Overview

Yarīm is a town located in the Ibb Governorate in the southern highlands of Yemen. Perched at approximately 2,850 meters above sea level, it is one of the highest permanently inhabited settlements in the Arabian Peninsula. Yarīm lies close to the ruins of Ẓafār, the ancient capital of the Ḥimyarite Kingdom, and thus occupies a significant position in both modern geography and pre-Islamic South Arabian history. Today, Yarīm functions as an important administrative, agricultural, and cultural hub in central Yemen, while also serving as the gateway to some of the most archaeologically rich regions in the country. ¹

Geography and Climate

Yarīm lies on the western Yemeni escarpment, about 150 km south of Ṣanʿāʾ, situated along the Sanaʿa–Taʿizz road, a principal route in Yemen’s highland transport network. The town is surrounded by volcanic mountains and rolling terraced hills, part of a larger volcanic field that includes Jabal Iryān and Jabal Ḥadūr. Its high-altitude subtropical climate features cool temperatures year-round, with moderate to heavy seasonal rainfall, particularly during the summer monsoon months. These conditions have historically allowed the development of rainfed agriculture and terrace farming. ²

Historical Significance

Although Yarīm itself is not attested in ancient inscriptions as a major center, its proximity to Ẓafār (just 10–15 km to the south) makes it a key location in the historical geography of the Ḥimyarite Kingdom. During the 3rd–6th centuries CE, this region served as the political and religious core of the Ḥimyarite monarchy, which united much of southern Arabia under its control. Following the decline of Ẓafār after the Aksumite invasions in the early 6th century CE, the area around Yarīm remained inhabited and agriculturally active, though no longer the seat of central power. ³

Archaeological Context

Modern-day Yarīm serves as the base of operations for archaeological exploration of Ẓafār. Excavations by scholars such as Paul Yule have revealed temples, inscriptions, palatial ruins, and administrative buildings in the area, confirming the strategic and symbolic role of the region in antiquity. In Yarīm, surveys found pre-Islamic ceramics and materials, though no major ancient core, underscoring its value through continuous settlement and proximity to older sites. ⁴

Cultural Significance

Yarīm, part of the Qaḥṭānī tribal region, traces its heritage to ancient Sabaean and Himyarite peoples. Its oral traditions and customs reflect pre-Islamic and early Islamic influences, while local pride in descent from Ḥimyarite kings and ties to ancient Ẓafār shape its cultural identity. ⁵

Contemporary Challenges

Like many Yemeni towns, Yarīm faces water shortages from over-irrigation, youth unemployment, rural–urban migration, cultural heritage risks, and security challenges since the 2015 civil war. However, its high elevation has spared it from much coastal warfare, keeping it strategically important. ⁶

Further Reading

https://historyofislam.org/sources-of-advent-of-islam
https://islamichistory.org/home/

End Notes

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This city was a metropolitan consisting of five or seven cities on both banks of the River Tigris.⁷

Today it is a small village by name of Madain in modern Iraq, where ruins of its magnificent past can be seen approximately 32 Km south of Baghdad.

Further Reading

Touraj Daryaee. Sasanian Persia: The Rise and Fall of an Empire. London: I. B. Tauris, 2009.

https://historyofislam.org/pre-islamic-arab-politics

Endnotes

The post    Capital City of Sasanian Empire appeared first on Islamic History.

Further Reading

Irfan Shaid, Byzantium and the Arabs in the sixth century Part 2 Volume II (Washington, D.C.: Dumbarton Oaks, 2002), 96 – 104.

https://historyofislam.org/pre-islamic-arab-politics

Endnotes

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Further Reading

Talbot Rice, “The Oxford Excavations in Hira, 1931,” Antiquity 6 no. 23 (Sep. 1932): 276 – 291.

www.historyofislam.org

Endnotes

The post Hirah appeared first on Islamic History.

Some mountain peaks rise up to three thousand meters here. The southernmost peaks of this mountain chain in Asir rise up to three thousand meters.  Their highest point, Jabl An-Nabi Shu’ayb (شعيب النبى جبل) in Yemen, is 3666 meters above sea level.

