Delta

Deltas have long played an important role in human history. These fertile areas where rivers flow into large bodies of water have served as fishing, farming, and living sites. Of the great deltas around the world, perhaps none has had a greater role in civilization than the delta of Egypt's Nile River. Greek historian Herodotus (c. 484–c. 425 b.c.e.), considered by many as the "Father of History," studied this great geologic feature. He is credited with coining the term "delta" for this type of landform because its triangular shape reminded him of the Greek letter ∆ (delta).

The shape of the land

A delta is a body of sediment deposited at the mouth of a river or stream where it enters an ocean or lake. Unlike other landforms affected by running water, a delta is not created primarily by water cutting into or eroding the landscape (erosion is the gradual wearing away of Earth surfaces through the action of wind and water). Water does not tear down a delta; instead, it builds up a delta.

A river creates a delta by laying down sediment or rock debris such as gravel, sand, silt, and clay that it has picked up and carried along its course. Alluvium (pronounced ah-LOO-vee-em) is the general term for sediment deposited by running water. A river's depth, its width, and its speed determine how much sediment it can carry. The Mississippi River flows at an average surface speed of about 2 miles (3 kilometers) per hour. Yet it drains between 1.2 and 1.8 million square miles (3.1 and 4.6 million square kilometers), which is more than 40 percent of the total area of the continental United States. Over the course of a year, it moves an average of 159 million tons (144 million metric tons) of sediment.

In general, deltas are similar in shape to another type of landform deposited by flowing water, alluvial (pronounced ah-LOO-vee-al) fans.

Found typically in desert and other arid (dry) environments, these fanlike deposits of sediment form where an intermittent, yet rapidly flowing canyon or mountain stream spills out onto a plain or relatively flat valley. An alluvial fan is a landform that forms on land. A delta is a landform that forms in water. (For further information on alluvial fans, see the Dune and other desert features chapter.)

A delta may be divided into three main zones: upper delta plain, lower delta plain, and subaqueous (pronounced sub-AY-kwee-us) delta plain. The upper delta plain is that part of the delta that is farthest inland. It lies above the high tide mark and is not affected by the action of waves or tides. (Tide is the periodic rising and falling of water in oceans and other large bodies of water in response to the gravitational attraction of the Moon and the Sun upon Earth.) The river or stream that forms the delta begins to divide in the upper delta plain into smaller channels called distributaries, which carry sediments toward the delta's edges. Immediately seaward of the upper delta plain is the lower delta plain. It occupies the area between high and low tides and, thus, periodically lies underwater. The landscape is affected by the action of distributaries, tides, and waves. Finally, the subaqueous delta plain is that part of the delta that lies below the low tide mark and, as a result, lies completely underwater.

The tug of war between land and water determines a delta's shape. It is a battle that pits the strength of a river's flow and the amount of sediment it carries against wave and tidal currents. Deltas build outward from a coast only if the slope from the shore is gentle and ocean currents are not strong enough to carry away the sediment deposited by the river. The three main varieties of deltas based on shape are the arcuate (pronounced AR-cue-et), the bird's foot, and the cuspate (pronounced KUSS-pate).

Delta: Words to Know

Alluvial fan:

A fanlike deposit of sediment that forms where an intermittent, yet rapidly flowing canyon or mountain stream spills out onto a plain or relatively flat valley.

Alluvium:

A general term for sediment (rock debris such as gravel, sand, silt, and clay) deposited by running water.

Bed load:

The coarse sediment rolled along the bottom of a river or stream.

Bottomset bed:

A fine, horizontal layer of clay and silt deposited beyond the edge of a delta.

Dissolved load:

Dissolved substances, the result of the chemical weathering of rock, that are carried along in a river or stream.

Distributaries:

The channels that branch off of the main river in a delta, carrying water and sediment to the delta's edges.

Erosion:

The gradual wearing away of Earth surfaces through the action of wind and water.

Foreset bed:

An inclined layer of sand and gravel deposited along the edge of a delta.

Suspended load:

The fine-grained sediment that is suspended in the flow of water in a river or stream.

Topset bed:

A horizontal layer of coarse sand and gravel deposited on top of a delta.

Arcuate deltas are the commonest form of delta. They are fan-shaped, with the wide portion of the fan farthest from the mainland. Crossed by many short, well-defined distributaries, these types of deltas are composed of relatively coarse sediments. Wave and river activity are fairly well balanced. The seaward edge of the delta is rather smooth because strong waves push the sediment back against that edge. The Nile Delta is an example of an arcuate delta.

