List Yayasan Baby Sitter, PRT, Perawat Orang Sakit/Lansia. List Yayasan Baby Sitter, PRT, Perawat Orang Sakit/Lansia. List of Yayasan Suster in Indonesia. Update Senin, 2. 0 Februari 2. List Baby Sitter ini direkomendasikan oleh netter dunia- ibu. Score/Rate: Score diberikan oleh rekan. Kwalifikasi Yayasannya bukan baby sitternya, dengan nilai 1 – 4, dimana angka 4 adalah angka untuk nilai sangat bagus sedangkan angka 1 adalah nilai paling jelek yang sebaiknya jangan menjadi tujuan. Saya menampilkan list yayasan baby sitter (bs) ini buat berbagi pengetahuan dan pengalaman. Saya tak ada kaitan dengan salah satu yayasan baby sitter manapun. Saya hanyalah seorang konsumen biasa yang ingin sharing agar yang mau atau yang sudah mengambil bs tak menghadapi masalahnya sendirian. Hi, mommies. Walaupun di depan kita kelihatan manis, sopan, dan rajin, ternyata sering sekali pada saat kita tidak melihat mereka berlaku kebalikannya. Jangan lupa melakukan cek latar belakang dan info kelengkapan kartu identitas calon babysitter. Hati- hati kalau ambil PRT dari iklan koran, sudah banyak para mommy’s yang menjadi korban. Jika ingin menambah atau mengedit data, silahkan hubungi email saya atau langsung di blog saya yang lain juga boleh addressnya http: //anitanet. Jika ingin ikutan sharing juga bisa langsung entry di blog lain saya tersebut, link url lengkapnya: http: //anitanet. Tip’s untuk menyewa pengasuh bayi, perawat bayi, babysitter (BS): Cari referensi saat mencari penyalur baby sitter dengan reputasi baik. Cari pengasuh bayi yang berpengalaman pendidikan khusus merawat bayi. Lakukan wawancara singkat dengan calon pengasuh bayi. Baby sitter harus orang yang bersih, sabar dan luwes dalam mengasuh bayi. Lakukan uji coba sebelum meyewa baby sitter. Masih banyak lagi » Account Options. Masuk; Setelan penelusuran.Selama masa percobaan, amati cara kerja baby sitter. Minta data pribadi dari agen penyalur (KTP dan Ijazah Kursus Mengasuh Bayi)Carilah yang bisa diajak bekerja sama dalam mendidik anak. Keterangan: BABY SITTER (BS) / PERAWAT BAYIadalah Pekerja yang bertugas merawat bayi, mulai dari memandikan, memberi makan minum, membuatkan susu, dan menyiapkan segala keperluan bayi. Serta memperhatikan kesehatan dan tumbuh kembang sang bayi. Ciri- ciri Baby Sitter Pemula: – Umurnya masih muda, semangat tinggi untuk belajar– Tidak begitu gesit bekerja karena sering kelihatan bingung– Masih perlu diajari, sering bertanya terutama dalam memasak makanan anak– Mommies bisa menerapkan standar mommies dalam merawat sang buah hati kepada baby sitter nya– Gajinya lebih murah– Memiliki Mommies yang sudah berpengalaman memiliki bayi dan tidak terlalu sibuk dan masih mememiliki waktu untuk mengurus sang buah hati– Baby Sitternya hanya bekerja pada saat Mommies sedang bekerja saja– Mommies masih bisa menerapkan standar mommies dalam merawat sang buah hati kepada baby sitter nya– Biasanya masih senang main hp saat bekerja. ![]() Hati-hati penipuan lowongan kerja, email perusahaan ternama biasanya menggunakan akhiran.co.id contoh: [email protected] info lebih lanjut klik disini. Ciri- ciri Baby Sitter Pengalaman: – Umurnya lebih dewasa– Terampil mengurus anak termasuk memasak makanan anak– Gesit dalam bekerja– Biasanya sulit diajari karena sudah memiliki standard kerja tersendiri– Semangat belajar sudah tidak banyak– Gaji mahal– Mommies memiliki kesibukan yang tinggi (sibuk)– Baby Sitternya bekerja full day siang dan malam, jadi buah hati biasanya tidur bersama baby sitternya– Memiliki Mommies yang belum berpengalaman memiliki bayi– Biasanya tidak lagi suka main hp saat bekerja. NANNY / PERAWAT BALITAadalah Pekerja yang bertugas merawat balita, hampir sama tugasnya dengan babysitter hanya saja sang anak sudah bisa beraktivitas sendiri. Selain menyiapkan segala keperluan balita, nanny pula lah untuk mengajak bermain dan belajar. CAREGIVER / PERAWAT LANSIAadalah Pekerja yang bertugas merawat lansia seperti menyiapkan segala keperluan sehari hari, menjaga kebersihan lansia dan lingkungannya, mengontrol apa saja obat dan suplemen yang harus di konsumsi lansia serta mengajaknya berjemur atau berjalan- jalan. PEMBANTU RUMAH TANGGA (PRT)adalah Pekerja yang bertugas mengurusi pekerjaan rumah tangga seperti menyapu, mengepel, memasak, mencuci