... The line of latitude midway between the poles, the
horizontal axis, is called the equator and defines the
line of zero latitude. The vertical axis, which defines
the line of zero longitude, is called the prime
meridian. For most geographic coordinate systems,
the prime meridian is the longitude that ...
... The information contained in this document is subject to change without notice.
U.S. GOVERNMENT RESTRICTED/LIMITED RIGHTS
Any software, documentation, and/or data delivered hereunder is subject to the terms of the License Agreement. In no
event shall the U.S. Government acquire greater than RESTRICT ...
... measured either in decimal degrees or in degrees,
minutes, and seconds (DMS). Latitude values are
measured relative to the equator and range from -90°
at the South Pole to +90° at the North Pole.
Longitude values are measured relative to the prime
...
... measured either in decimal degrees or in degrees,
minutes, and seconds (DMS). Latitude values are
measured relative to the equator and range from -90°
at the South Pole to +90° at the North Pole.
Longitude values are measured relative to the prime
...
... and provides information about data quality.
Geographic terms and concepts highlighted in bold in the text are briefly defined in the Glossary
of Terms, section 5. More details can be found in the 2001 Census Dictionary, Catalogue No. 92378-XIE. Supplementary information is provided in the appendice ...
... 4. Shape of Pangaea after Partial Modification of India, Alaska, and Oceania
□ After confirming that Pangaea was approximately round in shape, we partially
adjusted the locations and forms of the continents to match the circular frame.
(See red lines in .)
□ Main adjustment points.
- The s ...
... subduction of the Juan de Fuca plate underneath the North American plate and can erupt both quiet lava flows
and pyroclastic ash falls and ash flows (nuee ardentes).
Mt. Rainer is especially susceptible to lahars (volcanic debris flows and mudflows) from the unstable volcanic
rock that has been alte ...
... Make a Venn diagram that compares two cultural
groups and the components of their culture.
Student can draw an original representation of
culture within their environment, then exchange
their art piece with another student to analyze their
artwork and write descriptive piece to describe that
individ ...
... The qualitative and quantitative terrain analysis of each sub-region as well as of the whole region
was based on the terrain analysis data (morphological slopes, morphological discontinuities,
hydrographic network, planation surfaces – figures 2c, 3d). The qualitative terrain analysis was
done using ...
... c. transform [this one is more difficult]; for example: the San Andreas fault in
California, New Zealand (the Alpine fault), and the transform faults along the
southern boundary of the Nazca plate.
Sometimes the plate motions and interactions are more complicated. For example, for the North
American ...
... This map shows the plate boundaries that are used in the Discovering Plate Boundaries exercise. These data were
obtained from Dietmar Muller, a scientist at the University of Sydney in Australia.
While most plate boundary locations are generally agreed upon by scientists, some are not. Other plate b ...
... show through the paper). The volcanic islands and seamounts at the northern end of the Emperor
Seamounts, near the Aleutian trench, are over 65 million years old. At the “bend” in the seamount
chains that connects the Emperor and Hawaiian chains, the volcanic rocks are about 42 million years
old. A ...
... An ideal map projection retains all these graticule characteristics through the translation to the
map. But the ideal map projection can never be achieved and if a projection is designed to guarantee a
particular characteristic as true, others on it necessarily will be distorted. As a result map pro ...
... Overarching Skills
Geography integrates the study of the natural and human elements of Earth to reveal their
complex relationships. The study of the spatial relationships among the components of the
human and physical systems is enhanced by using the latest and most reliable geographic
information ...
... 19) One difference between any two different map projections must always be
A) how accurately relative sizes are portrayed.
B) scale.
C) the number of degrees from the Equator to the North Pole.
D) how the geographic grid is arranged.
E) how accurately shapes are portrayed.
Answer: D
...
... and environments that shape it. To gain mastery, students need reinforcement of geography skills on a
frequent basis. These pages contain 180 five-minute geography-based activities that offer ways to go
beyond the basic geography skills taught in textbooks. Students will find them not only instructi ...
... A basic overview and introduction to the study of geography, both physical and human. After a brief
introduction to the field of geography and the five themes of geography, students will learn about the
geography of the U.S. and all other regions in the world. They will have map tests on each of the ...
... properties of particular phenomena—and even predicting where things are likely to occur. Such undertakings
have fostered an interest in location theory, an element of contemporary human geography that seeks answers to a wide range of questions—some of them theoretical, others highly practical: Why a ...
... Slovakia is a country rich in low enthalpy geothermal sources. The potential of geothermal energy
is about 21, 456 TJ/year. On the basis of distribution of the collectors of geothermal energy
resources and geothermal field activity, 26 prospective areas (Fig. 3-2) or structures suitable for
exploita ...
... either have to cut it or stretch parts of it.
Mapmakers face a similar problem in showing
the surface of the round earth on a flat map.
When the earth’s surface is flattened, big gaps
open up. To fill in the gaps, mapmakers stretch
parts of the earth. They choose to show either
the correct shapes of ...
... clearly distinguished. The East Arabian Craton (platform) as well as its framing are noticeably detected.
Computation of entropy map from the satellite derived gravity field was earlier successfully tested by the authors in
the Eastern Mediterranean (Eppelbaum and Katz, 2015a). Application of the ad ...
... either have to cut it or stretch parts of it.
Mapmakers face a similar problem in showing
the surface of the round earth on a flat map.
When the earth’s surface is flattened, big gaps
open up. To fill in the gaps, mapmakers stretch
parts of the earth. They choose to show either
the correct shapes of ...
Cartography (from Greek χάρτης khartēs, ""map""; and γράφειν graphein, ""write"") is the study and practice of making maps. Combining science, aesthetics, and technique, cartography builds on the premise that reality can be modeled in ways that communicate spatial information effectively.The fundamental problems of traditional cartography are to:Set the map's agenda and select traits of the object to be mapped. This is the concern of map editing. Traits may be physical, such as roads or land masses, or may be abstract, such as toponyms or political boundaries.Represent the terrain of the mapped object on flat media. This is the concern of map projections.Eliminate characteristics of the mapped object that are not relevant to the map's purpose. This is the concern of generalization.Reduce the complexity of the characteristics that will be mapped. This is also the concern of generalization.Orchestrate the elements of the map to best convey its message to its audience. This is the concern of map design.Modern cartography is largely integrated with geographic information science (GIScience) and constitutes many theoretical and practical foundations of geographic information systems.
