By DONNA L. LILLIAN
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These are chunks of ocean crust, harder and more resistant than the surrounding sediments, which wash away with greater ease. 20 F BIRTH OF A VALLEY Let’s recap the geologic events we’ve been describing. For about 80 million years, the geography of California featured a volcanic mountain range that shed sediments into a trough at the western edge of North America, forming the Great Valley sequence, a diverse accumulation of sand and mud, now transformed into sandstone and shale. West of this trough, at the far edge of the continent, lay a crustal bulge.
Cool temperatures and the narrow proﬁle of the valley, which shades the edges of the vineyards, make full ripening di‹cult. These conditions are of little concern to Eisele, as he has no interest in producing the powerful fruit-driven wines from extremely ripe grapes that are the height of wine fashion THE UNDERPINNINGS OF TERROIR F 41 today. Rather, Volker Eisele Cabernets are more restrained, elegant wines that keep drawing one’s attention and curiosity rather than providing information and satisfaction with the ﬁrst mouthful or two.
Under pressure, these gels slowly compress. As they do, clay minerals segregate from the silica-rich gel and concentrate as thin layers that form the ribbon-like character seen in these outcrops. You might wonder about the presence of Great Valley sequence rocks in the Mayacamas Mountains, far west of the Central Valley—the trough in which they THE UNDERPINNINGS OF TERROIR F 39 FIGURE 19. An outcrop of the Great Valley sequence near the top of Oakville Grade. The rocks are ﬁne-grained sandstones cut by a multitude of fractures.