作者: 我沒有命令 時間: 2025-3-21 21:48
Hartlegierungen und Hartverbundwerkstoffenother area, providing often valuable clues as the the cause of differences in dimensions. In this contribution some examples of morphometric analysis on glacial geomorphology will be examined to illustrate the value of this method of study.作者: 侵略者 時間: 2025-3-22 00:46
Die Ursachen: Angebot oder Nachfrage?,in continental shelf and outwash-type sands, which are believed to have been partly in the form of permafrosted sandurs. Extraordinarily well-preserved sand volcanoes, sandstone dikes and plugs, kettles, eskers, parallel beach ridges, possible pingos and permafrost fracture fillings are described and illustrated.作者: llibretto 時間: 2025-3-22 06:47 作者: 改變 時間: 2025-3-22 12:15
Glacial Grooves and Periglacial Features in the Saharan Ordovicianin continental shelf and outwash-type sands, which are believed to have been partly in the form of permafrosted sandurs. Extraordinarily well-preserved sand volcanoes, sandstone dikes and plugs, kettles, eskers, parallel beach ridges, possible pingos and permafrost fracture fillings are described and illustrated.作者: 共同時代 時間: 2025-3-22 16:25
History of Glacial Lake Wawarsing, Southeast New Yorkeliminary review. In personal correspondence dated June 25, 1935, Professor MacClintock especially praises the concept and evidence which Dr. Heroy marshalled to document the stagnation theory for landform development in the study region.作者: 共同時代 時間: 2025-3-22 19:18 作者: 肥料 時間: 2025-3-23 00:36 作者: LURE 時間: 2025-3-23 05:21 作者: antidepressant 時間: 2025-3-23 08:07
Dialysis Cultures in Integrated Aquacultureipated growth by land use regulation. The responsibility for achieving these objectives rests with the residents of towns-the fundamental units of rural government. There is little doubt that planning, zoning ordinance adoption and code enforcement, with the attendant problems, constitute for towns a stiff test of the concept of home rule.作者: 避開 時間: 2025-3-23 13:06 作者: MARS 時間: 2025-3-23 16:03
Buried Glacial Geomorphologynge, at places markedly, and influence the economic, environmental, and engineering parameters. The interpretation of the buried surfaces — unconformities — is essential to determine the history of that part of the Pleistocene represented not only by the deposits, but also by the buried geomorphology of each.作者: exhilaration 時間: 2025-3-23 20:05
Conference proceedings 1982 different avenues for expression of scientific ideas, but the knowledge and publication explosion creates hardships for those who attempt to keep in tune with their specialties. It is not our purpose to add an unnecessary burden to this verbage increase. Instead we feel there comes a time when reas作者: 預(yù)測 時間: 2025-3-24 01:09
e are many different avenues for expression of scientific ideas, but the knowledge and publication explosion creates hardships for those who attempt to keep in tune with their specialties. It is not our purpose to add an unnecessary burden to this verbage increase. Instead we feel there comes a time when reas978-94-011-6493-1978-94-011-6491-7作者: Orthodontics 時間: 2025-3-24 05:00
https://doi.org/10.1007/978-3-030-65912-7ere the shear strength is high as a result of dissipation of excess pore-water pressure) or transverse compressional features (in places in the quarrying zone where the excess pore-water pressure can not be dissipated). As the englacial and superglacial sediment thicken, they obliterate the underlyi作者: Irrigate 時間: 2025-3-24 08:35
The Lyric Mode of ,: The I and the Other,ant zones, crudely measured by the length of eskers or ice-channel fillings, was at least 1.5 mi (2.4 km). The major source of sediments that comprise the morphologic sequences is suggested to have been a shear zone at the live ice-stagnant ice interface. Debris from this zone, transported by meltwa作者: Albinism 時間: 2025-3-24 11:19 作者: maudtin 時間: 2025-3-24 18:23
,Anhang mit Bildtafeln zu den L?tversuchen,y applies to all, for till is a typically dilatant system in that, under a deforming load, it must expand before continuous deformation can occur. Once dilatant, it continues to deform even under reduced load. An ice sheet thinning toward its terminus or wasting during the waning hemicycle imposes d作者: keloid 時間: 2025-3-24 19:30
Eigenschaften und Aufbau von Hartmetallen, eroding troughs 1,000 ft, reducing uplands and notching cols,. and greatly altered many drainage patterns. When considering the total topographic fabric of the Plateau it is important to use a multicyclic model of landscape denudation. Not only are glacial episodes of erosion-deposition important, 作者: FLING 時間: 2025-3-24 23:50
Career, Criticisms, Creed and Other Issues,clusions, dimensional lineation of ice crystals, and lineation of optic axes with maxima in fabric diagrams generally 10–35%. The fabrics are complicated and not uniform from one wedge to another, nor even necessarily from one part of a wedge to another. Not all fabrics can be explained. Deformation作者: 炸壞 時間: 2025-3-25 03:29
Die Technologie der Hartmetallee systems can be traced far out in the adjacent Bighorn Basin. Approaching the better preserved later moraine, the gravel of the Cody terrace-with weathering characteristics similar to the morainic deposits-thickens, rises in height above present stream grade, and merges with outwash materials exten作者: Keshan-disease 時間: 2025-3-25 08:55 作者: 吼叫 時間: 2025-3-25 12:05
A Glacial Process-Form Modelere the shear strength is high as a result of dissipation of excess pore-water pressure) or transverse compressional features (in places in the quarrying zone where the excess pore-water pressure can not be dissipated). As the englacial and superglacial sediment thicken, they obliterate the underlyi作者: 懶洋洋 時間: 2025-3-25 18:19
