The Shephelah or Shfela, lit. "lowlands" ( hbo, הַשְּפֵלָה ''hašŠǝfēlā'', also

Modern Hebrew Modern Hebrew ( he, עברית חדשה, ''ʿivrít ḥadašá ', , '' lit.'' "Modern Hebrew" or "New Hebrew"), also known as Israeli Hebrew or Israeli, and generally referred to by speakers simply as Hebrew ( ), is the standard form of the He ...

: , ''Šǝfēlat Yəhūda'', the "Judaean foothills"), is a transitional region of soft-sloping rolling hills in south-central

Israel Israel (; he, יִשְׂרָאֵל, ; ar, إِسْرَائِيل, ), officially the State of Israel ( he, מְדִינַת יִשְׂרָאֵל, label=none, translit=Medīnat Yīsrāʾēl; ), is a country in Western Asia. It is situated ...

stretching over between the Judaean Mountains and the Coastal Plain. Jewish National Fund (KKL), ''British Park – Scenic trails in Israel's Heartland''. Quote: "The Judean Plain is an intermediate region situated between the Coastal Plain to the west and the Judean Mountains to the east. The altitude of its hills varies from 150 to 450 meters above sea level, and geologically speaking, the plain is a syncline, i.e., a basin in which the layers of rock have folded downwards and sunk. [...] The plain consists of two distinct landscape units: the lower plain, to the west, where the hills are lower and separated by broad riverbeds; and the upper plain, where the valleys are deeper and the hills rise to a height of between 250 and 450 meters above sea level."
/ref> The different use of the term "Judean Plain", as either defining just the Coastal Plain segment stretching along the Judaean Mountains, or also including, or only referring to, the Shfela, often creates grave confusion. Today the Shfela is largely rural with many farms, but the cities of

Ashdod Ashdod ( he, ''ʾašdōḏ''; ar, أسدود or إسدود ''ʾisdūd'' or '' ʾasdūd'' ; Philistine: 𐤀𐤔𐤃𐤃 *''ʾašdūd'') is the sixth-largest city in Israel. Located in the country's Southern District, it lies on the Mediterran ...

, Ashkelon,

Rehovot Rehovot ( he, רְחוֹבוֹת ''Rəḥōvōt'', ar, رحوڤوت ''Reḥūfūt'') is a city in the Central District of Israel, about south of Tel Aviv. In it had a population of . Etymology Israel Belkind, founder of the Bilu movement, ...

Beit Shemesh Beit Shemesh ( he, בֵּית שֶׁמֶשׁ ) is a city located approximately west of Jerusalem in Israel's Jerusalem District, with a population of in . History Tel Beit Shemesh The small archaeological tell northeast of the modern city w ...

, and Kiryat Gat roughly surround it. The Bible assigned land in the Shfela to the tribes of Judah and

Dan Dan or DAN may refer to: People * Dan (name), including a list of people with the name ** Dan (king), several kings of Denmark * Dan people, an ethnic group located in West Africa **Dan language, a Mande language spoken primarily in Côte d'Ivoir ...

Biblical references

The Shfela is mentioned many times in the

Hebrew Bible The Hebrew Bible or Tanakh (;"Tanach"
'' (In the

King James Version The King James Version (KJV), also the King James Bible (KJB) and the Authorized Version, is an English translation of the Christian Bible for the Church of England, which was commissioned in 1604 and published in 1611, by sponsorship of K ...

, the Hebrew term "Shfela" tends to be translated as "vale" or "valley.") The Shfela was the site of many biblical battles. During the

Bar Kokhba revolt The Bar Kokhba revolt ( he, , links=yes, ''Mereḏ Bar Kōḵḇāʾ‎''), or the 'Jewish Expedition' as the Romans named it ( la, Expeditio Judaica), was a rebellion by the Jews of the Roman province of Judea, led by Simon bar Kokhba, ag ...

