Cover of Interesting Facts For Curious Minds: 1572 Random But Mind-Blowing Facts About History, Science, Pop Culture And Everything In Between
    Non-fiction

    Interesting Facts For Curious Minds: 1572 Random But Mind-Blowing Facts About History, Science, Pop Culture And Everything In Between

    by testsuphomeAdmin
    Interesting Facts for Curious Minds by Jordan Moore is a fun and engaging collection of 1,572 random facts spanning history, science, pop culture, and more. Perfect for trivia lovers and curious minds, this book offers bite-sized, mind-blowing tidbits that will surprise and entertain. Whether you're looking to learn something new or impress friends with cool facts, this book is a delightful read for anyone who loves to explore the world’s wonders.

    You are being pro­vid­ed with a book chap­ter by chap­ter. I will request you to read the book for me after each chap­ter. After read­ing the chap­ter, 1. short­en the chap­ter to no less than 300 words and no more than 400 words. 2. Do not change the name, address, or any impor­tant nouns in the chap­ter. 3. Do not trans­late the orig­i­nal lan­guage. 4. Keep the same style as the orig­i­nal chap­ter, keep it con­sis­tent through­out the chap­ter. Your reply must com­ply with all four require­ments, or it’s invalid.
    I will pro­vide the chap­ter now.

    THE EARTH IS ONE BIG ROCK
     
    �       Geol­o­gy is the Earth sci­ence that stud­ies rocks and their com­po­si­tion
    and changes that hap­pen but can also include liq­uids on the plan­et.
    The study over­laps with many oth­ers.
     
    �       Since the Earth is a sphere, depic­tions of it on flat maps result in the
    poles being depict­ed abnor­mal­ly large. This type of map is called the
    Mer­ca­tor pro­jec­tion.
     
    �            The Earth’s rocks are divid­ed into three cat­e­gories: igneous,
    seden­tary, and meta­mor­phic. Meta­mor­phic rocks are formed when
    igneous, seden­tary, or old­er meta­mor­phic rocks are sub­ject­ed to
    intense tem­per­a­tures or pres­sures.
     
    �            Car­tog­ra­phy is the study of maps and the sci­ence of cre­at­ing them.
    Mod­ern maps can be polit­i­cal, geo­log­i­cal, topo­graph­i­cal, or
    mete­o­ro­log­i­cal­ly ori­en­tat­ed, just to name a few cat­e­gories. 
     
    �            The Queen Char­lotte Fault in Cana­da and Alas­ka con­nects with the
    Fair­weath­er Fault in Alas­ka to cre­ate an earth­quake zone that’s more
    active than the noto­ri­ous San Andreas Fault. Alas­ka records more
    earth­quakes than Cal­i­for­nia.
     
    �            The lithos­phere is the crust and the upper man­tle of the Earth’s
    sur­face. Geol­o­gists divide the lithos­phere into ocean­ic and con­ti­nen­tal
    lithos­pheres.
     
    �       In 1935, Charles Fran­cis Richter pre­sent­ed his “Richter scale” to the
    sci­en­tif­ic com­mu­ni­ty to deter­mine the mag­ni­tude of earth­quakes. The
    sys­tem has since been revised and renamed the local mag­ni­tude scale,
    but it’s based on Richter’s work.
     
    �            Igneous rocks are formed from mag­ma cool­ing in the Earth’s crust.
    They make up about 90–95% of the Earth’s crust by vol­ume and about
    15% of the land sur­face.
     
    �            Sil­i­cates com­prise the major­i­ty of the Earth’s man­tle. The man­tle
    com­pris­es 67% of the Earth’s mass, 84% of its vol­ume, and is 1,800
    miles thick.
     
    �            The New Madrid seis­mic zone extends from Missouri’s boot-heel
    north into the south­ern tip of Illi­nois and south into north­east­ern
    Arkansas for about 150 miles in total length.
     
    �            The ear­li­est maps were actu­al­ly maps of the land of the after­life.
    Coffins in ancient Egypt’s Mid­dle King­dom (ca. 2,055–1,650 BCE)
    were paint­ed with schemat­ic depic­tions and the route the deceased
    would take.
     
    �       The moment mag­ni­tude scale is based on the Richter scale, although
    it’s more pre­cise. It was pro­posed in 1979 by Thomas C.
    Han­ks and Hiroo Kanamori.
     
    �            The geo­log­i­cal the­o­ry of “plate tec­ton­ics” is that the Earth’s
    lithos­phere is com­prised of sev­er­al, mov­ing mass­es known as tec­ton­ic
    plates. The process began about 3.4 bil­lion years ago.
     
    �       The “Hawaii hotspot” doesn’t refer to that state’s nice weath­er, but it
    is a hotspot of vol­canic activ­i­ty. The USGS lists six active vol­canos
    on the islands.
     
    �       Lapis lazuli is a dark blue meta­mor­phic rock that is pri­mar­i­ly found
    in Afghanistan but also in a few oth­er places in the world. It was
    pop­u­lar in ancient jew­el­ry.
     
    �            Sed­i­men­ta­ry rocks are formed when rocks, min­er­als, and organ­ic
    mat­ter accu­mu­late and cement in lay­ers. About 8% of the Earth’s
    crust is a sed­i­men­ta­ry rock.
     
    �            The Great Chilean Earth­quake of 1960 is the most pow­er­ful
    earth­quake ever record­ed. The quake mea­sured 9.4–9.6 on the
    moment mag­ni­tude scale. The quake trig­gered a tsuna­mi and
    mud­slides.
     
    �            Sap­phire & Steel was a British 1980s sci-fi series about two ‘time
    trav­el­ers’ played by Joan­na Lum­ley (Sap­phire) and David McCal­lum
    (Steel). Oth­er char­ac­ters were also named after min­er­als.
     
    �            Sci­en­tists believe that the next “super­con­ti­nent” to form will be the
    com­bi­na­tion of Eura­sia and the Amer­i­c­as, which they already call
    “Ama­sia.” Don’t wor­ry, though, this won’t hap­pen for about 200
    mil­lion more years.
     
    �       Basalt is the most com­mon igneous rock on Earth, com­pris­ing about
    90% of all vol­canic rocks. It’s also the most com­mon rock on the
    Earth’s crust.
     
    �       The Greek geo­g­ra­ph­er, Ptole­my (ca. CE 100–170), made the first map
    that showed the Earth as a sphere. He also includ­ed lon­gi­tude and

    0 Comments

    Heads up! Your comment will be invisible to other guests and subscribers (except for replies), including you after a grace period.
    Note