「clay s」の共起表現一覧(1語右で並び替え)
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Clays and shales (which are composed predominantly o | |
ium this is often the Aalter Formation (marine | clays and sands). |
he Kleiner Deister are characterised by marls, | clays and limestones. |
The wide part of the cove is where the weak | clays and greensands have been eroded. |
he sea has made its way through to the Wealdon | clays and begun eroding them. |
descendant of a Virginia family related to the | Clays and Adamses. |
This appearance results from | clays and silts suspended in its waters. |
It grows in sandy soils, red | clays, and old fields to the borders of swamps, stre |
iver Itchen, and as such the land is primarily | clays and shingles. |
or mudstone which contains variable amounts of | clays and aragonite. |
However, fine grained materials like | clays and silts had helped prevent vertical migratio |
ales, greenish and gray sandstones, bentonitic | clays and thin bands of ironstone. |
eral areas are mostly of softer sandstones and | clays and these form the gentler rolling landscapeof |
logy is dominated by metal oxides, hydroxides, | clays and carbonates after the original sulfide mine |
relatively non-resistant Eocene and Oligocene | clays and gravels which are protected from sea erosi |
n continued, with the Reading and London Beds ( | clays and sandstones) being deposited during the Ter |
A succession of | clays and sands was deposited into the subsiding bas |
Most schists have been derived from | clays and muds which have passed through a series of |
bridge marls, freshwater, estuarine and marine | clays and marls (70-120 ft.) rest upon the Bembridge |
te chalky soils and oak forests tend to prefer | clays and mountain, heath, cliff, estuarine or coast |
which is considerably more resistant than the | clays and sands, but less resistant than the limesto |
ene Reading beds consist of mottled and yellow | clays and sands, the latter are frequently hardened |
ire Basin, with chalk in the north overlain by | clays and sands of the Lambeth Group to the south. |
one, which lie between layers of softer marine | clays and mudstone, laid down in repeated marine ing |
he Lias Tablelands and is underlain by Rhaetic | clays and, lower down the slope Keuper Red Marl. |
Places that contain | clays and/or other hydrated minerals would be good p |
and 66% NaCl with the balance being insoluble | clays, anhydrite and in some locations carnallite. |
Ball | clays are kaolinitic sedimentary clays, that commonl |
Like stone, some | clays are effectively untreatable unless broken up. |
The | clays are yellowish gray to light olive gray in colo |
Ball | clays are relatively scarce deposits due to the comb |
shallow, wave-agitated waters, while silt and | clays are deposited in quieter, deep water far offsh |
The silica-enrichment of the limestones and | clays at Wurt Pit (known as the "Harptree Beds", of |
ollieries at Crookes Meadow, Grundy Common and | Clays before 1770. |
imen of Dollodon, IRSNB 1551 from Sainte-Barbe | Clays, Belgium, was originally assigned to Iguanodon |
e soils of Moulton are predominantly sands and | clays, but small quantities of ironstone may be foun |
amorphic recrystallization to form marble, and | clays can recrystallize to muscovite mica. |
Many minerals, such as | clays, chlorides, sulfates, and iron oxides, have be |
ing the area's land surface are unconsolidated | clays, clay shales, and poorly-cemented sands extend |
ted with inlaid patterns of different-coloured | clays, Craven Dunnill encaustic tiles were extensive |
-depositing environment with sands, silts, and | clays creating the peninsula and making way for flor |
ese sediments consist of a series of sands and | clays deposited on decaying organic matter that, ove |
s, gave her the opportunity to explore colored | clays, develop new glazes, and experiment with raw m |
rillonites expand considerably more than other | clays due to water penetrating the interlayer molecu |
land for crops and livestock; the presence of | clays for pottery in the muddy earth surrounding the |
All of these units are marine sands and | clays from the Ypresian (55.8 - 48.6 million years a |
ost of the Tweed-Saint Valley were filled with | clays from Lake Harrison, which filled much of Leice |
n 2006, Uruguay produced mostly agate, cement, | clays, gravel, gold, iron ore, marble, and steel. |
Ochre | clays have been used medicinally from the earliest t |
landmark now called 'Burletts' and located on | Clays Hill. |
The ceramic use of ball | clays in Britain dates back to at least the Roman er |
work identified coal on Vancouver Island, fire | clays in Pennsylvania, the Caribbean, South America, |
Ronjan Sodhi shot a perfect 50 hits out of 50 | clays in the final and set a new world record with a |
s of rock incorporated into the sandstones and | clays), indicating the presence of a river system ex |
ndstone, as well as a certain amount of silts, | clays, ironstone and limestone. |
ay on structures built in areas with expansive | clays is a major challenge in geotechnical engineeri |
of a mixture of sandstone ridges and low lying | clays known as the Western Weald. |
existed on the other side of the river at the | Clays Lane Estate and in Deptford the Deptford Housi |
The | Clays Lane Co-operative appealed against the order, |
