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Vesuvius and
Volcanic Ruins

79 AD

 

Vesuvius

 

The volcano Vesuvius sits behind the coastal town of Naples in South-Western Italy. The height of the cone in 1980 was 4,198 ft (1,280 m), but it varies considerably after each major eruption. At about 2,000 ft a semicircular ridge, called Mt. Somma, begins, following the cone on the north rising to nearly 4,000 ft. Between Mt. Somma and the cone itself is the Valle del Gigante (Giant's Valley). At the summit of the cone is a large crater, about 1,000 ft deep and 2,000 ft across, formed in the eruption of 1944.

Roman-Tour: [photo] Vinyards and Vesuvius

Mt. Vesuvius
1975

Roman-Tour: [photo] Vesuvius Eruption in 1944

Lava Flow
from Vesuvius

1944

 

After several centuries of quiescence, a series of earthquakes, lasting for six months and gradually increasing in violence, preceded a major eruption of Vesuvius that took place on December 16, 1631. From 1631 to 1944 many cycles of volcanic activity were observed. Severe eruptions, occurred in: 1631, 1660, 1682, 1694, 1698, 1707, 1737, 1760, 1767, 1779, 1794, 1822, 1834, 1839, 1850, 1855, 1861, 1868, 1872, 1906, and 1944. Eruptive stages varied in length from 6 months to 31 years. The periods between eruptions have varied from 18 months to 8 years. Vesuvius has been quiet now for half a century -- which can either be good or bad depending on how you look at it. More than two million people live in the area of Vesuvius and on its lower slopes. There are industrial towns along the coast of the Bay of Naples and small agricultural centres on the northern slopes of the volcano.

But Vesuvius is still an active volcano, it is just resting. Recently, French and Italian researchers discovered a massive layer of magma eight kilometres (five miles) below Mount Vesuvius, it stretches across 400 square kilometres (154 square miles). Research is now going on to discover how thick the magma pool is. When this magma breaks through to the surface again, it may cause massive destruction in the Naples area.

Spartacus and Vesuvius

SPARTACUS
about 109 - 71 BC
Thracian Gladiator

Spartacus was born in Thrace, became a soldier, and was captured by the Romans. He was sold as a slave to be made a gladiator. With 70 comrades, he escaped and raised a large army of rebel slaves. They hid on Mount Vesuvius.

In 73 BC, Spartacus and his army of slaves was besieged by the praetor Publius Claudius Pulcher on the summit of Vesuvius, which was then a wide, flat depression walled by rugged rocks festooned with wild vines. He and his men escaped by twisting ropes of vine branches and descending through unguarded fissures in the crater rim. Then they attacked and scattered Pulcher's army by attacking them from behind.

The Roman Senate sent another two legions to crush Spartacus. Facing two legions of Roman forces, Spartacus and his second-in-command, Crixus, divided their force to attack the Romans. Crixus was defeated and killed by one of the Roman legions. However, Spartacus managed to smash both legions with the force under his command. Following this victory Spartacus now had under his command 120,000 slaves. In another battle with the Roman legions at Picenum, Spartacus was again triumphant.

Spartacus intended to lead the slaves over the Alps and out of Italy, but the slaves forced him to march on Rome. The Senate sent out six legions, plus the previous two, all under the command of Licinius Crassus. This hugh army finally defeated Spartacus and his men. The Romans crucified six thousand slaves along the Appian Way as a warning to other slaves. It is unknown what happened in the end to Spartacus.

 

The Eruption of Vesuvius in 79 AD


Vesuvius entered the history of volcanology with the eruption of 79 AD, described by Pliny the Younger. The eruption destroyed Pompeii, Herculaneum, Oplonti and Stabiae and caused the death of Pliny the Elder among many other people. The prosperous residents of Pompeii, a provincial Roman city of 20,000 probably saw Vesuvius as just another beautiful mountain and their rich volcanic soil as a gift from the gods. Life was good, and it would go on just as it had for a millennium.

PRECURSERS

An earthquake occurred on 63 AD February 5. The earthquake created major damage to Pompeii and Herculaneum, and caused minor damage in Nuceria and Naples, where the emperor Nero was performing in the theatre. According to Seneca, the earthquakes lasted several days until they became milder. This earthquake swarm probably occurred at a shallow depth in the Vesuvian area, given the distribution and extent of the damage.

Seventeen years later, a new wave of heavy earthquakes occurred. Most people ignored them because earthquakes were so common in Campania. But this time, they were the forerunners of the Vesuvius eruption of 79 AD.

 

THE ERUPTION OF 79 AD

Pliny the Younger's letters to Tacitus and recent volcanic studies provide a background and description of the Vesuvian eruption.

