Synoniemen & Anagrammen | Engels woord SILT


SILT

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Aantal letters

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Is palindroom

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IL
LT
SI
SIL

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ILS
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Voorbeelden van het gebruik van SILT in een zin

  • Established as a borough in Lancashire in 1207, Liverpool became a significant town in the late 17th century, when the port at nearby Chester began to silt up.
  • However, the Blue Nile is the source of most of the water of the Nile downstream, containing 80% of the water and silt.
  • An aquifer is an underground layer of water-bearing material, consisting of permeable or fractured rock, or of unconsolidated materials (gravel, sand, or silt).
  • For example, sand and silt can be carried in suspension in river water and on reaching the sea bed deposited by sedimentation; if buried, they may eventually become sandstone and siltstone (sedimentary rocks) through lithification.
  • The plain is watered by the three great rivers, the Cydnus (Tarsus Çay Berdan River), the Sarus (Seyhan), and the Pyramus (Ceyhan River), each of which brings down much silt from the deforested interior and which fed extensive wetlands.
  • The sea is largely affected by the inflow of the Don, Kuban, and other rivers, which bring sand, silt, and shells, which in turn form numerous bays, limans, and narrow spits.
  • Although the county includes the relatively liberal cities of Carbondale and Glenwood Springs, this is somewhat outweighed by the nearby towns of Rifle, Silt, Parachute, and Battlement Mesa.
  • He was represented as the Nile River, the annual flooding of which deposited the fertile silt that enabled abundant harvests.
  • The flood deposited rich silt (fertile soil) on the river's banks, allowing the Egyptians to grow crops.
  • Since the annual flooding of the Nile brought with it silt and clay, and its water brought life to its surroundings, he eventually became known as the creator of human bodies and the life force kꜣ ("ka").
  • Point Pelee is the southernmost point of mainland Canada, and is located on a foundation of glacial sand, silt and gravel that bites into Lake Erie.
  • Loams and silt loams of the Baden, Tallapoosa and Fruithurst series are common on the northern outskirts.
  • The results were widespread soil liquefaction and a change in geography that produced "sunken lands", which were sandy berms of silt and sediment disturbed by the earthquakes.
  • Man-made ecologic damage eventually combined with a series of fires and floods, as well as an earthquake, destroyed the town and filled the Slough with silt during the 1860s, to ruin Pacheco's growing prosperity just as similar ones had done to the great classic ports of Ephesus and Troy.
  • Cultivated land north of the residential area lies on poorly drained loam, silt loam or fine sandy loam.
  • Lake Lorraine was originally a fresh-water body, but at some point in the 1990s the narrow sandbar that separated it from the Choctawhatchee Bay was breached and the former drainage channel to the tip of Black's Point became blocked by silt.
  • In recent years, due to drought, the lake had dried up; the town irrigation committee used this low water level to make improvements including dredging a large amount of silt buildup and reinforcing the dam, allowing water to be used more efficiently.
  • The soils are mostly brown silt loams and loams with slight to moderate acidity in surface layers (subsoils may be somewhat alkaline); their drainage varies.
  • Soils at Goldston are dominantly yellowish brown, moderately well drained to somewhat poorly drained silt loams of the Cid or Lignum soil series.
  • In the 1950s, the Army Corps of Engineers dredged the Schuylkill River to remove coal silt from upriver.
  • In 1896, an artesian well was drilled in Keller; the Double Springs filled with silt over time and eventually were plugged and lost until rediscovery in 1984.
  • Most of the city is underlain by smectite-rich clay which is locally capped by silt or fine sand; the high shrink-swell potential associated with smectite creates major challenges to urban infrastructure.
  • The soil is mostly Colby silt loam, weathered from the drift left by a glacier so long ago that erosion has mostly levelled it.
  • Marshall's soil is a patchwork of Almena, Auburndale and Spencer silt loams left by the last glacier, with peat soil accumulated in the low places.
  • The Karun, a tributary which joins the waterway from the Iranian side, deposits large amounts of silt into the river; this necessitates continuous dredging to keep it navigable.



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