Alu­minum ores — is the main source of alu­minum, which has wide appli­ca­tion in indus­try, con­struc­tion and alloy pro­duc­tion.

Cop­per is one of the most impor­tant non-fer­rous met­als, which is wide­ly used in elec­tri­cal engi­neer­ing and ener­gy.

Cobalt ores are an impor­tant source of strate­gic met­al, which is wide­ly used in high-tech indus­tries.

Tin ores are used in mod­ern tech­nolo­gies, in par­tic­u­lar in elec­tron­ics, mechan­i­cal engi­neer­ing and alloy pro­duc­tion.

Mer­cury ores are a strate­gi­cal­ly impor­tant raw mate­r­i­al used in the chem­i­cal, min­ing and instru­ment-mak­ing indus­tries.

Anti­mo­ny ores are a valu­able raw mate­r­i­al for many strate­gic indus­tries, from met­al­lur­gy and elec­tron­ics to med­i­cine.

Mag­ne­sium ores are formed under the con­di­tions of evap­o­ra­tion of salt basins or meta­mor­phism of ultra­maf­ic rocks.

Arsenic, which has long been used in med­i­cine, has found its appli­ca­tion in met­al­lur­gy, chem­i­cal indus­try and elec­tron­ics.

Nick­el ores — is an impor­tant source of nick­el, which is wide­ly used in met­al­lur­gy, chem­i­cal indus­try and alloy pro­duc­tion.

Peb­bles are a valu­able nat­ur­al mate­r­i­al that is wide­ly used in con­struc­tion, land­scape design and dec­o­ra­tion.

Syen­ite is a deep igneous rock that formed as a result of slow cool­ing of mag­ma.

In gen­er­al, the num­ber of Euro­pean coun­tries where ground­wa­ter pre­dom­i­nates in the struc­ture of water sup­ply is 65%.

The geo­graph­i­cal con­di­tions of the Kyiv region con­tributed to the active devel­op­ment of the sub­soil.

Geo­log­i­cal mon­u­ment – are objects of nat­ur­al ori­gin that char­ac­ter­ize the course of geo­log­i­cal process­es.

Min­er­al resources of the Autonomous Repub­lic of Crimea are an impor­tant strate­gic resource for the coun­try.

Min­er­als in Donet­sk region include sig­nif­i­cant reserves of hard coal, anti­mo­ny-mer­cury ores, dolomite, lime­stones, marls, etc.

Luhan­sk region is defined not only by cul­tur­al her­itage, but also by an incred­i­ble wealth of min­er­als.

Min­er­als of the Kher­son region are rep­re­sent­ed by more than 110 deposits, which we will talk about in the arti­cle.

Min­er­als of the Zapor­izhzhia region are not lim­it­ed to deposits of con­struc­tion raw mate­ri­als, many inter­est­ing objects have been found here.

Myko­laiv region rep­re­sents a sig­nif­i­cant min­ing region with a diverse range of min­er­al resources.

Min­er­als of the Dnipropetro­vsk region are of key impor­tance for indus­try.

With­in Kyiv region, three deposits and sev­er­al dozen occur­rences of kaolin have been iden­ti­fied.

The soft­ware ensures the effi­cien­cy and accu­ra­cy of the sur­vey­or’s work.

The sub­soil of Cherni­hiv region has a fair­ly diverse com­po­si­tion of min­er­als.

Cherkasy region is locat­ed at the inter­sec­tion of two sub­provinces in Ukraine.

The aquifers of the city of Kyiv are used to pro­vide res­i­dents of the cap­i­tal with high-qual­i­ty drink­ing water.

Khmel­nyt­skyi region is rich in var­i­ous non-min­er­al min­er­als.

The use of new tech­nolo­gies in field recla­ma­tion is becom­ing more and more pop­u­lar.

Mines of the Rivne region are an impor­tant ele­ment of the min­ing indus­try, which plays a key role in the devel­op­ment of the region.

Min­er­als of the Lviv region con­tribute to the devel­op­ment of the local econ­o­my.

The sta­bil­i­ty of the sides of the quar­ry is one of the most impor­tant con­di­tions for the safe­ty of pro­duc­tion process­es.