The time the eruption began is uncertain: the two Plinys directly observed the cloud at about 1 PM 24 August 79 AD from a distance of 21 km across the Bay of Naples from Pompeii. The eruption probably began sometime earlier since at about the same hour a messenger sent from Pompeii arrived.

Pliny the Younger said that the volcanic plume resembled a Mediterranean Pine Tree more than anything else. Like a tree, the cloud ascended in a column and at intervals expanded in different branches. It was at one moment white, at another dark and spotted, as if it had carried up earth or cinders.

During the time of the eruption, Pliny the Younger stayed in the proximity of Misenum from where he observed the eruption along with his mother. Her brother, Pliny the Elder, took a boat to go and help save friends across the bay. He died in the attempt.

Between 2-3 PM Pliny the Elder sails to get a better view of the disaster and to rescue a friend whose villa is at the foot of Vesuvius. Unable to land he goes to Stabiae.

Pumice and dust is falling at a rate of 20 centimetres (8 inches) an hour. Most residents survive the downpour because the material is too light to kill them.

6 PM Pliny the Elder arrives at the house of his friend, Pliny the Elder goes to sleep while the downpour of ash and soot continues.

The pumice is now coarser, indicating an increase in the intensity and violence of the eruption. Magma is flowing 10 times more rapidly than before - at 10 million kilograms (22 million lb) a second. This is known as the 'Plinian stage', after the chronicler of the disaster. The cloud column now rises to 32km (20 miles) - six times higher than airliners fly. There are continuous lightning strikes in the cloud

8-9 PM Upon waking after his nap. 'They consulted together as to whether they should hold out in the house, or wander about in the open. For the house now tottered under repeated and violent concussions, and seemed to rock to and fro as if torn from its foundations. In the open air, on the other hand, they dreaded the falling pumice-stones, light and porous though they were; yet this, by comparison, seemed the lesser danger of the two; a conclusion which my uncle arrived at by balancing reasons, and the others by balancing fears. They tied pillows upon their heads with napkins; and this was their whole defence against the showers that fell round them...'

9 PM The rest of the world was still light but at Stabiae there a deeper darkness prevailed than in the most obscure night... They thought it practical to go down to the shore to observe Vesuvius from close at hand if they could possibly put out to sea, but they found the waves still ran extremely high and contrary. There Pliny the Elder, having thrown himself down upon a disused sail, repeatedly called for and drank cold water.

1 AM Twelve hours after the eruption began, the night view of the volcano showed a spectacular display of lightning amid the volcanic cloud spewing from the crater. At times, the dense cloud of ash, smoke, and stone towered 12 miles high. Strong winds aloft blew the material southeast toward Pompeii and nearby Stabiae.

Up until now, the heavy column laden with dust, ash and rock had been supported by the sheer force pushing out of the volcano. But, at about midnight that force momentarily weakened. The superheated cloud collapsed upon itself and started to roll down the side of the mountain.

The leading edge of this pyroclastic flow was a fast-moving stream of hot ash and gases, hurtling downward at terrific speed. The second part was denser, consisting of pumice, rocks and soil, made liquid by temperatures that approached 750 degrees. The glowing cloud failed to reach Pompeii on the first try, but it easily engulfed Herculaneum. Everyone remaining in the town died.

Note: A pyroclastic flow is defined as: A ground-hugging avalanche of hot ash, pumice, rock fragments, and volcanic gas that rushes down the side of a volcano as fast as 100 km/hour (60 miles/hr) or more.

Pliny the Younger and his mother have stayed in Misenum, across the Bay of Naples. 'That night the earthquakes became so violent that one might think that the world was not being merely shaken but turned topsy-turvy. My mother flew to my chamber and they moved outside and sat in the forecourt of the house.

Another town at the foot of the volcano and even closer to the crater, Herculaneum, had been spared a heavy fall of ash because it was upwind. The residents thought they were safe. They weren’t.

2 AM A second pyroclastic flow surged down the mountain. Again, it failed to reach Pompeii. But the steady rain of rocks and ash were getting to be more of a hazard than those at ground level were prepared to bear. Remaining residents, who were still huddled in their houses, gathered what belongings they could collect and started out of the city. Yet, some remained.

In the proximity of the volcano these phenomena caused severe damage and deaths. However, most people living in the area had escaped during the day before, in the first phase of the eruption, before the high eruption column had deposited about 4 meters of pumice lapilli around and in Pompeii during the early morning hours of the 25th. Pompeii was mostly inhabited by animals like horses, which were unable to walk in the thick cover of lapilli, or watch dogs, which were left to guard houses. So only a few people died because of the ash fall.

