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Catalog #: 10_0008554

Title: Convair/General Dynamics Atlas

Corporation Name: Convair/General Dynamics

Additional Information: Atlas

Tags: Convair/General Dynamics Atlas, Atlas, Convair/General Dynamics

Repository: San Diego Air and Space Museum Archive

Catalog #: 10_0008545

Title: Convair/General Dynamics Atlas

Corporation Name: Convair/General Dynamics

Additional Information: Atlas

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Repository: San Diego Air and Space Museum Archive

Catalog #: 10_0008544

Title: Convair/General Dynamics Atlas

Corporation Name: Convair/General Dynamics

Additional Information: Atlas

Tags: Convair/General Dynamics Atlas, Atlas, Convair/General Dynamics

Repository: San Diego Air and Space Museum Archive

Catalog #: 10_0008452

Title: Convair/General Dynamics Atlas

Corporation Name: Convair/General Dynamics

Additional Information: Atlas

Tags: Convair/General Dynamics Atlas, Atlas, Convair/General Dynamics

Repository: San Diego Air and Space Museum Archive

Catalog #: 10_21113

Title: General Dynamics Convair Astronautics

Date: 1960-1965

Corporation Name: General Dynamics/Convair

Repository: San Diego Air and Space Museum Archive

PictionID:54637334 - Catalog:14_035181 - Title:Atlas Centaur Details: Building 18; Centaur Scale Model on Range Date: 03/04/1965 - Filename:14_035181.tif - - ---- Images from the Convair/General Dynamics Astronautics Atlas Negative Collection. The processing, cataloging and digitization of these images has been made possible by a generous National Historical Publications and Records grant from the National Archives and Records Administration---Please Tag these images so that the information can be permanently stored with the digital file.---Repository: San Diego Air and Space Museum

PictionID:44933199 - Catalog:14_015896 - Title:Atlas Details: Silo 1/10 Scale Model Mock Up; Overall Side View Date: 12/02/1959 - Filename:14_015896.tif - - - - Image from the Convair/General Dynamics Astronautics Atlas Negative Collection. The processing, cataloging and digitization of these images has been made possible by a generous National Historical Publications and Records grant from the National Archives and Records Administration---Please Tag these images so that the information can be permanently stored with the digital file.---Repository: San Diego Air and Space Museum

Catalog #: 10_0008792

Date: 1990-1993

Title: Convair/General Dynamics Plant and Personnel

Corporation Name: Convair/General Dynamics

Additional Information: Old Prints and Viewgraphs

Tags: Convair/General Dynamics Plant and Personnel, Old Prints and Viewgraphs, 1990-1993, Convair/General Dynamics

Repository: San Diego Air and Space Museum Archive

PictionID:44932625 - Catalog:14_015850 - Title:Sycamore Canyon Facilities - Filename:14_015850.tif - - - - Image from the Convair/General Dynamics Astronautics Atlas Negative Collection. The processing, cataloging and digitization of these images has been made possible by a generous National Historical Publications and Records grant from the National Archives and Records Administration---Please Tag these images so that the information can be permanently stored with the digital file.---Repository: San Diego Air and Space Museum

EMD power descends through Winlock, Washington while the dynamic brakes keep the speed in check.

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Catalog #: 10_0008352

Title: Convair/General Dynamics Plant and Personnel

Corporation Name: Convair/General Dynamics

Additional Information: William Bullock and GD Personnel

Tags: Convair/General Dynamics Plant and Personnel, William Bullock and GD Personnel , Convair/General Dynamics

Repository: San Diego Air and Space Museum Archive

Catalog #: 10_0005867

Date: 1955-1969

Title: Convair/General Dynamics Plant and Personnel

Corporation Name: Convair/General Dynamics

Additional Information: F-102/F-106 Personnel

Tags: Convair/General Dynamics Plant and Personnel, F-102/F-106 Personnel , 1955-1969, Convair/General Dynamics

Repository: San Diego Air and Space Museum Archive

© M J Anahory. These images are protected by copyright. You cannot copy or republish this photo without written consent of the copyright holder. Any copyright infringements will be followed up with action legal or otherwise.