The | Clays Lane estate consisted of an enclave of 57 shar |
Mrs albert finney lived in | clays lane stapenhil and was a bakers assistant and |
e is much 19th- and 20th-century housing along | Clays Lane, north of the village, and along Burton R |
Clays later became Costa Rica's first female diploma | |
grade titanium dioxide in Asia,English Indian | Clays Limited, Kerala Automobiles Ltd, the leading p |
This formed the new company English China | Clays, Lovering, Pochin, & Co. (ECLP): in 1956 the L |
was subsequently taken over by English Indian | Clays Ltd. in the year 2002. |
English Indian | Clays Ltd., a Company incorporated in India, was par |
l & financial collaboration with English China | Clays Ltd., U.K, the pioneer and the then world lead |
The weakness zone generated by the Keuper's | clays made easier its erosion compared with other sa |
Clays may be brought up with the salt, turning it da | |
es are the Jessamine County line to the south, | Clays Mill Road to the east, Twain Ridge Road to the |
ago) in the Bristol Avon Gorge as a result of | clays mingling with rock debris scree which had form |
Similar to many other | clays, montmorillonite swells with the addition of w |
The older Shelly | clays of the Woolwich Beds at Newhaven; with gypsum |
d high durability are found in the constituent | clays of the ochre mined at Wilgie Mia. |
llage this is overlain by Palaeocene sands and | clays of the Lambeth Group. |
This soap found its way to the | clays of a nearby stream, where local people found t |
It belongs to the Oxfordian and Kimmeridgian | clays of the Jurassic and can grow to a diameter in |
cies, A. prisca, was published from the London | Clays of England eight years earlier in 1926 by Chan |
ble Bed horizon followed by the sandstones and | clays of the Wadhurst Clay Formation interpreted as |
by J. M. W. Turner, and two paintings by P. J. | Clays of Brussels. |
The soils in the area include both | clays of the Allerton and Wentloog Series and peat s |
and (big voids) but bonding is poor while fine | clays offer better bonding but fewer gaps for the em |
finding hydrated minerals such as sulfates and | clays on Mars because they are usually formed in the |
London to such a degree that detecting certain | clays on a person's shoe would give away a locale. |
indicative of phyllosilicate minerals such as | clays or mica. |
Tight, impermeable subsurface lithology (tight | clays or other fine-grained material) make it diffic |
Localised | clays outcrop and the area was formerly known for it |
ed engobes (thin coatings of different colored | clays over the redware clay body we were using) inst |
Soils are predominantly alluvial | clays overlying Altcar series peats. |
rking today, having been sold to English China | Clays plc in 1964. |
English China | Clays plc or ECC was a mining company involved in th |
Clays Prairie | |
a floodplain where deposits of fine silts and | clays settle after a flood. |
AlO(OH)), and diaspore (α-AlO(OH)), as well as | clays, silt, and iron oxides and hydroxides. |
It occurs in lacustrine sediments with | clays, silts and arkosic sand often in varved sulfid |
These sands overlie shallow marine and coastal | clays, silts, and sands of the Cook Mountain Formati |
Clays soon took his place among the most famous Belg | |
others, such as John Mixtow, William Aleyn and | Clays Stephen, acted under virtual immunity from the |
2,000 and above are measured in loam soils and | clays, such as bentonite. |
s the assemblage is calcite, dolomite, quartz, | clays, talc, and muscovite. |
re of the water easily dislodges the cementing | clays that are in the cracks and void spaces of the |
y chondrites contain hydrous minerals, such as | clays, that formed when the water interacted with th |
ide are, to a considerable extent, simply soil | clays that have been formed in the pedosphere and er |
ck Rectory, Ockendon, South Chafford, Stifford | Clays, Tilbury Riverside and Thurrock Park, Tilbury |
ottery industries barium carbonate is added to | clays to precipitate soluble salts (calcium and magn |
wide range of well-drained soils, from sand to | clays to even white limestone areas. |
d the silt and sand which (together with older | clays) underlie the island's soil. |
ries in Malaga, and scientific analysis of the | clays used. |
Ball | clays usually contain three dominant minerals: from |
Clays was born on June 3, 1906 in Antwerp, Belgium t | |
Clays was a member of several Academies, Belgian and | |
Speeton Beds, in English geology, a series of | clays well exposed at Speeton, near Filey on the Yor |
This at first produces | clays which later also break down to form silica. |
and became suitable to mix with various other | clays which made them more plastic. |
vil's Punchbowl and a series of limestones and | clays which have been impregnated by silica at Wurt |
Co., Martyn Brothers and North Cornwall China | Clays, who joined together to form English China Cla |
made of stratified sandstones, siltstones and | clays, with deposits of anthracite in places. |
s made up of a series of sands and interbedded | clays, with four distinct bands of ironstone nodules |
own, crimson and every intermediate shade) and | clays with layers of lignite and ferruginous sandsto |
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