「gravels.」の共起表現(1語右で並び替え) - Weblio英語共起表現検索


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

「gravels.」の共起表現一覧(1語右で並び替え)

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cluding interglacial fluvial sands and marine gravels and cold-stage fluvial gravels.
"Some gravels and gravel-pits in Hampshire and Dorset", Pro
is is a site recognized for its fossiliferous gravels and sediments which are likely to have origin
embankment was partly composed of well graded gravels, and thus a very high modulus of embankmnet d
s they mixed with other clay minerals, sands, gravels, and vegetation before settling in low-lying
ns; the Cretaceous Dakota Sandstone; Tertiary gravels and basalts, and Quaternary landslide, eolian
tion when the valley was blocked by sands and gravels around Cadeby and Stoke Golding.
gments were found in the lower middle terrace gravels at a depth of almost 8 metres beneath the sur
The Pleistocene deposits include gravels, boulder-beds, sands, and till, overlain by c
ue was the use of blankets to filter sand and gravels, catching fine gold in the fabric's weave, th
cient Britons extracted alluvial tin from the gravels deposited by the river Teign.
ra planeri) measure from 12-14cm and spawn in gravels during the springtime.
bonate in the water here comes from limestone gravels eroded from the nearby mountains and deposite
Gravels exposed at Langport Railway Cutting show scou
plateau-deposits' which include ‘cannon-shot' gravels, fine sandy gravels and silty gravels with a
ornaments etc. Smaller fragments are used for gravels, for ornamental pathways.
A co-worker with Marr on Cambridgeshire gravels has successfully applied the Abbe Breuil's So
Some gravels have been found but for the most part, these
and pebbles with islands of sand and rounded gravels in midstream in the middle and lower tracts.
exposed localities for coldstage Pleistocene gravels in south Somerset and more particularly becau
ying glacial drift of boulder clay, sands and gravels, is the narrowest and deepest, particularly b
ia hydraulic mining exploited primarily river gravels, it was one form of placer mining, that is, w
the Brickearth overlies certain River Terrace Gravels, it has been reclassified on more recent maps
y are similar to those of Pauillac, with deep gravels lying on a hard sandstone base.
s a sequence of fluvial (or possibly glacial) gravels, marine intertidal silts and marine subtidal.
Rivers finds palaeolithic flints in concreted gravels of the Nile terraces near Thebes.
The Tertiary Gravels of the Sierra Nevada of California (USGS Prof
ly it is likely that alluvial deposits in the gravels of streams were exploited but later undergrou
The terrace gravels of the Loddon valley have been extracted in a
handaxe is a quartzite hand axe found in the gravels of the valley of the River Rea in the Saltley
moss agate is an agate found in the alluvial gravels of the Yellowstone River and its tributaries
rmission by the Duke of Sutherland to pan the gravels of the Helmsdale River and he prospected all
ith the discovery of placer gold in sands and gravels of streambeds, where the gold had eroded from
ith topaz and chrysoberyl in the gold-bearing gravels of the Sanarka.
extraordinarily infertile lateritic sands and gravels of Cape York proper, is quite densely populat
st; geologists can see exposures of the March gravels on the east side of the reserve.
It is found in granite and sandstone gravels on the slopes of the southern Sierra Nevada a
t Bourne sections have shown highly weathered gravels overlain by sandy silts and clay loams, the h
Park, the site is based on glacial sands and gravels overlying sandstone from the Late Triassic pe
of the Thames has gradually altered, exposing gravels that were initially colonised by grasses and
ibution flowing through sub-surface rocks and gravels that underlie the river and its floodplain (c
Gravels washed down from surrounding schist hills nat
non-resistant Eocene and Oligocene clays and gravels which are protected from sea erosion by the I
ick sequence of Pleistocene-aged cryoturbated gravels which exhibit scour-and-fill structures in th
                                                                                                    


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