dan menyeterika serta tugas- tugas lain yang berhubungan dengan pekerjaan rumah tangga lainnya. PEKERJA INFAL BIASAadalah Pekerja infal biasa bekerja saat anda membutuhkan pekerja sementara diluar musim mudik lebaran. Minimal pemesanan pekerja untuk jangka waktu tujuh hari. Mengenai gaji pekerja infal biasa dihitung harian. PEKEJA INFAL LEBARANadalah Pekerja infal lebaran bekerja pada saat masa lebaran dan menggantikan pekerja reguler yang sedang mudik. Jangka waktu bekerja biasanya 1. List Yayasan Baby Sitter, PRT, Perawat Orang Sakit/Lansia: 1. LPK MELATI JAKARTA (Rate 4/1) Komplek Gunung Sahari Permai Blok E1 Lt. Gunung Sahari Raya No 6. Rt. 0. 06/Rw. 0. 01 Jakarta Pusat cp. Mia Ph 0. 21- 4. 25. HP 0. 85. 1. 0. 59. Pimpinan Heny Hartaty SE, Email : yys. Saat ini menyediakan tenaga infal baby sitter dan asisten rumah tangga untuk Lebaran 2. Gaji infal baby sitter Rp 2. Gaji infal lansia/perawat orang sakit Rp. Gaji infal Asisten Rumah Tangga Rp 1. Dharma Asih (Rate 1/2) Bunder Raya no. A Senen (Dekat Stasiun Senen), Telp : 3. BS, aku ga pernah lihat)3. Elita Vitita, Telp : 3. Hidup Sehat (Rate 1/1), Jl. Surabaya, Jakarta Pusat, cp. Ibu Ani, Telp : 3. Telp : 3. 86. 40. Ibu Wiji, Telp : 3. Mitra Ananda, Menteng, Jakarta Pusat, Telp : 8. Uber Taxi Jakarta Review Pengalaman plus minus naik Uber taxi di Jakarta. OLX Indonesia, pusat jual beli online terbesar di Indonesia. Semua barang ada disini, dari handphone, komputer, otomotif, fashion bahkan rumah dan lowongan kerja. Informasi Lowongan Kerja Terbaru di Semarang Tahun 2017 Hi Ibu Anita, Saya membaca blog ibu dan ingin menanyakan apa saya bisa posting ini di blog ibu? Cinta Keluarga (Rate 1/1), Setiabudi Barat No. Jakarta, Telp. 0. Lpk cinta keluarga blacklist, kirimin BS yang gak bisa apa. Minta cepet. 2 dikirimin uang admin, tanya terus uda transfer belum. Ternyata BS abal. Yulie Vanillaxaveria@gmail. Submitted on 2. 01. Yayasan Theresia (Rate 1/4), Jl. Letjen Suprapto, Gg. Siaga V RT. 0. 05/0. No. Cempaka Baru, Kec. Kemayoran, Jakarta Pusat 1. Menuk Saragih,Telp. Sebaiknya jangan mengambil BS dari yayasan ini lihat komentar no. Dina Aryana. Sebaiknya jangan mengambil BS dari Yayasan Theresia (sharing dari Lydia 1. AM). Bertambah lagi yang menilai jelek yayasan ini, yaitu dari Bu Stevi yang mengatakan yayasan ini oper. Grace Submitted on 2. Yayasan theresia, tgk rekomen banget deh, pelayanan buruk dan janji tinggal janji. Berarti sudah 4 orang mommies yang memberi nilai sangat buruk buat yayasan ini. Sebaiknya para mommies tidak mengambil BS dari yayasan ini. Jakarta Selatan. 1. Abadi, Ciputat, Jakarta Selatan, Telp : 7. Yayasan Sekar Tanjung (Rate 4/1, 1/1), Jakarta Selatan cp. Agus, Telp : 7. 20. Sebaiknya jangan ambil BS dari sini, ini kutipan sharing dari Bu Imelda : dulu saya pernah dari Pak Agus, tapi semua baby sitternya kayanya gak bisa ditegur punya. Dulu emang perjanjiannya kalau dalam 3 bulan gak ada ganti b. Ibu Lien, Telp : 7. Bunda Kasih, Kemang/ Pasar Minggu, Jakarta Selatan, cp : Ibu Yanti / dr. Gunawan, Telp : 7. Andhika Putra, Kantor Pusat: Jalan Sungai Sambas 2 No. Kebayoran Baru – Jakarta Selatan. No Telp : 0. 21- 7. No. HP : 0. 81. 29. WA) / 0. 81. 80. 60. Kantor Cabang Jakarta Timur : Jalan Pelatnas PBSI No. RT0. 10/RW0. 01 Cipayung – Jakarta Timur No. Hp : 0. 81. 29. 09. WA) / 0. 81. 80. 60. CP Jeremy Farizky < jeremy. Emis Leo, Pamulang, Jakarta Selatan, Telp : 7. Fantasia, Jl. Gandaria I No. Kebayoran Baru, Jakarta Selatan, cp. Ibu Tina, Telp : 7. Ibu Ripka, Jl. Bambu Kuning No. Pejaten, Pasar Minggu, Jakarta Selatan, cp. Ibu Ripka / Bapak Iwan, Telp : 7. Kasih Agape, Ciputat, Jakarta Selatan, cp. Ibu Caroline, Telp : 7. Kasih Ananda, Kebayoran Lama, Jakarta Selatan, Telp : 7. Kasih Bunda, Jl. Lebak Bulus Raya No. Kampung Kapuk, Jakarta Selatan, Telp : 7. Nusantara, Jl. Pulo Raya III No. A, Jakarta Selatan, cp. Eni / Yulvia, Telp : 7. Garansi 1 th boleh ganti 2x, gaji BS balita mahir 4 th Rp. Rp. 1 jt (Terimakasih buat Tan Ernie yang sudah menambahkan data ini)1. Pelita Kasih, Jl. Jurangmangu 5 Bintaro Jaya Sektor 5 Menteng Bintaro, Jakarta Selatan, cp. Ibu Fadlila / Ibu Nelly, Telp : 7. Putri Pertiwi, Jl. Damai, Petukangan, cp. Ibu Karmila/Ibu Nia, Telp : 7. Rahayu, Tebet, Jakarta Selatan, Telp : 8. Ria Asih (Rate 1/1), Jl. Maritim II No. 2, Cilandak Barat / seberang SUBUD, Jakarta Selatan, cp. Bapak Riyanto, Telp : 7. Rona, cp. Rona, Telp : 7. Samino, Telp : 7. Setia Ananda, Pangkalan Jati, Jakarta Selatan, Telp : 7. Siti, Jl. 2. 