Catalog #: 10_0008584

Title: Convair/General Dynamics Atlas

Corporation Name: Convair/General Dynamics

Additional Information: Atlas

Tags: Convair/General Dynamics Atlas, Atlas, Convair/General Dynamics

Repository: San Diego Air and Space Museum Archive

Catalog #: 10_0008581

Title: Convair/General Dynamics Atlas

Corporation Name: Convair/General Dynamics

Additional Information: Atlas

Tags: Convair/General Dynamics Atlas, Atlas, Convair/General Dynamics

Repository: San Diego Air and Space Museum Archive

Carbon Fiber look kydex

Catalog #: 10_0008566

Title: Convair/General Dynamics Atlas

Corporation Name: Convair/General Dynamics

Additional Information: Atlas

Tags: Convair/General Dynamics Atlas, Atlas, Convair/General Dynamics

Repository: San Diego Air and Space Museum Archive

Catalog #: 10_0009315

Date: 1960-1969

Title: Convair/General Dynamics Atlas

Corporation Name: Convair/General Dynamics

Additional Information: AMR Florida

Tags: Convair/General Dynamics Atlas, AMR Florida , 1960-1969, Convair/General Dynamics

Repository: San Diego Air and Space Museum Archive

PictionID:44932855 - Catalog:14_015868 - Title:Facilities Details: Overall View of Tank 7-31 Date: 04/03/1958 - Filename:14_015868.tif - - - - Image from the Convair/General Dynamics Astronautics Atlas Negative Collection. The processing, cataloging and digitization of these images has been made possible by a generous National Historical Publications and Records grant from the National Archives and Records Administration---Please Tag these images so that the information can be permanently stored with the digital file.---Repository: San Diego Air and Space Museum

Catalog #: 10_0009065

Title: Convair/General Dynamics Plant and Personnel

Corporation Name: Convair/General Dynamics

Additional Information: Haringen Photos

Tags: Convair/General Dynamics Plant and Personnel, Haringen Photos, Convair/General Dynamics

Repository: San Diego Air and Space Museum Archive

Catalog #: 10_0008563

Title: Convair/General Dynamics Atlas

Corporation Name: Convair/General Dynamics

Additional Information: Atlas

Tags: Convair/General Dynamics Atlas, Atlas, Convair/General Dynamics

Repository: San Diego Air and Space Museum Archive

PictionID:44932309 - Catalog:14_015824 - Title:Sycamore Canyon Facilities Details - Filename:14_015824.tif - - - - Image from the Convair/General Dynamics Astronautics Atlas Negative Collection. The processing, cataloging and digitization of these images has been made possible by a generous National Historical Publications and Records grant from the National Archives and Records Administration---Please Tag these images so that the information can be permanently stored with the digital file.---Repository: San Diego Air and Space Museum

See the description for the set "Group Dynamics"

PictionID:45175227 - Catalog:14_016851 - Title:GD Astronautics Experiments Details: Dry Immersion Bed with Test Subject Lowered Date: 02/26/1965 - Filename:14_016851.TIF - - - - - Image from the Convair/General Dynamics Astronautics Atlas Negative Collection. The processing, cataloging and digitization of these images has been made possible by a generous National Historical Publications and Records grant from the National Archives and Records Administration---Please Tag these images so that the information can be permanently stored with the digital file.---Repository: San Diego Air and Space Museum

Catalog #: 10_0008595

Title: Convair/General Dynamics Atlas

Corporation Name: Convair/General Dynamics

Additional Information: Atlas

Tags: Convair/General Dynamics Atlas, Atlas, Convair/General Dynamics

Repository: San Diego Air and Space Museum Archive

Audi S6 Avant [4G / C7] Sportowy Układ Wydechowy CAPRISTO by auto-Dynamics.pl

 

Akustyczną artykulację dualistycznie doładowanej, widlastej jednostki napędowej, skutecznie w #AD, modyfikacyjnie trawestujemy. Redefiniując notację muzyczna w aspektach rytmicznych oraz kryteriach dynamicznych. Wypełniając pięciolinię motoryzacyjnie zorientowanymi, staccato & legato, V-Ósemkowo-zinterpretowanymi nutami. Audi S6 [4G /C7] by auto-Dynamics.pl

 

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PictionID:44932703 - Catalog:14_015856 - Title:Sycamore Canyon Facilities - Filename:14_015856.tif - - - - Image from the Convair/General Dynamics Astronautics Atlas Negative Collection. The processing, cataloging and digitization of these images has been made possible by a generous National Historical Publications and Records grant from the National Archives and Records Administration---Please Tag these images so that the information can be permanently stored with the digital file.---Repository: San Diego Air and Space Museum