6 AM. During the night of the first day of the eruption, and for most of the morning of the next day, the houses of Misenum where shaken by earthquakes that caused much panic. Pliny the Younger and his mother left town and climbed the "Monte di Procida" hill. On the top of the hill, wheeled-charts on flat land were shaken back and forth even if chocks were placed against the wheels. Seismic activity even that far away was magnitude 5.

At dawn on the 25th from their vantage point they saw the sea retreating. This retreat of the sea is probably related to a tsunami which came with the climax of the eruption.

A cloud reached the "Monte di Procida" hill, across the bay, where Pliny the Younger and his mother were. A dense haze followed us like a stream flowing on land and night fell on us, not like a night with clouds or without stars, but like the night in a closed place without a lamp.

Third surge cloud. This is much larger than the last. It runs out of energy just as it reaches the northern walls of Pompeii. The air in the city becomes increasingly hard to breathe, and the ground shakes with increasingly fierce earthquakes. Some try to flee but are faced with 2.4m (8ft) of hot ash and pumice.

7:30 AM Fourth surge cloud. The remaining inhabitants of Pompeii - 1,044 bodies have been found within the city walls - are killed within two minutes by the ash-and-dust-filled wind that sweeps over them at over 300km (185 miles) an hour with a temperature of at least 100°C (212° F).

8:30 AM Pliny the Elder remains on the shore with his companions. '· Flames, and a strong smell of sulphur, which was the forerunner of them, dispersed the rest of the company to flight; Pliny the elder they aroused. He raised himself up with the assistance of two of his slaves, but instantly fell; some unusually gross vapour, as I conjecture, having obstructed his breathing and blocked his windpipe.

Fifth surge cloud. This sweeps down through Herculaneum and Pompeii and into the countryside, cutting down many who had thought they had escaped. Possibly as many as 10,000 Pompeii residents - half the city's population - die. Then the cloud - looking like a black tidal wave - hit the headland of Misenum, just as it ran out of energy.

Again, Pliny the Younger and his mother were subjected to another cloud. Again they experienced the obscurity, and again the ash was dense and heavy. It took them some time to shake away the ash as we could have been covered and choked by its weight.

Pompeii had joined Herculaneum, 12 miles away, in death. Two further surges that evening sealed the cities in an earthen tomb.

Pompeii was buried under nine feet of ash, and a deep, hard layer left by the surges. Herculaneum, much closer to the mouth of the volcano, was buried to a depth of 65 feet or more, in a deposit as tough as concrete.

 

The 160 acres of Pompeii, was now buried deep in the earth. It slept that way until the town was rediscovered, excavated, and studied, nearly 2,000 years later. Herculaneum was a much more difficult dig to recover. However much of what we know about Roman life in the first century comes from the excavation of these cities.

Roman Villas and Wall Painting

Because of the eruption of Vesuvius in 79 AD we know far more than about Roman life at the end of the first century than for any other ancient culture.

Pompeii

Birth of Dionysos

 

Roman Pompeii: [fresco]  King Pentheus Torn Apart by Sex Crazed Maenads

King Pentheus Torn Apart
by Sex Crazed Maenads

Roman Pompeii: [fresco]  Pasipae and Daedulus with the Artificial Cow

Pasipae and Daedulus
with the Artificial Cow

 

Roman Pompeii: [fresco]  Priapus

The God Priapus
about 40 AD

Four Frescos from the Villa Vettii
about 50 AD
Pompeii, Italy

Roman Pompeii: [fresco] Perseus Frees Andromeda

Andromeda rescued
by Perseus

about 70 AD

Rome Pompeii: [fresco] couple drinking

Fresco within
an Outdoor Shrine

about 50 AD

Roman Pompeii: [fresco] Dionystic Mystery Frieze

Roman Pompeii: [fresco]  Dionystic Mystery Frieze -- detail 1

 

Roman Pompeii: [fresco] Dionystic Mystery Frieze -- detail 2

 

A Fresco and Two Detail Pictures
from the House of the Dionystic Mysteries
about 50 AD
Pompeii, Italy

Roman Pompeii: [fresco] Ipythalic Mercury

Ithythalic Mercury
from the Entry way
to a Home

Roman Pompeii: [photo] Courtyard of the Villa Venus Marinus

from the Villa
Venus Marinus

Roman Pompeii: [fresco] Venus Marinus Fresco

Detail of the Picture
at the Back of the Garden

Roman Pompeii: [fresco]  Sexual Locker Markers for the Suburban Baths

Locker Markers
in the Suburban Baths

Roman Pompeii: [fresco]  Sexual Locker Markers for the Suburban Baths - detail 1

First Locker Marker
[detail]

Roman Pompeii: [fresco]  Sexual Fresco from a Bordello - detail 1

Bordello Fresco

Six Brothel Frescos

 

Herculaneum

Because few human remains were found during early excavations, it was assumed that, unlike the people of Pompeii, most of the inhabitants succeeded in escaping toward Naples, in the direction opposite to the fall of lapilli and ashes. In the 1980s, however, excavations at the ancient shoreline of the Bay of Naples (an area that is now inland) uncovered more than 120 human skeletons, suggesting that numerous additional inhabitants had also perished while attempting to escape.


