J N Jennings
Datos Biográficos
| ID | 741097 |
|---|---|
| NOMBRE | J N Jennings |
| NOMBRES | J N |
| APELLIDO | Jennings |
| FIRMA | JENNINGS J N |
| AFILIACIONES | Australian National University |
| VERIFICADO | No |
| TOTAL DE OBRAS | 44 |
| TOTAL DE CITAS | 62 |
| TOTAL COMO AUTOR | 44 |
| TOTAL COMO EDITOR | 0 |
| PRIMER AÑO DE PUBLICACIÓN | 1939 |
| AÑO MÁS RECIENTE DE PUBLICACIÓN | 1986 |
| ÍNDICE H | 4 |
Karst Geomorphology
Karst Geomorphology
Structure and landforms in Australia
Differential erosion over a long subaerial history has resulted in a wide range of Australian structural landforms, commonly emphasized under the dry prevailing climate. They include Appalachian relief on ancient orogenic structures, more compact or even circular landforms associated with astroblemes and igneous intrusions, and linear features
A map of karst cave areas in Australia
A dot map of karst cave areas in Australia is presented together with a similar one redrawn from the National Atlas of the United States of America. The limitations of the map are described. The geographical circumstances behind Australia's poverty in these resources and the risks to which they are exposed are outlined
Swirlholes and related bedrock river channel forms
Needle ice raked ground
Of Time and Place. Essays in Honour of O.H.K. Spate
This book of essays honours Professor O.H.K. Spate of The Australian National University. Occupying the second University Chair of Geography to be created in Australia, Oskar Spate built a Department in the Research School of Pacific Studies there. Later, after serving for five years as Director of that School, he moved to its Department of Pacific and South Asian History where, as a Visiting Fellow, he is writing a three- volume history of the P…
Further results from limestone tablet experiments at Cooleman Plain
Periglacial small sorted net
Genetic variety in a‐tents and related features
Further instances of A‐tents in unglaciated granite terrain do not require fresh explanation. Three cases in glaciated country in a variety of rocks demonstrate an origin through pressure release as a result of glacial erosion and ice retreat. A‐tents in limestone on the unglaciated Cooleman Plain, N.S.W., are attributed to solutional offloading, though residual compressive stresses were probably released. In some cases the amount of apparent exp…
Late Quaternary Climates of Australia and New Guinea
Between 60,000 and 40,000 B.P., northeastern Queensland, south New South Wales, and southeastern South Australia were drier than at present. From 40,000–30,000 B.P. a colder climate than at present is indicated from one New Guinea area. Dryness became even more accentuated in northeastern Queensland, whereas many lakes filled up in the southern mainland, probably because of increasing precipitation effectiveness there. Before the end of this peri…
Any Millenniums Today, Lady?‘ the Geomorphic Bandwaggon Parade
Karst
Australian Geography 1951–1971
Karst
Origin and Implications of the A‐tent, a Minor Granite Landform
Karst spring
Ingrown meander and Meander Cave
(1970). Ingrown meander and Meander Cave. Australian Geographer: Vol. 11, No. 4, pp. 401-402
Periglacial blockstream
Landform Studies from Australia and New Guinea
A revised map of the desert dunes op Australia
Contributions to the Study of Karst
Landform Studies from Australia and New Guinea
Cliff‐top Dunes
Two maps of rainfall intensity in Australia
(1967). Two maps of rainfall intensity in Australia. Australian Geographer: Vol. 10, No. 4, pp. 256-262
On the Orientation of Parabolic or U-Dunes
Any Millenniums Today, Lady?‘ the Geomorphic Bandwaggon Parade
Landform Studies from Australia and New Guinea
The legacy of an ice gap
Australian Geography 1951–1971
Landform Studies from Australia and New Guinea
The Origin of the Broads
IN an R.G.S. Research Memoir just published,1 a theory attributing the origi of most of the Norfolk Broads to certain natural ph siographical processes was advanced. Briefly, it postulated that the formation of the broads could be explained in terms of a geologically very recent marine transgression of the Norfolk river valleys, during which a thick wedge of estuarine clay was laid down over the earlier valley peats; the broads themselves were th…
Origin and Implications of the A‐tent, a Minor Granite Landform
Cliff‐top Dunes
Needle ice raked ground
Periglacial small sorted net
Periglacial blockstream
Contributions to the Study of Karst
Two maps of rainfall intensity in Australia
