Glacial deposits and landforms at the terminus of a Laurentide ice stream, Oneida Lake, New York, from multichannel seismic reflection data

The deglaciation record of the Ontario Lowland and Mohawk Valley of North America is important for constraining the retreat history of the Laurentide Ice Sheet, end-Pleistocene paleoclimate, and ice-sheet processes. The Mohawk Valley was an important meltwater drainage route during the last deglaciation, with the area around modern Oneida Lake acting as a valve for meltwater discharge into the North Atlantic Ocean. The Mohawk Valley was occupied by the Oneida Lobe and Oneida Ice Stream during the last deglacial period. Multichannel seismic reflection data can be used to generate images of preglacial surfaces and internal structures of glacial bedforms and proglacial lake deposits, thus contributing to studies of deglaciation. This paper uses 217 km of offshore multichannel seismic reflection data to image the entire Quaternary section of the Oneida basin. A proglacial lake and paleo-calving margin is interpreted, which likely accelerated the Oneida Ice Stream, resulting in elongated bedforms observed west of the lake. The glacial bedforms identified in this study are buried by proglacial lake deposits, indicating the Oneida basin contains a record of glacial meltwater processes, including a 60-m-thick proglacial interval in eastern Oneida Lake.

Supplemental Material: A 740,000-yr-long Mohawk Lake record, Mohawk Valley, northeastern California, USA

Table S1. Stratigraphic descriptions from sites in Mohawk Valley. Table S2. Soil descriptions in Mohawk Valley. Figure S1. Stratigraphic columns for three sites along Jamison Creek (MV-47, MV-48, and MV-70). Figure S2. Stratigraphic column and photograph of site MV-45.

Supplemental Material: A 740,000-yr-long Mohawk Lake record, Mohawk Valley, northeastern California, USA

Table S1. Stratigraphic descriptions from sites in Mohawk Valley. Table S2. Soil descriptions in Mohawk Valley. Figure S1. Stratigraphic columns for three sites along Jamison Creek (MV-47, MV-48, and MV-70). Figure S2. Stratigraphic column and photograph of site MV-45.

Supplemental Material: A 740,000-yr-long Mohawk Lake record, Mohawk Valley, northeastern California, USA

Table S1. Stratigraphic descriptions from sites in Mohawk Valley. Table S2. Soil descriptions in Mohawk Valley. Figure S1. Stratigraphic columns for three sites along Jamison Creek (MV-47, MV-48, and MV-70). Figure S2. Stratigraphic column and photograph of site MV-45.

Short-Term Load Forecasting Using an Attended Sequential Encoder-Stacked Decoder Model with Online Training

The paper presents a new approach for the prediction of load active power 24 h ahead using an attended sequential encoder and stacked decoder model with Long Short-Term Memory cells. The load data are owned by the New York Independent System Operator (NYISO) and is dated from the years 2014–2017. Due to dynamics in the load patterns, multiple short pieces of training on pre-filtered data are executed in combination with the transfer learning concept. The evaluation is done by direct comparison with the results of the NYISO forecast and additionally under consideration of several benchmark methods. The results in terms of the Mean Absolute Percentage Error range from 1.5% for the highly loaded New York City zone to 3% for the Mohawk Valley zone with rather small load consumption. The execution time of a day ahead forecast including the training on a personal computer without GPU accounts to 10 s on average.

Quickening

This chapter highlights the works of Paul Schaefer and the archives of the Association for the Protection of the Adirondacks (AfPA) and other early conservation organizations. It analyses how Schaefer's foundation of a diverse coalition, aimed at protecting pristine Adirondack landscapes, culminated in the creation of the Adirondack Park Agency. The chapter reveals that the quickening of activism for wilderness protection in the United States took place in Schenectady, New York. It illustrates how a group of scientists and engineers who worked in the research labs of General Electric (GE) became more aware of threats to their wilderness and drew their passion toward political action. The chapter also describes the members of the Forest Preserve Association who multiplied their impact by encouraging established groups to join their cause. Their main prospects were the Adirondack Mountain Club, which represented hikers; the New York State Conservation Council, which represented hunters; and dozens of local outing groups like the Mohawk Valley Hiking Club. Ultimately, the chapter examines the impact of the Wilderness Act and how the New York's coalition of environmental became a powerful, well-coordinated political force.

Reviewer Acknowledgements

International Journal of Contemporary Education (IJCE) would like to acknowledge the following reviewers for their assistance with peer review of manuscripts for this issue. Many authors, regardless of whether IJCE publishes their work, appreciate the helpful feedback provided by the reviewers. Their comments and suggestions were of great help to the authors in improving the quality of their papers. Each of the reviewers listed below returned at least one review for this issue.Reviewers for Volume 4, Number 1 Aurora Q. Pestano, University of San Jose Recoletos, PhilippinesAziz Moummou, Ministry of Education, MoroccoBlessing Dwumah Manu, Jiangsu University, GhanaBožić-Lenard Dragana, University of Osijek Croatia, CroatiaBruna Gabriela Augusto Marçal Vieira, CEFET-MG, BrazilDina Radeljas, Mohawk Valley Community College, USAEdward Bolden, Case Western Reserve University, USAFederica Cornali, University of Turin, ItalyGiuseppe Maugeri, Ca' Foscari University, ItalyGraziano Serragiotto, Ca' Foscari University of Venice, ItalyInaad M Sayer, University of Human Development, IraqLi Li, Bath Spa University, UKMakrina Nina Zafiri, Aristotle University of Thessaloniki, GreeceMatthew Schatt, University of Florida, USANilgün Tosun, Trakya University, TurkeyRaymond Aaron Younis, ACU Australia, AustraliaTeresa Pozo-Rico, University of Alicante, SpainVassiliki Pliogou, Metropolitan College of Thessaloniki, GreeceVassilios Papadimitriou, University of Thessaly, Greece William OscarEditorial AssistantInternational Journal of Contemporary Education------------------------------------------------------------Redfame Publishing9450 SW Gemini Dr. #99416Beaverton, OR 97008, USATel: 1-503-828-0536 ext. 509Fax: 1-503-828-0537E-mail 1: [email protected] 2: [email protected]: http://ijce.redfame.com