, hollowed out hills were connected to form elaborate bunker systems for the combat with the Romans.

Geography

The Shfela consists of fertile rolling hills. Topographically, it represents the transition from the higher and more rugged Jerusalem and Hebron Mountains, whose foothills it forms, and the Coastal Plain. About 60 km (35 miles) long in north-south direction and only 13 km (8 miles) wide, it is subdivided into two parts: the western "Low Shephelah", which starts at an altitude of ca. 150 metres above sea level and rises to no more than ca. 200 metres above the Coastal Plain, and the eastern "High Shephelah" rising to altitudes between 250–450 metres above sea level. In the upper part the valleys descending from the Judean Mountains are deeper, and they broaden once they reach the lower part where the riverbeds create larger spaces between the hills. Where they reach the Shfela, the rivers can flow over substantial distances along the border between the mountains and the hills, forming longitudinal valleys. Passage between the east-west and north-south valleys has dictated the communication routes throughout history. In geological terms, the Shfela is a

syncline In structural geology, a syncline is a fold with younger layers closer to the center of the structure, whereas an anticline is the inverse of a syncline. A synclinorium (plural synclinoriums or synclinoria) is a large syncline with superimpose ...

, i.e. it formed as a basin whose rock layers were folded downwards, but is part of the wider south Judean

anticlinorium In structural geology, an anticline is a type of fold that is an arch-like shape and has its oldest beds at its core, whereas a syncline is the inverse of an anticline. A typical anticline is convex up in which the hinge or crest is the ...

-a regional formation characterised by upward folding. Typical to the Shfela are the

Senonian The Late Cretaceous (100.5–66 Ma) is the younger of two epochs into which the Cretaceous Period is divided in the geologic time scale. Rock strata from this epoch form the Upper Cretaceous Series. The Cretaceous is named after ''creta'', t ...

Eocene The Eocene ( ) Epoch is a geological epoch that lasted from about 56 to 33.9 million years ago (mya). It is the second epoch of the Paleogene Period in the modern Cenozoic Era. The name ''Eocene'' comes from the Ancient Greek (''ēṓs'', ...

chalk Chalk is a soft, white, porous, sedimentary carbonate rock. It is a form of limestone composed of the mineral calcite and originally formed deep under the sea by the compression of microscopic plankton that had settled to the sea floor. C ...

y formations. The soft Eocene chalk is known locally as ''kirton'', which tends to build a harder upper

calcrete Caliche () is a sedimentary rock, a hardened natural cement of calcium carbonate that binds other materials—such as gravel, sand, clay, and silt. It occurs worldwide, in aridisol and mollisol soil orders—generally in arid or semiarid regions ...

crust (''nari''), so that in the past people quarried the ''kirton'' while leaving the ''nari'' layer in place as a ceiling. Apart from using the extracted rock, they also utilised the generated underground hollows for different purposes (refuge, burial, storage etc.). One of the major characteristics is hills formed of

marl Marl is an earthy material rich in carbonate minerals, clays, and silt. When hardened into rock, this becomes marlstone. It is formed in marine or freshwater environments, often through the activities of algae. Marl makes up the lower part ...

-covered soft

, as opposed to the

Judean Hills The Judaean Mountains, or Judaean Hills ( he, הרי יהודה, translit=Harei Yehuda) or the Hebron Mountains ( ar, تلال الخليل, translit=Tilal al-Khalīl, links=, lit=Hebron Mountains), is a mountain range in Palestine and Israel w ...

which are made of hard chalk and

dolomite Dolomite may refer to: *Dolomite (mineral), a carbonate mineral *Dolomite (rock), also known as dolostone, a sedimentary carbonate rock *Dolomite, Alabama, United States, an unincorporated community *Dolomite, California, United States, an unincor ...