8 Pasar Jumat, Jakarta Selatan, cp. Ibu Siti, Telp. Ibu Rini, Telp : 7. Sr. Kristin, RS YPK, Kebayoran Baru Jakarta Selatan, cp. Kristin, Telp : 3. St. 2. 4, Kompleks Asisi, Menteng Dalam, Jakarta Selatan 1. Ibu Anton / Ibu Ida, Telp : 8. Harus telp tiap hari, harus ambil sendiri, pilih sendiri, jam- nya tertentu. Penerima telp- nya agak arogan)2. Tarsi, Bintaro Jakarta Selatan, Telp : 7. Tiara Cipta (Rate 1/1), RS. Fatmawati, Jakarta Selatan, Telp : 7. Titian, Jl. Tebet Timur Dalam 8 X No. Jakarta Selatan, Cp. Ibu Pur, Telp : 8. Triwahyu Handayani, Patal Senayan, Jakarta Selatan, cp. Darsono, Telp : 5. Mekar Sejati, (Rate 4/1), Cilandak KKO, cp. Ibu Astin/Bp. Taufik, 7. Anastasia, Jl. Banjar Sari II No. Jakarta Selatan. 1. Kasih Ibu Sejati, Jl. Mampang Prapatan XI, tlp. Saran: sebaiknya jangan ke No. Hiba Agency (cabang), jl. Yayasan Cendana Raya (Ibu Gito) jl. Uang admin 7. 10 rb + dp gaji pertama 5. Terimakasih buat Bu Mariasari yang sudah menambahkan data ini) Beberapa tahun lalu saya (Aer/Rohim) mengambil dari Yayasan tapi berhubung uang administrasi lumayan tinggi (dulu masih 6. Uang Administrasi Rp. BS dari sini, sharing Ibu Sylvia lihat komentar no. Ibu Tini, (Rate 1/1) Jl. Tebet Dalam IV Gg Keamanan 3 No. Tebet. Menyediakan PRT dan BS, untuk PRT via telp gaji ditawarkan 5. BS ditawarkan 7. 00rb. Tapi saat saya ke sana, ternyata nego langsung dengan PRT nyasendiri – tergantung beban pekerjaan juga. Akhirnya gaji yang saya janjikan 6. Garansi 2 bulan – diganti PRT/BS atau uang kembali setengah. O, iya uang administrasi 4. Terimakasih buat Aer/Rohim http: //aer- reborn. Sebaiknya jangan mengambil BS dari sini (lihat komentar no. Rini Astuti)3. 4. Yayasan Citra Kartini, Jl. Kucica XVI- Jf 1. No. 1. 7 Sektor 9 Bintaro Jaya. Website: http: //www. Email: info@citrakartini. BS dari sini ( not recommended) sharing dari ibu Esther Winata stock banyak tapi jelek dan malas)3. Al Ishlah Telp. 0. Pamulang. Ibu Nani.
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The Quartz Page: Occurrencelast modified: Thursday, 2. Sep- 2. 01. 1 0. 2: 1. CESTDocument status: usable, but incomplete. This chapter presents the most important geological environments in which quartz can be found. Many of these environments result in a characteristic appearance of the quartz specimen. Although the term . The veins can form under various conditions, and depending on these conditions, may or may not bear quartz crystals in them. The crack might form during folding of the rock in mountain- building processes, by shattering during tectonic events, by a decrease in pressure during the uplift of a rock, or because a rock cools down and shrinks. Hot brines that percolate the rocks and originate at greater depths with higher temperatures will precipitate the minerals they carry with them in cracks at lower temperatures and pressures. This process may continue until the crack is completely filled or may stop before, leaving . Hot brines that enter a crack in the rock from some distant hot source like a granite pluton first cool and precipitate most of their load rather quickly. The result is milky quartz, either massive or made of interlocked milky quartz crystals. Later, when the crystal growth slows down, the crystals may get less milky or even clear. In the majority quartz veins, most of the quartz is precipitated as massive, milky quartz, and well- formed crystals, if found at all, are only a small portion of the vein filling. These veins almost always run parallel to the major fracture zones of the large granite batholith that makes up large parts of northern Sardegna and the neighboring island of Corsica. A free standing quartz crystal can be seen sitting in a small pocket in the lower part of the image. ![]() Crystals were rarely clear at that location and often included small brown stains of iron oxides. The vein is not massive, but contains small pockets. Vertical quartz veins in a coarse-grained red granite at Cala Sarraina beach, at the northern end of the Costa Paradiso, Trinità