「GREEN SAND」の共起表現一覧(2語右で並び替え)
該当件数 : 50件
hamlet is situated on the scarp slope of the | Greensand Ridge, a high escarpment formed of Lower Gre |
ater issues from numerous springs within the | Greensand producing a locally raised water table and s |
The Upper | Greensand Formation, a whitish, limy sandstone, often |
ars in Jurassic/lower Cretaceous deposits of | greensand, so-called after the coloration caused by gl |
se sandstone of the Folkestone Beds of Lower | Greensand set among acidic heathland. |
e North Downs but is located on the parallel | Greensand Ridge and does not consist of chalk. |
ad begins a steady climb on the slope of the | Greensand Ridge, and after reaching the top to the wes |
case here, as Streat is built on the Sussex | Greensand Way, and there is also a north-south Roman o |
Both commons lie on | greensand and are covered with heathland. |
bove this corallian ridge, composed of Lower | Greensand, occur at Badbury Hill, Faringdon (Folly Hil |
pen space to walk and play, set in a wealden | greensand vale, between the new Riverhead Infants Scho |
alaeontological zones in the Chalk and Upper | Greensand of Britain were for the first time marked ou |
site shows rock exposures through the Upper | Greensand and Chalk which contain fossil crustaceans w |
Chert occurs as oval to irregular nodules in | greensand, limestone, chalk, and dolostone formations |
riassic Keuper marl, overlain with permeable | Greensand and clay-with-flints. |
ven to some fossil limb bones from the Lower | Greensand (Lower Cretaceous) of Kent, England, was for |
which follows the Great Stour river, and the | Greensand Way, from north to south, are both routed th |
astal ravine dropping 140 feet through Lower | Greensand rocks from clifftop farmland to Chale Bay. |
A Roman road, the | Greensand Way, from north of Lewes passed north of the |
it was the best accessible exposure to Lower | Greensand and Gault in the Leighton Buzzard area. |
A rotational slip in the Chalk, Upper | Greensand and Gault has developed, exposing a section |
e discovered bones of birds in the Cambridge | Greensand, and he also prepared a geological map of Ca |
egins its course west of Oldbury Hill on the | Greensand Ridge in the parish of Ightham and enters th |
The hill is formed from upper | greensand which is more resistant to erosion than the |
The Sussex | Greensand Way is a Roman road linking the London to Le |
The junction between the | Greensand and Keuper Marl forms a spring line. |
Corallian limestone that is topped by Lower | Greensand and Kimmeridge Clay. |
t of use, follows the free draining ridge of | greensand which lies north of the South Downs. |
London Outer Orbital Path, North Downs Way, | Greensand Way, London Countryway, Eden Valley Walk, Fo |
hich gives good access for walkers along the | Greensand Ridge long distance footpath which passes ne |
rforated the bottom of a coffee can and used | greensand to make his own water filter. |
The Lower | Greensand Formation of Lower Cretaceous age, containin |
It was found in a phosphatic nodule in | greensand deposits of Albian age. |
etween Farnham and Alton from the malmstone ( | Greensand) hills or "Hangers" around Binsted. |
er portions are the equivalents of the Lower | Greensand and part of the Gault. |
led attention to those also in the Cambridge | Greensand and remarked that they might be of use in ag |
ands and chert beds-and then narrow bands of | Greensand and sandstone. |
ish is located on the southward slope of the | Greensand ridge, south of Maidstone on the A229 Hastin |
ith a southerly aspect and a soil of loam on | greensand readily suitable for cultivation. |
The Wealden Group is overlain by the Lower | Greensand and the Gault Formation, consisting of the G |
stone including flint, chalk, limestone and | greensand with the walls remaining almost at their ori |
The Upper | Greensand of the North Downs is a thin bed of one or t |
d in the Upper Chalk Formation and Cambridge | Greensand of the UK (up to the late Cenomanian age, 94 |
After crossing the | Greensand Ridge the road runs virtually straight from |
ilway between Maidstone and Headcorn was the | Greensand Ridge to the south of Maidstone. |
e North Downs excluding the roughly parallel | Greensand Ridge to the south. |
n the valley between the North Downs and the | Greensand ridge to the north east of Sevenoaks town. |
metres (771 ft)) is the highest point on the | Greensand Ridge to the north of the Weald. |
ills where outcrops of both Cretaceous Upper | Greensand and underlying Triassic Keuper Marls occur. |
r lies on the south-facing escarpment of the | Greensand Ridge, which at this point forms St. Martha' |
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