Catalog #: 10_0009115

Title: Convair/General Dynamics Plant and Personnel

Corporation Name: Convair/General Dynamics

Additional Information: Haringen Photos

Tags: Convair/General Dynamics Plant and Personnel, Haringen Photos, Convair/General Dynamics

Repository: San Diego Air and Space Museum Archive

General Dynamics F-16AM Fighting Falcon

c/n: 61-629

History: 83-1076, [15133]

 

Portuguese Air Force

Catalog #: 10_0006398

Date: 1970-1979

Title: Convair/General Dynamics Tomahawk

Corporation Name: Convair/General Dynamics

Additional Information: Tomahawk

Tags: Convair/General Dynamics Tomahawk, Tomahawk, 1970-1979, Convair/General Dynamics

Repository: San Diego Air and Space Museum Archive

Catalog #: 10_0008562

Title: Convair/General Dynamics Atlas

Corporation Name: Convair/General Dynamics

Additional Information: Atlas

Tags: Convair/General Dynamics Atlas, Atlas, Convair/General Dynamics

Repository: San Diego Air and Space Museum Archive

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Catalog #: 10_0008605

Title: Convair/General Dynamics Atlas

Corporation Name: Convair/General Dynamics

Additional Information: Atlas

Tags: Convair/General Dynamics Atlas, Atlas, Convair/General Dynamics

Repository: San Diego Air and Space Museum Archive

Call No.: 10-001416

Title: Convair/General Dynamics Atlas Lifting Body Little Joe II

Year: 1964-1966

Corp. Name: Convair/General Dynamics

Description: 8 x 10 Black and White Glossy Print

Repository: San Diego Air and Space Museum Archive

PictionID:44932589 - Catalog:14_015847 - Title:Sycamore Canyon Facilities - Filename:14_015847.tif - - - - Image from the Convair/General Dynamics Astronautics Atlas Negative Collection. The processing, cataloging and digitization of these images has been made possible by a generous National Historical Publications and Records grant from the National Archives and Records Administration---Please Tag these images so that the information can be permanently stored with the digital file.---Repository: San Diego Air and Space Museum

PictionID:44933225 - Catalog:14_015898 - Title:Atlas Details: Silo 1/10 Scale Model Mock Up; Lower Section Date: 12/02/1959 - Filename:14_015898.tif - - - - Image from the Convair/General Dynamics Astronautics Atlas Negative Collection. The processing, cataloging and digitization of these images has been made possible by a generous National Historical Publications and Records grant from the National Archives and Records Administration---Please Tag these images so that the information can be permanently stored with the digital file.---Repository: San Diego Air and Space Museum

Catalog #: 10_0008579

Title: Convair/General Dynamics Atlas

Corporation Name: Convair/General Dynamics

Additional Information: Atlas

Tags: Convair/General Dynamics Atlas, Atlas, Convair/General Dynamics

Repository: San Diego Air and Space Museum Archive

General Dynamics F-16D Fighting Falcon of the 55th Fighter Squadron, "Fighting Fifty Fifth", 20th Fighter Wing from Shaw AFB participating in Red Flag 13-3 SEAD (Suppression of Enemy Air Defense), aka "Wild Weasel," exercises at Nellis AFB.

El campo de pseudocráteres de Landbrotshólar es el mayor de Islandia. Se sitúa en el SE, cerca de la ciudad de Kirkjubæjarklaustur.

 

Los pseudocráteres o conos desenraizados se formaron dentro del flujo de lava del Eldgjá. Thorodssen, en 1894, fue el primero en sugerir que estas lavas se originaron en la erupción del año 934, Thorarinsson (1951, 1981) lo dudó en varias ocasiones, pero finalmente llegó a la misma conclusión. Más tarde, Larsen G (1979) lo demostró definitivamente. Sin embargo, Jónsson (1987) señaló la complejísima tefrocronología de la región de Landbrotshólar, informando del hallazgo de restos vegetales en capas suprayacentes a las lavas, que dieron una edad de 14C de hace 2000 años, por lo que el debate sobre el origen de estas lavas sigue abierto.

 

En 1793, Sveinn Pálsson fue el primero en estudiar el campo de conos de Landbrotshólar, describiéndolos como conos de

piroclastos con una cubierta de lava (es decir, de spatter soldados) y siendo el primero en sugerir que se habían formado por erupciones secundarias.