Where the action of waves is weak and that of a river is strong, an irregular-shaped delta forms that extends out into the water well beyond the local shoreline. Resembling the spread claws of a bird's foot, this type of delta is called a bird's foot delta. Fine sediments and shifting distributaries mark this river-dominated delta. Bird's foot deltas are not common along ocean coasts because the action of ocean currents and waves is often as strong if not stronger than that of rivers. The Mississippi Delta, on the Gulf of Mexico, is a bird's foot delta.

Cuspate deltas form where a river drops sediment onto a straight shoreline with strong waves that hit head-on. The waves force the sediment to spread outwards in both directions from the river's mouth, making a pointed tooth shape with sides that curve inward. Few distributaries are found in cuspate deltas. The Tiber Delta in Italy is a classic example.

Forces and changes: Construction and destruction

Deltas are found throughout the world, except at the poles. Most of the world's great rivers—the Amazon, the Ganges-Brahmaputra, the Huang He, the Mississippi, the Nile—have built massive deltas. All have a few characteristics in common: they drain large land areas, they carry large quantities of sediment, and they empty at coasts that are geologically quiet (no earthquake or volcanic activity).

Deltas are geologically young landforms. Present-day deltas began forming no more than 7,000 years ago, when sea levels stopped rising after the last ice age ended. Over Earth's history, as sea levels have risen and fallen in response to glacial periods, deltas have formed and have been covered over. The current deltas of some rivers are built on the remains of numerous deltas stretching back millions of years. Yet their surface can change rapidly and significantly. The key to the creation of a delta, and its continual formation, is a river and the sediment it transports.

Running water

Water is a natural force of erosion everywhere on Earth. As it surges over a landscape, water picks up and transports as much material from the surface as it can carry. Gravity and steep slopes aid rushing water in carrying increasingly larger and heavier objects. Erosion by water begins as soon as raindrops hit the ground and loosen small particles. During heavy rains, sheets of water flow over the ground, loosening and picking up even

more particles. This water quickly concentrates into channels, which then become streams that flow into rivers.

The amount and size of the material that a river can transport depends on the velocity, or speed, of the river. A fast-moving river carries more sediment and larger material than a slow-moving one. A river that is turbulent or agitated can also lift and carry more rocks and sediment than one that flows gently.

The sediment load in a river consists mainly of two parts. The first part is the coarse material that moves along the bed or bottom of the river. This is known as the bed load. As it is carried along, this coarse sediment acts as an abrasive, scouring and eating away at the banks and bed of the river. The river then picks up any newly loosened and eroded material. The second part is the fine-grained material that is suspended in the flow of water as the river moves downstream. This is the suspended load. Rivers also carry a dissolved load. These dissolved substances are the result of the chemical weathering of rock, which alters the internal structure of minerals by removing or adding elements.

A river will continue to carry its load as long as its velocity remains constant or increases (if it increases, it can carry an even larger load). Any change in the geography of the landscape that causes a river channel to bend or rise will slow the flow of water in a river. As soon as a river's speed decreases, it loses the ability to carry all of its load and a portion will be deposited, depending on how much the river slows down. Particles will be deposited by size with the largest settling out first.

Laying it down in a delta

When a river meets the standing water of an ocean at a coast, it quickly loses velocity and the heaviest particles drop out. The fine suspended load may be carried farther out into the water before it settles out and sinks to the bottom. Sediments deposited in a delta are laid down in layers known as beds. Bottomset beds are those nearly horizontal or flat layers of fine clay and silt that form underwater farthest from the mouth of the river. Closer to the mouth, yet still underwater, are foreset beds of sand and gravel that slope steeply down toward the bottomset beds at an angle up to 25 degrees. Thin, horizontal layers of coarser sand and gravel that are deposited on the surface of the delta are topset beds. As a delta increases in size and advances farther out into the water, the topset beds cover the foreset beds, which in turn cover the bottomset beds.

As more sediments are brought by the river to the delta, especially in times of flooding, the main river may become choked with sediment. When this occurs, the river branches into distributaries, finding the least resistant path to the shoreline. When sandy deposits block the distributaries, they then become inactive, and smaller, active distributaries branch off. As the process continues, distributaries constantly shift position across the surface of the delta.

