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Doane Rock
Doane Rock is a glacial erratic located in Eastham, Massachusetts on the grounds of the Cape Cod National Seashore. It is the largest exposed boulder on Cape Cod. It stands 18 feet (5.5 m) high and extends below the ground an estimated 12 feet (3.7 m). This boulder is named after Deacon John Doane, one of Eastham's original settlers. It has also been called Enochs or Enos rock for the deacon's son, as well as Great Rock. The rock was left by the glaciers (Laurentide Ice Sheet The Laurentide Ice Sheet was a massive sheet of ice that covered millions of square miles, including most of Canada and a large portion of the Northern United States, multiple times during the Quaternary glacial epochs, from 2.58 million years a ...; 18,000–12,000 years ago) between what is now the Salt Pond Visitors Center and Coast Guard Beach. Doane Rock is located just off Doane Road about one mile past the Salt Pond Visitor Center on National Park Service land. Limited parking is available n ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Doane Rock 2006
Doane may refer to: Surname * D. Howard Doane, American agricultural expert * George Washington Doane (1799-1859), American churchman and bishop * Gustavus Cheyney Doane - U.S. Army Cavalry, member of Washburn-Langford-Doane Expedition * Henry Doane (1905-1999), American landscape painter and commercial artist * John Doane (c 1590), early settler of Eastham, Massachusetts * J. Chalmers Doane Canadian Musician and Educator * Ken Doane (born 1986), American professional wrestler * Mary Ann Doane, American professor * Melanie Doane (born 1967), Canadian pop singer-songwriter * Percy Gray Doane (1877-1945), of New York City * Rennie Wilbur Doane (1871–1942), American entomologist * Seth Doane, American journalist * William Croswell Doane (1832-1913), American Bishop of the Episcopal church * William Howard Doane (1832-1915), American hymn writer * Brigham Doane, American professional hardcore wrestler * , co-founder of Doane College * Chris Doane (born 1961), Lead singer ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacial Erratic
A glacial erratic is glacially deposited rock differing from the type of rock native to the area in which it rests. Erratics, which take their name from the Latin word ' ("to wander"), are carried by glacial ice, often over distances of hundreds of kilometres. Erratics can range in size from pebbles to large boulders such as Big Rock () in Alberta. Geologists identify erratics by studying the rocks surrounding the position of the erratic and the composition of the erratic itself. Erratics are significant because: *They can be transported by glaciers, and they are thereby one of a series of indicators which mark the path of prehistoric glacier movement. Their lithographic origin can be traced to the parent bedrock, allowing for confirmation of the ice flow route. *They can be transported by ice rafting. This allows quantification of the extent of glacial flooding resulting from ice dam failure which release the waters stored in proglacial lakes such as Lake Missoula. Erratics ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eastham, Massachusetts
Eastham () is a town in Barnstable County, Massachusetts, United States, Barnstable County being coextensive with Cape Cod. The population was 5,752 at the 2020 census. For geographic and demographic information about the village of North Eastham, please see North Eastham, Massachusetts. History Originally inhabited by the Nauset tribe, Eastham was the site where in 1620 a hunting expedition landed, comprised from the crew of the sailing vessel ''Mayflower'', which had stopped in Provincetown harbor on Cape Cod Bay after a rough crossing of the Atlantic Ocean, which led to the first encounter of the Pilgrims and the local Nauset people at First Encounter Beach. The area would not be settled by Europeans, however, until 1644. The original lands included what are now the towns of Truro, Wellfleet, Eastham, Orleans and a small portion of Chatham. Eastham town was officially incorporated in 1651. Eastham is the birthplace of Freeman Hatch, who in 1853 set the world record for a si ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cape Cod National Seashore
The Cape Cod National Seashore (CCNS), created on August 7, 1961, by President John F. Kennedy, encompasses on Cape Cod, in Massachusetts. It includes ponds, woods and beachfront of the Atlantic coastal pine barrens ecoregion. The CCNS includes nearly of seashore along the Atlantic-facing eastern shore of Cape Cod, in the towns of Provincetown, Truro, Wellfleet, Eastham, Orleans and Chatham. It is administered by the National Park Service. Places of interest Notable sites encompassed by the CCNS include Marconi Station (site of the first two-way transatlantic radio transmission), the Highlands Center for the Arts (formerly the North Truro Air Force Station), the Dune Shacks of Peaked Hill Bars Historic District (a 1,950-acre historic district containing dune shacks and the dune environment), and the glacial erratic known as Doane Rock. A former United States Coast Guard station on the ocean in Truro is now operated as a 42-bed youth hostel by Hostelling International USA. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Doane Rock
Doane Rock is a glacial erratic located in Eastham, Massachusetts on the grounds of the Cape Cod National Seashore. It is the largest exposed boulder on Cape Cod. It stands 18 feet (5.5 m) high and extends below the ground an estimated 12 feet (3.7 m). This boulder is named after Deacon John Doane, one of Eastham's original settlers. It has also been called Enochs or Enos rock for the deacon's son, as well as Great Rock. The rock was left by the glaciers (Laurentide Ice Sheet The Laurentide Ice Sheet was a massive sheet of ice that covered millions of square miles, including most of Canada and a large portion of the Northern United States, multiple times during the Quaternary glacial epochs, from 2.58 million years a ...; 18,000–12,000 years ago) between what is now the Salt Pond Visitors Center and Coast Guard Beach. Doane Rock is located just off Doane Road about one mile past the Salt Pond Visitor Center on National Park Service land. Limited parking is available n ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
John Doane
