2 edition of Lake St. Martin crypto-explosion crater and geology of the surrounding area found in the catalog.
Lake St. Martin crypto-explosion crater and geology of the surrounding area
H. R. McCabe
by Manitoba Mines Branch, Dept. of Mines and Natural Resources in Winnipeg
Written in English
Bibliography: p. 67-69.
|Statement||by H. R. McCabe and B. B. Bannatyne.|
|Contributions||Bannatyne, B. B., joint author.|
|LC Classifications||TN27.M3 A325 no. 3/70, QE613.5.C35 A325 no. 3/70|
|The Physical Object|
|Number of Pages||79|
|LC Control Number||73177045|
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LAKE ST. MARTIN CRVPTO-EXPLOSION CRATER AND GEOLOGY OF THE SURROUNDING AREA INTRODUCTION Thisreport presents a preliminary diSCUSSion of data obtained in a core hole drilling pro gramme in the Lake St.
Martin area. The data indicate that the Lake St. Martin structure is a crypto-explosion crateroflate Permian or possibly early Triassic age (2.
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Compra Lake St. Martin Crypto-Explosion Crater and Geology of the Surrounding Area. SPEDIZIONE GRATUITA su ordini idoneiFormat: Copertina flessibile. The term cryptoexplosion structure (or cryptovolcanic structure) means an explosion of unknown cause.
The term is now largely obsolete. It was once commonly used to describe sites where there was geological evidence of a large-scale explosion within the Earth's crust, but no definitive evidence for the cause such as normal volcanic sites are usually circular with signs of anomalous.
The St. Martin meteorite crater lies immediately north of Lake St. Martin between Lake Winnipeg to the east and Lake Manitoba to the west. Even though there is no surface expression, from drilling data, the structure was suspected as an impact crater with the discovery of shock metamorphic effects.
• review of elevation data relevant to the Project area. Geology and Soils ecodistrict occupies a small area surrounding Lake St. Martin between Lake Winnipeg and Lake () as a crypto-explosion crater consisting of a crater or hole 14 miles ( km) in diameter and more than 1, feet (about m) deep, with a central core 2 to.
Geology, Stratigraphic 91 Geology 49 Paleontology 13 Phosphoria Formation 5 Sedimentation And Deposition 4 + More; Call Number. Q - Science 79 T - Technology.
2 Format. Books 90 Computer Programs 1 Publication Year. 65 to The ejecta blanket surrounding Gale may have been as thick as ˜ m, which has implications for the amount of erosion that has occurred since Gale Crater formed. Search the history of over billion web pages on the Internet.
The eastern half of Isla del Sol is primarily comprised of a meter-thick layer of dark limestone, extending both above and below the brilliant blue of the lake surface. 28 Riddled with springs, it rises in cliffs and steep hillsides from the lake.
As we shall see in Chapter 9, the electromagnetic properties of such carbonaceous strata, like. An illustration of an open book. Books. An illustration of two cells of a film strip.
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An illustration of text ellipses. Leybourne et al ; McCabe ). The Lake St. Martin impact structure was described by McCabe () as a crypto-explosion crater consisting of a crater or hole 14 miles ( km) in diameter and more than 1, feet (about m) deep, with a central core 2 to 3 miles ( to.
Introduction. More than 50 years of exploration of the surfaces of planets, moons, asteroids, and even of comet nuclei, have firmly established the fundamental role that impact cratering has played as a planetary process and surface-modifying agent on nearly all solid bodies in the solar system (Fig.
1 a–f), throughout its entire history of billion years. The lake has a maximum depth of about 80 m and the crater rim rises about – m above the lake level. The area forms part of a tropical forest environment with warm climate, high rainfall, and high organic activity. Chemical weathering is intense, leading to the formation of locally thick lateritic soils.
Copernic Agent Search Results Search: Found: Date: 1. explosion deep mine (All the words) result(s) on 7/23/ AM.