Nymphaeum (Olympia)

Lion-head spout from Olympia

The ancients had many methods of obtaining water from a source, all either pump-up or gravity flow. The simplest pump-up was a woman filling and carrying a water vessel to the location of use. If the source was not a surface one they dug for it, as at Mycenae, where a tunnel led down to a spring. Potential energy is added in pump-up, not necessarily by humans, but also by animals and mechanical devices.

In gravity flow the water loses potential energy. The water must always be kept moving downhill. Rain capture is one such system, in which rain falling on a roof or terrace drains into a gutter and exits the latter from a spout. So many lion's head spouts were found at Olympia that all the larger buildings must have had them. The method is not effective, however, if it does not rain. A second method is spring capture, in which a spring empties into a collection basin and is piped or channeled from there, such as Delphi had. There was, however, no Mount Parnassus at Olympia.

Current, open reconstruction of the "home of the nymphs," the distribution point of the aqueduct to Olympia

None of these methods being effective for municipal water, the Romans became adept at stream capture. Military camps were sited at locations where a stream would run through the camp, usually halfway up a hill. Larger settlements tapped streams from elevated terrain many miles away. The Romans built chutes, or aqueducts, that descended at a low gradient, crossing valleys on bridges and going through hills in tunnels. The key engineering principle was that the downward slope must be kept over the entire length. At the terminus was an elaborate distribution structure, called in the 2nd century a nymphaeum, "home of the nymphs," or water goddesses.

It is in the building of these systems that Herodes Atticus had become in essence a civil engineer with expertise in water supply. It was the duty of wealthy men to manage projects such as these, as it had been under the Republic, at their own expense, or assisted by empire funds, although they could levy taxes to cover it (not a popular method).[note 3] Prominent men who refused the duty found themselves in public odium, or worse, imperial odium.

The Nymphaeum at Olympia was excavated 1877–1878[5] and the results were published in 1892.[6] The initial excavators believed they had found a spring capture, which they called "the exedra" (ex-hedra for *ex-sedra, "sitting room") in the sense of "spring house." The name stuck for decades. They saw it as a kind of grotto carved into the hill from which a spring was presumed to have flowed.[note 4]

Some troubling questions remained. If that much water was flowing from the hill, why was it not still flowing? Moreover, there were no seats, and the site was too elevated for easy access. Soon they discovered a large cistern at the back of the main wall fed by a brick tunnel going eastward through the base of the hill along the "treasury terrace" and then turning into the hill.[note 5][7] The tunnel is mounted atop a buttressed wall for stability and elevation control. Whether it was visible in ancient times is unknown. The visible length is 88 m (96 yd),[8] elevation at cistern 50 m (160 ft), elevation at hill entrance 55 m (180 ft). The 20-foot difference gave plenty of momentum to the flow, which must have come jetting impressively out the spouts of the Nymphaeum.[note 6]

The hill above the wall has since been sacrificed to the road, which passes through a cut. A "cave" opening is visible at the top of the cut, about 70 m (230 ft).[note 7] The cut has removed any subterranean phases of the aqueduct leading into the hill. At the time of the cut it is not certain the excavators knew the aqueduct came out of the hill.[note 8] A French map of 1878 and a Russian map of 1885 show the aqueduct on the terrace but no road. Dörpfeld's map of 1887 shows it with worksheds along it (long since gone). The date of the road is therefore most likely 1886 (given accurate maps).

• 
  Russian map of Olympia, 1885
• 
  After Dörpfeld's map of 1887
• 
  The aqueduct shown behind the Treasury of Cyrene, shored up by a metal framework

Adler believed the source was the upper Kladeos "in the southwestern spur of Erymanthus Mountain."[9] The terrain map shows Erymanthos as a massif in the vicinity of Pothos (37.70253°N 21.68732°E / 37.70253; 21.68732 and Lalas (37.71020°N 21.72002°E / 37.71020; 21.72002), with a long ridge extending to the SW, of which Kronion is the very last hill. The Kladeos begins in the vicinity of the village of Kladeos to the north of the spur; however, it is far too northward to be Adler's 1 km from Olympia.