d' Agultu, Sassari Province. How are geodes created and where can you find them? A geode is a spherical rock which contains a hollow cavity lined with crystals. How to Crack Open a Geode. If you've discovered a geode (a rounded rock formation with crystals or banding inside), you'll want to crack it open as safely and neatly. Geodes, reverse sceptor amethyst geode, dugway geode, Brazilial Agate crystal geode bookends, rare Mooralla geode, Ocos Geode lot of 5. Like the veins presented in Figs. It is a polished plate of slightly metamorphosed limestone (that is, it has been turned into marble) with a piece of a fossilized coral reef. How To Crack Open A Thunderegg Dig SitesThe rock is of Lower Miocene age. From a marble quarry at Josheghan village, at the southern slopes of the Karkas Mountains, Esfahan Province, Iran. In other cases there is an obvious pattern in the orientations of the veins: for example, when a igneous rock shrinks during cooling, the cracks may develop into a regular system of fissures that might be filled with quartz from percolating hot brines. The image shows a small pocket with small quartz crystals in an irregular vein in a granitic rock at the Kingston Mountain range in southern California. Small slightly smoky rock crystals have grown in random orientations on the milky gray vein quartz. Different from the veins shown so far these crystals have not been growing from the host rock, but grew in a fissure inside already present, massive quartz vein. From the western slopes of the Inyo Mountains, east of Aberdeen, Owens Valley, California. The outer parts bordering the host rock are mostly made of milky quartz while the core is made of more translucent quartz or even clear crystals. There is a brown line running through the base of the specimen that separates two quartz veins that formed successively. It is difficult to say which part is older, the upper or the lower, but if we assume it is the lower, the following happened: A crack formed in the host rock and was filled with hot brines. First milky quartz crystals grew, seen at the base of the specimen and immediately below the brown line. The crystals continued to grow into the gap from both walls, almost filling it out completely (there's a little pocket left near the middle of the lower vein). Note the sandwich structure with a darker core and a brighter border zone. Then the crack widened again, this time much more than before. The crack did not run through the freshly grown crystals, but along the upper border of the vein, along the brown line. Again, hot brines entered the vein and quartz started to grow from the rock walls, this time in two major phases. The first phase of crystal growth is marked by the gray zone above the brown line; note the typical quartz crystal shapes with milky phantoms at the left end of the specimen. In a second phase milky quartz overgrew the older crystals and continued to grow to finally form the rock crystals on top. From the Hakenkr. Sometimes colored minerals precipitate along with the quartz and amplify this pattern. Chlorite is often found in quartz veins but its major growth phase tends to be at lower temperatures than quartz, very often when the temperature has fallen so much that the quartz crystal growth wanes. A nice example of a pattern that is caused by successive phases of hot brines entering a crack is the specimen to the right. One can identify three major phases marked by dark green zig- zag lines of chlorite (the last one on the the rock crystals on top of the specimen). In addition one can see a zebra- like pattern of milky and translucent quartz zones. From Langvasseid, S. This image shows a part of the Eschbacher Klippen, a quartz vein outcrop that has weathered out of the softer surrounding rocks in the Taunus mountains north- west of Frankfurt, Germany. Although the rock appears brown, it is almost pure quartz and only superficially stained by iron and manganese oxides. The wall is up to 1. Some of the outer parts of it were initially filled with baryte that was later replaced by quartz. Field of view about 5. Initially, platy baryte crystals had grown in parts of the vein, but later they were replaced by quartz. The platy morphology is still visible