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Lake Albany
Glacial Lake Albany was a prehistoric North American proglacial lake that formed during the end of the Wisconsinan glaciation. It existed between 15,000 and 12,600 years ago and was created when meltwater from a retreating glacier, along with water from rivers such as the Iromohawk, became ice dammed in the Hudson Valley. Organic materials in Lake Albany deposits have been carbon dated to approximately 11,700 years ago. The lake spanned approximately from present-day Poughkeepsie to Glens Falls. Lake Albany drained about 10,500 years ago through the Hudson River due to post-glacial rebound. When the lake drained it exposed the sandy and gravelly glaciolacustrine deposits left by the glacier, along a broad plain just west of Schenectady, where the Mohawk emptied into the lake. Dune and deltaic A river delta is a landform shaped like a triangle, created by deposition of sediment that is carried by a river and enters slower-moving or stagnant water. This occurs where a river ente ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacial Lakes Albany, Champlain, Hitchcock, Winsooski, & Merrimack
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 and icehouse Earth, 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 m ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schenectady, New York
Schenectady () is a city in Schenectady County, New York, United States, of which it is the county seat. As of the 2020 census, the city's population of 67,047 made it the state's ninth-largest city by population. The city is in eastern New York, near the confluence of the Mohawk and Hudson rivers. It is in the same metropolitan area as the state capital, Albany, which is about southeast. Schenectady was founded on the south side of the Mohawk River by Dutch colonists in the 17th century, many of whom came from the Albany area. The name "Schenectady" is derived from the Mohawk word ''skahnéhtati'', meaning "beyond the pines" and used for the area around Albany, New York. Residents of the new village developed farms on strip plots along the river. Connected to the west by the Mohawk River and Erie Canal, Schenectady developed rapidly in the 19th century as part of the Mohawk Valley trade, manufacturing, and transportation corridor. By 1824, more people worked in manufac ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Champlain Sea
The Champlain Sea (french: Mer de Champlain) was a prehistoric inlet of the Atlantic Ocean into the North American continent, created by the retreating ice sheets during the closure of the last glacial period. The inlet once included lands in what are now the Canadian provinces of Quebec and Ontario, as well as parts of the American states of New York and Vermont. Origins The mass of ice from the continental ice sheets had depressed the rock beneath it over millennia. At the end of the last glacial period, while the rock was still depressed, the Saint Lawrence and Ottawa River valleys, as well as modern Lake Champlain, at that time the Lake Vermont, were below sea level and flooded with rising worldwide sea levels, once the ice no longer prevented the ocean from flowing into the region. As the land gradually rose again, in the process known as isostatic rebound, the sea coast gradually retreated to its current location. The sea lasted from about 13,000 years ago to about ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Colonie, New York
Colonie is a town in Albany County, New York, United States. It is the most-populous suburb of Albany, and is the third-largest town in area in Albany County, occupying approximately 11% of the county. Several hamlets exist within the town. As of the 2020 census, the town had a total population of 85,590. The name is derived from the Dutch ''Colonye'' or "Colonie", derived from the Colonie of Rensselaerswyck. All the land outside the Village of Beverwyck (now Albany) was referred to as the "Colonie". The town of Colonie is north of Albany and is at the northern border of the county. Within the town of Colonie are two villages, one also known as Colonie and the other known as Menands. History This area was once part of the Rensselaerwyck manor. The town of Colonie was formed in 1895 after the rural residents of the town of Watervliet opposed the state's proposal to transform the entire town into the city of Watervliet. The town and village of Green Island was also s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lisha Kill
Lisha Kill is a hamlet in the town of Colonie, Albany County, New York, United States. Lisha Kill lies on New York Route 5 (Central Avenue) in the western section of the town. The hamlet received its name from the creek of the same name, Lisha Kill, ''kill'' being Dutch for creek or stream. The stream is also referred to as Lisha's Kill and received its name from a local legend about a Native American woman who is buried along its banks. History Lisha Kill's history is intimately tied to the creek of the same name. Originally called Lysiens Kill, local legend says Lisha's Kill is named for a Native American woman who was buried along its banks. Some of the earliest settlers were of the Lansing family, a family long associated with nearby Albany, Cohoes, and Lansingburgh; Jacob Lansing is considered the first to have settled in the area and John V.A. Lansing, another early settler, arrived in 1792. His house still stands and has been on the National Register of Historic Plac ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Patroon Creek
Patroon Creek is a stream in Albany County, New York, Albany County, New York (state), New York, United States and is a tributary of the Hudson River which flows south to New York Harbor and the Atlantic Ocean. The creek's source (river or stream), source is Rensselaer Lake in the western section of the City (New York), city of Albany, New York, Albany. Patroon Creek received its name from the patroon of Rensselaerswyck. History Patroon Creek, starting with Henry Hudson's discovery of the Hudson River, was a part of the Dutch Republic, Dutch colony New Netherland and the patroonship of Rensselaerswyck, founded in 1630. On the 1632 Map of Rensselaerswyck the mouth of the Patroon Creek is labeled as "Bloommaert's Burt", and Patroon Creek gained the name of Bloomaert's Kill (body of water), Kill, ''kill'' being the Dutch language, Dutch word for creek or stream. Another early name for the kill was Fifth Kill, it being the fifth (and final) kill (counting from the south) in the colonia ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rill
