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Home > Art, Film & Photography > Struktur Bumi: Hidrologi, Lempeng Tektonik, Tektonik Lempeng, Tektonika Lempeng, Banjir, Oseanografi, Mintakat Riparian, Cknet-Ina, Litosfer
Struktur Bumi: Hidrologi, Lempeng Tektonik, Tektonik Lempeng, Tektonika Lempeng, Banjir, Oseanografi, Mintakat Riparian, Cknet-Ina, Litosfer

Struktur Bumi: Hidrologi, Lempeng Tektonik, Tektonik Lempeng, Tektonika Lempeng, Banjir, Oseanografi, Mintakat Riparian, Cknet-Ina, Litosfer


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About the Book

Sumber: Wikipedia. Halaman: 32. Bab: Hidrologi, Lempeng tektonik, Tektonik lempeng, Tektonika lempeng, Banjir, Oseanografi, Mintakat riparian, Cknet-ina, Litosfer, Akuifer artesis, Kepulauan Galapagos, Hidrosfer, Cincin Api Pasifik, Kerak bumi, Siklus air, Presipitasi, Lempeng Indo-Australia, Gunung meletus, Pergeseran Benua, Alfred Wegener, Lempeng Pasifik, Hidrogeologi, Ofiolit, Pangea, Rodinia, Mata air, Hidrografi, Lempeng Sunda, Lempeng Eurasia, Teori geosinklin, Pusat Data Oseanografi Britania, Gosong pasir, Punggung tengah samudra, Laut Labrador, Subduksi, Air tawar, Air asin, Air permukaan, Lempeng Burma, Kerak samudera, Busur Sunda, Palung, Dry dam, Diastropisme. Kutipan: Teori tektonika Lempeng (bahasa Inggris: ) adalah teori dalam bidang geologi yang dikembangkan untuk memberi penjelasan terhadap adanya bukti-bukti pergerakan skala besar yang dilakukan oleh litosfer bumi. Teori ini telah mencakup dan juga menggantikan Teori Pergeseran Benua yang lebih dahulu dikemukakan pada paruh pertama abad ke-20 dan konsep seafloor spreading yang dikembangkan pada tahun 1960-an. Bagian terluar dari interior bumi terbentuk dari dua lapisan. Di bagian atas terdapat litosfer yang terdiri atas kerak dan bagian teratas mantel bumi yang kaku dan padat. Di bawah lapisan litosfer terdapat astenosfer yang berbentuk padat tetapi bisa mengalir seperti cairan dengan sangat lambat dan dalam skala waktu geologis yang sangat lama karena viskositas dan kekuatan geser (shear strength) yang rendah. Lebih dalam lagi, bagian mantel di bawah astenosfer sifatnya menjadi lebih kaku lagi. Penyebabnya bukanlah suhu yang lebih dingin, melainkan tekanan yang tinggi. Lapisan litosfer dibagi menjadi lempeng-lempeng tektonik (tectonic plates). Di bumi, terdapat tujuh lempeng utama dan banyak lempeng-lempeng yang lebih kecil. Lempeng-lempeng litosfer ini menumpang di atas astenosfer. Mereka bergerak relatif satu dengan yang lainnya di batas-batas lempeng, baik divergen (menjauh), konvergen (ber...


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Product Details
  • ISBN-13: 9781233920198
  • Publisher: Books LLC, Wiki Series
  • Publisher Imprint: Books LLC, Wiki Series
  • Height: 246 mm
  • No of Pages: 34
  • Spine Width: 2 mm
  • Weight: 82 gr
  • ISBN-10: 1233920197
  • Publisher Date: 14 Sep 2011
  • Binding: Paperback
  • Language: Indonesian
  • Returnable: N
  • Sub Title: Hidrologi, Lempeng Tektonik, Tektonik Lempeng, Tektonika Lempeng, Banjir, Oseanografi, Mintakat Riparian, Cknet-Ina, Litosfer
  • Width: 189 mm


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