JUD

I Want a Doughnut

Metode dan teknik pembelajaran partisipatif

IELTS Practice Tests

This title provides essential practice in all four modules of the IELTS examination: Listening, Reading, Writing and Speaking.

IELTS 1 Testbuilder Pack 2E

Jurus Cepat Kuasai CorelDraw

Buku ini membantu Anda menguasai CorelDraw secara cepat. Video tutorial disertakan untuk membantu Anda membuat desain-desain yang sangat kompleks dan panjang. Ukuran File Latihan dan Video Tutorial sebesar 2.6 Gb Kunjungi situs kami untuk mengunduh file latihan dan video tutorial: www.thinkjubilee.com

Evaluasi Program Pendidikan Luar Sekolah

Master Quranic Arabic in 24 hours

Have you ever wanted to learn the language in which the final revelation (Quran) was revealed? Maybe you thought learning Arabic was too difficult for you or that you were too old to learn a new language. Well in fact, not only is learning Quranic Arabic remarkably easy, it is also quite fun as you ll see throughout this 24-hour course. Even if you have little or no knowledge of Arabic, you ll feel comfortable going through these tutorials from the comfort of your home. At the end of each hour you will be able to put your knowledge into practice and begin to understand Quranic Arabic.

Memahami keberadaan Mahkamah Konstitusi di Indonesia

On Constitutional Court in Indonesian legal system.

Restrukturisasi dinas daerah bidang pengembangan potensi lokal

Cooperative Learning

Pendidikan luar sekolah

History and development of nonformal education in Indonesia.

Naskah akademik pengembangan pendidikan nonformal ke depan

Pola mobilitas pekerjaan

Pengambilan keputusan (decision making)

Tentang pengambilan keputusan

Manajemen program pendidikan untuk pendidikan luar sekolah dan pengembangan sumber daya manusia

Community empowerment dalam industri pariwisata di Bali

Effects of cooperative learning on achievement in secondary schools

Model kelembagaan pemerintah daerah untuk penguatan masyarakat lokal dalam mencapai efektifitas otonomi daerah

Layer Parallel Shortening: A Mechanism Used to Determine the Sequence of Deformation of the Little Water Syncline in the Tendoy Mountains, Southwestern Montana

The Little Water syncline is a complex structural feature within the Tendoy thrust sheet which formed during two temporally overlapping deformational episodes during the Late Cretaceous. The NNW-trending Four Eyes Canyon thrust and the structurally lower Tendoy thrust are associated with NE-SW-shortening related to the Cordilleran (Sevier-style) fold-thrust belt. The Tendoy thrust forms the structural front of the Cordilleran fold-thrust belt in southwestern Montana and its detached, NNW-trending overturned limb (of the Little Water syncline) was over-ridden by the Four Eyes Canyon thrust. Earlier research primarily used stratigraphic evidence coupled with geometric interpretations to suggest that: 1) clasts found in the syn-tectonic (Cretaceous) Beaverhead Formation were derived from the Four Eyes Canyon thrust; 2) Laramide-style deformation occurred before emplacement of the Tendoy thrust sheet; and 3) that the Tendoy thrust was then emplaced over the syn-tectonic Beaverhead Formation. The NE-trending (approximately 30o), overturned northern flank (at nearly right angles to the detached overturned limb) of the Little Water syncline has long been argued to be a structural feature associated with NW-SE-shortening (1̃20o) generally related to the Laramide Snowcrest thrust system. In this study of the Little Water syncline, I have used layer-parallel-shortening (LPS) strain-indicators (fossils and pellets) to obtain the initial direction of shortening preserved in: 1) the NNW-trending, detached, vertical-to-overturned, western limb; 2) the steeply-dipping-to-overturned, northwestern limb; and 3) the moderately W-dipping, upright, N-trending eastern limb to determine the initial deformation (Sevier or Laramide) that affected the syncline. When bedding is unfolded, LPS strain: at 11 of 14 sites is consistent with NE-SW-shortening (221o) associated with the Sevier orogeny; at 2 sites is consistent with N-S-shortening; and at 1 site is consistent with E-W-shortening. No sites have LPS strain consistent with NW-SE-shortening. Hence Sevier LPS strain occurred before Laramide deformation. The 3 sites (sites 1, 2, and 5) where LPS strain lies outside of Sevier-shortening (221o +20o), but not within the range of Laramide shortening (1̃10o-290o) likely represent Sevier LPS strain affected by local factors not accounted for in the retro-deformational sequence used to restore bedding to horizontal in this study. .