W V Lewis
Dados Biográficos
| ID | 1686552 |
|---|---|
| NOME | W V Lewis |
| PRENOMES | W V |
| SOBRENOME | Lewis |
| ASSINATURA | LEWIS W V |
| VERIFICADO | Não |
| TOTAL DE OBRAS | 33 |
| TOTAL DE CITAÇÕES | 32 |
| TOTAL COMO AUTOR | 33 |
| TOTAL COMO EDITOR | 0 |
| PRIMEIRO ANO DE PUBLICAÇÃO | 1931 |
| ANO MAIS RECENTE DE PUBLICAÇÃO | 1961 |
| ÍNDICE H | 4 |
Geology
Glaciers
The Behaviour of Cirque Glaciers
Aspects of Agriculture and Settlement in Peru
The Earth beneath the Sea
Geophysical Investigations of the Commonwealth Trans-Antarctic Expedition
Coastal and Submarine Morphology
The Karstlands of Jamaica
The Evolution of the Relief of the Cam Valley
An East Coast Survey
The Coast of S. E. Iceland near Ingolfshofdi
The Problem of Tors
Pediment Land Forms in Little Namaqualand, South Africa
This account of erosional piedmont surfaces, or pediments, in part of Little Namaqualand, South Africa, is based on field trips in 1949 and 1950 aided by grants from the University of Cape Town Staff Research Fund. Little has hitherto been written of this region, but its wealth of land forms and the useful supporting evidence of air photographs render it a profitable field of study. The physical sub-regions of Little Namaqualand are shown below. …
The Range of Variation of the British Climate
Physical Geography
The Function of Meltwater in Cirque Formation
The Determination of Gradients on Enemy-Held Beaches
Physical Names for the Map of Britain
Wave-Trough Experiments on Beach Profiles
Miniature Spits and Embankments on a Lake-Shore, Iceland
A SERIES of miniature spits and embankments examined during a Cam? bridge expedition to Iceland in 1937 si ulated to a high degree their greater counterparts round the British coasts. It seems therefore that scale reductions of 10 or 100 to 1 do not materially affect the mechanism of spitbuilding. The lake occupied a mountain-girt hollow in the eastern foothills of Snaefell, East Iceland. It is shown in Fig. 1, taken from a plane-table survey mad…
Water Levels in Fowlmere and Other Breckland Meres
Past Sea-Levels at Dungeness
Past Sea-Levels at Dungeness
The Function of Meltwater in Cirque Formation
Snow-Patch Erosion in Iceland
SNOW-PATCH erosion seems to be very important under peri-glacial conditions, and yet, as Bow an J has noted, there has been little mention of it. The subject was dealt with briefly after the Cambridge Iceland Expedi? tion, 1932,2 and in order to amplify the field-work carried out on that occasion a second visit was arranged for the summer of 1937. The site chosen was Snaefell, a Late Glacial volcano 3 with subsidiary cones, a few miles distant fr…
Past Sea-Levels at Dungeness
Snow-Patch Erosion in Iceland
SNOW-PATCH erosion seems to be very important under peri-glacial conditions, and yet, as Bow an J has noted, there has been little mention of it. The subject was dealt with briefly after the Cambridge Iceland Expedi? tion, 1932,2 and in order to amplify the field-work carried out on that occasion a second visit was arranged for the summer of 1937. The site chosen was Snaefell, a Late Glacial volcano 3 with subsidiary cones, a few miles distant fr…
Coastal and Submarine Morphology
The Formation of Dungeness Foreland
The Effect of Wave Incidence on the Configuration of a Shingle Beach
The Cambridge Expedition to Vatnajokull, 1932
Pediment Land Forms in Little Namaqualand, South Africa
This account of erosional piedmont surfaces, or pediments, in part of Little Namaqualand, South Africa, is based on field trips in 1949 and 1950 aided by grants from the University of Cape Town Staff Research Fund. Little has hitherto been written of this region, but its wealth of land forms and the useful supporting evidence of air photographs render it a profitable field of study. The physical sub-regions of Little Namaqualand are shown below. …
Nivation, River Grading, and Shoreline Development in South-East Iceland