. The valleys and lower areas contain soil with a high sand content, as well as large tracts of fertile areas. Seasonal

swamp A swamp is a forested wetland.Keddy, P.A. 2010. Wetland Ecology: Principles and Conservation (2nd edition). Cambridge University Press, Cambridge, UK. 497 p. Swamps are considered to be transition zones because both land and water play a role in ...

s can develop during the

rainy season The rainy season is the time of year when most of a region's average annual rainfall occurs. Rainy Season may also refer to: * ''Rainy Season'' (short story), a 1989 short horror story by Stephen King * "Rainy Season", a 2018 song by Monni * '' ...

. The southern part is made up of

loess Loess (, ; from german: Löss ) is a clastic, predominantly silt-sized sediment that is formed by the accumulation of wind-blown dust. Ten percent of Earth's land area is covered by loess or similar deposits. Loess is a periglacial or aeoli ...

, while north of Ashkelon consists of

clay Clay is a type of fine-grained natural soil material containing clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4). Clays develop plasticity when wet, due to a molecular film of water surrounding the clay pa ...

. The Shfela has a temperate Mediterranean to

semi-arid climate A semi-arid climate, semi-desert climate, or steppe climate is a dry climate sub-type. It is located on regions that receive precipitation below potential evapotranspiration, but not as low as a desert climate. There are different kinds of semi ...

. A series of east-west valleys cuts the Shfelah into districts. From north to south, they are: the Valley of Ayalon,

Sorek Valley Naḥal Sorek ( he, נחל שורק, translation=Brook of Sorek; ar, وادي الصرار, translit=Wadi al-Sirar), also Soreq, is one of the largest, most important drainage basins in the Judean Hills. It is mentioned in the Book of Judges 16:4 ...

Valley of Elah The Valley of Elah or Ella Valley ("the valley of the terebinth"; from the he, עמק האלה ''Emek HaElah''), called in ar, وادي السنط, Wadi es-Sunt, is a long, shallow valley in Israel and the West Bank best known as the place de ...

, Guvrin Valley, Valley of Lachish, and Valley of Adorayim. The biblical towns established there guarded settlements of the interior and took advantage of trade passing along this route. Ayalon was the primary access corridor to

Jerusalem Jerusalem (; he, יְרוּשָׁלַיִם ; ar, القُدس ) (combining the Biblical and common usage Arabic names); grc, Ἱερουσαλήμ/Ἰεροσόλυμα, Hierousalḗm/Hierosóluma; hy, Երուսաղեմ, Erusałēm. i ...

along the ascent of

Horon Horon ( pnt, χορόν, khorón) is a traditional folk dance from Pontus or Eastern Black Sea Region in Turkey. Name Etymology The term ''horon'' derives from Greek ''choros'' ( el, χορός, khorós), which means "dance." The earliest ins ...

. Caves are a major feature of the southern part of the Shfela, many of them bell-shaped such as those in Beit Guvrin.

History and archaeology

Archaeological surveys in the Shephelah have found evidence of habitation during the Late Bronze period. During the early Iron Age, the population of what has been widely believed to be a Canaanite enclave between the rising centres of both coastal Philistia and the Israelite/Judahite highlands, went into decline, though a string of settlements survived on the eastern edge. In the Iron Age IIA–B, population growth resumed and by the 8th century BCE it was densely populated, not so much by natural growth but as a result of incoming settlers, beginning with the short-lived settlement at

Khirbet Qeiyafa Khirbet Qeiyafa ( ar, خربة قيافة), also known as Elah Fortress and in Hebrew as Horbat Qayafa ( he, חורבת קייאפה), is the site of an ancient fortress city overlooking the Elah Valley and dated to the first half of the 10th ...

. The overall estimated numbers for inhabitants range from 50,000 to 100,000, over numerous sites such as Tel Lachish, Azekah,

Tel Burna Tel Burna is an Israeli archaeological site located in the Shephelah (Judean foothills), along the banks of Nahal Guvrin, not far from modern-day Qiryat Gat. History and identification The site was primarily inhabited in the Bronze and Iron Ages, ...