The particular circumstances of the burial of Herculaneum, unlike those of Pompeii, led to the formation over the city of a compact mass of tufaceous material about 50 to 60 feet (15 to 18 metres) deep. Although this layer made excavation very difficult, it preserved Herculaneum and prevented tampering and looting. The special conditions of ground humidity made possible the conservation of wooden frameworks of houses, wooden furniture, the hull of a sizable boat, pieces of cloth, and food (carbonized loaves of bread left within ovens). Thus, Herculaneum offers a detailed impression of private life that is only with difficulty achieved in other centres of the ancient world. Excavation began in the 18th century, when all memory of the existence of Herculaneum had been lost for centuries and the only available reports of it were those that had come down through the authors of antiquity, without any information as to the exact position of the ancient city. Quite by accident, in 1709, during the digging of a well, a wall was discovered that was later found to be a part of the stage of the Herculaneum theatre. Tunnels were soon dug at the site by treasure hunters, and many of the theatre area's artifacts were removed. Regular excavations were started in 1738 under the patronage of the king of Naples, and from 1750 to 1764 the military engineer Karl Weber served as director of excavations. Under Weber, diagrams and plans of the ruins were produced, and numerous artifacts were uncovered and documented. Magnificent paintings and a group of portrait statues were excavated from a building thought to be the ancient basilica of Herculaneum, and a large number of bronze and marble works of art were recovered from a suburban villa, called the Villa of the Papyri because of its having contributed a whole library of ancient papyri in Greek. These papyri, on philosophical subjects of Epicurean inspiration, are preserved in the National Library of Naples.

The excavations were resumed in 1823 with the intention of discontinuing the previous tunneling and instead working from above ground, a method used with success at Pompeii; up to 1835 the work proved to be of value, bringing to light the first houses of Herculaneum, among which was the peristyle of the House of Argus. Abandoned and again resumed in 1869, after the unification of Italy, the excavations continued until 1875, when, because of the poor results obtained and the presence of the inhabited dwellings of Resina (now Ercolano), they were once more abandoned.

After the efforts of the English archaeologist Charles Waldstein to internationalize the excavations at Herculaneum (1904) by collecting contributions for this purpose from various nations in Europe and America, the work was finally resumed in May 1927 with Italian state funds and with the object of conducting the excavations with the same continuity as those of Pompeii. The results of this work, interrupted only by World War II, made it possible to have a clear picture of the ancient city. The larger decumanus (“main road”) forms one side of the quarter of the ancient forum with its public buildings. The insulae (“blocks”) to the south of the decumanus are laid out in a strictly geometric pattern facing the cardines (“crossroads”). Many of the nobler houses afforded their patrons a view of the bay. Inside the residential quarter, houses of rich republican and patrician construction alternate with houses of the middle class (such as the Trellis House), also finely decorated, or with commercial houses and workshops.


The public monuments uncovered include the palaestra (sports ground), with a large portico surrounding a vast central piscina (swimming pool), and thermae (baths), one of which adjoins the former beachfront. This bath is in a remarkable state of preservation, having remained largely protected against the pyroclastic flows of the eruption.

Excavation continues, since the demolition of part of Ercolano, at the forum of the ancient city and at the ancient coastline.

 

 

Roman Herculaneum: [photo] Main Street Decumanus Maximus

Decumanus Maximus

Roman Herculaneum: [photo]  Shop Interior

Shop Interior along the Decumanus Maximus

Roman Herculaneum: [photo]  Woman's Changing Room in  the Baths

Woman's Changing Room in the Baths

Roman Herculaneum: [photo]  Cult Statue of the Hydra in the Gymnasium

Cult Statue of the Hydra in the Gymnasium

Roman Herculaneum: [photo]  Courtyard of the Villa  of Nepture and Amphitrite

Courtyard Villa of Nepture and Amphitrite

Roman Herculaneum: [fresco]  Nepture and Amphitrite - Villa  of Nepture and Amphitrite

Mosaic Wall Decoration
Villa of Nepture and Amphitrite

 

 

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2005-10-16