The Greatest Sediment Load

The Huang He is the second longest river in China. It begins in the highlands of Tibet and flows eastward for 3,000 miles (4,830 kilometers) before it empties into Bohai Bay. Along its course, it drains more than 290,000 square miles (751,100 square kilometers) of land area. It is the muddiest river in the world, carrying more sediment than any other. Each year, it transports an estimated 1.6 billion tons (1.45 billion metric tons) of sediment. Because that sediment colors the water of the river yellow, the river is also known as the "Yellow River." Much of that sediment is deposited in a delta that has formed at the mouth of the Huang He. It increases in size by as much as 20 square miles (50 square kilometers) each year.

A delta is often a patchwork of marshes, swamps, lakes, and tidal flats (muddy or marshy areas that are covered and uncovered by the rising and falling tides). During the normal flow of the main river in a delta, all the water is guided out to the ocean by the active distributaries. Sediment is deposited in these channels and immediately offshore to them. The areas between the channels receive no sediment. In times of flood, water flows out of the distributaries over the delta surface, depositing sediment. Coarse sandy particles are deposited first, producing low ridges or embankments along the banks of the distributaries. These are known as natural levees (pronounced LEH-veez).

When the balance between a river and ocean is shifted, the delta will either enlarge or decrease in size. If waves and currents are not strong enough to carry most of the sediments away, those sediments will collect over time to form landmasses laced with distributaries that extend a delta farther and farther out to sea. Floods and periods of heavy rain bring more sediment to a delta, building it up. Periods of drought, however, have the opposite effect. Human activity may also affect the size of a delta. If forests or similar types of land upstream are cleared, increased erosion may occur, sending more sediment downstream to build up a delta. If a dam is built on or water is otherwise diverted from a river, the velocity of the river and the amount of sediment it can carry will decrease. Consequently, the delta at its mouth will shrink.

Spotlight on famous forms

Ganges River Delta, Bangladesh and India

The combined Ganges and Brahmaputra Rivers have formed the largest delta in the world, the Ganges River Delta (sometimes called the Ganges-Brahmaputra Delta). Approximately 220 miles (345 kilometers) wide, the delta covers an area of roughly 40,790 square miles (105,645 square kilometers). Almost 1.1 billion tons (1 billion metric tons) of sediment is discharged from these rivers annually. This has produced the Bengal Fan, a deposit of sediment on the floor of the Bay of Bengal that stretches outward 1,865 miles (3,000 kilometers) in length and 620 miles (1,000 kilometers) in width. In places close to shore, the Bengal Fan measures up to 7.5 miles (12 kilometers) thick.

A glacier at about 22,100 feet (6,735 meters) in the Himalayan Mountains is the source of the Ganges River. The river flows southeast across India to combine with the Brahmaputra in Bangladesh. The Brahmaputra River has its source in Tibet along the northern slope of the Himalayan Mountains. From there, it flows across the Assam Valley of India into Bangladesh. The rising Himalayan Mountains provide much of the sediment load of these two rivers.

In Bangladesh, the rivers join to form the Padma, the main channel to the sea. The united rivers branch into many distributaries, forming the vast and fertile Ganges River Delta. The delta region covers roughly 25 percent of India's total territory. The delta's southern portion is covered largely with a swamp forest roughly 6,525 square miles (16,900 square kilometers) in area. Known as the Sunderbans, it is home to the endangered Royal Bengal tiger.

Mississippi Delta, Louisiana

The waters of almost half a continent flow through the Mississippi River. About 159 million tons (144 million metric tons) of sediment—70 percent of which consists of clay, silt, and fine sand—are carried by the river annually. Where it empties into the Gulf of Mexico in southern Louisiana, the river slows and drops its sediment load, forming the Mississippi Delta. The giant bird's foot delta, featuring a large middle toe, marks the seaward growth of land into the gulf.

The delta, the most fertile area of Louisiana, covers about 13,000 square miles (33,670 square kilometers), roughly 25 percent of the state's land area. It measures about 12 miles (19 kilometers) long and 30 miles (48 kilometers) wide. In the delta, the Mississippi River breaks into a number of distributaries, the most important of which are the Atchafalaya (pronounced uh-cha-fuh-LIE-uh) River and the Bayou Lafourche (pronounced BYE-oo luh-FOOSH). The main river continues southeast through the delta to enter the gulf through several mouths, including Southeast Pass, South Pass, and Pass à Loutre.

