The ruins of Tiwanaku are made up of impressive architectural structures such as palaces, temples and pyramids, as well as giant monoliths and figurative representations. Though the site is still not fully excavated, what has been exposed shows a remarkable complex of buildings, which include: the Akapana (Akapana East, and Pumapunku stepped platforms); Puerta del Sol (The Gateway of the Sun); Puerta del Luna (The Gateway of the Moon); Kalasasaya, Kheri Kala, and Putuni enclosures; and a semi-subterranean Temple.
The adjacent Lake Titicaca is fed by rainfall and meltwater from glaciers on the sierras that abut the Altiplano. Five major river systems feed into Lake Titicaca. In order of their relative flow volumes these are Ramis, Coata, Ilave, Huancane, and Suchez. More than 20 other smaller streams empty into Titicaca, and the lake has 41 islands, some of which are densely populated.
Several rivers feed into Lake
Titicaca from snow melt and rainwater, but only one river flows out (to the
south) and to Lake Poopo and the Salar de Coipass, and Salar de Uyni salt flats
beyond
Since 2000 Lake Titicaca has experienced constantly receding water levels. Between April and November 2009 alone the water level has 32-inches and has now reached the lowest level since 1949. This drop is caused by shortened raining seasons and the melting of glaciers feeding the tributaries of the lake, the result of these drops over the centuries has been to leave salt flats where saltwater lake runoffs occurred
White area at bottom right of image
is the area of a once water-filled lake called Tauca, now the area known as
Salar de Coipasa (Salt of Coipasa) and Salar de Uyuni (Salt of Uyuni), where
the original ocean waters trapped as lakes when the mountains rose, evaporated,
leaving enormous salt deposits across the land
In addition, according to many upcoming geologists, the idea that mountains raised “recently,” is becoming more and more understood. Only ten years ago, Carmala Garzione, associate professor of Geology at the University of Rochester, and her associates John M. Eiler, professor of geochemistry at Cal Tech, and professor Prosenjit Ghosh, of the Institute of Science in Bangaluru, India, wrote in an article in Science, that while the Andes originally rose slowly over time, they recently “shot up suddenly.” Likewise, Gregory D. Hoke, Earth Sciences at Syracuse University and post-doctoral research fellow, corroborates the swift-rise theory and shows that not just the mountains, but a broad region more than 350 miles wide rose to some degree with the Andes. In research soon to be published in the journal Earth and Planetary Science Letters, Hoke describes his findings on how rivers carved deep canyons into the flanks of the Andes as the mountain range rose. By dating the incisions and mapping the depth and extent of the canyons, Hoke shows that the surface uplift that occurred in the sedimentary basin where Garzione took her measurements must have happened across the entire width of the Andes Mountain range.
It should also be noted with care that on the former surf line of the raised beaches at Valparaiso, Chile, now at 1,300 feet, the seashells are not even decayed—a clear indication of a “recent” up thrust of the mountain. Geologist Li Siguang, also known as J.S. Lee, (J for Zhongkui/Jung-kuei, S for Siguang), the founder of China’s geomechanics (Earth Mechanics: the study of the behavior of soil and rock), and Vice President of Chinese Academy of Sciences and minister of Geology, reports “At the same time convincing evidence was brought forth that the mountain ranges in western China have been elevated since the Glacial Age” (J.S. Lee, The Geology of China, Thomas Murby & Co., London, 1939, p 207).
The last ice age is claimed to have
ended around 11,000 years ago as the ice sheets cracked, calved, broke up, and melted, raising
the sea levels world-wide. While this is speculation, the ice sheets obviously
receded from off North America and Asia to their present locations
In Kashmir, the German Helmut de Terra, a geologist, explorer, archaeologist, anthropologist and author, who conducted a number of scientific expeditions into Asia and the Americas, was the first to produce a glaciological map of the Eastern Himalayas. He also found sea bottom deposits at an elevation of 5,000 feet or more and tilted, at an angle of 40º degrees. He showed where “these deposits contain so-called Paleolithic, meaning ‘Old Stone Age,’ fossils”—at 5000-feet elevation! (Arnold Heim and August Gousser, The Throne of the Gods, An Account of the First Swiss Expedition to the Himalayas, Macmillan Co., New York, 1939, p218). As Heim added, “The fact is that this change occurred in historical times, however fantastic changes so extensive may seem to a modern geologist.”
According to these scientists, who are obviously not advocates of the mainstream belief in changes, especially those of mountain range lift taking millions of years, “it can be demonstrated that the mountain chains of the Caucasus, China, Tibet, the Rockies, the Alps and the Andes all rose to their present heights in historical times.” In fact, there is the same “late” dating from all parts of the earth.”
Consider the Andes. At 11,500 feet, a curious whitish streak runs along the side of the mountain range for over 300 miles. It is composed of the calcified remains of marine plants. This shows that these slopes were once part of the seashore. In fact, many lakes up in the Andes region are completely salt. One such lake is Titicaca, where a watermark of salt along the lake shore now runs at an angle to the water level. Originally it would have had to have been horizontal. Clearly the land was not only thrust up to its present altitude, but was tilted in the process.
Not only is the water saline, but on the beach of this lake high in the mountains, there are seashells as well as traces of seaweed, which tells us that the lake at one time must have been a bay or inlet of the sea. Even today, various sea creatures (including sea horses) survive in the lake, and this lofty, almost sterile region is capable of sustaining only a scant population.
So how did the city exist at such a high elevation?
(See the next post, “Tiwanaku and Titicaca’s 4000-foot Leap – Part III,” for more on the lake that sits astride the Peruvian-Bolivian border and located just north of the ancient city of Tiwanaku)
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