The Morphologic Sequence Concept and Deglaciation of Southern New Englandant zones, crudely measured by the length of eskers or ice-channel fillings, was at least 1.5 mi (2.4 km). The major source of sediments that comprise the morphologic sequences is suggested to have been a shear zone at the live ice-stagnant ice interface. Debris from this zone, transported by meltwa作者: 描述 時間: 2025-3-25 21:45 作者: 一夫一妻制 時間: 2025-3-26 02:31
Origins of Drumlinsy applies to all, for till is a typically dilatant system in that, under a deforming load, it must expand before continuous deformation can occur. Once dilatant, it continues to deform even under reduced load. An ice sheet thinning toward its terminus or wasting during the waning hemicycle imposes d作者: ANIM 時間: 2025-3-26 05:01
Reappraisal of the Glaciated Appalachian Plateau eroding troughs 1,000 ft, reducing uplands and notching cols,. and greatly altered many drainage patterns. When considering the total topographic fabric of the Plateau it is important to use a multicyclic model of landscape denudation. Not only are glacial episodes of erosion-deposition important, 作者: 膽小鬼 時間: 2025-3-26 10:51 作者: 柔軟 時間: 2025-3-26 15:40
The Relation of River Terrace Formation to Glaciation in the Shoshone River Basin, Western Wyominge systems can be traced far out in the adjacent Bighorn Basin. Approaching the better preserved later moraine, the gravel of the Cody terrace-with weathering characteristics similar to the morainic deposits-thickens, rises in height above present stream grade, and merges with outwash materials exten作者: SLAY 時間: 2025-3-26 20:29
Glacial Landforms and Civil Engineerings but for their full appreciation in civil engineering work patient study on the ground is still essential. Just as geology alone was found to be inadequate, leading to the development of soil mechanics, so today it is becoming generally recognized that soil mechanics must be used against a backgrou作者: 解開 時間: 2025-3-26 23:19
The Evolution of the Rocky Mountain Glacial Model River Mountains, that is now used far beyond the provincial boundaries of the state. Although basically sound, existing controversy suggests a current need for evaluation of this chronological model, whose history gives a nice example of the nature of scientific work.作者: 漫步 時間: 2025-3-27 01:56
A Glacial Process-Form Modelhe glacial margin (the glacier is frozen to its bed in most places, excess pore-water pressure is dissipated by marginal seepage, and the glacial flow is upward) and an abrasion zone behind the margin (the bed is thawed and the glacier is sliding, excess pore-water pressure is not dissipated, and th作者: TOXIN 時間: 2025-3-27 07:09
The Morphologic Sequence Concept and Deglaciation of Southern New Englanded mostly of meltwater deposits and referred to as .. Sequences are distinguished according to differences in depositional environment, such as fluvial, lacustrine, and marine, and by the presence or absence of an ice-contact head of outwash. The construction of profiles to show depositional gradien作者: Shuttle 時間: 2025-3-27 12:11
Morphometry in Glacial Geomorphology significant aspects of the morpology of the features investigated. As geomorphology is concerned with the understanding of the shape of features, morphometry provides essential material on which to base a valid analysis. From morphometric measurements it is possible to obtain the mean dimensions of作者: 古老 時間: 2025-3-27 13:51 作者: 熄滅 時間: 2025-3-27 18:50
Origins of Drumlinsposition, the tendency is to develop a form which imposes minimum resistance to glacier flow. Erosion commonly precedes deposition, but either may dominate in shaping of a particular drumlin field..Drumlin form is affected by protrusions in the glacially overridden topography and by character and ab作者: BLA 時間: 2025-3-27 21:56 作者: Antimicrobial 時間: 2025-3-28 04:21 作者: 改變 時間: 2025-3-28 09:26 作者: prediabetes 時間: 2025-3-28 14:15 作者: SOBER 時間: 2025-3-28 16:16
Glacial Grooves and Periglacial Features in the Saharan Ordovicianh-language audiences. (A comprehensive, detailed report is available only in French.) Some special problems are discussed in more detail..Remarkable deep and almost rectilinear glacial grooving can be followed across almost flat terrain for tens of kilometers. Scattered evidences confirming the glac作者: Harass 時間: 2025-3-28 22:26 作者: intimate 時間: 2025-3-29 00:29 作者: 圖畫文字 時間: 2025-3-29 03:36 作者: 有毛就脫毛 時間: 2025-3-29 08:32 作者: CHURL 時間: 2025-3-29 15:24
https://doi.org/10.1007/978-3-030-65912-7he glacial margin (the glacier is frozen to its bed in most places, excess pore-water pressure is dissipated by marginal seepage, and the glacial flow is upward) and an abrasion zone behind the margin (the bed is thawed and the glacier is sliding, excess pore-water pressure is not dissipated, and th作者: 故意釣到白楊 時間: 2025-3-29 17:40 作者: Harness 時間: 2025-3-29 22:48 作者: 地殼 時間: 2025-3-30 02:21 作者: 人類學(xué)家 時間: 2025-3-30 07:53
,Anhang mit Bildtafeln zu den L?tversuchen,position, the tendency is to develop a form which imposes minimum resistance to glacier flow. Erosion commonly precedes deposition, but either may dominate in shaping of a particular drumlin field..Drumlin form is affected by protrusions in the glacially overridden topography and by character and ab作者: 易于交談 時間: 2025-3-30 11:05
Eigenschaften und Aufbau von Hartmetallen,ing many differences when compared with non-glaciated areas to the south. For clarity the Plateau is divided into 11 sections, each with its own characteristic suite of geomorphic features. In the United States the Plateau is unsurpassed in many landforms such as the Finger Lakes, through valleys, g