In hillslope geomorphology, a rill is a shallow channel (no more than a few inches/decimeters deep) cut into soil by the erosive action of flowing surface water. Similar but smaller incised channels are known as microrills; larger incised channels are known as gullies. Artificial rills are channels constructed to carry a water supply from a distant water source. In landscape or garden design, constructed rills are an aesthetic water feature. Rills created by erosion Rills are narrow and shallow channels which are eroded into unprotected soil by hillslope runoff. Since soil is regularly left bare during agricultural operations, rills may form on farmland during these vulnerable periods. Rills may also form when bare soil is left exposed following deforestation, or during construction activities. Rills are fairly easily visible when first incised, so they are often the first indication of an ongoing erosion problem. Unless soil conservation measures are put into place, ri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Till
image:Geschiebemergel.JPG, Closeup of glacial till. Note that the larger grains (pebbles and gravel) in the till are completely surrounded by the matrix of finer material (silt and sand), and this characteristic, known as ''matrix support'', is diagnostic of till. image:Glacial till exposed in roadcut-750px.jpg, Glacial till with tufts of grass Till or glacial till is unsorted glacier, glacial sediment. Till is derived from the erosion and entrainment of material by the moving ice of a glacier. It is deposited some distance down-ice to form terminal, lateral, medial and ground moraines. Till is classified into primary deposits, laid down directly by glaciers, and secondary deposits, reworked by fluvial transport and other processes. Description Till is a form of '' glacial drift'', which is rock material transported by a glacier and deposited directly from the ice or from running water emerging from the ice. It is distinguished from other forms of drift in that it is depos ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Albany Pine Bush
The Albany Pine Bush, referred to locally as the Pine Bush, is one of the largest of the 20 inland pine barrens in the world. It is centrally located in New York's Capital District within Albany and Schenectady counties, between the cities of Albany and Schenectady. The Albany Pine Bush was formed thousands of years ago, following the drainage of Glacial Lake Albany. The Albany Pine Bush is the sole remaining undeveloped portion of a pine barrens that once covered over , and is "one of the best remaining examples of an inland pine barrens ecosystem in the world." By 2008 it included all parcels of the Albany Pine Bush Preserve (a state nature preserve spanning ), the properties that connect these protected parcels, and some of the surrounding areas that abut the preserve. The Woodlawn Preserve and surrounding areas in Schenectady County are the western sections of the Pine Bush, separated geographically by other properties from the Albany Pine Bush Preserve in Albany Co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Topsoil
Topsoil is the upper layer of soil. It has the highest concentration of organic matter and microorganisms and is where most of the Earth's biological soil activity occurs. Description Topsoil is composed of mineral particles and organic matter and usually extends to a depth of 5-10 inches (13–25 cm). Together these make a substrate capable of holding water and air which encourages biological activity. There are generally a high concentration of roots in topsoil since this is where plants obtain most of their vital nutrients. It also plays host to significant bacterial, fungal and entomological activity without which soil quality would degrade and become less suitable for plants. Bacteria and fungi can be essential in facilitating nutrient exchange with plants and in breaking down organic matter into a form that roots can absorb. Insects also play important roles in breaking down material and aerating and rotating the soil. Many species directly contribute to the health ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
United States Geological Survey
The United States Geological Survey (USGS), formerly simply known as the Geological Survey, is a scientific agency of the United States government. The scientists of the USGS study the landscape of the United States, its natural resources, and the natural hazards that threaten it. The organization's work spans the disciplines of biology, geography, geology, and hydrology. The USGS is a fact-finding research organization with no regulatory responsibility. The agency was founded on March 3, 1879. The USGS is a bureau of the United States Department of the Interior; it is that department's sole scientific agency. The USGS employs approximately 8,670 people and is headquartered in Reston, Virginia. The USGS also has major offices near Lakewood, Colorado, at the Denver Federal Center, and Menlo Park, California. The current motto of the USGS, in use since August 1997, is "science for a changing world". The agency's previous slogan, adopted on the occasion of its hundredt ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lens (geology)
In geology, a lens or lentil is a body of ore or rock that is thick in the middle and thin at the edges, resembling a convex lens in cross-section. To thin out in all directions is to "lens out", also known as "lensing". The adjectives "lenticular" and "lentiform" are used to describe lens-like formations. Lenticle is a synonym for lentil, but may also refer to a fragment of rock that is lens-shaped. "Lenticule" is used for small lentil. A lentil may also refer a minor unit in a formation of rock, similar to a member but not generally spread out over a large geographical area. In this usage, the lentil thins out towards its edges. Lenticular bedding is a special form of rock interbedded mudrock and cross-laminated rippled sandstone Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) . ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
