CHARACTERIZING SHORT-TERM (1970-PRESENT) LAKE CHANGE IN THE HIGH-MOUNTAIN TROPICS AND AMAZON OF ECUADOR

2018 ◽  
Author(s):  
Melina Feitl ◽  
◽  
Sherilyn C. Fritz ◽  
Xavier Benito Granell ◽  
Miriam Steinitz-Kannan
Keyword(s):  
High Mountain ◽  
Short Term ◽  
Lake Change

Long and short time evolution of deep seated gravitational slope deformation: contribution to knowledge of phenomena for the management of alea in the Alpine mountains

2020 ◽  
Author(s):  
Clément Boivin
Keyword(s):  
Time Evolution ◽  
Slope Deformation ◽  
Tectonic Activity ◽  
High Mountain ◽  
Mountain Range ◽  
Short Term ◽  
Future Evolution ◽  
Short Time ◽  
Short Time Evolution

<p>"LONG AND SHORT TIME EVOLUTION OF DEEP SEATED GRAVITATIONAL SLOPE DEFORMATION: CONTRIBUTION TO KNOWLEDGE OF PHENOMENA FOR THE MANAGEMENT OF ALEA IN THE ALPINE MOUNTAINS"</p><p> </p><p>C.Boivin <sup>a</sup>, J.P. Malet <sup>a</sup>, C. Bertrand <sup>b</sup>, F. Chabaux <sup>c</sup>, J. van der Woerd <sup>a</sup>, Y. Thiery <sup>d</sup>, F. Lacquement <sup>d</sup></p><p><sup>a  </sup>Institut de Physique du Globe de Strasbourg – IPGS/DA - UMR 7516 CNRS-Unistra</p><p><sup>b </sup> Laboratoire Chrono-Environnement – LCE / UMR 6249 CNRS – UFC</p><p><sup>c</sup>  Laboratoire d’Hydrologie et de Géochimie de Strasbourg – BISE / UMR 7517 – Unistra</p><p><sup>d</sup>  Bureau de Recherches Géologiques et Minières</p><p> </p><p>          The <strong>Deep Seated Gravitational Slope Deformation (DSGSD)</strong> are defined like a set of rock mass characterized by a generally slow movement and which can affect all the slopes of a valley or a mountain range (Agliardi and al., 2001, 2009; Panek and Klimes., 2016). The DSGSD is identified in many mountains (ex: Alps, Alaska, Rocky Mountains, Andes…) and it can affect both isolated low relief and very high mountain ranges (Panek and Klimes., 2016). This deep instability are identified in many case like the origin zone for important landslide like the example of La Clapière landslide in the Alpes Maritimes (Bigot-Cormier et al., 2005). The DSGSD represent an important object we must understand to anticipate catastrophic landslides.</p><p>          Actually, many factors that could be at the origin or controlling the evolution of DSGSD have been identified such as for example the structural heritage, the climate or the tectonic activity (Agliardi 2000; 2009; 2013; Jomard 2006; Sanchez et al., 2009; Zorzi et al., 2013; Panek and Klimes., 2016; Ostermann and Sanders., 2017; Blondeau 2018). The long-term and short-term evolution of DSGSD is still poorly understood but represents an important point to characterize in order to predict future major landslides. A first inventory of DSGSD began to be carried out by certain studies such as Blondeau 2018 or Crosta et al 2013 in the Alps. These same studies have also started to prioritize the factors controlling the evolution of DSGSD.</p><p>          It is in order to better understand the short-term (<100 years) and long-term (> 100 years) evolution of the DSGSD of the French Alpine massifs and the link with the occurrence of landslides, that this thesis project is developed. The main objective of this project, will be proposed models of the evolution of DSGSD since the last glaciations. But also to propose key interpretations of the future evolution to locate the areas likely to initiate landslides. Two study areas in the French Alpine massifs were chosen because they represent areas of referencing and localization gaps in DSGSD: Beaufortain and Queyras. They have the advantage of having a low lithological diversity making it possible to simplify the identification of the factors influencing the evolution of DSGSD. A geomorphological analysis on satellite data and on the ground is carried out to locate the DSGSD. Several dating (<sup>14</sup>C, <sup>10</sup>Be or <sup>36</sup>Cl) will be carried out to reconstruct the history of these objects and understand the factors that controlled their evolution.</p>

scholarly journals Palaeo-earthquake magnitudes on the Dzhungarian fault, N. Tien shan, and implications for the rupture processes of intraplate strike-slip faults