Climate

The Yemen Highlands are not arid.  They receive up to thirty cm of rainfall per year, mainly due to monsoons that come from October through March from the Indian Ocean.  This area supports terrace farming. The highlands of Yemen have even fewer clusters of Junipers and boast a hundred-kilometre-long river, Hajr (Wādi al Hajr الحجر وادى).  That is the only river on the peninsula, though it is seasonal.

Further reading

Paul Sanlaville, “Geographic Introduction” in Roads of Arabia, ed. ‘Ali ibn Ibrāhīm Ghabbān, Beatrice Andre-Salvini Francoise Demange, Carine Juvin and Marianne Cotty, (Paris: Louvre, 2010), 55 – 68.

William Bayne Fisher, The Middle East.  A Physical, Social and Regional Geography, London: Methuen & Co. Ltd, 1952.

History of Islam, Geography and Climate of Pre-Islamic Arabia, https://historyofislam.org/geography-and-climate/

The post Yemen Highlands appeared first on Islamic History.

The Tihamah coastal plain is dry, sometimes interspersed with marshes though.  Thanks to the Red Sea, Tihamah is cool. Daytime temperature during summer averages 32°c while winter temperature is around 16°c. These regions receive regular rainfall. Humidity on the coast is so high in the summer that a mist often sprinkles the coastal areas in the daytime, and a warm fog hangs in the air at night. Tihamah received a surprisingly cool, humid breeze in summer.

Further reading

Alois Musil, The Northern Ḥeijāz: A Topographical Itinerary, New York: Czech Academy of Sciences and Arts, 1926.

Paul Sanlaville, “Geographic Introduction” in Roads of Arabia, ed. ‘Ali ibn Ibrāhīm Ghabbān, Beatrice Andre-Salvini Francoise Demange, Carine Juvin and Marianne Cotty, (Paris: Louvre, 2010), 55 – 68.

Peter Vincent, Saudi Arabia: An Environmental Overview, London: Taylor & Francis, 2007.

William Bayne Fisher, The Middle East.  A Physical, Social and Regional Geography, London: Methuen & Co. Ltd, 1952.

History of Islam, Geography and Climate of Pre-Islamic Arabia, https://historyofislam.org/geography-and-climate/

The post Tihamah appeared first on Islamic History.

The eastern end of the Najd Plateau merges into the low and flat plains of Hasa (الاحساء).

Najd plateau is interspersed by small mountain systems here and there, like Jabl Tuwayq (طوىق جبل).

Ancient volcanic activity has created many volcanic fields in the northern part of Arabia called ḥarrah (حره).  The largest of them is Harrat ash Shaam (الشام حرۃ) that spreads from northwestern Saudi Arabia into Jordan and Southern Syria.

Climate

Tropic of Cancer passes through the center of Najad, though there is nothing tropical.  Summer is hot in Najd.  The temperature averages around 45 °c and may reach up to 54 °c on a hot summer day.  December and January are the coolest months.  Though the temperature averages around 14 °c in winter, high wind produces biting cold.  Rarely does the temperature fall to a freezing point.

Extremely dry climate and hot temperatures have converted many parts of the Najad Plateau into true sand deserts. The most renowned of them is Ruba al Khali (Ruba ul Khāli الخالى ربع).  Located over the Lower third of the Najd plateau, Ruba al Khali is so called because it is devoid of any life.  It does not receive any rain.  It has a reputation for being the largest contiguous sand desert on the planet and the most desolate region of the world.  Its sand is estimated to be one hundred and eighty meters deep.  Nobody has ever dwelled here, but ancient Arabs used to cross it on camels.

Najd’s northern part rarely receives any rain.  It has converted into a barren, stony and sandy desert called Nefud (Nefūd نفود).  The sand of Nefud has a reddish tinge due to the presence of iron ores.  Nefud merges into the Syrian Desert towards the north.

Along the side of Jabl Tuwayq and towards its east is the long and narrow Dahna (Dahna’ الدهناء) desert.  It is a narrow strip of sand that connects Ruba al Khali with Nefud.

Further reading

Alois Musil, The Northern Nejd, New York: Czech Academy of Sciences and Arts, 1928.

