1. Название Исследования. Цели и задачи (презентация 1, слайд 3)
2. Цитата С. Кузнецова (каталог, с. 1)
3. Методы исследования (презентация 1, слайд 4)
4. Выходные данные исследования (каталог, 2-я обложка)
Изменения на архитектурном рынке Москвы
5. События, факторы и инициативы, повлиявшие на архитектурный рынок Москвы. Иллюстрированный тайм-лайн: листалка по годам. По 1-2 картинке на год (каталог, с. 6-9)
6. Новые инициативы - листалка с активными ссылками (каталог, с. 10-11)
7. Новые задачи и запросы архитектурного рынка (презентация 1, слайд 6)
Коллективный портрет АБ нового поколения
8. Коллаж с портретами (презентация 1, слайд 2 - аналог) + облако тегов и тезисы (презентация 1, слайд 19)
9. Годы основания бюро (презентация 1, слайд 8)
10.Форма юридического лица (презентация 1, слайд 9)
11. Количество учредителей/партнеров (презентация 1, слайд 10)
12. Количество сотрудников (презентация, слайд 11)
29. Взаимодействие с официальными и бюджетными институциями (презентация 1, слайд 30-31)
Рекомендации по поддержке молодых бюро
30. Листалка: Конкурсная практика; Гранты, льготы, оплата труда; Расширение рынка; Повышение статуса профессии в обществе (презентация 1, слайды 32-36)
Мнения экспертов
31. листалка из 20 комментариев (каталог, с. 20-21 - аналог)
Каталог бюро
32. Листалка (см. презентация 2)
No single scientific definition of the term exists, and it has been applied to a variety of rock features that fall into one of four general categories: - A glacial erratic is a boulder that was transported and deposited by glaciers or ice rafts to a resting place on soil, on bedrock, or on other boulders. It usually has a different lithology from the other rocks around it. Not all glacial erratics are balancing rocks; some are firmly seated on the ground. Some balancing erratics have come to be known as rocking stones, also known as logan rocks, logan stones, or logans, because they are so finely balanced that the application of just a small force may cause them to rock or sway. A good example of a rocking stone is the Logan Rock in Cornwall, England, United Kingdom; another is the Trembling Rock in Brittany, France. - A perched block, also known as a perched boulder or perched rock, is a large, detached rock fragment that most commonly was transported and deposited by a glacier to a resting place on glacial till, often on the side of a hill or slope. Some perched blocks were not produced by glacial action, but were the aftermath of a rock fall, landslide, or avalanche.
An erosional remnant is a persisting rock formation that remains after extensive wind, water, and/or chemical erosion. To the untrained eye, it may appear to be visually like a glacial erratic, but instead of being transported and deposited, it was carved from the local bedrock. Many good examples of erosional remnants are seen in Karlu Karlu/Devils Marbles Conservation Reserve in the Northern Territory of Australia. - A pedestal rock, also known as a rock pedestal or mushroom rock, is not a true balancing rock, but is a single continuous rock form with a very small base leading up to a much larger crown. Some of these formations are called balancing rocks because of their appearance. The undercut base was attributed for many years to simple wind abrasion, but is now believed to result from a combination of wind and enhanced chemical weathering at the base where moisture would be retained longest. Some pedestal rocks sitting on taller spire formations are known as hoodoos.