 

La lava de la fisura de Eldgjá es la mayor colada del mundo originada en tiempos históricos, con un volumen de unos 18 km3. La fisura se prolonga por 75 kilómetros, desde el volcán de Katla en el sur hacia Vatnajökull en el NE. La lava de Eldgjá fluyó unos 40 kilómetros antes de derramarse por la boca de la garganta del río de Skaftá sobre las llanuras aluviales de Landbrot y de Medalland. En la mitad de Medalland de la colada, hay dos pequeños campos de pseudocráteres: Hestalandshólar y Laekjalandshólar.

 

Sin embargo, es en la zona de Landbrot donde se encuentra el mayor campo de pseudocráteres, el de Landbrotshólar, con un área de unos 50 km2 y un número de conos que se cuenta por millares. Parte del campo está cubierto por la lava del Laki de 1783, por lo que se estima que la superficie original pudo haber sido de 150 km2. En 27 km2 del total de 50 km2, Hoskuldsson y Jaupart contaron 4739 cráteres, lo que da una media de 176 cráteres/km2. Los mismos autores midieron la distribución de diámetros basales de 2812

cráteres, lo que dio una media de 21 m (mínimo 4 m y máximo 86 m). Existe una relación directa entre el tamaño de los pseudocráteres y su densidad espacial. Además, los estudios estadísticos de los cráteres indican que suelen ser más pequeños que sus contrapartidas volcánicas con chimenea.

 

Los depósitos volcánicos de los pseudocráteres son principalmente bombas y cenizas que proceden de la lava infrayacente y de los materiales que se encuentran por debajo de ésta. El examen detallado de la estratigrafía demuestra que, durante la primera fase de la

formación del edificio, la mayoría de los productos proyectados distalmente son sedimentos infrayacentes a la colada, mientras que los materiales proximales están formados por la lava misma. En los productos proximales, de grano grueso, es frecuente observar cantos rodados. En los distales abundan los materiales más finos, como las cenizas. El estudio detallado de los granos muestra que la mayoría están muy redondeados y son vítreos, presentando una ligera alteración, lo que le da un tono parduzco a los depósitos.

 

Las condiciones ambientales en el momento de su formación se pueden deducir de la litología, que sugiere que las áreas inundadas por la lava fueron lechos fluvioglaciales y zonas pantanosas. Antes de la erupción del Eldgjá, la zona de Landbrotshólar era un sandur del río Skaftá. En los sandur es frecuente observar la presencia de arenas de grano fino que contienen hasta un 60% de agua en sus poros. Las arenas de los sandur islandeses están formadas principalmente por fragmentos de vidrio volcánico. Además, dentro de los

sandur son frecuentes las zonas pantanosas y fangosas, que a su vez son ricas en materia orgánica. En cualquier caso, estas zonas son capaces de retener un importante volumen de agua, que queda atrapada cuando una colada fluye sobre ellas. Sin embargo, el continuo aumento del peso de la lava tiende a extraer el agua de los poros de los materiales infrayacentes, causando su desestabilización por lasdiferencias de densidad que aparecen. El espaciado y el tamaño de los pseudocráteres va a estar controlado por el espesor de la capa de sedimentos saturados de agua.

 

Hoskuldsson y Jaupart plantean dos causas de la formación del campo de pseudocráteres de Landbrotshólar.

 

Primero, las lavas que cubren las arenas saturadas de agua pueden inducir la desestabilización de éstas y hacer que se inyecten dentro de la colada. Esto explicaría algunas de las características observadas, como la erupción de las arenas basales al principio y la posterior salida de las lavas por el pseudocráter, dando una erupción continuada. En este caso, la densidad y el tamaño de los cráteres serían pequeños.

 

En segundo lugar, el agua atrapada en las zonas fangosas ricas en materia orgánica va a producir explosiones. La materia orgánica ofrece más resistencia al flujo de la lava que las arenas, por lo que aquí el agua va a tener mayor importancia como agente explosivo, por lo que habrá escasas proyecciones del subsuelo. Esta explicación está de acuerdo con el hecho de que en los cráteres apenas se

encuentran diamictitas y turba. En este caso, la densidad y el tamaño de los cráteres es mayor.

 

Thordarson, T. & Hoskuldsson, A. (2002): "Iceland. Classic Geology in Europe 3". Terra Publishing, Hertfordshire, Gran Bretaña.

 

Hoskuldsson, A. & Jaupart, C. (2005): "Landbrotshólar Pseudocrater Field, SE Iceland: Dynamics and growth of rootless cones within a lava flow". Geophysical Research Abstracts, Vol. 7, 08845.

  

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The pseudocrater field of Landbrotshólar is the largest in Iceland. It is situated in the SE, near the city of Kirkjubæjarklaustur.