in the rock. The gray- green color in the lower right corner is caused by chlorite inclusions. This image is also shown in the milky quartz section. It is, to my knowledge, the world's largest known quartz vein. At some places it has been weathered out of the rock to stand out as a wall up to 3. The Akademie der Geowissenschaften Hannover has a nice aerial image of the Pfahl. This specimen consists of smoky quartz, parts of which are almost clear, although there are no crystal faces. The parallel white lines that run through the specimen indicate fracture caused by tectonic activities. From the Turbechepf (or Turbek. The quartz in them did not grow in already present cracks in the rock. The quartz substance originates in the surrounding rock and has been concentrated in lenses. So the lenses got thicker in time and do not contain any pockets. At the same time, the original layering pattern gets disturbed by the redistribution process and the rocks may assume an undulating or . This mobilization and deposition of material from the neighboring rocks in veins pockets and is sometimes called lateral secretion to stress the difference from the deposition of material that has entered the rock in fluids and that originates at some distance. Note that the term lateral secretion also includes the deposition of material in crystal- bearing pockets. The minerals in the grains of the rock are usually not perfectly- built crystals, but contain a lot of impurities and show many faults in their crystal lattice, like dislocations and twinning. Quartz with impurities and lattice faults tends to dissolve more quickly (Blum et al., 1. As their formation involves a local redistribution and segregation of already present minerals, this type of quartz is sometimes called segregation quartz. These veins typically run roughly parallel to the layers of the rocks. It should be obvious that in this type of quartz vein cavities or pockets that bear any crystals cannot form during their formation. However, crystal- bearing pockets may be associated with them, as shown in the section Alpine- Type Fissures or Clefts. The veins are up to 5. Seen at the western slopes of Storenuten mountain, north of the Ringedalsvatnet lake at Odda, southwest Norway (field of view about 5- 6 m). Seen at the road SS1. Mandas and Seui, at the Lago del Flumendosa, Nuoro Province, Sardegna, Italy. The rock has been tilted, and the rocks have been slightly folded, but only on a large scale (field of view about 8. Seen at the SS1. 98, north of Gairo, Ogliastra, Nuoro Province, Sardegna, Italy. Although the layering of the schist is very disturbed, the rock as a whole has not been subject to shearing or folding, and on a large scale the layers remain horizontal over a large distance (field of view about 1 m). At the Grimsel Pass, Kanton Bern, Switzerland. Individual layers get thinner around the milky quartz lense. Also note that there is a sharp border between the quartz and the host rock, no transition zone. Some of the schist's layers run through the quartz lense, indicating that the quartz lens has widened in several phases. This is also proof that the observed pattern is not a boudinage. Sometimes a rock is called a migmatite because of the presence of segregation quartz veins in it, but this is a misnomer: segregation quartz forms at hydrothermal conditions, while in migmatites the segregation of minerals into vein- like structures is caused by partial melting of the rock. The dark and bright components are called melanosome and leucosome, respectively, and they are not monomineralic, but composed of different minerals: the leucosome is mostly made of quartz and feldspar and often approaches a granitic composition, the melanosome is enriched in dark minerals, very often biotite. At the Paso Novena (Nufenenpass), Val Bedretto, Ticino, Switzerland. The leucosome looks much more grainy and the borders between the leucosome and the melanosome are more irregular and less well defined than those at segregation quartz veins. This paragraph is about quartz occurrences in hydrothermal ore veins. These are cracks in the rock that have been filled with various minerals that precipitated from hot fluids. During the solidification of an intruded