Paul Sanlaville, “Geographic Introduction” in Roads of Arabia, ed. ‘Ali ibn Ibrāhīm Ghabbān, Beatrice Andre-Salvini Francoise Demange, Carine Juvin and Marianne Cotty, (Paris: Louvre, 2010), 55 – 68.

Peter Vincent, Saudi Arabia: An Environmental Overview, London: Taylor & Francis, 2007.

William Bayne Fisher, The Middle East.  A Physical, Social and Regional Geography, London: Methuen & Co. Ltd, 1952.

History of Islam, Geography & Climate of Pre-Islam Arabia, https://historyofislam.org/geography-and-climate/

The post Najd appeared first on Islamic History.

It comprises the main mountain range of Arabia, which stretches from the northern end of the peninsula down to the south, becoming wider and higher while reaching the south.  Around Mecca, about midway down its length, this mountain chain has a break.  This break separates Hejaz in the north from Asir (Asīr عسير) in the south.

Ancient volcanic activity has created many volcanic fields in the northern part of Arabia called ḥarrah (حره).  The largest of them is Harrat ash Shaam (الشام حرۃ) that spreads from the northwestern Saudi Arabia into Jordan and Southern Syria.

The Tropic of Cancer passes through the center of Hejaz, though there is nothing tropical.  Summer is hot in Hejaz. Temperature averages around 45 °c and may reach up to 54 °c on a hot summer day. Sandstorms and dust storms are natural hazards in Hejaz. The worst sandstorms are associated with shamāl (شمال), the north-westerly wind that is strongest in summer.

December and January are the coolest months.  Though the temperature averages around 14 °c in winter, the high wind produces biting cold.  Rarely does the temperature fall below freezing.

Further reading

Alois Musil, The Northern Ḥeijāz: A Topographical Itinerary, New York: Czech Academy of Sciences and Arts, 1926.

Paul Sanlaville, “Geographic Introduction” in Roads of Arabia, ed. ‘Ali ibn Ibrāhīm Ghabbān, Beatrice Andre-Salvini Francoise Demange, Carine Juvin and Marianne Cotty, (Paris: Louvre, 2010), 55 – 68.

Peter Vincent, Saudi Arabia: An Environmental Overview, London: Taylor & Francis, 2007.

William Bayne Fisher, The Middle East.  A Physical, Social and Regional Geography, London: Methuen & Co. Ltd, 1952.

History of Islam, Geography & Climate of Pre-Islam, https://historyofislam.org/geography-and-climate/

The post Hejaz appeared first on Islamic History.

Hasa plain has numerous salt pans called sabkhah (سبخه).

Climate

The Hasa coastal plain is dry.  Thanks to the Persian Gulf, Hasa is cool. Daytime temperature during summer averages 32°c while winter temperature is around 16°c. It receives regular rainfall.  Humidity on the coast is high, and it can receive surprisingly cool, humid breezes in summer.

Underground water comes near the surface in some arid places of the Arabian Peninsula.  Sometimes this water starts running on the ground as a spring. Otherwise, it can be tapped by digging a well.  These areas are called oases (wāḥtah واحۃ).  Such groundwater is most abundant in the Hasa plain, producing the largest oases on the peninsula, named Hofuf (Hofūf الھفوف).

Further reading

Federico S. Vidal, The Oasis of al-Hasa. New York: Arabian American Oil Company, 1955

The post Hasa Plain appeared first on Islamic History.

Asir is not that arid.  It receives up to thirty cm of rainfall per year, mainly due to monsoons that come from October through March from the Indian Ocean.

Further reading

Paul Sanlaville, “Geographic Introduction” in Roads of Arabia, ed. ‘Ali ibn Ibrāhīm Ghabbān, Beatrice Andre-Salvini Francoise Demange, Carine Juvin and Marianne Cotty, (Paris: Louvre, 2010), 55 – 68.

Peter Vincent, Saudi Arabia: An Environmental Overview, London: Taylor & Francis, 2007.

William Bayne Fisher, The Middle East.  A Physical, Social and Regional Geography, London: Methuen & Co. Ltd, 1952.

History of Islam, Geography and Climate of Pre-Islam Arabia, https://historyofislam.org/geography-and-climate/

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