(1967). Two maps of rainfall intensity in Australia. Australian Geographer: Vol. 10, No. 4, pp. 256-262
Swirlholes and related bedrock river channel forms
Genetic variety in a‐tents and related features
Further instances of A‐tents in unglaciated granite terrain do not require fresh explanation. Three cases in glaciated country in a variety of rocks demonstrate an origin through pressure release as a result of glacial erosion and ice retreat. A‐tents in limestone on the unglaciated Cooleman Plain, N.S.W., are attributed to solutional offloading, though residual compressive stresses were probably released. In some cases the amount of apparent exp…
Karst
Karst
A revised map of the desert dunes op Australia
Solution doline and subjacent karst doline
(1966). Solution doline and subjacent karst doline. Australian Geographer: Vol. 10, No. 2, pp. 132-133
Limestone Ranges of the Fitzroy Basin, Western Australia
The Norfolk Broads
Coastal Dune Lakes as Exemplified from King Island, Tasmania
IT is useful to define types of land forms and to classify them genetically, for we thus provide ourselves with a convenient f amework f concepts against which the geomorphological details of particular regions can be matched and which brings out the relationship and comparative importance of the various operative factors. Never? theless it is true that simple types which fall unequivocally into the single categories of the textbooks are rarities…
The influence of wave action on coastal outline in plan
(1955). The influence of wave action on coastal outline in plan. Australian Geographer: Vol. 6, No. 4, pp. 36-44
The Imperial College Expedition to Jan Mayen Island
The Imperial College Expedition to Jan Mayen Island
The Origin of the Broads
IN an R.G.S. Research Memoir just published,1 a theory attributing the origi of most of the Norfolk Broads to certain natural ph siographical processes was advanced. Briefly, it postulated that the formation of the broads could be explained in terms of a geologically very recent marine transgression of the Norfolk river valleys, during which a thick wedge of estuarine clay was laid down over the earlier valley peats; the broads themselves were th…
The influence of wave action on coastal outline in plan
(1955). The influence of wave action on coastal outline in plan. Australian Geographer: Vol. 6, No. 4, pp. 36-44
The Problem of Tors
The legacy of an ice gap
On the Orientation of Parabolic or U-Dunes
Coastal Dune Lakes as Exemplified from King Island, Tasmania
IT is useful to define types of land forms and to classify them genetically, for we thus provide ourselves with a convenient f amework f concepts against which the geomorphological details of particular regions can be matched and which brings out the relationship and comparative importance of the various operative factors. Never? theless it is true that simple types which fall unequivocally into the single categories of the textbooks are rarities…
The Norfolk Broads
Further Remarks on the Tasmanian Muttonbird
as Schweinfurth (1961) has demonstrated very well in this journal. Perhaps the geographical facet of the natural history of these birds which has most signi ficance is that of their migrations (fig. 1). This is best documented in the case of the Bass Strait muttonbird or Short-tailed Shearwater, Puffinus tenuirostris (Ser venty, 1953 & 1956; Marshall & Serventy, 1956). Preceded by their parents, the fledglings in their hunger leave their rookerie…
Collapse doline
Floodplain Lakes in the Ka Valley, Australian New Guinea
A Preliminary Report on the Karst Morphology of the Nullarbor Plains
Limestone Ranges of the Fitzroy Basin, Western Australia
Solution doline and subjacent karst doline
(1966). Solution doline and subjacent karst doline. Australian Geographer: Vol. 10, No. 2, pp. 132-133
Coastal Landforms
Cliff‐top Dunes
Two maps of rainfall intensity in Australia
(1967). Two maps of rainfall intensity in Australia. Australian Geographer: Vol. 10, No. 4, pp. 256-262
Semi‐blind valley
Blind valley
Karst cave
A revised map of the desert dunes op Australia
Contributions to the Study of Karst
Landform Studies from Australia and New Guinea
Periglacial blockstream
Geography (37 obras) · Geology (33 obras) · Geology (32 obras) · Archaeology (18 obras) · Paleontology (12 obras) · Karst (11 obras) · Karst Systems and Hydrogeology (11 obras) · Paleontology (11 obras) · Geology and Paleoclimatology Research (10 obras) · Physical geography (10 obras)