Горный парк «Рускеала» — объект культурного наследия и главный туристический комплекс Республики Карелия.

На месте заполненного грунтовыми водами бывшего карьера до 1990-х годов функционировал мраморно-известковый завод, а каменоломни Рускеалы начинают свою историю с 1765 году.

В книге подробно рассказывается история добычи мрамора на Рускеальских мраморных ломках, о применении рускеальского мрамора в архитектуре Санкт-Петербурга.

Книга полезна и интересна краеведам, историкам, географам, геологам, работникам музеев, экскурсоводам и туристам.

The East African Orogen (EAO) marks one of earth’s greatest collision zones, a global feature in space (about 6000 km long where it is preserved in Africa and Antarctica; Fig. 1) and in time (350 million years of evolution) (Stern, 1994). The EAO formed when fragments of East and West Gondwana collided, beginning ~630 Ma ago (Meert, 2003). The southern part of the EAO is also known as the Mozambique Belt and is thought to be where the most intense continent-continent collision occurred. The Mozambique Belt is thus dominated by deformed, metamorphosed, and anatectically reworked older crust <...>

The earliest people in the Front Range area left scant record. During the Pleistocene, the first migrations of Oriental people crossed the Bering land bridge and some eventually moved into Colorado. Cliffdwelling Pueblo cultures developed in southwestern Colorado about 2000 years ago, with more nomadic tribes like the Ute and Apache arriving in Colorado about 700 years ago (Brown, 1985).

Structure, Stratigraphy, Sedimentary Environments and Coal Deposits of the Jura-Cretaceous Kootenay Group, Crowsnest Pass Area, Alberta and British Columbia 
Lead-Zinc and Copper-Zinc Deposits in Southeastern British Columbia
Basal Type Uranium Deposits, Okanagan Region, South Central British Columbia
Quaternary Stratigraphy of the Region Between Calgary and the Porcupine Hills 
Structural Geology of the Foothills and Front Ranges West of Calgary, Alberta 
Saskatchewan Uranium Field Trip Guide 

Район уникальных и интереснейших геологических объектов – Озѐрного свинцово-цинкового и Ермаковского фтор-бериллиевого месторождений, находится в Западном Забайкалье, входящем в состав южного складчатого обрамления Сибирской платформы.

This guidebook describes the sections of the Upper Carboniferous and Lower Permian of the Preuralian Foredeep, and gives lithological and paleontological characteristics of the deposits. The guidebook is intended for geologist and paleontologist who study Carboniferous and Permian stratigraphy and paleontology, and for students and teachers of fieldwork techniques.