Hinterland in the context of "City region"

Singapore, officially the Republic of Singapore, is an island country and city-state in Southeast Asia. Its territory comprises one main island, 63 satellite islands and islets, and one outlying islet. The country is about one degree of latitude (137 kilometres or 85 miles) north of the equator, off the southern tip of the Malay Peninsula, bordering the Strait of Malacca to the west, the Singapore Strait to the south along with the Riau Islands in Indonesia, the South China Sea to the east and the Straits of Johor along with the State of Johor in Malaysia to the north.

In its early history, Singapore was a maritime emporium known as Temasek; subsequently, it was a major constituent of several successive thalassocratic empires. Its contemporary era began in 1819, when Stamford Raffles established Singapore as an entrepôt trading post of the British Empire. In 1867, Singapore came under direct British control as part of the Straits Settlements. During World War II, Singapore was occupied by Japan in 1942 and returned to Britain as a Crown colony following Japan's surrender in 1945. Singapore gained self-governance in 1959 and in 1963 became part of the new federation of Malaysia, alongside Malaya, North Borneo and Sarawak. Ideological differences led to Singapore's expulsion from the federation two years later; it became an independent sovereign country in 1965. After early years of turbulence and despite lacking natural resources and a hinterland, the nation rapidly developed to become one of the Four Asian Tigers.

The Duchy of Croatia (Modern Croatian: Kneževina Hrvatska; also Duchy of the Croats, Modern Croatian: Kneževina Hrvata; Latin: Ducatus Chroatorum; Greek: Χρωβατία) was a medieval state that was established by White Croats who migrated into the area of the former Roman province of Dalmatia c. 7th century AD. Throughout its existence the Duchy had several seats – namely, Klis, Solin, Knin, Bijaći and Nin. It comprised the littoral – the coastal part of today's Croatia – except Istria, and included a large part of the mountainous hinterland as well.

The Croats settled in Dalmatia after defeating the Pannonian Avars, during the time of Byzantine emperor Heraclius I. The Duchy was in the center of competition between the Byzantine Empire and the Carolingian Empire for rule over the area. Croatian rivalry with Venice emerged in the first decades of the 9th century and would continue through the following centuries. Croatia also waged battles with the Bulgarian Empire (founded c. 681; Bulgar-Croatian relations improved greatly afterwards) and with the Arabs; it also sought to extend its control over important coastal city-states under the rule of Byzantium. Croatia experienced periods of vassalage to the Franks or to the Byzantines and of de facto independence until 879, when Duke Branimir was recognized as an independent ruler by Pope John VIII. The Duchy was ruled by the Trpimirović and Domagojević dynasties from 845 to 1091. Around 925, during the rule of Tomislav, Croatia became a kingdom.

Byzantine Venetia (Greek: Bενετικὰ, romanized: Venetikà), also known as the Byzantine Maritime Venetia (Latin: Venetia maritima), or Maritime Venice (Italian: Venezia marittima), was a territory of the Byzantine Empire, within the Exarchate of Ravenna, that existed from the middle of the 6th century, up to the second half of the 7th century. Its territory was corresponding to the coastal belt of ancient Venetia and Istria, encompassing coastal regions of present-day Veneto, and Friuli-Venezia Giulia, including the Venetian Lagoon. Its territory did not include hinterland of the old Venetian province, which was conquered by the Lombards. Within Byzantine domains in Italy, Maritime Venetia had a peripheral position, characterized by a patchwork of settlements without major urban centers, besides Oderzo (Latin: Opitergium), the capital city of the province.

The Domini di Terraferma (lit. 'mainland domains') or Stato da Tera (lit. 'mainland state') was the hinterland territories of the Republic of Venice beyond the Adriatic coast in Northeast Italy. They were one of the three subdivisions of the Republic's possessions, the other two being the original Dogado (Duchy) and the Stato da Màr (maritime territories).

The Israeli coastal plain (Hebrew: מישור החוף, romanized: Mishor HaḤof, lit. 'coastal plain') is the Israeli segment of the Levantine coastal plain of the Mediterranean Sea, extending 187 kilometres (116 mi) north to south. It is a geographical region defined morphologically by the sea, in terms of topography and soil, and also in its climate, flora and fauna. It is narrow in the north and broadens considerably towards the south, and is continuous, except the short section where Mount Carmel reaches almost all the way to the sea. The Coastal Plain is bordered to the east by – north to south – the topographically higher regions of the Galilee, the low and flat Jezreel Valley, the Carmel range, the mountains of Samaria, the hill country of Judea known as the Shephelah, and the Negev Mountains in the south. To the north it is separated from the coastal plain of Lebanon by the cliffs of Rosh HaNikra, which jut out into the sea from the Galilee mountains, but to the south it continues into the Egyptian Sinai Peninsula.