magmatic rock body it releases hot watery fluids rich in volatile compounds (HF, CO2, H3. BO3) that enter cracks in the surrounding rocks. Geodes from Spiritrockshop. Click on any photo to see a larger version. HOW GEODES FORM There are conflicting views about how geodes form, but most geologists agree that they begin as bubbles, sometimes in submarine limestone sediments, sometimes in a lava flow. Occasionally they form around the body of a sea creature on the ocean floor. Over time, the bubble is cast in a hard shell of silica, and water containing dissolved material is trapped inside. The precipitate that results is composed of a variety of minerals, usually quartz or calcite, but also aragonite, magnetite, barite and chalcopyrite. Manythousands of years later, weathering lifts the hard little silica orb away from the surrounding rock. The exterior of the sphere appears dull and pitted, which is no doubt why the Greeks called them “geoides”, meaning . However, on the inside, they can look heavenly. The precipitate forms a lining of inward projecting crystals and since different minerals harden at varying temperatures, the material forms layers(called Fortifications). Sometimes a cavity may be completely filled by layers. Purists refer to these geodes as nodules. Crack open a nodule and instead of a hollow crystalline core, you might find halos of brilliantly hued agate, produced where chalcedony- laden water precipitated within the shell. Geodes can also be filled with surrounding silt and sediments, forming a “mud ball.” If a crystal breaks off inside the geode, you can hear rattling (the only guarantee of a hollow geode!), these are often called “rattle stones”. Occasionally, water gets trapped in the geodes, forming what is called an “enhydro”, (Greek for “water inside”). WHERE TO FIND GEODESThe best locations to look are in deserts - the western states, especially Arizona, Utah, and Nevada are popular hunting grounds. California's Riverside and Imperial counties are particularly renowned for their geodes, as is Keokuk, Iowa, Mexico, Australia, Germany, Uruguay and Brazil. Click on links below for: Arkansas Geodes. Arkansas Geodes are very similar to a mix of Aragonite rich Kentucky Geodes and the Keokuk crystal geodes. Dugway Geodes. 6 to 8 million years ago, volcanic activity in Western Utah deposited an igneous rock called rhyolite. Trapped gases formed pockets in the rhyolite, which eventually became lined with chalcedony and quartz from groundwater. Most Dugway Geodes fluoresce a lime green color due to minute amounts of a secondary mineral that bonded with the quartz when it was growing. Western Utah. The lakes wave activity eroded the rhyolite and actually moved the geodes several miles away to their current location in Juab County, Utah. Choyas(Mexican Coconut) Geodes. Choyas geodes are mined in a 4. Chihuahua, Mexico called Las Choyas. Nicknamed “coconut geodes” because of their roundness and size, Choyas are literally hand dug with a pick axe out of tough bentonite clay. Miners fill potato sacks with the geodes and raise them up narrow shafts from 7. Composed mainly of any variety of quartz, including the ever popular amethyst, Choyas are especially fascinating because of the wide variety of secondary minerals found in them. Septarian Geodes. Septarian geodes formed 1. Gulf of Mexico reached up to southern Utah. When sea life died, it became trapped in sediments and formed mud balls. As the sea receded, the mud balls dried and cracked in the sun. The sea returned, and calcium from newly decomposing shells eventually seeped into the cracks and re- crystallized as calcite (yellow.) The thin brown wall is aragonite and the gray exterior is bentonite clay. The name Septarian comes from the Latin “septum”, meaning dividing wall. Brazilian Agate Geodes. Brazilian geodes are worked in a large open pit mining operation in Rio Grande de Sol, Brazil. These geodes are filled with beautiful layers of banded agate that form under relatively low temperatures of 4. A striking feature of the agate is the occurrence of dendritic inclusions resembling trees, bushes or even sunbursts, caused by a mineral growth of manganese oxide. Thunder Egg. According to ancient Native American legend, when