Thread
Keeping in tone with my Giza posts of today, some of the great work done for the book:
Secrets of the Pyramid of Khufu
by Stefan Bergdoll, 2022
Again, these are large images that tolerate great deal of zoom in. The last ones will have written data of interest.
Thread:
Some amazing drawings of Giza, do use right click and open in new tab or copy them into your machine. they are enormous and very detailed by John Shae Perring, 1813-1869
Map of the pyramids of Ghizeh and vicinity Part 1
Map of the pyramids of Ghizeh and vicinity. Part 2.
Great Pyramid. Vertical and horizontal sections. Fig. 1. Vertical section from south to north through passages and chambers ; Fig. 2. Plan and horizontal section through A-B.
Although most think it a settled matter, the dimensions of the Great Pyramid are still, and will continue to be, a matter of debate because of the absence of defined corners. Here are some of the most mentioned measures:
Memphis is located south of the Nile Delta, on the west bank of the river, and about 15m/24km south of modern Cairo. Closely associated with the ancient city’s site are the cemeteries, or necropolises, of Memphis, where the famous pyramids of Egypt are located.
According to a commonly accepted tradition, Memphis was founded about 2925 BCE by Menes, who supposedly united the two prehistoric kingdoms of Upper and Lower Egypt
The original name was The White Walls, and the term may have referred originally to the king’s palace, which would have been built of whitewashed brick. The modern name of Memphis is a Greek version of the Egyptian Men-nefer
This cave is located at 38º 28' 61" N 8º 59' 73" W down the mountains and dense vegetation (Vale do Solitário - covered forest), in towards Portinho da Arrábida. More specifically on the southern slope of the Arrábida mountain massif, at the base of a small cliff.
Discovered by chance, between 1856/1857, by a shepherd and friends, who were carrying out their daily routines, of grazing the cattle. From a speleological point of view, it is a deep cavity, resulting from the intense karst (bellow) activity of the area surrounding the cave
It consists of limestone rock from the Jurassic - J²p. Developing at an altitude of 210m/689ft, along a bedding joint. It presents a semi-vertical progression in the west-east direction, with a gap of -21m/69ft. Its area of about 174sqm/1873sqft.