Search results
Results from the WOW.Com Content Network
Upper Mesa Falls is a waterfall on the Henrys Fork in the Caribou-Targhee National Forest. Upstream from Lower Mesa Falls, it is roughly 16 miles (26 km) away from Ashton, Idaho. [2] Upper Mesa Falls is roughly 114 feet (35 m) high and 200 feet (61 m) wide. [3]
The Center received the first prize for innovative use of technology, in the Stockholm Challenge in 2004, for its work called The Archeological Map of Egypt. [4] All archaeological sites within Sharqia Governorate areas are accurately defined on small scale maps, providing a detailed and precise database.
In Ancient Egypt, the Bronze Age begins in the Protodynastic period, c. 3150 BCE. The archaic Early Bronze Age of Egypt, known as the Early Dynastic Period of Egypt, [35] [36] immediately follows the unification of Lower and Upper Egypt, c. 3100 BCE. It is generally taken to include the First and Second Dynasties, lasting from the Protodynastic ...
To the south was Upper Egypt, stretching to Aswan. The terminology "Upper" and "Lower" derives from the flow of the Nile from the highlands of East Africa northwards to the Mediterranean Sea. The two kingdoms of Upper and Lower Egypt were united c. 3000 BC, but each maintained its own regalia: the hedjet or White Crown for Upper Egypt and the ...
Lower Mesa Falls is a 65-foot (20 m) waterfall on the Henrys Fork in Fremont County, Idaho. It is located in the Caribou-Targhee National Forest on the Mesa Falls Scenic Byway . [ 2 ] It is downstream of Upper Mesa Falls .
The modern, arid Sahara. The Sahara was not a desert during the African humid period. Instead, most of northern Africa was covered by grass, trees, and lakes. The African humid period (AHP; also known by other names) was a climate period in Africa during the late Pleistocene and Holocene geologic epochs, when northern Africa was wetter than today.
The Sahara is the world's largest hot desert. [18] [19] It is located in the horse latitudes under the subtropical ridge, a significant belt of semi-permanent subtropical warm-core high pressure where the air from the upper troposphere usually descends, warming and drying the lower troposphere and preventing cloud formation.
In ancient Egypt, Upper Egypt was known as tꜣ šmꜣw, [3] literally "the Land of Reeds" or "the Sedgeland", named for the sedges that grow there. [4]In Arabic, the region is called Sa'id or Sahid, from صعيد meaning "uplands", from the root صعد meaning to go up, ascend, or rise.