The 1 km only gets you upriver as far as the north of the village of Archaia Olympia. Adler apparently based the number on elevation. The 50 m elevation of the river at that point matches the 50 m elevation of the top of the Nymphaeum. As an established archaeologist would have been familiar with both the hydrology and terrain maps, an explanation might be sought in the original date of his comment, which was perhaps before discovery and excavation of the remaining aqueduct. The high end of the aqueduct at about 55 m is matched by the elevation of the river at Koskinas 2 km north of Olympia. If the water did come from a tunnel through the hill, the terrain on the other side is at about 60 m, but the cave in the road cut is about 70 m. An aqueduct of 74 m on the north side of the spur would have to reach the sources of the Kladeos in Erymanthos, near Mageiras at 3.5 km from Olympia.

There are, however, good reasons for thinking the engineers did not run the aqueduct to the north of the spur. If the existing sources from the middle Kladeos were not adequate, then the different branches of the upper Kladeos, each containing less water, would not be either. Since the climate is about the same as it was and the geology has not changed much, the ancient water was probably most copious where the modern water is, in the higher mountains to the east, the sources of the municipal water supplies there.

The surviving aqueduct enters from the east, not the west, placing it on the southeastern face of the ridge. The only other remnant was a projection above the surface on a hilltop in the village of Miraka, now in downtown Pisa, reported about the time of the excavation of Olympia. The projection was presumably removed during urban renewal. The elevation is about 108 m (354 ft), but only ephemeral streams are in the vicinity, not much good for permanent water sources. The population used them for discharge of waste water, which descended to the Alpheios.[10]^: 254

The average precipitation in Greece today is roughly 600 mm per year in the plains and 2000 mm or more per year in the mountains.[10]^: 252 The imbalance was probably not much different in classical times; i.e., the water was to be found in the mountains, which is where Herodes Atticus' engineers would have looked for it, in the "hills of Linaria and Muria."[11] However, urban Linaria is at 44 m (144 ft), 4.53 km (2.81 mi) from Olympia; Muria at 60 m (200 ft) 6.77 km (4.21 mi), so the flow was not from those places. Ephemeral rivers extend north to the required elevations, but being ephemeral they transported only waste water, not drinking water.

A little further to the east, at 15.14 km (9.41 mi) from Olympia and 115 m (377 ft) elevation, is the right-bank tributary of the Alfeios, the Erymanthos, descending copiously from the heights of Mount Erymanthos through rapids. The mountain stream descends as a pebble-bottom ditch choked with vegetation from springs and waterfalls of the upper col until it reaches Tripotama as a good-sized, fast-flowing shallow river. There it enters Erymanthos gorge. There are no tracks along its whitewater extent through there until it reaches Haratsariou gorge, where there is a road crossing over an iron bridge, the Nemouta bridge. Southward from there a difficult hiking trail crosses the mouths of two ravines conducting additional water through a cascading region known as Nemouta Falls, some 30 waterfalls draining a wider region, which enhance the flow below.[12]

The Erymanthos looking upstream from the bridge above the modern water treatment plant.

Further up the Alfeios is another tributary, the Ladon, of similar flow. A hydroelectric dam has been placed across it at 37.5861°N 21.795°E / 37.5861; 21.795, Ladon Lake. The lake is far to the north, but at lower elevations the Erymanthos rises faster than the Ladon by about 20 m, which excludes the Ladon from being the source of the aqueduct at Miraka. The Erymanthos, then, is the best logical choice for the source of the aqueduct according to the circumstantial evidence. Starting in 2013, a new water treatment plant on the Elis side of the middle Erymanthos river began delivering (via gravity-flow underground channels) a fixed rate of 0.6 cubic meters per second of drinking water on a fixed monthly schedule to all the communities downstream in the Alfeios system as far as Pyrgos; i.e., all north and central Elis. Hydroelectric and irrigational water is taken from different streams on an optimal allocation basis. Evidently, the value of the Erymanthos for municipal supplies has long been known and appreciated.

All the hydrologic circumstances together offer a credible view of Herodes Atticus' engineering plan and account for its success, although little of it can as yet be proved by regional archaeology. Before Herodes, Olympia depended on wells, rainfall, and the Olympia municipal water system; i.e., the Kladeos, for its water supplies, which became less adequate as the whole system was taxed by population growth and Roman internationalism. Herodes liberated Olympia from dependence on local water and brought in water from the Pisa municipal system, which was probably already tapping the Erymanthos, as there was plenty of water for all.