John Doane (c.1590 - 1685/6) was a politician in English Colonial North America. He arrived in Plymouth Colony on an unknown ship sometime between 1628 and 1632. During his long life he is considered a person of note in Plymouth Colony serving in many government capacities associated with the colony government, such as government committees and deputy for Plymouth as well as Assistant Governor in 1632/33. He left government service for a time in the 1630s to serve as deacon in the Plymouth Church. English Origins John Doane stated he was born in England and in his 1678 will he stated he was age about eighty-eight years of age making his birth year being about 1590. Nothing else is known of his English ancestry. There is no record of John Doane being in Leiden, Holland, although he was a Plymouth church deacon. In Plymouth Colony In 1632/33 he was Assistant Governor.Robert Charles Anderson, ''Pilgrim Village Family Sketch: John Doane'' (a collaboration between American Ancestor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Laurentide Ice Sheet
The Laurentide Ice Sheet was a massive sheet of ice that covered millions of square miles, including most of Canada and a large portion of the Northern United States, multiple times during the Quaternary glacial epochs, from 2.58 million years ago to the present. The last advance covered most of northern North America between c. 95,000 and c. 20,000 years before the present day and, among other geomorphological effects, gouged out the five Great Lakes and the hosts of smaller lakes of the Canadian Shield. These lakes extend from the eastern Northwest Territories, through most of northern Canada, and the upper Midwestern United States (Minnesota, Wisconsin, and Michigan) to the Finger Lakes, through Lake Champlain and Lake George areas of New York, across the northern Appalachians into and through all of New England and Nova Scotia. At times, the ice sheet's southern margin included the present-day sites of coastal towns of the Northeastern United States, and cities such as Bos ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coast Guard Beach (Eastham, Massachusetts)
Coast Guard Beach is part of the Cape Cod National Seashore in Eastham, Massachusetts. From mid-June to Labor Day, the parking area at this location is closed to all but park staff and visitors who are disabled, and access is provided by shuttle bus from the Little Creek parking area (across from the Doane Area). Although the parking lot at Coast Guard Beach is open the remainder of the year, parking is limited. There are seasonal restrooms and a wheelchair-accessible rampway to the beach. Coast Guard Beach is popular among locals and tourists for surfing and boogie boarding. It is one of five Cape Cod National Seashore beaches that are on the ocean side of the Cape, generally providing a better surf than beaches on the bay side. Low tide exposes a fairly flat stretch of beach, making it also popular for skimboarding. History The Outer Beach The outer beach, or "backside," of Cape Cod has been the notorious graveyard for more than 3,000 ships since the wreck of the ''Sparrow ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arthur Newell Strahler
Arthur Newell Strahler (February 20, 1918 – December 6, 2002) was a geoscience professor at Columbia University who in 1952 developed the Strahler Stream Order system for classifying streams according to the power of their tributaries. Strahler was largely responsible for the shift from qualitative to quantitative geomorphology Geomorphology (from Ancient Greek: , ', "earth"; , ', "form"; and , ', "study") is the scientific study of the origin and evolution of topographic and bathymetric features created by physical, chemical or biological processes operating at or n ... during the mid 20th century. Significant works *Strahler, A. N. (1952). "Dynamic basis of geomorphology". ''Geological Society of America Bulletin'' 63: 923–938. *Strahler, A. N. (1952). "Hypsometric (Area-Altitude) analysis of erosional topography". ''Geological Society of America Bulletin'' 63: 1117–1142. *Strahler, A. N. (1957). "Quantitative analysis of watershed geomorphology". ''Eos, Transactions A ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Barnstable County, Massachusetts
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are the fo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landmarks In Barnstable County, Massachusetts
A landmark is a recognizable natural or artificial feature used for navigation, a feature that stands out from its near environment and is often visible from long distances. In modern use, the term can also be applied to smaller structures or features, that have become local or national symbols. Etymology In old English the word ''landmearc'' (from ''land'' + ''mearc'' (mark)) was used to describe a boundary marker, an "object set up to mark the boundaries of a kingdom, estate, etc.". Starting from approx. 1560, this understanding of landmark was replaced by a more general one. A landmark became a "conspicuous object in a landscape". A ''landmark'' literally meant a geographic feature used by explorers and others to find their way back or through an area. For example, the Table Mountain near Cape Town, South Africa is used as the landmark to help sailors to navigate around southern tip of Africa during the Age of Exploration. Artificial structures are also sometimes built t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacial Erratics Of Massachusetts
A glacial period (alternatively glacial or glaciation) is an interval of time (thousands of years) within an ice age that is marked by colder temperatures and glacier advances. Interglacials, on the other hand, are periods of warmer climate between glacial periods. The Last Glacial Period ended about 15,000 years ago. The Holocene is the current interglacial. A time with no glaciers on Earth is considered a greenhouse climate state. Quaternary Period Within the Quaternary, which started about 2.6 million years before present, there have been a number of glacials and interglacials. At least eight glacial cycles have occurred in the last 740,000 years alone. Penultimate Glacial Period The Penultimate Glacial Period (PGP) is the glacial period that occurred before the Last Glacial Period. It began about 194,000 years ago and ended 135,000 years ago, with the beginning of the Eemian interglacial. Last Glacial Period The last glacial period was the most recent glacial period wi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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