THE Cambridge Iceland Expedition 1932 (I) enabled the writer to examine both the coastal and inland topography of South-East Iceland. The problems arising out of this visit which are to be discussed in this paper comprise three independent aspects of geomorphology, but they are here grouped together because the observations were made in the same region. Incipient Corries.-The mountains of South-East Iceland present a wealth of features which seem…
Miniature Spits and Embankments on a Lake-Shore, Iceland
A SERIES of miniature spits and embankments examined during a Cam? bridge expedition to Iceland in 1937 si ulated to a high degree their greater counterparts round the British coasts. It seems therefore that scale reductions of 10 or 100 to 1 do not materially affect the mechanism of spitbuilding. The lake occupied a mountain-girt hollow in the eastern foothills of Snaefell, East Iceland. It is shown in Fig. 1, taken from a plane-table survey mad…
The Function of Meltwater in Cirque Formation
The Culbin Sands and Burghead Bay
The Effect of Wave Incidence on the Configuration of a Shingle Beach
The Effect of Wave Incidence on the Configuration of a Shingle Beach
The Formation of Dungeness Foreland
The Cambridge Expedition to Vatnajokull, 1932
The Cambridge Expedition to Vatnajokull, 1932
The Hagavatn Gorge
Nivation, River Grading, and Shoreline Development in South-East Iceland
THE Cambridge Iceland Expedition 1932 (I) enabled the writer to examine both the coastal and inland topography of South-East Iceland. The problems arising out of this visit which are to be discussed in this paper comprise three independent aspects of geomorphology, but they are here grouped together because the observations were made in the same region. Incipient Corries.-The mountains of South-East Iceland present a wealth of features which seem…
The Culbin Sands and Burghead Bay
Snow-Patch Erosion in Iceland
SNOW-PATCH erosion seems to be very important under peri-glacial conditions, and yet, as Bow an J has noted, there has been little mention of it. The subject was dealt with briefly after the Cambridge Iceland Expedi? tion, 1932,2 and in order to amplify the field-work carried out on that occasion a second visit was arranged for the summer of 1937. The site chosen was Snaefell, a Late Glacial volcano 3 with subsidiary cones, a few miles distant fr…
Past Sea-Levels at Dungeness
Past Sea-Levels at Dungeness
The Function of Meltwater in Cirque Formation
Water Levels in Fowlmere and Other Breckland Meres
Physical Names for the Map of Britain
Wave-Trough Experiments on Beach Profiles
Miniature Spits and Embankments on a Lake-Shore, Iceland
A SERIES of miniature spits and embankments examined during a Cam? bridge expedition to Iceland in 1937 si ulated to a high degree their greater counterparts round the British coasts. It seems therefore that scale reductions of 10 or 100 to 1 do not materially affect the mechanism of spitbuilding. The lake occupied a mountain-girt hollow in the eastern foothills of Snaefell, East Iceland. It is shown in Fig. 1, taken from a plane-table survey mad…
The Determination of Gradients on Enemy-Held Beaches
The Function of Meltwater in Cirque Formation
The Range of Variation of the British Climate
Physical Geography
The Problem of Tors
Pediment Land Forms in Little Namaqualand, South Africa
This account of erosional piedmont surfaces, or pediments, in part of Little Namaqualand, South Africa, is based on field trips in 1949 and 1950 aided by grants from the University of Cape Town Staff Research Fund. Little has hitherto been written of this region, but its wealth of land forms and the useful supporting evidence of air photographs render it a profitable field of study. The physical sub-regions of Little Namaqualand are shown below. …
An East Coast Survey
The Coast of S. E. Iceland near Ingolfshofdi
The Evolution of the Relief of the Cam Valley
Geography (27 obras) · Geology (23 obras) · Geology (23 obras) · Oceanography (8 obras) · Oceanography (8 obras) · Physical geography (8 obras) · Archaeology (6 obras) · Environmental Science (6 obras) · Coastal and Marine Dynamics (4 obras) · Cryospheric studies and observations (4 obras)