Geologists believe the present delta has been built outward into the gulf over the last 600 years. The river has built its unique shape because it carries so much sediment and the Gulf of Mexico has such a limited tidal range. One result of this is that the river's distributaries travel very long distances to reach the gulf. Over time, the river switches its route to the

sea, taking a shorter and more energy-efficient route. The Mississippi River has done this at least five times in the last 5,000 years.

Okavango Delta, Botswana

The Okavango (pronounced oh-kah-VANG-go) Delta is the world's largest inland delta. Instead of flowing into an ocean or a large lake, the Okavango River spreads over 6,000 square miles (15,540 square kilometers) of the Kalahari Desert in a maze of intricate waterways and reed-lined channels. This creates a diverse ecosystem that supports the greatest concentration of birds, animals, and fish in Africa.

Rain falling on the highlands in central Angola forms the Cubango River. It flows through Namibia as the Kuvango River before finally entering Botswana as the Okavango River. Each year, some 2.9 trillion gallons (11 trillion liters) of water carrying more than 2 million tons (1.8 million metric tons) of sediment enter the delta, which occupies a depression that contained a large prehistoric lake.

A notable feature about the Okavando Delta is the seasonal flooding that begins in mid-summer in the northern section and ends about six

months later in the southern section. As a result, water rises in the north as it recedes in the south during summer, and rises in the south as it drops in the north during winter. Despite this latter drop, the north remains wet all year. The nature of the annual floods is gentle. Plains and islands disappear under water, then reappear in an ever-changing landscape.

For More Information

Web Sites

"Delta." Kent National Grid for Learning. http://www.kented.org.uk/ngfl/rivers/River%20Articles/delta.htm (accessed on August 26, 2003).

"Deltas." Department of Geological Sciences, Salem State College. http://www.salem.mass.edu/~lhanson/gls214/gls214_deltas.html (accessed on August 26, 2003).

"Ganges River Delta (image)." Earth Observatory, NASA. http://earthobservatory.nasa.gov/Newsroom/NewImages/images.php3?img_id=4793 (accessed on August 26, 2003).

"Major Deltas of the World." Department of Geology and Geophysics, University of Wyoming. http://faculty.gg.uwyo.edu/heller/Sed%20Strat%20Class/Sedstrat6/slideshow_6_1.htm (accessed on August 26, 2003).

"Mississippi River Delta (image)." Earth Observatory, NASA. http://earthobservatory.nasa.gov/Newsroom/NewImages/images.php3?img_id=9304 (accessed on August 26, 2003).

"Okavango Delta and Makgadikgadi Pans, Botswana (image)." Visible Earth, NASA. http://visibleearth.nasa.gov/cgi-bin/viewrecord?9152 (accessed on August 26, 2003).

"When Rivers Run Into the Ocean." Missouri Botanical Garden. http://mbgnet.mobot.org/fresh/rivers/delta.htm (accessed on August 26, 2003).

Delta

Deltas are complex depositional landforms that develop at the mouths of rivers . They are composed of sediment that is deposited as a river enters a standing body of water and loses forward momentum. Famous deltas include the Mississippi delta in Louisiana and the Nile delta in Egypt.

Every river flows, under the force of gravity , from its headwaters to its mouth. The mouth of a river is the location at which the river enters a standing body of water, such as a lake, sea, or the ocean. As the river enters standing water and the current is no longer confined to a channel, it spreads out, slows down, and eventually stops. The reduction in speed of the current causes the river to become unable to continue carrying suspended sediment. As sediment is deposited a series of smaller channels, called distributary channels, forms causing the shoreline to build out, or prograde. The landform created is the delta. In smaller rivers with weaker currents, forward momentum may cease almost immediately upon reaching the lake or ocean. This is especially true where the river empties into an area of strong wave action. In this case, no significant delta will be formed. Larger rivers, such as the Amazon, may be able to maintain some current for several miles out to sea, creating an extensive delta.

As a river reaches and enters a standing body of water, sediment is deposited according to grain size. The coarsest sediment, such as sand , is dropped first, closest to the mouth of the river. With progressive distance from the mouth, finer sediment including fine sand, silt, and clay is deposited. This results in a distinct sequence of layers, known as topsets, foresets, and bottomsets. The topsets, as the name implies, are the uppermost layer. They are comprised of the coarse sediment forming the area of the delta that is above sea level. The foresets include fine sand grading into silt and clay deposited in seaward sloping layers beyond the mouth. Bottomsets are made up of clay particles, carried furthest out to sea where they settle into horizontal layers. Although this sequence is

deposited laterally with increasing distance from land, as a delta progrades the bottomsets are covered by new foresets, which are then covered by topsets as sediment builds up, and so on. The resultant coarsening up sequence is a distinguishing feature of deltaic deposits.

