A big hello to the Maplewood Rock and Gem club in Edmonds WA.
Maplewood Rock & Gem Club fosters community spirit by encouraging the lapidary arts and and appreciating the earth sciences of geology, fossils, minerals, and gem stones. Members join together to enjoy each other’s company as we explore new avenues of learning through field trips, lectures, seminars, craft workshops, and special shows and events. Maplewood welcomes adults, youth and junior members who actively contribute to the growth and liveliness of the group.
Contact us at: email@example.com
Maplewood Rock and Gem Club welcomes new adult members for $20 per year, and $15 for juniors. Family memberships are $45.
Meetings are held once a month. Visitors are encouraged and heartily welcomed! We have several programs throughout the year as well.
Meetings start at 7:00 pm.
Board Meetings – 1st Thursday of each month
Regular meetings – 3rd Monday of each month
Very nice news letter- click here for PDF
-nice article on septarian nodules in above PDF:
…Septarian concretions or septarian nodules, are concretions containing angular cavities or cracks, which are called “septaria“. The word comes from the Latin word septum; “partition”, and refers to the cracks/separations in this kind of rock. There is an incorrect explanation that it comes from the Latin word for “seven”, septem, referring to the number of cracks that commonly occur. Cracks are highly variable in shape and volume, as well as the degree of shrinkage they indicate. Although it has commonly been assumed that concretions grew incrementally from the inside outwards, the fact that radially oriented cracks taper towards the margins of septarian concretions is taken as evidence that in these cases the periphery was stiffer while the inside was softer, presumably due to a gradient in the amount of cement precipitated.
The process that created the septaria, which characterize septarian concretions, remains a mystery. A number of mechanisms, i.e. the dehydration of clay-rich, gel-rich, or organic-rich cores; shrinkage of the concretion’s center; expansion of gases produced by the decay of organic matter; brittle fracturing or shrinkage of the concretion interior by either earthquakes or compaction; and others, have been proposed for the formation of septaria (Pratt 2001). At this time, it is uncertain, which, if any, of these and other proposed mechanisms is responsible for the formation of septaria in septarian concretions (McBride et al. 2003). Septaria usually contain crystals precipitated from circulating solutions, usually of calcite. Siderite or pyrite coatings are also occasionally observed on the wall of the cavities present in the septaria, giving rise respectively to a panoply of bright reddish and golden colors. Some septaria may also contain small calcite stalagtites and well-shaped millimetric pyrite single crystals….