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    A Móri borvidék az Észak-Dunántúli szőlőtermelő tájba tartozik. A borvidék mikroklímájára, uralkodó szélirányára, rányomja bélyegét a Vértes és a Bakony között húzódó Móri árok. A Móri árok tektonikai törésvonal a Bakony és a Vértes között. Homokos dombsoraival kitûnõ szõlõtermõ terület. A Vértes alacsony, sasbérces-árkos szerkezetû karsztos középhegység.

    A Bakonyt és a Vértest a Móri-árok süllyedékrendszere választja el. Ennek alapzatában kúpkarsztos felsõ-kréta-eocén peneplénmaradványok ismerhetõk fel harmadidõszaki durvatörmelékes üledékekkel fedve. A mai morfológiai jellemzőjét a felsõ-pliocén-negyedidõszaki felszínformálódás szabta meg kavicssapkás tanúhegyekkel, hosszanti, széles dombhátakkal, tagolt hegylábfelszínekkel, szõlõkultúrás, lankás hegylábi lejtõkkel.

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    Ez a hazai viszonyainkat tekintve közepes értékű szőlőtermesztési viszonyokat tesz lehetővé. Mindazonáltal, a hegyek, dombok déli-délnyugati oldalain a kedvező mezo- és mikroklíma jó termőhelyi viszonyokat alakíthat ki. A meredek domboldalakon a teraszos művelés elemeit is megtaláljuk.