「GREEN SAND」の共起表現(2語左で並び替え)

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共起表現

「GREEN SAND」の共起表現一覧(2語左で並び替え)

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

共起表現

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