Figure 4.3 Marie Tharp and geologist Bruce Heezen study the final version of Heinrich Berann's World Ocean Floor Panorama in Beranns studio, Austria, 1977. Berann was engaged by the U.S. Navy and the National Geographic Society to incorporate Tharp's work and data from other sources in a unified form. One of Berann's beautiful maps is induded as Figure 4.22. Lamont-Doherty Earth Obsenatoryof Colu mbia GREENLAND HuSON BAY NORTH AMERICA DUBCIN MADERA CARACAS AMAON AFRICA SOUTH AMERICA Figure 4.22 Heinrich Berann's hand-drawn map of a portion of the Atlantic Ocean floor showing some major oceanic features: mid-ocean ridge, transform faults, fracture zones, submarine canyons, seamounts, continen- tal rises, trenches, and abyssal plains. If the ocean evaporated, the ridge system would be Earths most remark- able and obvious feature. Depths are in feet. The map is vertically exaggerated. A CAN ATERAS AA AABYSAL P ALCOA Al uminum Company

Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
Problem 1LR
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Why would the U.S. Navy have been interested in seeing such deepwater
charts produced?

Figure 4.3 Marie Tharp and geologist Bruce Heezen study the final
version of Heinrich Berann's World Ocean Floor Panorama in Beranns
studio, Austria, 1977. Berann was engaged by the U.S. Navy and the
National Geographic Society to incorporate Tharp's work and data
from other sources in a unified form. One of Berann's beautiful maps is
induded as Figure 4.22.
Lamont-Doherty Earth Obsenatoryof Colu mbia
Transcribed Image Text:Figure 4.3 Marie Tharp and geologist Bruce Heezen study the final version of Heinrich Berann's World Ocean Floor Panorama in Beranns studio, Austria, 1977. Berann was engaged by the U.S. Navy and the National Geographic Society to incorporate Tharp's work and data from other sources in a unified form. One of Berann's beautiful maps is induded as Figure 4.22. Lamont-Doherty Earth Obsenatoryof Colu mbia
GREENLAND
HuSON BAY
NORTH
AMERICA
DUBCIN
MADERA
CARACAS
AMAON
AFRICA
SOUTH AMERICA
Figure 4.22 Heinrich Berann's hand-drawn map of a portion of the Atlantic Ocean floor showing some major
oceanic features: mid-ocean ridge, transform faults, fracture zones, submarine canyons, seamounts, continen-
tal rises, trenches, and abyssal plains. If the ocean evaporated, the ridge system would be Earths most remark-
able and obvious feature. Depths are in feet. The map is vertically exaggerated.
A CAN
ATERAS AA
AABYSAL P
ALCOA Al uminum Company
Transcribed Image Text:GREENLAND HuSON BAY NORTH AMERICA DUBCIN MADERA CARACAS AMAON AFRICA SOUTH AMERICA Figure 4.22 Heinrich Berann's hand-drawn map of a portion of the Atlantic Ocean floor showing some major oceanic features: mid-ocean ridge, transform faults, fracture zones, submarine canyons, seamounts, continen- tal rises, trenches, and abyssal plains. If the ocean evaporated, the ridge system would be Earths most remark- able and obvious feature. Depths are in feet. The map is vertically exaggerated. A CAN ATERAS AA AABYSAL P ALCOA Al uminum Company
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