Tel Zayit Tel Zayit ( he, תל זית, ar, Tell Zeita, Kirbat Zeita al Kharab) is an archaeological tell in the Shephelah, or lowlands, of Israel, about 30 km east of Ashkelon. History The site, roughly , shows evidence of human settlement throughout ...

Khirbet el-Qom Khirbet el-Qom () is an archaeological site in the village of al-Kum, West Bank, in the territory of the biblical Kingdom of Judah, between Lachish and Hebron, 14 km to the west of the latter. Excavations Archaeological excavations were co ...

, Tel Erani, Tel Harasim and Tel Nagila. This colonization, together with the inhabitants of the Canaanite enclave, identified with the highland Israelite/Judahite culture, and its expansion coincides with the decline of Philistia.Avraham Faust
'Between the Highland Polity and Philistia,'
in BASOR, vol.383 2020pp.115-137pp.117-119,122,124. During the decline and ultimate destruction of Judah by the Assyrians and Babylonians, the region was taken over gradually by the Edomites and it became the core of what was known in Greek as Idumea. The Shephela flourished during the Hellenistic period, was strongly affected by the First Jewish-Roman War (66–70) and was largely depopulated of Jews as a result of the

Bar Kochba revolt The Bar Kokhba revolt ( he, , links=yes, ''Mereḏ Bar Kōḵḇāʾ‎''), or the 'Jewish Expedition' as the Romans named it ( la, Expeditio Judaica), was a rebellion by the Jews of the Roman province of Judea, led by Simon bar Kokhba, aga ...

(132–136). It flourished again in the Byzantine period and was the scene of one of the major battles during the

Muslim Muslims ( ar, المسلمون, , ) are people who adhere to Islam, a monotheistic religion belonging to the Abrahamic tradition. They consider the Quran, the foundational religious text of Islam, to be the verbatim word of the God of Abrah ...

Arab conquest The spread of Islam spans about 1,400 years. Muslim conquests following Muhammad's death led to the creation of the caliphates, occupying a vast geographical area; conversion to Islam was boosted by Arab Muslim forces conquering vast territories ...

of the 7th century.

Archaeological sites

* Azekah *

Tel Batash Timnath or Timnah was a Philistine city in Canaan that is mentioned in the Hebrew Bible in and in connection with Samson. Modern archaeologists identify the ancient site with a tell lying on a flat, alluvial plain, located in the Sorek Valley ...

* Beit Guvrin * Beit Jimal * Tell Beit Mirsim *

* Tel Eton * Gezer * Imwas and Emmaus Nicopolis * Tel Halif * Hurvat Itri * Jarmuth *

Tell ej-Judeideh Tell ej-Judeideh ( ar, تل الجديدة / خربة الجديدة) is a tell in modern Israel, lying at an elevation of above sea-level. The Arabic name is thought to mean, "Mound of the dykes." In Modern Hebrew, the ruin is known by the n ...

* Kharruba *

Keilah Keilah (), meaning Citadel, was a city in the lowlands of Judah (). It is now a ruin, known as ''Kh. Qeila'', near the modern village of Qila, east of Beit Gubrin, and about west of Kharas.Amit (n.d.), p. 308 History The earliest historical ...

* Tel Lachish *

Lavnin Lavnin (''Hurvat Libnah'' / ''Tel Lavnin'' / ''Kh. Tell el-Beida'')()( ar, خربة تل البيضة), is a late Bronze Age archaeological site situated in Israel's Adullam region, rising some above sea level. The site lies northwest of Bayt Jib ...

* Khirbet a-Ra'i * Sokho * *

Tell Zayit Tel Zayit ( he, תל זית, ar, Tell Zeita, Kirbat Zeita al Kharab) is an archaeological tell in the Shephelah, or lowlands, of Israel, about 30 km east of Ashkelon. History The site, roughly , shows evidence of human settlement throughout ...

* Zorah

References

External links