Matches in DBpedia 2016-04 for { <http://wikidata.dbpedia.org/resource/Q20687079> ?p ?o }
Showing triples 1 to 47 of
47
with 100 triples per page.
- Q20687079 abstract "Many glacial erratic boulders (often simply called glacial erratics) can be found in the Puget Sound region as far south as the Yelm area where the Puget Lobe of the glacier reached its maximum extent.The Pleistocene ice age glaciation of Puget Sound created many of the geographical features of the region, including Puget Sound itself, and the erratics are one of the remnants of that age. According to Nick Zentner of Central Washington University Department of Geological Sciences, "Canadian rocks [are] strewn all over the Puget lowland, stretching from the Olympic Peninsula clear over to the Cascade Range." Erratics can be found at altitudes up to about 1,300–1,600 feet (400–490 m) in the Enumclaw area, along with kames, drumlins, and perhaps also the unique Mima mounds. The soil of Seattle, the state's largest city, is approximately 80% glacial drift, most of which is Vashon glacial deposits (till), and nearly all of the city's major named hills are characterized as drumlins (Beacon Hill, First Hill, Capitol Hill, Queen Anne Hill) or drift uplands (Magnolia, West Seattle). Boulders greater than 3 meters in diameter are "rare" in the Vashon till, but can be found, as seen in the table below.".
- Q20687079 thumbnail Martha_Lake_Erratic_2015_1.jpg?width=300.
- Q20687079 wikiPageExternalLink waglacialerratics.ess.washington.edu.
- Q20687079 wikiPageWikiLink Q1011590.
- Q20687079 wikiPageWikiLink Q1040770.
- Q20687079 wikiPageWikiLink Q1054064.
- Q20687079 wikiPageWikiLink Q1362720.
- Q20687079 wikiPageWikiLink Q1438765.
- Q20687079 wikiPageWikiLink Q1507935.
- Q20687079 wikiPageWikiLink Q1510424.
- Q20687079 wikiPageWikiLink Q1513207.
- Q20687079 wikiPageWikiLink Q1513976.
- Q20687079 wikiPageWikiLink Q1585716.
- Q20687079 wikiPageWikiLink Q181908.
- Q20687079 wikiPageWikiLink Q187408.
- Q20687079 wikiPageWikiLink Q191704.
- Q20687079 wikiPageWikiLink Q192701.
- Q20687079 wikiPageWikiLink Q19878093.
- Q20687079 wikiPageWikiLink Q20712201.
- Q20687079 wikiPageWikiLink Q225469.
- Q20687079 wikiPageWikiLink Q2610088.
- Q20687079 wikiPageWikiLink Q3030228.
- Q20687079 wikiPageWikiLink Q3131132.
- Q20687079 wikiPageWikiLink Q3292203.
- Q20687079 wikiPageWikiLink Q3480552.
- Q20687079 wikiPageWikiLink Q372934.
- Q20687079 wikiPageWikiLink Q427711.
- Q20687079 wikiPageWikiLink Q430267.
- Q20687079 wikiPageWikiLink Q5083.
- Q20687079 wikiPageWikiLink Q5115859.
- Q20687079 wikiPageWikiLink Q520549.
- Q20687079 wikiPageWikiLink Q588153.
- Q20687079 wikiPageWikiLink Q604141.
- Q20687079 wikiPageWikiLink Q657810.
- Q20687079 wikiPageWikiLink Q6823200.
- Q20687079 wikiPageWikiLink Q6861924.
- Q20687079 wikiPageWikiLink Q7116309.
- Q20687079 wikiPageWikiLink Q7457541.
- Q20687079 wikiPageWikiLink Q7979189.
- Q20687079 wikiPageWikiLink Q7979192.
- Q20687079 wikiPageWikiLink Q803903.
- Q20687079 wikiPageWikiLink Q852989.
- Q20687079 wikiPageWikiLink Q859199.
- Q20687079 wikiPageWikiLink Q917402.
- Q20687079 comment "Many glacial erratic boulders (often simply called glacial erratics) can be found in the Puget Sound region as far south as the Yelm area where the Puget Lobe of the glacier reached its maximum extent.The Pleistocene ice age glaciation of Puget Sound created many of the geographical features of the region, including Puget Sound itself, and the erratics are one of the remnants of that age.".
- Q20687079 label "Glacial erratic boulders of the Puget Sound region".
- Q20687079 depiction Martha_Lake_Erratic_2015_1.jpg.