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annabellemarocco.hatenablog.com
| | dionnecauterucci.hatenablog.com
0.9 parsecs away

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| | I do my thing and you do yours. I am not on this world to live up to your dreams, so you are not in this world to live up to mine. You are you and I am I, however, if by chance we discover one another well, then it is nice. Otherwise, it can't be helped.
| | margueritacanes.hatenablog.com
1.5 parsecs away

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| | I do my thing and you do your own. I'm not present in this earth to live up to your hopes, and furthermore you are not in this world to live up to mine. You're you and I am I, naturally, if by chance we find one another well, its pleasurable. If it's not,
| | socorrokras.hatenablog.com
1.9 parsecs away

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| | I do my thing and you do yours. I am not here in this planet to live up to your wants, and additionally you're not in this world to live up to mine. You are you and I am I, and if by chance we find one another, then it is nice. If it is not, it cannot be
| | egqsj.copernicus.org
13.1 parsecs away

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| Abstract. In the last decades surface exposure dating using cosmogenic nuclides has emerged as a powerful tool in Quaternary geochronology and landscape evolution studies. Cosmogenic nuclides are produced in rocks and sediment due to reactions induced by cosmic rays. Landforms ranging in age from a few hundred years to tens of millions of years can be dated (depending on rock or landform weathering rates) by measuring nuclide concentrations. In this paper the history and theory of surface exposure dating are reviewed followed by an extensive outline of the fields of application of the method. Sampling strategies as well as information on individual nuclides are discussed in detail. The power of cosmogenic nuclide methods lies in the number of nuclides availa...