Skip to main content

Quartz

  Quartz   Quartz is hexagonal and commonly occurs as crystals ranging in size form microscopic to crystals weighing several tons. Where it crystallizes unhindered by other crystals, such as in cavities in rock or in a liquid containing few other crystals, it shows well-developed hexagonal prisms and sometimes showing apparent hexagonal pyramids or dipyramid. When it crystallizes in an environment where growth is inhibited by the surroundings, it rarely show crystal faces. It is also found as microcrystalline masses, such as in the rock chert, and as  fibrous masses, such as in chalcedony. Vitreous lusture.   As visible crystals, Quartz is one of the more common rock forming minerals. It occurs in siliceous igneous rocks such as volcanic rhyolite and plutonic granitic rocks. It is common in metamorphic rocks at all grades of metamorphism, and is the chief constituent of sand. Because it is highly resistant to chemical weathering, it is found in a wide variety of sedimentary r
Post a Comment

Terms and Conditions

Terms and Conditions

Welcome to GEO-GENIUS!

These terms and conditions outline the rules and regulations for the use of GEO-GENIUS's Website, located at https://destro53a.blogspot.com.

By accessing this website we assume you accept these terms and conditions. Do not continue to use GEO-GENIUS if you do not agree to take all of the terms and conditions stated on this page.

The following terminology applies to these Terms and Conditions, Privacy Statement and Disclaimer Notice and all Agreements: "Client", "You" and "Your" refers to you, the person log on this website and compliant to the Company’s terms and conditions. "The Company", "Ourselves", "We", "Our" and "Us", refers to our Company. "Party", "Parties", or "Us", refers to both the Client and ourselves. All terms refer to the offer, acceptance and consideration of payment necessary to undertake the process of our assistance to the Client in the most appropriate manner for the express purpose of meeting the Client’s needs in respect of provision of the Company’s stated services, in accordance with and subject to, prevailing law of Netherlands. Any use of the above terminology or other words in the singular, plural, capitalization and/or he/she or they, are taken as interchangeable and therefore as referring to same.

Cookies

We employ the use of cookies. By accessing GEO-GENIUS, you agreed to use cookies in agreement with the GEO-GENIUS's Privacy Policy.

Most interactive websites use cookies to let us retrieve the user’s details for each visit. Cookies are used by our website to enable the functionality of certain areas to make it easier for people visiting our website. Some of our affiliate/advertising partners may also use cookies.

License

Unless otherwise stated, GEO-GENIUS and/or its licensors own the intellectual property rights for all material on GEO-GENIUS. All intellectual property rights are reserved. You may access this from GEO-GENIUS for your own personal use subjected to restrictions set in these terms and conditions.

You must not:

  • Republish material from GEO-GENIUS
  • Sell, rent or sub-license material from GEO-GENIUS
  • Reproduce, duplicate or copy material from GEO-GENIUS
  • Redistribute content from GEO-GENIUS

This Agreement shall begin on the date hereof.

Parts of this website offer an opportunity for users to post and exchange opinions and information in certain areas of the website. GEO-GENIUS does not filter, edit, publish or review Comments prior to their presence on the website. Comments do not reflect the views and opinions of GEO-GENIUS,its agents and/or affiliates. Comments reflect the views and opinions of the person who post their views and opinions. To the extent permitted by applicable laws, GEO-GENIUS shall not be liable for the Comments or for any liability, damages or expenses caused and/or suffered as a result of any use of and/or posting of and/or appearance of the Comments on this website.

GEO-GENIUS reserves the right to monitor all Comments and to remove any Comments which can be considered inappropriate, offensive or causes breach of these Terms and Conditions.

You warrant and represent that:

  • You are entitled to post the Comments on our website and have all necessary licenses and consents to do so;
  • The Comments do not invade any intellectual property right, including without limitation copyright, patent or trademark of any third party;
  • The Comments do not contain any defamatory, libelous, offensive, indecent or otherwise unlawful material which is an invasion of privacy
  • The Comments will not be used to solicit or promote business or custom or present commercial activities or unlawful activity.

You hereby grant GEO-GENIUS a non-exclusive license to use, reproduce, edit and authorize others to use, reproduce and edit any of your Comments in any and all forms, formats or media.

Hyperlinking to our Content

The following organizations may link to our Website without prior written approval:

  • Government agencies;
  • Search engines;
  • News organizations;
  • Online directory distributors may link to our Website in the same manner as they hyperlink to the Websites of other listed businesses; and
  • System wide Accredited Businesses except soliciting non-profit organizations, charity shopping malls, and charity fundraising groups which may not hyperlink to our Web site.

These organizations may link to our home page, to publications or to other Website information so long as the link: (a) is not in any way deceptive; (b) does not falsely imply sponsorship, endorsement or approval of the linking party and its products and/or services; and (c) fits within the context of the linking party’s site.

We may consider and approve other link requests from the following types of organizations:

  • commonly-known consumer and/or business information sources;
  • dot.com community sites;
  • associations or other groups representing charities;
  • online directory distributors;
  • internet portals;
  • accounting, law and consulting firms; and
  • educational institutions and trade associations.

We will approve link requests from these organizations if we decide that: (a) the link would not make us look unfavorably to ourselves or to our accredited businesses; (b) the organization does not have any negative records with us; (c) the benefit to us from the visibility of the hyperlink compensates the absence of GEO-GENIUS; and (d) the link is in the context of general resource information.

