur every 50 years, with the lake filling with warm, acidic water in between'

MOUNT RUAPEHU, TONGARIRO NATIONAL PARK, NORTH ISLAND, NEW ZEALAND: ‘A sequence of very explosive Plinian eruptions occurred at Ruapehu between about 22,600 and 10,000 years in the past,’ says Ford. ‘Since then, just one vent has most likely been energetic, at Crater Lake within the summit area. Main eruptions in historic instances appear to happen each 50 years, with the lake filling with heat, acidic water in between’

MOUNT ARARAT, TURKEY: 'Mount Ararat, near the Turkey–Armenia border, consists of two volcanoes,' explains Ford, 'Great Ararat and Little Ararat. Great Ararat is the highest peak in Turkey with an elevation of 5,137m (16,854ft). Ararat is a complex or compound volcano, one that has changed either its eruptive habit or location of the main vent area. The mountain is considered by some to be the resting place of Noah’s Ark'

MOUNT ARARAT, TURKEY: ‘Mount Ararat, close to the Turkey–Armenia border, consists of two volcanoes,’ explains Ford, ‘Nice Ararat and Little Ararat. Nice Ararat is the best peak in Turkey with an elevation of 5,137m (16,854ft). Ararat is a fancy or compound volcano, one which has modified both its eruptive behavior or location of the principle vent space. The mountain is taken into account by some to be the resting place of Noah’s Ark’

All images taken from the book Volcano by Robert J Ford (ISBN 978-1-83886-063-9) published by Amber Books Ltd (www.amberbooks.co.uk) and available from bookshops and online booksellers (RRP £19.99/$24.95)

All photos taken from the ebook Volcano by Robert J Ford (ISBN 978-1-83886-063-9) revealed by Amber Books Ltd (www.amberbooks.co.uk) and obtainable from bookshops and on-line booksellers (RRP £19.99/$24.95)



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