Jabal al-Lawz () is a

mountain A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher t ...

located in northwest

Saudi Arabia Saudi Arabia, officially the Kingdom of Saudi Arabia (KSA), is a country in West Asia. Located in the centre of the Middle East, it covers the bulk of the Arabian Peninsula and has a land area of about , making it the List of Asian countries ...

, near the

Jordan Jordan, officially the Hashemite Kingdom of Jordan, is a country in the Southern Levant region of West Asia. Jordan is bordered by Syria to the north, Iraq to the east, Saudi Arabia to the south, and Israel and the occupied Palestinian ter ...

ian border, above the

Gulf of Aqaba The Gulf of Aqaba () or Gulf of Eilat () is a large gulf at the northern tip of the Red Sea, east of the Sinai Peninsula and west of the Arabian Peninsula. Its coastline is divided among four countries: Egypt, Israel, Jordan, and Saudi Arabia. ...

at above sea level. The name means 'mountain of

almond The almond (''Prunus amygdalus'', Synonym (taxonomy)#Botany, syn. ''Prunus dulcis'') is a species of tree from the genus ''Prunus''. Along with the peach, it is classified in the subgenus ''Amygdalus'', distinguished from the other subgenera ...

s'. The peak of Jabal al-Lawz, consists of a light-colored, calc-alkaline

granite Granite ( ) is a coarse-grained (phanerite, phaneritic) intrusive rock, intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly coo ...

that is intruded by

rhyolite Rhyolite ( ) is the most silica-rich of volcanic rocks. It is generally glassy or fine-grained (aphanitic) in texture (geology), texture, but may be porphyritic, containing larger mineral crystals (phenocrysts) in an otherwise fine-grained matri ...

and

andesite Andesite () is a volcanic rock of intermediate composition. In a general sense, it is the intermediate type between silica-poor basalt and silica-rich rhyolite. It is fine-grained (aphanitic) to porphyritic in texture, and is composed predomina ...

dikes Dyke or dike may refer to: General uses * Dyke (slang), a slang word meaning "lesbian" * Dike (geology), formations of magma or sediment that cut through and across the layering of adjacent rocks * Dike (mythology), ''Dikē'', the Greek goddess ...

which generally trend eastward. Between 1300 and 2200 meters elevation, Jabal al-Lawz has relict Mediterranean woodlands of ''

Juniperus phoenicea ''Juniperus phoenicea'', the Phoenicean juniper or Arâr, is a juniper found throughout the Mediterranean region. Description ''Juniperus phoenicea'' is a large evergreen shrub or small tree reaching tall, with a trunk up to in diameter and ...

'', with an understory of ''Achillea santolinoides, Artemisia sieberi'', and ''Astracantha echinus'' subsp. ''arabica''. In discussions about the location of

biblical Mount Sinai Mount Sinai (, ''Har Sīnay'') is the mountain at which the Ten Commandments were given to the Prophets in Judaism, Hebrew prophet Moses by God in Judaism, God, according to the Book of Exodus in the Hebrew Bible/Old Testament. In the Book of ...

, Jabal Maqlā ('Burnt Mountain') is often believed to be ''Jabal al-Lawz'' by various authors such as

Bob Cornuke Bob Cornuke (born 1951) is an American writer and president of the Bible Archaeology Search and Exploration Institute (BASE), which is operated from his home in Colorado Springs, Colorado. He describes himself as a Biblical archaeologist, but has n ...

, Ron Wyatt, and Lennart Möller as shown by local and regional maps and noted by other investigators. In contrast to the real Jabal al-Lawz, the summit of Jabal Maqlā consists mainly of dark-colored

hornfel Hornfels is the group name for a set of contact metamorphic rocks that have been baked and hardened by the heat of intrusive igneous masses and have been rendered massive, hard, splintery, and in some cases exceedingly tough and durable. These p ...

s derived from

metamorphosed Metamorphic rocks arise from the transformation of existing rock to new types of rock in a process called metamorphism. The original rock (protolith) is subjected to temperatures greater than and, often, elevated pressure of or more, causi ...

volcanic rock Volcanic rocks (often shortened to volcanics in scientific contexts) are rocks formed from lava erupted from a volcano. Like all rock types, the concept of volcanic rock is artificial, and in nature volcanic rocks grade into hypabyssal and me ...

s that originally were

silicic Silicic is an adjective to describe magma or igneous rock rich in silica. The amount of silica that constitutes a silicic rock is usually defined as at least 63 percent. Granite and rhyolite are the most common silicic rocks. Silicic is the g ...

and

mafic A mafic mineral or rock is a silicate mineral or igneous rock rich in magnesium and iron. Most mafic minerals are dark in color, and common rock-forming mafic minerals include olivine, pyroxene, amphibole, and biotite. Common mafic rocks include ...

lava flows Lava is molten or partially molten rock (magma) that has been expelled from the interior of a terrestrial planet (such as Earth) or a moon onto its surface. Lava may be erupted at a volcano or through a fracture in the crust, on land or unde ...

tuff Tuff is a type of rock made of volcanic ash ejected from a vent during a volcanic eruption. Following ejection and deposition, the ash is lithified into a solid rock. Rock that contains greater than 75% ash is considered tuff, while rock co ...

breccia Breccia ( , ; ) is a rock composed of large angular broken fragments of minerals or Rock (geology), rocks cementation (geology), cemented together by a fine-grained matrix (geology), matrix. The word has its origins in the Italian language ...

s, and fragmental greenstones. The middle and lower slopes of Jabal Maqlā consist of light-colored granite, which has

intruded Intrusive rock is formed when magma penetrates existing rock, crystallizes, and solidifies underground to form ''intrusions'', such as batholiths, dikes, sills, laccoliths, and volcanic necks.Intrusive RocksIntrusive rocks accessdate: March 27 ...

into the overlying hornfels. This is the same granite that comprises Jabal al-Lawz. Jabal Maqla is about 7 kilometers to the south, and a few hundred meters lower. Claims made by some writers, including Bob Cornuke, Ron Wyatt, and Lennart Möller, that Jabal Maqlā, possibly identified as ''Jabal al-Lawz'', is the real

have been rejected by such scholars as James Karl Hoffmeier (Professor of Old Testament and Ancient Near Eastern History and Archaeology), who details what he calls Cornuke's "monumental blunders". Remains both of pillars and cairns at the site have been described as "similar to rock cairns of uncertain use and often uncertain date found at other sites throughout northern and western Arabia."

References

External links

* {{Mountains in the Arabian Peninsula Lawz Midian Two-thousanders of Asia

See also

References

External links