The sequence of topsets, foresets, and bottomsets provides an accurate picture of a simple delta system. Large marine deltas are often more complex, depending on whether the river, wave action, or the tides play the most important role. In stream-dominated deltas, fluvial deposition processes remain strongest, and distributary channels build far out to sea. These deltas are known as bird's foot deltas because of the appearance of the collection of channels extending into the sea. The Mississippi delta is probably the most famous example of a bird's foot delta. In wave-dominated deltas, distributary channels are not maintained for any great distance out to sea; rather, wave action reforms their sediment into barrier islands oriented perpendicular to the direction of flow. This type of delta is more compact, and shaped like a triangle. The Nile delta in Egypt is an example of a wave-dominated delta. Lastly, tide-dominated deltas are also compact, but broad tidal channels and sand bars form parallel to the tide direction. The Mekong delta in Vietnam is an example of a tide-dominated delta.

See also Alluvial system; Estuary; Landforms; Sedimentation

DELTA

Often called Lower Egypt, the land between the mouths of the Nile.

The delta is a triangular area (shaped like the Greek letter Δ) that has been built up by the silt carried within the waters of the Nile River. When the Nile approaches the Mediterranean, much of the solid wastes and organic matter picked up during its long trip to the sea is screened out at the marshy estuaries and left behind to build more delta land. Although in ancient Egypt the Nile delta had seven mouths, today it has two—the Damietta on the east and Rosetta on the west—and many small channels. The broad coastal rim of the delta measures about 150 miles (240 km) from Alexandria in the west to Port Saʿid in the east. It is about 100 miles (160 km) from the Mediterranean coast south to Cairo, Egypt's capital.

The delta landscape is flat and mostly fertile, but the area nearest the coast is marshy, dominated by brackish inlets and lagoons. Since the construction of the Delta Barrages in the early nineteenth century, most of the farmland has been converted from basin to perennial irrigation, which supports two or three crops per year instead of one. Almost half the inhabitants are small landowners, sharecroppers, or peasants working for wages who live in villages surrounded by the lands they till. The others live in towns or cities. Fruits, vegetables, and cotton are the important delta crops. Delta Egyptians have generally had more contact with the outside world than have Upper Egyptians and are therefore more Westernized.

Bibliography

Metz, Helen Chapin, ed. Egypt: A Country Study, 5th edition. Washington, DC: U.S. Government Printing Office, 1991.

arthur goldschmidt

delta A discrete protuberance of sediment formed where a sediment-laden current enters an open body of water, at which point there is a reduction in the velocity of the current. This results in rapid deposition of the sediment, which forms a body, for example, at the mouth of a river where the river discharges into the sea or a lake. There is a characteristic coarsening upwards of sediments. A river provides the sediments to form a delta; but the shape and nature of a delta is controlled by a variety of factors including climate, water discharge, sediment load, rate of subsidence of the sea or lake floor, and the nature of the river-mouth processes (particularly tidal and wave energy). One classification of delta types, based on variations in transport patterns on the delta, subdivides deltas into three classes: (a)river-dominated (e.g. the Mississippi and Po);(b)wave-dominated (e.g. the Rhône and Nile); and(c)tide-dominated (e.g. the Ganges and Mekong).See also Gilbert-type delta.

delta A discrete protuberance of sediment formed where a sediment-laden current enters an open body of water, at which point there is a reduction in the velocity of the current. This results in rapid deposition of the sediment, which forms a body, for example at the mouth of a river where the river discharges into the sea or a lake. There is a characteristic coarsening upwards of sediments. A river provides the sediments to form a delta; but the shape and nature of a delta is controlled by a variety of factors including climate, water discharge, sediment load, rate of subsidence of the sea or lake floor, and the nature of the river-mouth processes (particularly tidal and wave energy). One classification of delta types, based on variations in transport patterns on the delta, subdivides deltas into three classes: (a) river-dominated, e.g. the Mississippi and Po; (b) wave-dominated, e.g. the Rhône and Nile; (c) tide-dominated, e.g. the Ganges and Mekong. See also GILBERT-TYPE DELTA.