2020 ◽  
Author(s):  
Chia-Hsin Tsai ◽  
Richard Walker ◽  
Simon Daout ◽  
Kanatbek Abdrakhmatov ◽  
Aidyn Mukambayev ◽  
...  
Keyword(s):  
Kinematic Model ◽  
Strike Slip ◽  
Tien Shan ◽  
High Mountain ◽  
Short Term ◽  
Lithospheric Deformation ◽  
Large Earthquakes ◽  
Northern Tien Shan ◽  
Fault Length

<p>Long-term and present-day crustal deformation in the northern Tien Shan is poorly known, but is a key to understanding the mode of lithospheric deformation deep within the continental interiors, as well as the hazards posed by the slow-moving intraplate faults. Driven by the India-Asia collision, the NW-SE strike-slip faults and the E-W range-front thrust faults in the interior of Tien Shan together accommodate about 15-20 mm/yr of shortening. Here we focus on the NW-SE striking Dzhungarian fault (DZF) and the E-W striking Lepsy fault (LPF), which are large oblique strike-slip faults bounding the Dzhungarian Alatau, northern Tien Shan. Two large historical earthquakes in ~1716 and 1812 (Mw 8) were recorded in this region, and clear fault traces as well as scarps are visible from satellite images along some of the main faults. However, their geometries, slip rates, mode of deformation, expected earthquake magnitudes and recurrence interval have not been studied in details. A previous study suggested that the LPF ruptured in a seismic event around 400 yrBP that might be the 1716 earthquake known from historical records. Offsets of over 15 m were found over a fault length of 120 km, indicating a magnitude in the range Mw 7.5-8.2. The slip to length ratio for the LPF is unusally high, suggesting either that faults in this region are capable of generating very large earthquakes for a given fault length, or that the rupture length is underestimated.</p><p>Using a combination of high-resolution digital elevation models (DEMs) and orthophotos from High Mountain Asia (NASA), Pleiades optical imagery (CNES), drone photos and multi-temporal interferometric synthetic-aperture radar (InSAR) from the Sentinel-1 satellites, we identify the geomorphic signatures and quantify the long-term and short-term strain accumulation along the faults. The ~400 km DZF shows evidence for relatively ‘fresh’ rupturing along much of its length. We calculate an average lateral slip per event of 9.9 m from offset stacking analysis, which underlines the potential future large earthquakes on this fault. The proximity of the DZF and LPF ruptures and equivalent level of preservation opens the possibility that they were formed in a single earthquake event, with a moment-magnitude greater than 8. We also present estimates of long-term and short-term rates of slip across the DZF in order to estimate average recurrence intervals and to build a kinematic model of the faulting in the Northern Tien Shan.</p>

scholarly journals Isotope Stratification in High Mountain Glaciers: Examples from the Peruvian Andes and Himalaya

1983 ◽  
Vol 29 (103) ◽  
pp. 417-424 ◽  
Author(s):  
Jerzy Grabczak ◽  
Jerzy Niewodniczański ◽  
Kazimierz Różański
Keyword(s):  
Snow Cover ◽  
Deuterium Content ◽  
High Mountain ◽  
Natural Conditions ◽  
Short Term ◽  
Peruvian Andes ◽  
Mountain Glaciers ◽  
The Andes ◽  
Equilibrium Process ◽  
The Himalaya

Abstract18O and deuterium content was measured in snow and ice samples collected from two crevasses on temperate glaciers high in the Andes and in the Himalaya. The results show that, due to intense exposure to sun, a significant part of the annual accumulation of snow is removed by melting and sublimation, the latter being predominant. There is strong empirical evidence that in natural conditions which are characteristic of both the glaciers studied sublimation of the snow cover can be approximated by the thermodynamic equilibrium process. The short-term fluctuations, though slightly moderated, and longer-term variations can still be observed in the deeper parts of the glaciers in spite of firnification of the snow.

