- published: 01 Oct 2014
- views: 39981
North America is a continent entirely within the Northern Hemisphere and almost all within the Western Hemisphere. It can also be considered a northern subcontinent of the Americas. It is bordered to the north by the Arctic Ocean, to the east by the Atlantic Ocean, to the west and south by the Pacific Ocean, and to the southeast by South America and the Caribbean Sea.
North America covers an area of about 24,709,000 square kilometers (9,540,000 square miles), about 16.5% of the earth's land area and about 4.8% of its total surface. North America is the third largest continent by area, following Asia and Africa, and the fourth by population after Asia, Africa, and Europe.
In 2013, its population was estimated at nearly 565 million people in 23 independent states, or about 7.5% of the world's population, if nearby islands (most notably the Caribbean) are included.
North America was reached by its first human populations during the last glacial period, via crossing the Bering land bridge. The so-called Paleo-Indian period is taken to have lasted until about 10,000 years ago (the beginning of the Archaic or Meso-Indian period). The Classic stage spans roughly the 6th to 13th centuries. The Pre-Columbian era ended with the arrival of European settlers during the Age of Discovery and the Early Modern period. Present-day cultural and ethnic patterns reflect different kind of interactions between European colonists, indigenous peoples, African slaves and their descendants. European influences are strongest in the northern parts of the continent while indigenous and African influences are relatively stronger in the south. Because of the history of colonialism, most North Americans speak English, Spanish or French and societies and states commonly reflect Western traditions.
The North American Datum (NAD) is the datum now used to define the geodetic network in North America. A datum is a formal description of the shape of the Earth along with an "anchor" point for the coordinate system. In surveying, cartography, and land-use planning, two North American Datums are in use: the North American Datum of 1927 (NAD27) and the North American Datum of 1983 (NAD83). Both are geodetic reference systems based on slightly different assumptions and measurements.
In 1901 the United States Coast and Geodetic Survey adopted a national horizontal datum called the United States Standard Datum, based on the Clarke Ellipsoid of 1866. It was fitted to data previously collected for regional datums, which by that time had begun to overlap. In 1913, Canada and Mexico adopted that datum, so it was also renamed the North American Datum.
As more data were gathered, discrepancies appeared, so the datum was recomputed in 1927, using the same spheroid and origin as its predecessor.
Coordinates: 40°N 100°W / 40°N 100°W / 40; -100
The United States of America (USA), commonly referred to as the United States (U.S.) or America, is a federal republic composed of 50 states, a federal district, five major territories and various possessions. The 48 contiguous states and Washington, D.C., are in central North America between Canada and Mexico. The state of Alaska is in the northwestern part of North America and the state of Hawaii is an archipelago in the mid-Pacific. The territories are scattered about the Pacific Ocean and the Caribbean Sea. At 3.8 million square miles (9.842 million km2) and with over 320 million people, the country is the world's third or fourth-largest by total area and the third most populous. It is one of the world's most ethnically diverse and multicultural nations, the product of large-scale immigration from many countries. The geography and climate of the United States are also extremely diverse, and the country is home to a wide variety of wildlife.
In this video we explain the basic concepts behind geodetic datums, where they are used, and why it is important to know about and use the correct datums. For more information on geodetic datums, visit http://www.geodesy.noaa.gov/.
The North American Datum is the datum now used to define the geodetic network in North America. A datum is a formal description of the shape of the Earth along with an "anchor" point for the coordinate system. In surveying, cartography, and land-use planning, two North American Datums are in use: the North American Datum of 1927 and the North American Datum of 1983. Both are geodetic reference systems based on slightly different assumptions and measurements. This video is targeted to blind users. Attribution: Article text available under CC-BY-SA Creative Commons image source in video
The North American Vertical Datum of 1988 is the vertical control datum of orthometric height established for vertical control surveying in the United States of America based upon the General Adjustment of the North American Datum of 1988. NAVD 88 was established in 1991 by the minimum-constraint adjustment of geodetic leveling observations in Canada, the United States, and Mexico. It held fixed the height of the primary tidal bench mark, referenced to the International Great Lakes Datum of 1985 local mean sea level height value, at Rimouski, Quebec, Canada. Additional tidal bench mark elevations were not used due to the demonstrated variations in sea surface topography, i.e., that mean sea level is not the same equipotential surface at all tidal bench marks. This video is targeted to bl...
02.05.2016 ALll thanksss Hd youtube HD
The purpose of this exercise is to introduce the student to datum shifts, the Project tool, and the interpolation and contouring tool in ArcGIS Spatial Analyst. You will compute the geodetic datum shifts between North American Datum 1983 (NAD83) and North American Datum 1927 (NAD27) using a specific transformation method (NADCON). To make the project useful you will compute the datum shift in seconds of longitude and seconds of latitude for all 58,000 of the USGS 7.5 minute quadrangles (1:24,000 scale ) in the continental United States.
In this video, we explore the history of geodetic datums in the United States, and how they were established at a national level to assure consistency across mapping applications. For more information on geodetic datums, visit http://www.geodesy.noaa.gov/.
Developed in partnership with COMET Program/MetEd, "What is the Status of Today's Geodetic Datums?" examines the use of the current primary geodetic datums used in the U.S. (NAD 83 and NAVD 88), the challenges in maintaining these datums, and the inconsistencies that arise when they are used together with the latest satellite-based mapping technologies. For more information on geodetic datums, visit http://www.geodesy.noaa.gov/. Original video source: http://www.ngs.noaa.gov/corbin/class_description/NGS_Video_Library.shtml
Most common used geographic coordinate reference system is World Geodetic System 1984 (WGS 84). Since it is difficult to manipulate with degrees and in some contexts it is not enough precise, many countries established their own metric coordinate system. QGIS Library has a lot of predefined coordinate reference systems, but if any local system doesn't exist in library, you can look for it on web. The link is spatialreference.org. For my own practice I downloaded one part of California map and reproject it from WGS 84 to mostly common use coordinate reference system in California - North America Datum 1983 (shorten NAD83). From Raster - Reprojections, open Warp (Reproject), select input and output files and define source and target spatial reference system. If desired CRS doesn't exist...