The plain can be conventionally divided into a number of areas: the Northern Coastal Plain borders the Galilee in its northern part, and the Jezreel Valley in its southern part between Akko and Haifa, where it is also called the Plain of Zebulon; Hof HaCarmel, or the Carmel Coastal Plain, runs along the Mount Carmel range; the Sharon Plain continues down to northern Tel Aviv; the Central Coastal Plain stretches from Tel Aviv to the northern limit of the Gaza Strip, with the Nahal Shikma [he] stream as its limit – there Israel's access to the Mediterranean ends and the Israeli Southern Coastal Plain, also known as the Western Negev, actually consists of the hinterland of the Strip. For almost its entire length, the plain has sandy beaches, and a Mediterranean climate, except at its southern end where the climate is semi-arid.

The Low Countries (Dutch: de Lage Landen; French: les Pays-Bas), historically also known as the Netherlands (Dutch: de Nederlanden), is a historical and geographically coastal lowland region in Northwestern Europe forming the lower basin of the Rhine–Meuse–Scheldt delta and consisting today of the three modern "Benelux" countries: Belgium, Luxembourg, and the Netherlands (Dutch: Nederland, which is singular). Also sometimes included are parts of France (such as Nord and Pas-de-Calais) and the German regions of East Frisia, Guelders and Cleves. Since the creation of the Holy Roman Empire, the region has been divided into numerous different entities.

Historically, the regions without access to the sea linked themselves politically and economically to those with access to form various unions of ports and hinterland, stretching inland as far as parts of the German Rhineland. Not only physically-low-altitude areas but also some hilly or elevated regions are now therefore considered part of the Low Countries, including Luxembourg and southern Belgium. Within the European Union, the region's political grouping is still referred to as the Benelux (short for Belgium-Netherlands-Luxembourg).

Kilindini Harbour is a large, natural deep-water inlet extending inland from Mombasa, Kenya. It is 25–30 fathoms (46–55 m) at its deepest center, although the controlling depth is the outer channel in the port approaches with a dredged depth of 17.5 m (57 ft). It serves as the harbour for Mombasa, with a hinterland extending to Uganda. Kilindini Harbour is the main part of the Port of Mombasa, the only international seaport in Kenya and the biggest port in east Africa. It is managed by the Kenya Ports Authority (KPA). Apart from cargo handling, Mombasa is frequented by cruise ships.

Kilindini is a Swahili term meaning "deep down" or "in the depths" in reference to the depth of the channel. Kilindini Harbor is an example of a natural geographic phenomenon called a ria, formed millions of years ago when the sea level rose and engulfed a river that was flowing from the mainland.

Cagliari (/kælˈjɑːri/, also UK: /ˌkæliˈɑːri, ˈkæljəri/, US: /ˈkɑːljəri/; Italian: [ˈkaʎʎari] ; Sardinian: Casteddu [kasˈteɖːu] ; Latin: Caralis [käˈɾaːlɪs]) is an Italian municipality and the capital and largest city of the island of Sardinia, an autonomous region of Italy. It has about 146,627 inhabitants, while its metropolitan city, 16 other nearby municipalities, has about 417,079 inhabitants. According to Eurostat, the population of the functional urban area, the commuting zone of Cagliari, rises to 476,975. Cagliari is the 26th largest city in Italy.

An ancient city with a long history, Cagliari has seen the rule of several civilisations. Under the buildings of the modern city there is a continuous stratification attesting to human settlement over the course of some five thousand years, from the Neolithic to today. Historical sites include the prehistoric Domus de Janas, partly damaged by cave activity, a large Carthaginian era necropolis, a Roman era amphitheatre, a Byzantine basilica, three Pisan-era towers and a strong system of fortification that made the town the core of Spanish Habsburg imperial power in the western Mediterranean Sea. Its natural resources have always been its sheltered harbour, the often powerfully fortified hill of Castel di Castro, the modern Casteddu, the salt from its lagoons, and, from the hinterland, wheat from the Campidano plain and silver and other ores from the Iglesiente mines.