Distribution, Relative Abundance and Conservation Status of Corroboree Frogs, Pseudophrne-Corroboree Moore (Anura, Myobatrachidae)

1989 ◽  
Vol 16 (5) ◽  
pp. 537 ◽  
Author(s):  
WS Osborne
Keyword(s):  
Relative Abundance ◽  
Conservation Status ◽  
High Mountain ◽  
Summer Drought ◽  
Latitudinal Distribution ◽  
Short Term ◽  
Range Contraction ◽  
Adverse Conditions

A survey of the distribution and abundance of the corroboree frog, Pseudophryne corroboree, was carried out over five summers between December 1984 and April 1989. The species has a restricted high-mountain distribution, occurring as three disjunctive populations: Snowy Mountains, Fiery Range and Brindabella Range. The Snowy Mountains and Fiery Range populations are relatively widespread, occupying areas of 400 and 550 km2 respectively. In contrast, the Brindabella Range population is restricted to about 60 km2. The abundance of the Snowy Mountains population has been considerably reduced throughout much of its range, perhaps because of frequent summer drought between 1979 and 1984. Although P. corroboree is rare, its range is largely within conservation reserves, and its relatively broad latitudinal distribution has prevented adverse conditions from affecting all populations. The decline in abundance of the distinctive Snowy Mountains population may be a response to adverse short-term weather, or it may be part of a decline and range contraction over a longer period.

scholarly journals Isotope Stratification in High Mountain Glaciers: Examples from the Peruvian Andes and Himalaya

1983 ◽  
Vol 29 (103) ◽  
pp. 417-424 ◽  
Author(s):  
Jerzy Grabczak ◽  
Jerzy Niewodniczański ◽  
Kazimierz Różański
Keyword(s):  
Snow Cover ◽  
Deuterium Content ◽  
High Mountain ◽  
Natural Conditions ◽  
Short Term ◽  
Peruvian Andes ◽  
Mountain Glaciers ◽  
The Andes ◽  
Equilibrium Process ◽  
The Himalaya

Abstract18O and deuterium content was measured in snow and ice samples collected from two crevasses on temperate glaciers high in the Andes and in the Himalaya. The results show that, due to intense exposure to sun, a significant part of the annual accumulation of snow is removed by melting and sublimation, the latter being predominant. There is strong empirical evidence that in natural conditions which are characteristic of both the glaciers studied sublimation of the snow cover can be approximated by the thermodynamic equilibrium process. The short-term fluctuations, though slightly moderated, and longer-term variations can still be observed in the deeper parts of the glaciers in spite of firnification of the snow.

Conceptual short-term memory (CSTM) supports core claims of Christiansen and Chater

2016 ◽  
Vol 39 ◽  
Author(s):  
Mary C. Potter
Keyword(s):  
Working Memory ◽  
Rapid Serial Visual Presentation ◽  
Language Comprehension ◽  
Short Term Memory ◽  
Visual Presentation ◽  
Long Term Memory ◽  
Short Term ◽  
Term Memory ◽  
Use Of Knowledge

AbstractRapid serial visual presentation (RSVP) of words or pictured scenes provides evidence for a large-capacity conceptual short-term memory (CSTM) that momentarily provides rich associated material from long-term memory, permitting rapid chunking (Potter 1993; 2009; 2012). In perception of scenes as well as language comprehension, we make use of knowledge that briefly exceeds the supposed limits of working memory.

