Matches in SemOpenAlex for { <https://semopenalex.org/work/W2156678081> ?p ?o ?g. }
Showing items 1 to 62 of
62
with 100 items per page.
- W2156678081 endingPage "87" @default.
- W2156678081 startingPage "84" @default.
- W2156678081 abstract "The structure of the Lower Drift, and the limited area to which it is confined, conspire to show that this country first encountered, and for a long period sustained, the glacial conditions while principally in the state of land; for not only do the limited superficial extent of the formation and its rapid attenuation in all directions, from its great development on the Cromer coast, necessitate an inference that only a small part of England was under water at the time of the deposition of the Lower Drift, but the great masses of chalk and chalky debris that were carried into the marine sediment require us to admit the presence, near at hand, of some terrestrial chalk-area from which these masses were detached; and I imagine that it does not require any illustration here to satisfy geologists of the fact, so obvious from the appearance of the Cromer Cliffs, that much of the chalk of Norfolk was, at the time these masses were imbedded, occupied by a great glacier, from whose seaward termination they were carried and dropped into the marine sediment. In such a state of things we should naturally look for some evidences inland of the terrestrial glaciation which this structure involves. The beds in section on the Cromer Coast, forming the Lower Drift, although of so great a thickness there, alter, as I have elsewhere shown, both in their appearance and thickness inland. South-eastwards, in the direction of Norwich and the Yare Valley, the Lower Drift, or" @default.
- W2156678081 created "2016-06-24" @default.
- W2156678081 creator A5017963059 @default.
- W2156678081 date "1867-02-01" @default.
- W2156678081 modified "2023-09-25" @default.
- W2156678081 title "On a Section at Litcham affording Evidence of Land-Glaciation during the earlier part of the Glacial Period in England" @default.
- W2156678081 doi "https://doi.org/10.1144/gsl.jgs.1867.023.01-02.18" @default.
- W2156678081 hasPublicationYear "1867" @default.
- W2156678081 type Work @default.
- W2156678081 sameAs 2156678081 @default.
- W2156678081 citedByCount "0" @default.
- W2156678081 crossrefType "journal-article" @default.
- W2156678081 hasAuthorship W2156678081A5017963059 @default.
- W2156678081 hasBestOaLocation W21566780812 @default.
- W2156678081 hasConcept C100970517 @default.
- W2156678081 hasConcept C107038049 @default.
- W2156678081 hasConcept C111919701 @default.
- W2156678081 hasConcept C127313418 @default.
- W2156678081 hasConcept C142362112 @default.
- W2156678081 hasConcept C151730666 @default.
- W2156678081 hasConcept C15739521 @default.
- W2156678081 hasConcept C166957645 @default.
- W2156678081 hasConcept C205649164 @default.
- W2156678081 hasConcept C2780129039 @default.
- W2156678081 hasConcept C2781291010 @default.
- W2156678081 hasConcept C41008148 @default.
- W2156678081 hasConcept C95457728 @default.
- W2156678081 hasConceptScore W2156678081C100970517 @default.
- W2156678081 hasConceptScore W2156678081C107038049 @default.
- W2156678081 hasConceptScore W2156678081C111919701 @default.
- W2156678081 hasConceptScore W2156678081C127313418 @default.
- W2156678081 hasConceptScore W2156678081C142362112 @default.
- W2156678081 hasConceptScore W2156678081C151730666 @default.
- W2156678081 hasConceptScore W2156678081C15739521 @default.
- W2156678081 hasConceptScore W2156678081C166957645 @default.
- W2156678081 hasConceptScore W2156678081C205649164 @default.
- W2156678081 hasConceptScore W2156678081C2780129039 @default.
- W2156678081 hasConceptScore W2156678081C2781291010 @default.
- W2156678081 hasConceptScore W2156678081C41008148 @default.
- W2156678081 hasConceptScore W2156678081C95457728 @default.
- W2156678081 hasIssue "1-2" @default.
- W2156678081 hasLocation W21566780811 @default.
- W2156678081 hasLocation W21566780812 @default.
- W2156678081 hasOpenAccess W2156678081 @default.
- W2156678081 hasPrimaryLocation W21566780811 @default.
- W2156678081 hasRelatedWork W1999743581 @default.
- W2156678081 hasRelatedWork W2064705856 @default.
- W2156678081 hasRelatedWork W2079193679 @default.
- W2156678081 hasRelatedWork W2104121056 @default.
- W2156678081 hasRelatedWork W2333540133 @default.
- W2156678081 hasRelatedWork W2414870198 @default.
- W2156678081 hasRelatedWork W2527095771 @default.
- W2156678081 hasRelatedWork W2911869918 @default.
- W2156678081 hasRelatedWork W3143944402 @default.
- W2156678081 hasRelatedWork W4293280157 @default.
- W2156678081 hasVolume "23" @default.
- W2156678081 isParatext "false" @default.
- W2156678081 isRetracted "false" @default.
- W2156678081 magId "2156678081" @default.
- W2156678081 workType "article" @default.