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  2. Wilkes-Barre Area High School - Wikipedia

    en.wikipedia.org/wiki/Wilkes-Barre_Area_High_School

    Wilkes-Barre Area High School is a high school in the Wilkes-Barre Area School District, located in Plains, Pennsylvania.The student body mascot is the Wolfpack.The school opened in August 2021, replacing James M. Coughlin High School, G. A. R. Memorial Junior/Senior High School, and Elmer L. Meyers Junior/Senior High School.

  3. Northern Basin and Range ecoregion - Wikipedia

    en.wikipedia.org/wiki/Northern_Basin_and_Range...

    The largest of the Northern Basin and Range subregions, the High Lava Plains covers 10,262 square miles (26,578 km 2) in Oregon and 5,740 square miles (14,867 km 2) in Nevada, featuring a variety of land uses, including rangeland, wildlife habitat, irrigated pastureland and cropland, historic gold and silver mines, and active opal mines and ...

  4. Wilkes-Barre Area School District - Wikipedia

    en.wikipedia.org/wiki/Wilkes-Barre_Area_School...

    As of 2020–2021, total student enrollment in the district was 7.089, according to National Center for Education Statistics data. The district operates five elementary schools, one middle school, one junior high school and one high school, Wilkes-Barre Area High School.

  5. AOL Mail

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    Get AOL Mail for FREE! Manage your email like never before with travel, photo & document views. Personalize your inbox with themes & tabs. You've Got Mail!

  6. Geology of Tasmania - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Tasmania

    The Barrington Chert is finely laminated and has flaggy bedding. It is found in the Dial Range and Fossey Mountain Troughs, up to 1 km thick. The Motton Spilite lies on top of the chert. It consists of pillow lava, massive lava flows, sediments made from volcanic fragments, and chert breccia. The basalt is an ocean floor type.

  7. Lava field - Wikipedia

    en.wikipedia.org/wiki/Lava_field

    The two main types of lava field structures are defined as sheet flow lava and pillow lava. Sheet flow lava appears like a wrinkled or folded sheet, while pillow lava is bulbous, and often looks like a pile of pillows atop one another. [2] An important aspect of lava flow morphology is a phenomenon known as lava flow inflation.

  8. Scotch Plains-Fanwood Regional School District - Wikipedia

    en.wikipedia.org/wiki/Scotch_Plains-Fanwood...

    The Scotch Plains-Fanwood Regional School District is a regional public school district serving students from two communities in Union County, in the U.S. state of New Jersey. The district serves students in pre-kindergarten through twelfth grade , who come from the Township of Scotch Plains and the Borough of Fanwood .

  9. Public Schools of the Tarrytowns - Wikipedia

    en.wikipedia.org/wiki/Public_Schools_of_the...

    Union Free School District of the Tarrytowns, also known as Public Schools of the Tarrytowns, is a school district headquartered in Sleepy Hollow, New York. The district includes most of Sleepy Hollow (within the Town of Mount Pleasant ) and a portion of Tarrytown (within the Town of Greenburgh ).