Ultrastructural Changes of Canine Kidneys During 24-Hour Perfusion on a LI-400 Preservation System

1971 ◽  
Vol 29 ◽  
pp. 316-317
Author(s):  
M. O. Magnusson ◽  
D. G. Osborne ◽  
T. Shimoji ◽  
W. S. Kiser ◽  
W. A. Hawk
Keyword(s):  
Electron Microscopy ◽  
Electrolyte Solution ◽  
Ultrastructural Changes ◽  
Midline Incision ◽  
Short Term ◽  
Pentobarbital Anesthesia ◽  
Pulsatile Perfusion

Short term experimental and clinical preservation of kidneys is presently best accomplished by hypothermic continuous pulsatile perfusion with cryoprecipitated and millipore filtered plasma. This study was undertaken to observe ultrastructural changes occurring during 24-hour preservation using the above mentioned method.A kidney was removed through a midline incision from healthy mongrel dogs under pentobarbital anesthesia. The kidneys were flushed immediately after removal with chilled electrolyte solution and placed on a LI-400 preservation system and perfused at 8-10°C. Serial kidney biopsies were obtained at 0-½-1-2-4-8-16 and 24 hours of preservation. All biopsies were prepared for electron microscopy. At the end of the preservation period the kidneys were autografted.

Polychlorinated biphenyl induced hepatocyte alterations

1987 ◽  
Vol 45 ◽  
pp. 716-717
Author(s):  
D.N. Collins ◽  
J.N. Turner ◽  
K.O. Brosch ◽  
R.F. Seegal
Keyword(s):  
Lipid Droplets ◽  
Wistar Rats ◽  
Homovanillic Acid ◽  
Polychlorinated Biphenyl ◽  
Corn Oil ◽  
Environmental Pollutants ◽  
Short Term ◽  
Pcb Congeners ◽  
Urinary Levels ◽  
The Brain

Polychlorinated biphenyls (PCBs) are a ubiquitous class of environmental pollutants with toxic and hepatocellular effects, including accumulation of fat, proliferated smooth endoplasmic recticulum (SER), and concentric membrane arrays (CMAs) (1-3). The CMAs appear to be a membrane storage and degeneration organelle composed of a large number of concentric membrane layers usually surrounding one or more lipid droplets often with internalized membrane fragments (3). The present study documents liver alteration after a short term single dose exposure to PCBs with high chlorine content, and correlates them with reported animal weights and central nervous system (CNS) measures. In the brain PCB congeners were concentrated in particular regions (4) while catecholamine concentrations were decreased (4-6). Urinary levels of homovanillic acid a dopamine metabolite were evaluated (7).Wistar rats were gavaged with corn oil (6 controls), or with a 1:1 mixture of Aroclor 1254 and 1260 in corn oil at 500 or 1000 mg total PCB/kg (6 at each level).

Acetaminophen: Macula densa hypersecretory activity by induced hepatotoxicity

1987 ◽  
Vol 45 ◽  
pp. 934-935
Author(s):  
S.S. Poolsawat ◽  
C.A. Huerta ◽  
S.TY. Lae ◽  
G.A. Miranda
Keyword(s):  
Cell Proliferation ◽  
Liver Function ◽  
Chronic Inflammation ◽  
Foam Cell ◽  
Term Effect ◽  
Short Term ◽  
Drug Induced ◽  
Experimental Induction ◽  
Tissue Alterations ◽  
Toxic Responses

Introduction. Experimental induction of altered histology by chemical toxins is of particular importance if its outcome resembles histopathological phenomena. Hepatotoxic drugs and chemicals are agents that can be converted by the liver into various metabolites which consequently evoke toxic responses. Very often, these drugs are intentionally administered to resolve an illness unrelated to liver function. Because of hepatic detoxification, the resulting metabolites are suggested to be integrated into the macromolecular processes of liver function and cause an array of cellular and tissue alterations, such as increased cytoplasmic lysis, centrilobular and localized necroses, chronic inflammation and “foam cell” proliferation of the hepatic sinusoids (1-4).Most experimentally drug-induced toxicity studies have concentrated primarily on the hepatic response, frequently overlooking other physiological phenomena which are directly related to liver function. Categorically, many studies have been short-term effect investigations which seldom have followed up the complications to other tissues and organs when the liver has failed to function normally.

Sign in / Sign up

Export Citation Format

Share Document