 

The pseudocraters or rootless cones were formed within the lava flow of the Eldgjá. Thorodssen, in 1894, was the first author to suggest that these lavas originated in the eruption of the year 934, Thorarinsson (1951, 1981) hesitated several times, but he finally came to the same conclusion. Later, Larsen G (1979) showed it definitively. However, Jónsson (1987) pointed out the complex tephrochronology of the Landbrotshólar region, reporting the discovery of vegetable remains in layers overlapping the lavas, which gave a 14C age of 2000 years ago, so the debate about the origin of these lavas continues. In 1793, Sveinn Pálsson was the first to study the field of cones of Landbrotshólar, describing them as cones of pyroclasts with a lava cover (ie, from spatter) and being the first to suggest that they had been formed by secondary eruptions.

 

The lava of the Eldgjá fissure is the largest lava flow in the world originated in historical times, with a volume of about 18 km3. The fissure extends for 75 kilometers, from the Katla volcano in the south to Vatnajökull in the NE. The lava of Eldgjá flowed about 40 kilometers before spilling through the mouth of the Skaftá river gorge over the alluvial plains of Landbrot and Medalland. In the Medalland zone, there are two small fields of pseudocraters: Hestalandshólar and Laekjalandshólar.

 

However, it is in the Landbrot area where the largest pseudocraters field, Landbrotshólar, is located, with an area of about 50 km2 and a number of cones that is counted by thousands. Part of the field is covered by lava from the Laki volcano of 1783, so it is estimated that the original area could have been 150 km2. In 27 km2 of the total of 50 km2, Hoskuldsson and Jaupart counted 4739 craters, which gives an average of 176 craters / km2. The same authors measured the distribution of basal diameters of 2812 craters, which gave an average of 21 m (minimum 4 m and maximum 86 m).

 

There is a direct relationship between the size of

pseudocraters and their spatial density. In addition, statistical studies of craters indicate that they are usually smaller than their volcanic counterparts with a chimney.

 

The volcanic deposits of the pseudocraters are mainly bombs and ashes that come from the lava below and from the materials that are below it. The detailed examination of the stratigraphy shows that, during the first phase of the building formation, most of the distally projected products are sediments underlying the flow, while the proximal materials are formed by the lava itself. Boulders are often observed in coarse-grained proximal products. In distal products, finest materials abound, like ashes. The detailed study of the grains shows that most are very rounded and vitreous, presenting a slight alteration, which gives a brownish tone to the deposits.

 

The environmental conditions at the time of their formation can be deduced from the lithology, which suggests that areas flooded by lava were fluvioglacial beds and swampy areas. Before the eruption of the Eldgjá, ​​the Landbrotshólar area was a sandur

of the Skaftá river. In sandur it is common to observe the presence of fine grained sands that contain up to 60% water in their pores. The sands of Icelandic sandur are mainly formed by fragments of volcanic glass. In addition, within sandur are frequent swampy and muddy areas, which in turn are rich in organic matter. In any case, these areas are capable of retaining a large volume of water, which is trapped when lava flows over them. However, the increasing weight of the lava tends to extract water from the pores of the underlying materials, causing their destabilization by differences in density. The spacing and size of the pseudocraters will be controlled by the thickness of the water-saturated sediment layer.

 

Hoskuldsson and Jaupart raise two causes of the formation of the pseudocrater field of Landbrotshólar.

 

First, the lavas that cover the water-saturated sands can induce the destabilization of these and cause them to be injected inside the flow. This would explain some of the observed characteristics, such as the eruption of the basal sands at the beginning and the later exit of the lavas by the pseudocrater, giving a continued eruption. In this case, the craters density and size would be small.

 

Second, water trapped in muddy areas rich in organic matter will produce explosions. Organic matter offers more resistance to the lava flow than sand, so here the water will have greater importance as an explosive agent, so there will be little projections of the subsoil. This explanation is in agreement with the fact that one can hardly find diamictites and peat in the craters. In this case, the density and size of the craters is greater.

  

Thordarson, T. & Hoskuldsson, A. (2002): "Iceland. Classic Geology in Europe 3". Terra Publishing, Hertfordshire, Great Britain.

 

Hoskuldsson, A. & Jaupart, C. (2005): "Landbrotshólar Pseudocrater Field, SE Iceland: Dynamics and growth of rootless cones within a lava flow". Geophysical Research Abstracts, Vol. 7, 08845.

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