These organizations may link to our home page so long as the link: (a) is not in any way deceptive; (b) does not falsely imply sponsorship, endorsement or approval of the linking party and its products or services; and (c) fits within the context of the linking party’s site.

If you are one of the organizations listed in paragraph 2 above and are interested in linking to our website, you must inform us by sending an e-mail to GEO-GENIUS. Please include your name, your organization name, contact information as well as the URL of your site, a list of any URLs from which you intend to link to our Website, and a list of the URLs on our site to which you would like to link. Wait 2-3 weeks for a response.

Approved organizations may hyperlink to our Website as follows:

  • By use of our corporate name; or
  • By use of the uniform resource locator being linked to; or
  • By use of any other description of our Website being linked to that makes sense within the context and format of content on the linking party’s site.

No use of GEO-GENIUS's logo or other artwork will be allowed for linking absent a trademark license agreement.

iFrames

Without prior approval and written permission, you may not create frames around our Webpages that alter in any way the visual presentation or appearance of our Website.

Content Liability

We shall not be hold responsible for any content that appears on your Website. You agree to protect and defend us against all claims that is rising on your Website. No link(s) should appear on any Website that may be interpreted as libelous, obscene or criminal, or which infringes, otherwise violates, or advocates the infringement or other violation of, any third party rights.

Your Privacy

Please read Privacy Policy

Reservation of Rights

We reserve the right to request that you remove all links or any particular link to our Website. You approve to immediately remove all links to our Website upon request. We also reserve the right to amen these terms and conditions and it’s linking policy at any time. By continuously linking to our Website, you agree to be bound to and follow these linking terms and conditions.

Removal of links from our website

If you find any link on our Website that is offensive for any reason, you are free to contact and inform us any moment. We will consider requests to remove links but we are not obligated to or so or to respond to you directly.

We do not ensure that the information on this website is correct, we do not warrant its completeness or accuracy; nor do we promise to ensure that the website remains available or that the material on the website is kept up to date.

Disclaimer

To the maximum extent permitted by applicable law, we exclude all representations, warranties and conditions relating to our website and the use of this website. Nothing in this disclaimer will:

  • limit or exclude our or your liability for death or personal injury;
  • limit or exclude our or your liability for fraud or fraudulent misrepresentation;
  • limit any of our or your liabilities in any way that is not permitted under applicable law; or
  • exclude any of our or your liabilities that may not be excluded under applicable law.

The limitations and prohibitions of liability set in this Section and elsewhere in this disclaimer: (a) are subject to the preceding paragraph; and (b) govern all liabilities arising under the disclaimer, including liabilities arising in contract, in tort and for breach of statutory duty.

As long as the website and the information and services on the website are provided free of charge, we will not be liable for any loss or damage of any nature.

Comments

Post a Comment

Popular posts from this blog

Types Of Metamorphic Textures

  STRUCTURES OF METAMORPHIC ROCKS (MACROTEXTURES): (i)                 Slaty cleavage : A pervasive, parallel foliation (layering) of fine-grained platy minerals (chlorite) in a direction perpendicular to the direction of maximum stress. It produces the rocks slate and phyllite. (ii)           Schistose : Schist has a lepidoblastic foliation if this foliation is defined by oriented mica, and a nematoblastic foliation if such a foliation is defined by the orientation of prismatic minerals as amphiboles and pyroxenes. (iii)        Gneissic :   A complex banded texture made of schistose layers or bands alternating with bands commonly characterized by a granoblastic texture. (iv)            Granoblastic: Granular, interlocking equi-dimensional grains of subequal size; no preferred orientation or cleavage. (v)              Hornfelsic : Fine-grained, granular interlocking grains, possibly of variable shapes and sizes. No preferred orientation. (vi)              Cataclastic : •
Post a Comment
Read more

HYDROTHERMAL ORE DEPOSITS

  HYDROTHERMAL ORE DEPOSITS                                                   Figure 1.1 HYDROTHERMAL PROCESS     Concentration by hot aqueous (water-rich) fluids flowing through fractures and pore spaces in rocks.   The fluid temperature ranges from 50 to 500 degree C. These fluid can be the final product of volcanic differentiation or the ground water got heated by contact of magma or chamber.   Hydrothermal deposits are produced when groundwater circulates to depth and heats up either by coming near to the hot igneous body at depth or by circulating to great depth along the geothermal gradient.   Such hot water can dissolve valuable substances throughout a large volume of rock. As the hot water moves into cooler areas of the crust, the dissolved substances are precipitated from the hot water solution. If the cooling takes place rapidly,  T hey might occur in open fractures or upon reaching a body of cool surface water, then precipitation will take place over a limi
3 comments
Read more

TEXTURES OF CLASTIC SEDIMENTARY ROCKS

TEXTURES OF CLASTIC SEDIMENTARY ROCKS           When sediment is transported and deposited, it leaves clues to the mode of transport and deposition. For example, if the mode of transport is by sliding down a slope, the deposits that result are generally chaotic in nature, and show a wide variety of particle sizes. Grain size and the interrelationship between grains gives the resulting sediment texture. Thus, we can use the texture of the resulting deposits to give us clues to the mode of transport and deposition.   Figure 1.1 - Type of sorting Sorting :-   The degree of uniformity of grain size. Particles become sorted on the basis of  density, because of the energy of the transporting medium. High energy currents can carry larger fragments. As the energy decreases, heavier particles are deposited and lighter fragments continue to be transported. This results in sorting due to density. If the particles have the same density, then the heavier particles will also be larger,
Post a Comment
Read more