the Thunder Spirits living in the highest recesses of snowcapped Mount Hood and Mount Jefferson became angry with one another, amid violent thunder and lightning storms they would hurl masses of these spherical rocks at each other. The hostile gods obtained these weapons by stealing eggs from the Thunderbirds' nests, thus the source of the name . The formation in which the geodes are found is 5. Brazil. Farmers have gathered the Oco’s for many years. After the crops have been harvested and the farmers are unable to work, the fields are tilled under allowing the Oco’s to appear. They are then gathered and sold for cutting into the geode half. This owner was the first to actually mine these small geodes. They were first brought to the USA by Luis Arzola of Juarez, Chihuahua, naming them after his daughter iliana. Delma Perry of El Paso Texas was the first to electroplate these magnificent small geodes (ilianites) and the rush was soon on as every jewelry house in the USA had to have these. They played out soon thereafter. A new claim was filed in 1. Keokuk Geodes Missouri Monster Geodes. Iowa geodes have long been objects of curiosity, their sparkling interiors containing some of the most beautiful crystals to be found anywhere in the Midwest. Although geodes are known from many localities around the world, one of the most productive and famous collecting regions is encompassed within a 3. Keokuk, Iowa. Rock collectors commonly refer to geodes from this region as . The township of Mooralla consisting mainly of a few buildings, is a few kilometres to the southeast. Access is via a rough track, which is often difficult to travel on, particularly following bouts of wet weather. The collecting area itself is Victoria’s only . The treasured smoky quartz . Where once good specimens could be extracted from near the surface, holes are now dug down to depths approaching 6 metres in the main part of the field. For those that like smaller specimens, loose crystals, or the other minerals that are occasionally found, shallow holes to about 2 meters deep at the perimeters of the field will fulfill their needs. Idar- oberstein Geodes. Geodes from the twin towns of Idar- Oberstein in the Nahe region of Germany are now very rare to find. Once abundant these agate geodes have all but disappeared from the collecting world. Through the years Idar- oberstein has become known as the gem cutting capital of the world. Sadly, all the local specimens have been well picked over and famous quarry's like the Setz are all now closed down. Most of the gems and stones from this famous location are now imported from Brazil. Mexican Reverse Scepter Amethyst Geode. These rare geodes are from a single source undisclosed location deep in the mountains of Mexico. We were lucky to get some of these before they disappeared into the annals of time, and may never be seen again. Kentucky Geodes. Kentucky geodes are . The Aragonite geodes sometimes have voids which display beautiful caverns. The more solid chalcedony and quartz geodes display yellows, reds and blues. Trancas Geodes. Mexican “Trancas” geodes were first found in 1. El Paso, Texas near Estacion Rancasm Aldama, Chihuahua province, Mexico. They contain mostly clear or drusy chalcedony quartz linings and may have secondary calcite or fluorite. Some VERY unique and Different Geodes that we find will be shown on this page. These are all . There are many Specialty Geodes from the Deccan Plains and Morocco. San Andreas Fault Geode. Very Rare Geode finds from the infamous San Andreas Fault Zone. How To Open A Geode. There are many different ways to open a geode, but no matter how you do it, the key is to be patient and not get in a hurry. With the flat chisel you have a better chance of opening the geode along the line you want it to open on. This method is mainly used in groups with children to protect pieces from flying and injuring someone. They cost in the $5. SAW CUTTINGThis is the most expensive method by far of opening geodes. Lapidary saws run in the $1. The main problem with sawing geodes is to tightly hold the geode in place while at the same time not applying so much pressure that the geode breaks from the vise. 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