「GREEN SAND」の共起表現(1語左で並び替え) - Weblio英語共起表現検索


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Weblio 辞書 > 英和辞典・和英辞典 > GREEN SANDの意味・解説 > GREEN SANDに関連した共起表現

「GREEN SAND」の共起表現一覧(1語左で並び替え)

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the town is Folly Hill or Faringdon Hill, a Greensand outcrop (at grid reference SU 298957).
ghts of way: Vanguard Way, Pilgrims' Way and Greensand Way.
in by cover sands with erratics of flint and Greensand chert.
stone including flint, chalk, limestone and greensand with the walls remaining almost at their ori
e discovered bones of birds in the Cambridge Greensand, and he also prepared a geological map of Ca
led attention to those also in the Cambridge Greensand and remarked that they might be of use in ag
d in the Upper Chalk Formation and Cambridge Greensand of the UK (up to the late Cenomanian age, 94
It was found in a phosphatic nodule in greensand deposits of Albian age.
Chert occurs as oval to irregular nodules in greensand, limestone, chalk, and dolostone formations
ll recovered from the Late Oligocene Kokoamu Greensand Formation (27-28 MYA) at Duntroon, New Zeala
es recovered from the Late Oligocene Kokoamu Greensand Formation (27-28 MYA) at Duntroon, New Zeala
The Wealden Group is overlain by the Lower Greensand and the Gault Formation, consisting of the G
The Lower Greensand Formation of Lower Cretaceous age, containin
Corallian limestone that is topped by Lower Greensand and Kimmeridge Clay.
se sandstone of the Folkestone Beds of Lower Greensand set among acidic heathland.
bove this corallian ridge, composed of Lower Greensand, occur at Badbury Hill, Faringdon (Folly Hil
it was the best accessible exposure to Lower Greensand and Gault in the Leighton Buzzard area.
ced important papers on the Cretaceous Lower Greensand Group.
er portions are the equivalents of the Lower Greensand and part of the Gault.
astal ravine dropping 140 feet through Lower Greensand rocks from clifftop farmland to Chale Bay.
ven to some fossil limb bones from the Lower Greensand (Lower Cretaceous) of Kent, England, was for
etween Farnham and Alton from the malmstone ( Greensand) hills or "Hangers" around Binsted.
ars in Jurassic/lower Cretaceous deposits of greensand, so-called after the coloration caused by gl
e of timber, located on the northern edge of Greensand Ridge.
t of use, follows the free draining ridge of greensand which lies north of the South Downs.
ands and chert beds-and then narrow bands of Greensand and sandstone.
Both commons lie on greensand and are covered with heathland.
ith a southerly aspect and a soil of loam on greensand readily suitable for cultivation.
e North Downs excluding the roughly parallel Greensand Ridge to the south.
e North Downs but is located on the parallel Greensand Ridge and does not consist of chalk.
riassic Keuper marl, overlain with permeable Greensand and clay-with-flints.
lk and the southern ridges are predominantly greensand.
The Sussex Greensand Way is a Roman road linking the London to Le
ide a road upon the line of the Roman Sussex Greensand Way.
case here, as Streat is built on the Sussex Greensand Way, and there is also a north-south Roman o
It stands on the Greensand Way.
hamlet is situated on the scarp slope of the Greensand Ridge, a high escarpment formed of Lower Gre
The village is located on the Greensand Ridge 9 miles (14.4 km) north of Ashford.
wn and begins to climb - this time up to the Greensand Ridge.
The junction between the Greensand and Keuper Marl forms a spring line.
ilway between Maidstone and Headcorn was the Greensand Ridge to the south of Maidstone.
ater issues from numerous springs within the Greensand producing a locally raised water table and s
r lies on the south-facing escarpment of the Greensand Ridge, which at this point forms St. Martha'
ish is located on the southward slope of the Greensand ridge, south of Maidstone on the A229 Hastin
n the valley between the North Downs and the Greensand ridge to the north east of Sevenoaks town.
which follows the Great Stour river, and the Greensand Way, from north to south, are both routed th
through the surrounding hills and along the greensand way.
s Back section of the North Downs and by the Greensand Ridge.
hich gives good access for walkers along the Greensand Ridge long distance footpath which passes ne
metres (771 ft)) is the highest point on the Greensand Ridge to the north of the Weald.
es of the North Downs (to the north) and the Greensand Ridge (to the south).
egins its course west of Oldbury Hill on the Greensand Ridge in the parish of Ightham and enters th
A Roman road, the Greensand Way, from north of Lewes passed north of the
ad begins a steady climb on the slope of the Greensand Ridge, and after reaching the top to the wes
After crossing the Greensand Ridge the road runs virtually straight from
mation and I. lydekkeri in the younger Upper Greensand.
lying ground is made of Gault Clay and Upper Greensand.
The hill is formed from upper greensand which is more resistant to erosion than the
A rotational slip in the Chalk, Upper Greensand and Gault has developed, exposing a section
ills where outcrops of both Cretaceous Upper Greensand and underlying Triassic Keuper Marls occur.
site shows rock exposures through the Upper Greensand and Chalk which contain fossil crustaceans w
The Upper Greensand of the North Downs is a thin bed of one or t
The Upper Greensand Formation, a whitish, limy sandstone, often
alaeontological zones in the Chalk and Upper Greensand of Britain were for the first time marked ou
rforated the bottom of a coffee can and used greensand to make his own water filter.
London Outer Orbital Path, North Downs Way, Greensand Way, London Countryway, Eden Valley Walk, Fo
pen space to walk and play, set in a wealden greensand vale, between the new Riverhead Infants Scho
                                                                                                    


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