The design of peat devel­op­ment requires com­pli­ance with the stan­dards of bal­anced use of resources.

Valu­able min­er­als of the Ode­sa region play an impor­tant role in the devel­op­ment of Ukraine.

Min­er­als of the Volyn region and their role in the bal­anced devel­op­ment of the region.

Min­er­als of the Ivano-Frankivsk region are key for its eco­nom­ic devel­op­ment.

Many min­er­al deposits have been found on the ter­ri­to­ry of Cher­nivt­si region.

Spe­cial water use is an impor­tant com­po­nent of enter­prise activ­i­ty.

Com­mis­sion­ing a deposit is a com­plex process that includes sev­er­al stages and requires high tech­ni­cal com­pe­tence.

The ter­ri­to­ry of the Sumy region is famous for its deposits of com­bustible min­er­als.

Oper­a­tional recon­nais­sance is car­ried out to clar­i­fy data about the object of oper­a­tion.

Min­er­als of the Polta­va region have great poten­tial for the eco­nom­ic devel­op­ment and indus­try of Ukraine.

420 min­er­al deposits are record­ed on the ter­ri­to­ry of Kharkiv region.

Con­struc­tion min­er­als of the Ternopil region play a deci­sive role in the econ­o­my.

Zhy­to­myr Oblast is a unique region in terms of the num­ber and vari­ety of min­er­als.

Min­er­als of the Vin­nyt­sia region are of great impor­tance for the devel­op­ment of indus­try, ener­gy and con­struc­tion.

Kirovohrad region is con­sid­ered one of the most resource-inten­sive in Ukraine.

The ter­ri­to­ry of the Kyiv region is locat­ed with­in the Dnipro-Donet­sk depres­sion and the Ukrain­ian shield and its slopes.

Lead and zinc ores are wide­ly used in the pro­duc­tion of alloys, for anti-radi­a­tion pro­tec­tion, elec­tron­ics and med­i­cine.

Flint — is a hard sed­i­men­ta­ry rock that is wide­ly used in the pro­duc­tion of abra­sives, dec­o­ra­tion and archi­tec­tur­al ele­ments.

Chalk is a soft sed­i­men­ta­ry rock con­sist­ing main­ly of cal­cite remains of marine organ­isms.

Nepheline is a min­er­al of the class of alu­mi­nosil­i­cates and a valu­able indus­tri­al raw mate­r­i­al of great impor­tance.

Bischof­ite is a nat­ur­al min­er­al-chlo­ride rich in mag­ne­sium, which is formed dur­ing the evap­o­ra­tion of salt pools.

Corun­dum is a super­hard alu­minum oxide formed in meta­mor­phic and mag­mat­ic con­di­tions and has a char­ac­ter­is­tic glassy shine.

Molyb­de­num is wide­ly used in met­al­lur­gy for alloy­ing ultra-strong steels for demand­ing appli­ca­tions.

Vana­di­um — is a strate­gic met­al with wide appli­ca­tions in the steel, avi­a­tion, ener­gy and chem­i­cal indus­tries.

Lithi­um ores — is a source of strate­gic met­al used for bat­ter­ies, met­al­lur­gy and ceram­ics.

Beryl­li­um ores are a valu­able source of a light­weight and strong met­al used in the aero­space, elec­tron­ics, and defense indus­tries.

Ura­ni­um ores are nat­ur­al min­er­al for­ma­tions con­tain­ing ura­ni­um at con­cen­tra­tions suit­able for indus­tri­al extrac­tion.

Rubid­i­um and cesium are rare alka­li met­als that occur main­ly in rare-met­al peg­matites and salt deposits.

Iodine and bromine are halo­gens of sig­nif­i­cant indus­tri­al impor­tance, and in Ukraine they are con­cen­trat­ed in min­er­al waters.

Mar­shal­lite con­sists of tiny quartz crys­tals that may seem insignif­i­cant, but they have great prac­ti­cal and sci­en­tif­ic impor­tance.

Ice­land spar is a unique vari­ety of cal­cite capa­ble of split­ting a light beam into two rays.

Talc is an extreme­ly soft, lay­ered sil­i­cate that forms dur­ing the meta­mor­phism of ultra­maf­ic rocks and can be eas­i­ly ground into a pow­der.