The road to choosing custom projections is not paved with sundrops and lilies. It is time to start learning the nuts and bolts of coordinate systems. Minute Markers: -0:27- Geodesy, the geoid. -1:10- Ellipsoid, geographic coordinate system. -2:09- Can't effectively measure with ellipsoid. -3:21- Planar coordinate system. -3:49- Geodetic datums. -5:41- Projections. -6:47- REMEMBER this, degrees vs. linear units. -7:10- Three types of projections. -7:32- Recap. All images included are in the public domain, though the geoid image was originally created here I believe (correct me if I'm wrong): http://www.esa.int/spaceinimages/Images/2004/10/The_Earth_s_gravity_field_geoid_as_it_will_be_seen_by_GOCE
In this video we explain the basic concepts behind geodetic datums, where they are used, and why it is important to know about and use the correct datums. For more information on geodetic datums, visit http://www.geodesy.noaa.gov/.
The North American Datum is the datum now used to define the geodetic network in North America. A datum is a formal description of the shape of the Earth along with an "anchor" point for the coordinate system. In surveying, cartography, and land-use planning, two North American Datums are in use: the North American Datum of 1927 and the North American Datum of 1983. Both are geodetic reference systems based on slightly different assumptions and measurements. This video is targeted to blind users. Attribution: Article text available under CC-BY-SA Creative Commons image source in video
The North American Vertical Datum of 1988 is the vertical control datum of orthometric height established for vertical control surveying in the United States of America based upon the General Adjustment of the North American Datum of 1988. NAVD 88 was established in 1991 by the minimum-constraint adjustment of geodetic leveling observations in Canada, the United States, and Mexico. It held fixed the height of the primary tidal bench mark, referenced to the International Great Lakes Datum of 1985 local mean sea level height value, at Rimouski, Quebec, Canada. Additional tidal bench mark elevations were not used due to the demonstrated variations in sea surface topography, i.e., that mean sea level is not the same equipotential surface at all tidal bench marks. This video is targeted to bl...
02.05.2016 ALll thanksss Hd youtube HD
The purpose of this exercise is to introduce the student to datum shifts, the Project tool, and the interpolation and contouring tool in ArcGIS Spatial Analyst. You will compute the geodetic datum shifts between North American Datum 1983 (NAD83) and North American Datum 1927 (NAD27) using a specific transformation method (NADCON). To make the project useful you will compute the datum shift in seconds of longitude and seconds of latitude for all 58,000 of the USGS 7.5 minute quadrangles (1:24,000 scale ) in the continental United States.
In this video, we explore the history of geodetic datums in the United States, and how they were established at a national level to assure consistency across mapping applications. For more information on geodetic datums, visit http://www.geodesy.noaa.gov/.
Developed in partnership with COMET Program/MetEd, "What is the Status of Today's Geodetic Datums?" examines the use of the current primary geodetic datums used in the U.S. (NAD 83 and NAVD 88), the challenges in maintaining these datums, and the inconsistencies that arise when they are used together with the latest satellite-based mapping technologies. For more information on geodetic datums, visit http://www.geodesy.noaa.gov/. Original video source: http://www.ngs.noaa.gov/corbin/class_description/NGS_Video_Library.shtml
Most common used geographic coordinate reference system is World Geodetic System 1984 (WGS 84). Since it is difficult to manipulate with degrees and in some contexts it is not enough precise, many countries established their own metric coordinate system. QGIS Library has a lot of predefined coordinate reference systems, but if any local system doesn't exist in library, you can look for it on web. The link is spatialreference.org. For my own practice I downloaded one part of California map and reproject it from WGS 84 to mostly common use coordinate reference system in California - North America Datum 1983 (shorten NAD83). From Raster - Reprojections, open Warp (Reproject), select input and output files and define source and target spatial reference system. If desired CRS doesn't exist...
The road to choosing custom projections is not paved with sundrops and lilies. It is time to start learning the nuts and bolts of coordinate systems. Minute Markers: -0:27- Geodesy, the geoid. -1:10- Ellipsoid, geographic coordinate system. -2:09- Can't effectively measure with ellipsoid. -3:21- Planar coordinate system. -3:49- Geodetic datums. -5:41- Projections. -6:47- REMEMBER this, degrees vs. linear units. -7:10- Three types of projections. -7:32- Recap. All images included are in the public domain, though the geoid image was originally created here I believe (correct me if I'm wrong): http://www.esa.int/spaceinimages/Images/2004/10/The_Earth_s_gravity_field_geoid_as_it_will_be_seen_by_GOCE
not american, barely north american. ten thousand years of history (but hey, who's counting anyway?) dissolved and forgotten in just over five hundred. hold on man, let me check my notes. two continents chock full of people can be destroyed and gone unnoticed? are you kidding me? survival should be based on fairness, not fitness. and just remember that as three hundred million sing 'this land is your land' we scream 'basta ya'. this country is still wet to the touch, saturated with greed conquest and blood⦠conveniently stuffed under the rug. this may be overdue: fuck you. a different time? well that can't replace the countless cultures that have been erased. established in 1492, i'm not american.