113 in 1928? Validation of Delina Filkins as the First “Second-Century Teenager”

Delina Filkins was born May 4, 1815 in Stark, Herkimer County, New York, a small village of less than 2000 persons in the Hudson River Valley, Upstate New York. Her father, William Ecker, and mother, Susanna Herwick, were descended from Dutch and German settlers that came to the Mohawk Valley, New York, in the 1700s. Living her entire life in the same area within a ten-mile radius, her life spanned over 113 years. With the exception of her great age and her generally good health, Delina’s life was rather ordinary: she lived most of it on the family farm, helping with family tasks such as spinning yarn and making clothes. Delina married John Filkins, a local farmer, at age 18 and they had six (possibly seven) children together, two of whom outlived her. Delina was noted for her age in very late life, with local coverage from about 1916, then reaching national attention in the 1920s. With the understanding that Delina’s age was generally considered to be reliable by the press at the time, her case is a candidate for the earliest validated person to reach age 113+. This chapter takes a closer look at the case and the documents available and concludes that the amount and consistency of the available documentation suggest that Delina Filkins did indeed reach age 113 in 1928.

Reviewer Acknowledgements

International Journal of Contemporary Education (IJCE) would like to acknowledge the following reviewers for their assistance with peer review of manuscripts for this issue. Many authors, regardless of whether IJCE publishes their work, appreciate the helpful feedback provided by the reviewers. Their comments and suggestions were of great help to the authors in improving the quality of their papers. Each of the reviewers listed below returned at least one review for this issue.Reviewers for Volume 3, Number 2 Aurora Q. Pestano, University of San Jose Recoletos, PhilippinesAziz Moummou, Ministry of Education, MoroccoBlessing Dwumah Manu, Jiangsu University, GhanaBožić-Lenard Dragana, University of Osijek Croatia, CroatiaBruna Gabriela Augusto Marçal Vieira, CEFET-MG, BrazilDina Radeljas, Mohawk Valley Community College, USAEdward Bolden, Case Western Reserve University, USAFederica Cornali, University of Turin, ItalyFroilan Delute Mobo, Philippine Merchant Marine Academy, PhilippinesGiuseppe Maugeri, Ca' Foscari University, ItalyGraziano Serragiotto, Ca' Foscari University of Venice, ItalyInaad M Sayer, University of Human Development, IraqIosif Fragkoulis, Hellenic Open University, GreeceJavier Fombona, Univ. Oviedo, SpainLi Li, Bath Spa University, UKMatthew Schatt, University of Florida, USAMurat Tezer, Near East University, CyprusNesrin Ozturk, Ege University, TurkeyRaymond Aaron Younis, ACU Australia, AustraliaSaid K. Juma, State University of Zanzibar, TanzaniaSandro Sehic, Oneida BOCES, USASuriadi Samsuri, Institute of Islamic Religion Sultan Muhammad Syafiuddin Sambas, IndonesiaTeresa Pozo-Rico, University of Alicante, SpainVassiliki Pliogou, Metropolitan College of Thessaloniki, Greece William OscarEditorial AssistantInternational Journal of Contemporary Education------------------------------------------------------------Redfame Publishing9450 SW Gemini Dr. #99416Beaverton, OR 97008, USATel: 1-503-828-0536 ext. 509Fax: 1-503-828-0537E-mail 1: [email protected] 2: [email protected]: http://ijce.redfame.com

Northward subglacial drainage during the Mackinaw Interstade in the Cayuga basin, central New York, USA

The history of deglaciation in the Finger Lakes region since the Valley Heads readvance is questioned by recent research in the Cayuga basin, which concludes that, instead of forming a series of proglacial lakes, drainage during the Mackinaw Interstade was into the Laurentide ice sheet. First suspected in the Dryden–Virgil Valley where there is an absence of a lake outlet or surficial lacustrine deposits, this conclusion was explicitly revealed in the Sixmile–Willseyville trough where ice margin channels funneled water into the ice front. Further support was found in the Cayuga Inlet Valley, where a kettle kame terrane sloped northward into the ice front. Northward drainage was preceded by southerly drainage, with reversal occurring about 16.3 kyr ago. Multi-channel seismic profiles at the south end of Lake Cayuga reveal a south-sourced subaqueous sedimentary fan at the base of the lacustrine sequence. This fan is correlated with a coarse and heterogeneous clastic sequence penetrated in water wells in the City of Ithaca and requires northward drainage into a subglacial lake, which precludes the existence of proglacial lakes Ithaca, Newberry, and Hall. The proposed subglacial flow path is through the Cayuga trough, exiting the ice front eastward in the Mohawk Valley. Subglacial drainage from the Cayuga trough probably was part of a regional subglacial drainage system during the Mackinaw Interstade. Studies north of Lake Ontario have led to the proposal of a subglacial lake in the Ontario basin at that time, which likely also drained into the Mohawk Valley.