Shun­gite — is a car­bon-con­tain­ing meta­mor­phic rock enriched with amor­phous car­bon and known for its sorp­tion prop­er­ties.

Phl­o­go­pite is a min­er­al from the mica group known for its fire resis­tance, ther­mal insu­la­tion prop­er­ties and dec­o­ra­tive appeal.

Andesite — is an vol­canic or sub­vol­canic rock of por­phyry struc­ture con­sist­ing main­ly of medi­um pla­gio­clase.

Anorthosite is an igneous rock of the gab­bro group, which lies in mas­sifs and is char­ac­ter­ized by almost com­plete dom­i­nance of pla­gio­clase.

Form­ing in deep con­di­tions, dior­ite acquires a coarse-grained struc­ture and dec­o­ra­tive prop­er­ties.

Gab­bro is an intru­sive igneous rock of the main com­po­si­tion, which forms sig­nif­i­cant mas­sifs and is wide­ly used as a valu­able raw mate­r­i­al.

Feldspars — are a group of alu­mi­nosil­i­cate min­er­als that are the most com­mon rock-form­ing com­po­nents of the earth­’s crust.

Migmatite is a com­plex rock that con­sists of two or more com­po­nents (pale­o­so­ma and neo­so­ma), usu­al­ly repeat­ed lay­ered.

Dacite is a medi­um-sil­i­cate vol­canic rock between andesite and rhy­o­lite, con­sist­ing main­ly of pla­gio­clase and quartz.

Gneiss is a durable rock that is formed under the influ­ence of high tem­per­a­tures and pres­sure in the depths of the earth­’s crust.

Mon­zonite is a coarse-grained (phaner­it­ic) igneous rock. It is known for its inter­me­di­ate com­po­si­tion between two types of rocks: dior­ite and syen­ite.

Paly­gorskite, also known as atta­pulgite, is a clay min­er­al, an hydrous mag­ne­sium sil­i­cate with a fil­a­men­tous chain-lay­ered struc­ture.

Pla­giogran­ite. Intru­sive rock as a wit­ness of the deep process­es of the plan­et Pla­giogran­ite is a light-gray gran­ite char­ac­ter­ized by […]

Hafni­um and zir­co­ni­um are impor­tant met­als which, due to their unique physic­o­chem­i­cal prop­er­ties, are wide­ly used in nuclear ener­gy.

Micro­cline — is a com­mon rock-form­ing min­er­al of gran­ites and peg­matites, rep­re­sent­ed by var­i­ous shades of col­or.

Zakarpat­tia Region, locat­ed in west­ern Ukraine, impress­es with its nat­ur­al beau­ty and diver­si­ty of resources.

Arte­sian waters are pres­sur­ized ground­wa­ter occur­ring at sig­nif­i­cant depths between two imper­me­able rock lay­ers.

In order to reduce risks and oper­a­tional costs, a promis­ing tech­nol­o­gy has emerged — unmanned aer­i­al vehi­cles.

The extrac­tion of min­er­al resources can sig­nif­i­cant­ly dam­age the envi­ron­ment.

PGE are a rare and valu­able raw mate­r­i­al for many branch­es of mod­ern indus­try.

Brick and tile raw mate­ri­als — are nat­ur­al clay rocks that have wet plas­tic­i­ty and the abil­i­ty to hard­en after fir­ing.

Rare earth ele­ments are a group of met­als that give mate­ri­als unique prop­er­ties

Sand­stone is a dense sed­i­men­ta­ry rock formed from cement­ed grains of quartz and feldspar.

Mus­covite is a trans­par­ent, lay­ered mica min­er­al char­ac­ter­ized by high elas­tic­i­ty and a glassy lus­ter.

Dia­mond is the hard­est nat­ur­al min­er­al, dis­tin­guished by its extra­or­di­nary trans­paren­cy, bril­liance, and ther­mal con­duc­tiv­i­ty.

Alu­nite is a sul­fate min­er­al formed by hydrother­mal alter­ation, occur­ring as white or pink mass­es.

Pyro­phyl­lite is a soft lay­ered sil­i­cate with a scaly tex­ture.