del·ta¹ / ˈdeltə/ • n. 1. the fourth letter of the Greek alphabet (Δ, δ), transliterated as “d.” ∎  [as adj.] the fourth in a series of items, categories, etc. ∎  (Delta) [followed by Latin genitive] Astron. the fourth (usually fourth-brightest) star in a constellation: Delta Cephei. 2. a code word representing the letter D, used in radio communication. • symb. ∎  (δ) Math. variation of a variable or function. ∎  (Δ) Math. a finite increment. ∎  (δ) Astron. declination. del·ta² • n. a triangular tract of sediment deposited at the mouth of a river, typically where it diverges into several outlets. DERIVATIVES: del·ta·ic / delˈtāik/ adj.

delta [from triangular shape of the Nile delta, like the Greek letter delta ], a deposit of clay, silt, and sand formed at the mouth of a river where the stream loses velocity and drops part of its sediment load. No delta is formed if the coast is sinking or if there is an ocean or tidal current strong enough to prevent sediment deposition. Coarse particles settle first, with fine clays last and found at the outer regions of the delta. The three main varieties of deltas are the arcuate (the Nile), the bird's-foot (the Mississippi), and the cuspate (the Tiber). The Nile, Mississippi, Niger, Rhine, Danube, Kuban, Volga, Amu Darya, Indus, Ganges-Brahmaputra, Ayeyarwady, Tigris and Euphrates, and Huang He (Yellow) rivers are among those that have formed large deltas, many of which are fertile lands that support dense agricultural populations.

delta the fourth letter of the Greek alphabet (Δ, δ), transliterated as ‘d’.

The word is used for a triangular tract of sediment deposited at the mouth of a river, typically where it diverges into several outlets. Originally (in the mid 16th century) the term was applied specifically as the Delta (of the River Nile), from the shape of the Greek letter.
Delta Force the name of an elite American military force whose main responsibilities are rescue operations and special forces work.

Delta, Canada, Nigeria, USA 1. Nigeria: a state established in 1991 and so‐called because the delta of the River Niger acts as its eastern boundary.2. USA: there are six cities with this name, some so‐called because of their triangular shape and some because of river deltas.

delta Fan-shaped body of alluvium deposited at the mouth of a river. A delta is formed when a river deposits sediment as its speed decreases while it enters the sea. Most deltas are extremely fertile areas, but are subject to frequent flooding.

delta Used to indicate some period of time: for example, in ‘I will post again. The delta will be about two days.’ Derived from the mathematical use of the Greek delta symbol for a small quantity.

delta triangular tract of alluvial land at the mouth of a river, orig. of the Nile. XVI. Name of the fourth letter of the Greek alphabet. Δ, derived from Phoenician daleth (Δ).

delta •abetter, begetter, better, bettor, biretta, bruschetta, carburettor (US carburetor), debtor, feta, fetter, forgetter, getter, go-getter, Greta, Henrietta, letter, Loretta, mantelletta, operetta, petter, Quetta, setter, sinfonietta, sweater, upsetter, Valletta, vendetta, whetter •bisector, collector, connector, convector, corrector, defector, deflector, detector, director, ejector, elector, erector, hector, injector, inspector, nectar, objector, perfecter, projector, prospector, protector, rector, reflector, rejector, respecter, sector, selector, Spector, spectre (US specter), vector •belter, delta, helter-skelter, melter, pelta, Shelta, shelter, swelter, welter •pre-emptor, tempter •assenter, cementer, centre (US center), concentre (US concenter), dissenter, enter, eventer, fermenter (US fermentor), fomenter, frequenter, inventor, lamenter, magenta, placenta, polenta, precentor, presenter, preventer, renter, repenter, tenter, tormentor •inceptor, preceptor, receptor, sceptre (US scepter) •arrester, Avesta, Chester, contester, ester, Esther, fester, fiesta, Hester, investor, jester, Leicester, Lester, molester, Nestor, pester, polyester, protester, quester, semester, sequester, siesta, sou'wester, suggester, tester, trimester, vesta, zester •Webster • dexter • Leinster •Dorchester • Poindexter • newsletter •genuflector • implementer •experimenter • trendsetter •epicentre (US epicenter) •typesetter • jobcentre • photosetter •Cirencester • interceptor • Sylvester